A wave dashing on the shore
A wave hitting a breakwater in the Gulf of Santa Catalina

Shipping in Hong Kong harbor
The sea is important for human development and trade, as in China's Pearl River Delta. The ports of Hong Kong, Shenzhen, and Guangzhou are separately the 3rd, 4th, and 5th busiest in the world.

The sea, the world ocean, or simply the ocean, is the connected body of salty water that covers 70.8% of the Earth's surface.[1] The sea moderates the Earth's climate and has important roles in the water cycle, carbon cycle, and nitrogen cycle. Although the sea has been travelled and explored since prehistory, the modern scientific study of the sea—oceanography—dates broadly to the British Challenger expedition of the 1870s.[2] The sea is conventionally divided into four or five large sections, such as the Pacific, called oceans while smaller sections, such as the Mediterranean, are known as seas.

Owing to the present state of continental drift, the Northern Hemisphere is now fairly equally divided between land and sea (a ratio of about 2:3) but the South is overwhelmingly oceanic (1:4.7).[3] Salinity in the open ocean is generally in a narrow band around 3.5% by mass, although this can vary in more landlocked waters, near the mouths of large rivers, or at great depths. About 85% of the solids in the open sea are sodium and chloride. Deep-sea currents are produced by differences in salinity and temperature. Surface currents are formed by the friction of waves produced by the wind and by tides, the changes in local sea level produced by the gravity of the Moon and Sun. The direction of all of these is governed by surface and submarine land masses and by the rotation of the Earth (the Coriolis effect).

Former changes in the sea levels have left continental shelves, shallow areas in the sea close to land. These nutrient-rich waters teem with life, which provide humans with substantial supplies of food—mainly fish, but also shellfish, mammals, and seaweed—which are both harvested in the wild and farmed. The most diverse areas surround great tropical coral reefs. Whaling in the deep sea was once common but whales' dwindling numbers prompted international conservation efforts and finally a moratorium on most commercial hunting. Oceanography has established that not all life is restricted to the sunlit surface waters: even under enormous depths and pressures, nutrients streaming from hydrothermal vents support their own unique ecosystem. Life may have started there and aquatic microbial mats are generally credited with the oxygenation of Earth's atmosphere; both plants and animals first evolved in the sea.

The sea is an essential aspect of human trade, travel, mineral extraction, and power generation. This has also made it essential to warfare and left major cities exposed to earthquakes and volcanoes from nearby faults; powerful tsunami waves; and hurricanes, typhoons, and cyclones produced in the tropics. This importance and duality has affected human culture, from early sea gods to the epic poetry of Homer to the changes induced by the Columbian Exchange, from Viking funerals to Basho's haikus to hyperrealist marine art, and inspiring music ranging from the shanties in The Complaynt of Scotland to Rimsky-Korsakov's "The Sea and Sinbad's Ship" to A-mei's "Listen to the Sea". It is the scene of leisure activities including swimming, diving, surfing, and sailing. However, population growth, industrialization, and intensive farming have all contributed to present-day marine pollution. Atmospheric carbon dioxide is being absorbed in increasing amounts, lowering its pH in a process known as ocean acidification. The shared nature of the sea has made overfishing an increasing problem.


  • Definition 1
  • Physical science 2
    • Seawater 2.1
    • Waves 2.2
    • Tides 2.3
    • Currents 2.4
    • Basins 2.5
    • Coasts 2.6
    • Sea level 2.7
    • The water cycle 2.8
    • The carbon cycle 2.9
    • Acidification 2.10
  • Marine life 3
    • Habitats 3.1
    • Algae and plants 3.2
    • Animals and other life 3.3
  • Humans and the sea 4
    • Navigation and exploration 4.1
    • Trade 4.2
    • Fishing 4.3
    • Law 4.4
    • War 4.5
    • Travel 4.6
    • Leisure 4.7
    • Power generation 4.8
    • Extractive industries 4.9
    • Pollution 4.10
    • Indigenous sea peoples 4.11
    • In culture 4.12
  • See also 5
  • Notes 6
  • References 7
  • Cited texts 8
  • External links 9


The interconnected system of the world's oceans and their various divisions.

The sea is the interconnected system of all the Earth's [4]—the Atlantic, Pacific, Indian, and Arctic—and the waters of the Southern Ocean, either considered separately or included within the other four.[5] This sense and the narrower use of a sea to describe specific, smaller bodies of seawater such as the Red Sea both date to Old English; the larger sense has required a definite article since Early Middle English.[5]

As the term has been applied over time, there are no sharp distinctions between seas and oceans, although seas are smaller and are—with the notable exception of the Sargasso Sea created by the North Atlantic Gyre[6](p90)—usually bounded by land on a smaller scale than multiple continents.[7] Seas are generally larger than lakes and contain salt water, but the Sea of Galilee is a freshwater lake.[8] There is no accepted technical definition of sea among oceanographers;[1] as a matter of international law, the United Nations Convention on the Law of the Sea states all the ocean is "the sea".[12][2]

Physical science

Jack Smidt. NASA photograph AS17-148-22727. 7 December 1979.
The "Blue Marble" in its original orientation, showing the junction of the Indian and Atlantic at the Cape of Good Hope.

Earth is the only known planet with seas of liquid water on its surface,[6](p22) although Mars possesses ice caps and similar planets in other solar systems may have oceans.[14] It is still unclear where Earth's water came from, but, seen from space, our planet appears as a "blue marble" of its various forms: oceans, ice caps, clouds.[15] Earth's 1,360,000,000 cubic kilometers (330,000,000 cu mi) of sea contain about 97.2 percent of its known water[16][3] and cover more than 70 percent of its surface.[6](p7) Another 2.15% of Earth's water is frozen, found in the sea ice covering the Arctic Ocean, the ice cap covering Antarctica and its adjacent seas, and various glaciers and surface deposits around the world. The remainder (about 0.65% of the whole) form underground reservoirs or various stages of the water cycle, containing the freshwater encountered and used by most terrestrial life: vapor in the air, the clouds it slowly forms, the rain falling from them, and the lakes and rivers spontaneously formed as its waters flow again and again to the sea.[16] The sea's dominance of the planet is such that the British author Arthur C. Clarke once noted that "Earth" would have been better named "Ocean".[6](p7)

The marine ecosystems. Both are informed by chemical oceanography, which studies the behavior of elements and molecules within the oceans: particularly, at the moment, the ocean's role in the carbon cycle and carbon dioxide's role in the increasing acidification of seawater. Marine and maritime geography charts the shape and shaping of the sea, while marine geology (geological oceanography) has provided evidence of continental drift and the composition and structure of the Earth, clarified the process of sedimentation, and assisted the study of volcanism and earthquakes.[22]


Solutes in seawater at 35 salinity[25]
Solute of water
(by mass)
% of total
Chloride 19 .3 55 .0
Sodium 10 .8 30 .6
Sulfate 2 .7 7 .7
Magnesium 1 .3 3 .7
Calcium 0 .41 1 .2
Potassium 0 .40 1 .1
Bicarbonate 0 .10 0 .4
Bromides 0 .07 0 .2
Carbonate 0 .01 0 .05
Strontium 0 .01 0 .04
Borate 0 .01 0 .01
Fluoride 0 .001 < 0 .01
All others < 0 .001 < 0 .01
Global salinity map (Aug.–Sept. 2010 & 2011) produced by the ESA's Soil Moisture and Ocean Salinity satellite. Released 2012.
The first global map of oceanic surface salinity, produced by the ESA's SMOS satellite (2011). The salinity varies from 32 (purple) to 38 (red).

Seawater is invariably salty and, although its degree of saltiness (salinity) can vary, about 90% of the water in the ocean has 34–35 g (1.2 oz.) of dissolved solids per liter, producing a salinity between 3.4 and 3.5%.[26] (In order to easily describe small differences, however, oceanographers usually express salinity as a millage [] or part per thousand [ppt] instead of using percents.) The surface salinity of waters in the Northern Hemisphere are generally closer to the 34 mark, while those in the South are closer to 35.[3] The solutes in ocean water come both from inflowing river water and from the ocean floor.[27] The relative composition of the solutes is stable throughout the world's oceans:[25][28] sodium (Na) and chloride (Cl) make up about 85%. Other solutes include metal ions such as magnesium (Mg) and calcium (Ca) and negative ions such as sulfate (SO₄), carbonate (CO₃), and bromides. In the absence of other pollution, seawater would not be harmful to drink except that it is much too saline;[4] similarly, it cannot be used for irrigating most plants without being desalinated. For scientific and technical purposes, a standardized form of artificial seawater is often used.

Variations in salinity are caused by many factors: currents flowing between the seas; incoming freshwater from rivers and glaciers; precipitation; the formation and melting of sea ice; and evaporation, which is in turn affected by temperature, winds, and waves. For example, the upper level of the Baltic Sea has a very low salinity (10 to 15) because the low temperatures of the surrounding climate produce minimal evaporation; it has many inflowing rivers; and its small connection to the North Sea tends to create a cold, dense under-layer that hardly mixes with the surface waters.[31] By contrast, the Red Sea lies between the Sahara and Arabian Deserts; it has high evaporation but little precipitation; it has few (and mostly seasonal) inflowing rivers; and its connection to other seas—the Suez Canal in the north and the Bab-el-Mandeb in the south—are both very narrow. Its salinity averages 40.[32] The Mediterranean is a little lower, at 37, while some landlocked lakes are much higher: The Dead Sea has 300 grams (11 oz) of dissolved solids per liter (300).

Annual mean sea surface temperature from World Ocean Atlas 2009.
Mean surface temperature (2009), from -2 °C (light violet) to 30 °C (light pink).

Annual mean sea surface temperature from World Ocean Atlas 2009.

Sea temperature chiefly depends on the amount of solar radiation it absorbs. In the tropics where sunlight falls more directly, the temperature of the surface layers can rise to over 30 °C (86 °F); near the poles, the temperature is in equilibrium with the sea ice at its freezing point. Its salinity makes this lower than freshwater's, usually about −1.8 °C (28.8 °F). These temperature differences contribute to the continuous circulation of water through the sea. Warm surface currents cool as they move away from the tropics; as the water becomes denser, it sinks. The cold water in the deep sea moves back towards the equator before welling up again to the surface. Deep seawater has a temperature between −2 and 5 °C (28 and 41 °F) in all parts of the globe.[33] In freezing seas, ice crystals begin to form on the surface. These break into small pieces and coalesce into flat discs that form a thick suspension known as frazil. In calm conditions, frazil will freeze into a thin, flat sheet called nilas, which thickens as new ice forms in the sea beneath it. In turbulent waters, frazil instead join together into larger flat discs known as "pancakes". These slide over and under one another to form floes. During these processes, salt water and air are trapped amid the ice. Nilas forms with a salinity around 12–15 and is grayish in color but grows fresher over time: after a year, it is bluish and closer to 4–6 saline.[29][34]

Annual mean dissolved oxygen levels at the sea surface from World Ocean Atlas 2009.
Mean surface oxygen levels (2009), from 0.15 (light violet) to 0.45 (light pink) moles of O₂ per cubic meter.

Annual mean dissolved oxygen levels at the sea surface from World Ocean Atlas 2009.

The amount of light that penetrates the sea depends on the angle of the sun, the local weather, and the sea's turbidity. Of the light that reaches the surface of the sea, much of it is reflected at the surface and its red wavelengths are absorbed in the top few meters. Yellow and green reach greater depths, and the longer blue and violet wavelengths may penetrate as deep as 1,000 m (3,300 ft).

The hydrogen sulfide (H₂S).[36] It is projected that global warming will reduce oxygen both in surface and deep waters, due to oxygen's decreased solubility as temperatures increase[37] and increased oceanic stratification.[38]


A map of mean wave height for the period Oct. 3-12, 1992. NASA.
Mean wave height (1992), from 0 m (light violet) to 6 m (white). Note the large swells in the southern oceans.

Diagram of water molecules as waves pass
Movement of fluid parcels as waves pass.

Ocean surface waves are oscillations caused by the friction from air moving across the surface of the water. This friction transfers energy and forms surface waves in the water perpendicular to the direction of the wind. The top of a wave is known as its crest and its foot as its trough; the distance between two crests is the wavelength. These waves are mechanical: as they approach, the water molecules at a given point rise up and, as they pass, the water molecules go down, tracing a roughly circular path. The energy is passed across the surface and does not represent a horizontal motion of the water itself. The sea state of the ocean is determined by the size of these waves, which—on the open ocean—depends upon the wind speed and the fetch, the distance over which the wind blows upon the water. The smallest waves are called ripples. As strong and prolonged winds push against ripples' raised crests, larger and more irregular waves form, which known as seas. These waves reach their maximum height when the rate at which they are traveling nearly matches the speed of the wind and, over time, they naturally separate[5] into long, powerful waves with a common direction and wavelength. These swells are particularly common in the Roaring Forties of the Southern Hemisphere where the wind blows continuously.[39][40] When the wind dies down, ripples easily disappear owing to water's surface tension, but seas and swells are only slowly reduced by gravity and destructive interference from other waves.[39] Constructive interference, however, can also cause individual rogue waves much higher than normal.[41] Most waves are less than 3 m (10 ft) high[41] and it is not unusual for strong storms to double or triple that height;[42] offshore construction such as wind farms and oil platforms use these measurements in computing the hundred-year wave they are designed against.[43] Rogue waves, however, have been documented at heights above 25 meters (82 ft).[44][45]

Diagram showing waves shoaling
When waves enter shallow water, they slow down and their amplitude (height) increases.

As waves approach land and move into shallow water, they change their behavior. If approaching at an angle, waves may bend or wrap rocks and headlands. When the wave reaches a point where its deepest oscillating molecules contact the seabed, friction begins to slow the wave down. This pulls the crests closer together and increases the waves' height. When the ratio of a wave's height to its wavelength exceeds 1:7, it "breaks", toppling over in a mass of foaming water.[41] This rushes in a sheet up the beach before retreating into the sea under the influence of gravity.[39]

Tsunami in Thailand
The 2004 tsunami rushing ashore in Thailand. An estimated 8,000 Thais were killed; 220,000 other people died around the Indian Ocean.[46]

A tsunami is an unusual form of wave caused by a sudden and powerful event such as an underwater earthquake or landslide, a meteorite impact, a volcanic eruption, or a collapse of land into the sea. These events can temporarily lift or lower the surface of the sea in the affected area, usually by a few feet. The potential energy of the displaced seawater is turned into kinetic energy, creating a shallow wave radiating outwards at a velocity proportional to the square root of the depth of the water. Tsunamis, therefore, travel much faster in the open ocean than on a continental shelf.[47] Despite traveling at speeds of over 600 mph (970 km/h),[48] tsunamis in deep seas have wavelengths from 80 to 300 miles (130 to 480 km) and an amplitude of less than three feet.[49] Standard surface waves in the same region may only have wavelengths of a few hundred feet and speeds up to 65 mph (105 km/h) but, when compared to their possible amplitudes of up to 45 ft (14 m), tsunamis at this stage are often able to pass unnoticed.[49] Tsunami warning systems rely on the fact that seismic waves caused by earthquakes travel around the world at around 14,400 kilometers (8,900 mi) per hour, allowing threatened regions to be alerted to the possibility of a tsunami.[50] Measurements from a network of sea-level measuring stations make it possible to confirm or cancel a tsunami warning.[51] A trigger event on the continental shelf may cause a local tsunami on the land side and a distant tsunami that travels out across the ocean. The energy of the wave is dissipated only gradually but is spread out over the wave front. As the wave radiates away from the source, the front gets longer and the average energy reduces, so distant shores will generally be hit by weaker waves. However, as the speed of the wave is controlled by the water depth, it does not travel at the same speed in all directions and this affects the direction of the wave front. This effect, known as refraction, can focus the strength of an advancing tsunami on some areas while weakening it in others, according to the undersea topography along its path.[52][53]

Just as with other waves, moving into shallow water causes the tsunami to slow but grow in height.[49] Either the trough or the crest of the tsunami can arrive at the coast first.[47] In the former case, the sea draws back and leaves subtidal areas unusually exposed.[54] When the crest arrives, it does not usually break but rushes inland, flooding all in its path. Much of the disaster's destruction can be produced by these flood waters, which drain back into the sea while pulling people and debris along. Several tsunamis can be caused by a single geological event. In such cases, it is common for the later waves to arrive between eight minutes and two hours after the first, which may not be the biggest or most destructive.[47] Occasionally, in a shallow bay or estuary, a tsunami may transform into a bore.[48]


Diagram showing how the sun and moon cause tides
High tides (blue) at the nearest and furthest points of the Earth from the Moon

Tides are the regular rise and fall in water level experienced by seas and oceans in response to the gravitational influences of the Moon and the Sun, and the effects of the Earth's rotation. At any given place, the water rises over the course of the tidal cycle to a maximum height known as "high tide" before ebbing away again to a minimum "low tide" level. As the water recedes, it uncovers more and more of the foreshore or intertidal zone. The difference in height between the high tide and low tide is known as the tidal range or tidal amplitude.[55][56] Tidal bores can occur at the mouths of rivers, where the force of the incoming tide pushes waves of seawater upstream against the current. At Hangzhou in China, the bore can reach 9 meters (30 ft) high and travel up to 40 km (25 mi) per hour.

Most places experience two high tides each day, occurring at intervals of about 12 hours and 25 minutes, half the period that it takes for the Earth to make a complete revolution and return the Moon to its previous position relative to an observer. The Moon's mass is some 27 million times smaller than the Sun, but it is 400 times closer to the Earth.[57] Tidal force or tide-raising force decreases rapidly with distance, so the moon has more than twice as great an effect on tides as the Sun.[57] A bulge is formed in the ocean at the place where the Earth is closest to the Moon, because it is also where the effect of the Moon's gravity is stronger. On the opposite side of the Earth, the lunar force is at its weakest and this causes another bulge to form. These bulges rotate around the Earth as the moon does. The Sun's effect is less powerful but, when the Sun, Moon and Earth are all aligned at the full and new moons, the combined effect results in the high "spring tides". In contrast, when the Sun is at 90° from the Moon as viewed from Earth, the combined gravitational effect on tides is correspondingly reduced, causing the lower "neap tides".[55]

Tidal flows of seawater are resisted by the water's inertia and can be affected by land masses. In places like the Gulf of Mexico where land constrains the movement of the bulges, only one set of tides may occur each day. Inshore from an island, there may be a complex daily cycle with four high tides. The island straits at Chalkis on Euboea experience strong currents which abruptly switch direction, generally four times per day but up to 12 times per day when the moon and the sun are 90 degrees apart.[58][59] Where there is a funnel-shaped bay or estuary, the tidal range can be magnified. The Bay of Fundy in Canada can experience spring tides of 15 m (49 ft). Although tides are regular and predictable, the height of high tides can be lowered by offshore winds and raised by onshore winds. The high pressure at the center of an anticyclones pushes down on the water and is associated with abnormally low tides while low-pressure areas may cause extremely high tides.[55] A storm surge can occur when high winds pile water up against the coast in a shallow area and this, coupled with a low pressure system, can raise the surface of the sea at high tide dramatically. In 1900, Galveston, Texas, experienced a 15 ft (5 m) surge during a hurricane that overwhelmed the city, killing over 3,500 people and destroying 3,636 homes.[60]


Mean surface density (2009), from 1020 (light violet) to 1028 (light pink) kilograms per cubic meter.

Wind blowing over the surface of the sea causes friction at the interface between air and sea. Not only does this cause waves to form but it also makes the surface seawater move in the same direction as the wind. Although winds are variable, in any one place they predominantly blow from a single direction and thus a surface current can be formed. Westerly winds are most frequent in the mid-latitudes while easterlies dominate the tropics.[61] When water moves in this way, other water flows in to fill the gap and a circular movement of surface currents known as a gyre is formed. There are five main gyres in the world's oceans: two in the Pacific, two in the Atlantic, and one in the Indian Ocean. The North Atlantic gyre that produces the Sargasso Sea accumulates salinity levels as high as 38.[3] Other smaller gyres are found in lesser seas and a single gyre flows around Antarctica. These gyres have followed the same routes for millennia, guided by the topography of the land, the wind direction, and the Coriolis effect. The surface currents flow in a clockwise direction in the Northern Hemisphere and anticlockwise in the Southern Hemisphere. The water moving away from the equator is warm, while that flowing towards it has lost most of its heat. These currents tend to moderate the Earth's climate, cooling the equatorial region, and warming regions at higher latitudes.[62] Global climate and weather forecasts are powerfully affected by the world ocean, so global climate modelling makes use of ocean circulation models as well as models of other major components such as the atmosphere, land surfaces, aerosols, and sea ice.[63] Ocean models make use of a branch of physics, geophysical fluid dynamics, that describes the large-scale flow of fluids such as seawater.[64]

Map showing surface currents
Surface currents: red–warm, blue–cold

Surface currents only affect the top few hundred meters (yards) of the sea, but there are also large-scale flows in the ocean depths caused by the movement of deep water masses. A main deep ocean current flows through all the world's oceans and is known as the thermohaline circulation or global conveyor belt. This movement is slow and is driven by differences in density of the water caused by variations in salinity and temperature.[65] At high latitudes, the water is chilled by the low atmospheric temperature and becomes saltier as sea ice crystallizes out. Both these factors make it denser and the water sinks. From the deep sea near Greenland, such water flows southwards between the continental landmasses on either side of the Atlantic. When it reaches the Antarctic, it is joined by further masses of cold, sinking water and flows eastwards. It then splits into two streams that move northwards into the Indian and Pacific Oceans. Here it is gradually warmed, becomes less dense, rises towards the surface, and loops back on itself. Some flows back into the Atlantic. It takes a thousand years for this circulation pattern to be completed.[62]

The global conveyor belt shown in blue with warmer surface currents in red

Besides gyres, there are temporary surface currents that occur under specific conditions. When waves meet a shore at an angle, a longshore current is created as water is pushed along parallel to the coastline. The water swirls up onto the beach at right angles to the approaching waves but drains away straight down the slope under the effect of gravity. The larger the breaking waves, the longer the beach, and the more oblique the wave's approach, the stronger the longshore current is.[66] These currents can shift great volumes of sand or pebbles, create spits, and make beaches disappear and water channels silt up.[62] A rip current can occur when water piles up near the shore from advancing waves and is funnelled out to sea through a channel in the seabed. It may occur at a gap in a sandbar or near a man-made structure such as a groyne. These strong currents can have a velocity of 1 m/s (3.3 ft/s), can form at different places at different stages of the tide, and can carry away unwary swimmers.[67] Temporary upwelling currents occur when the wind pushes water away from the land and deeper water rises to replace it. This cold water is often rich in nutrients and creates blooms of phytoplankton and a great increase in the productivity of the sea.[62]


Three types of plate boundary

Bathymetry is the mapping and study of the topography of the ocean floor. Methods used for measuring the depth of the sea include single or multibeam echosounders, laser airborne depth sounders and the calculation of depths from satellite remote sensing data. This information is used for determining the routes of undersea cables and pipelines, for choosing suitable locations for siting oil rigs and offshore wind turbines and for identifying possible new fisheries.[68] The Earth is composed of a magnetic central core, a mostly liquid mantle, and a hard rigid outer shell (or lithosphere), which is composed of the Earth's rocky crust and the deeper and mostly solid outer layer of the mantle. The crust below land is known as continental while that under the abyssal sea is called oceanic. The latter is composed of relatively dense basalt and is some five to ten kilometers (three to six miles) thick. The relatively thin lithosphere floats on the weaker and hotter mantle below and is fractured into a number of tectonic plates.[69] In mid-ocean, magma is constantly being thrust through the seabed between adjoining plates to form mid-oceanic ridges and here convection currents within the mantle tend to drive the two plates apart. Parallel to these ridges and nearer the coasts, one oceanic plate may slide beneath another oceanic plate in a process known as subduction. Deep trenches are formed here and the process is accompanied by friction as the plates grind together. The movement proceeds in jerks which cause earthquakes. Heat is also produced and magma is forced up, creating underwater mountains, some of which grow into volcanic islands. Near some boundaries between the land and sea, the slightly denser oceanic plates slide beneath the continental plates and more subduction trenches are formed. As they grate together, the continental plates are deformed and buckle causing mountain building and seismic activity.[70][71]

The Earth's deepest trench is the Mariana Trench which extends for about 2,500 kilometers (1,600 mi) across the seabed. It is near the Mariana Islands, a volcanic archipelago in the West Pacific. Though it averages just 68 km (42 mi) wide, its deepest point is 10.994 kilometers (nearly 7 miles) below the surface of the sea.[72] An even longer trench runs alongside the coast of Peru and Chile, reaching a depth of 8,065 m (26,460 ft) and extending for approximately 5,900 km (3,700 mi). It occurs where the oceanic Nazca Plate slides under the continental South American Plate and is associated with the upthrust and volcanic activity of the Andes.[73]


The zone where land meets sea is known as the coast and the part between the lowest spring tides and the upper limit reached by splashing waves is the shore. A beach is the accumulation of sand or shingle on the shore.[74] A headland is a point of land jutting out into the sea and a larger promontory is known as a cape. The indentation of a coastline—especially between two headlands—is a bay; a small bay with a narrow inlet is a cove and a large bay or bay-shaped sea may be referred to as a gulf.[75] Coastlines are influenced by a number of factors including the strength of the waves arriving on the shore, the gradient of the land margin, the composition and hardness of the coastal rock, the inclination of the off-shore slope, and the changes of the level of the land due to local uplift or submergence. Normally, waves roll towards the shore at the rate of six to eight per minute. These are known as constructive waves as they tend to move material up the beach and have little erosive effect. Storm waves arrive on shore in rapid succession and are known as destructive waves, as their swash moves beach material seawards. Under their influence, the sand and shingle on the beach is ground together and abraded. Around high tide, the power of a storm wave impacting on the foot of a cliff has a shattering effect as air in cracks and crevices is compressed and then expands rapidly with release of pressure. At the same time, sand and pebbles have an erosive effect as they are thrown against the rocks. Along with other weathering processes such as frost, this tends to undercut the cliff. Gradually, a wave-cut platform develops at the foot of the cliff and this has a protective effect, reducing further wave-erosion.[74]

Material worn from the margins of the land eventually ends up in the sea, where it is subject to attrition as currents flowing parallel to the coast scour out channels and transport material away from its place of origin. Sediment carried to the sea by rivers settles on the seabed causing deltas to form in estuaries. All these materials move back and forth under the influence of waves, tides, and currents.[74] Dredging removes material and deepens channels but may have unexpected effects elsewhere on the coastline. Governments make efforts to prevent flooding through building breakwaters, seawalls, and other defenses against the sea. In Britain, the Thames Barrier protects London from storm surges,[76] while the failure of the dykes and levees around New Orleans during Hurricane Katrina created a humanitarian crisis in the United States. Land reclamation in Hong Kong permitted the construction of Hong Kong International Airport through the leveling and expansion of two smaller islands.[77]

Following the adoption of the present UNCLOS, the coastline under international law is a state's baseline (sea), which is generally but not always equivalent to its low-water line.[78]

Sea level

Variations in sea level around the world (1992) from -1.4 m (light violet) to +1.0 m (light pink).

Over most of geologic time, the sea level has been higher than it is today.[6](p74) The main factor affecting sea level over time is the result of changes in the oceanic crust, with a downward trend expected to continue in the very long term.[79] At the last glacial maximum some 20,000 years ago, the sea level was 120 meters (390 ft) below its present-day level. For at least the last 100 years, the sea level has been rising at an average rate of about 1.8 mm (0.071 in) per year.[80] Most of this rise can be attributed to an increase in the temperature of the sea and the resulting slight thermal expansion of the upper 500 m (1,600 ft) of water. Additional contributions, as much as one quarter of the total, come from water sources on land, such as melting snow and glaciers and extraction of groundwater for irrigation and other agricultural and human needs.[81] The rising trend from global warming is expected to continue until at least the end of the 21st century.[82]

The water cycle

The sea plays a part in the water cycle, in which water evaporates from the ocean, travels through the atmosphere as vapor, condenses, falls (usually as rain or snow) again, and then largely returns to the sea.[83] Even in the Atacama Desert, where little rain ever falls, dense clouds of fog known as the camanchaca blow in from the sea and support plant life.[84] In large land masses, geologic features can block the access of some regions to the main sea. These endorheic basins, particularly in central Asia, sometimes build up permanent salt lakes as inflowing waters evaporate and their dissolved minerals accumulate over time. The largest of these is the Caspian Sea, although it is sometimes counted as a proper sea owing to its basin of (now-landlocked) oceanic crust. Other notable examples include the Aral Sea in central Asia and the Great Salt Lake in the western United States.[85] The waters of these basins still eventually return to the sea through evaporation, the flow of ground water, and (over geologic time) the opening up of the basins by continental drift.

The carbon cycle

Oceans contain the greatest quantity of actively-cycled carbon in the world and are second only to the Monaco has standardized surveying and charting of the sea[150] and, from 1924, the Discovery Investigations studied whales and mapped the seas around Antarctica.[22] The spherical Bathysphere was able to descend to 434 meters (1,424 ft) in 1930 on a cable[151] and, in the 1940s, Jacques Cousteau helped develop the first successful scuba gear and popularize underwater diving. The Cold War and oil exploration funded further deep sea research: by 1960, the self-powered Trieste could take her crew 10,915 m (35,810 ft) into the Mariana Trench[152] and a US Navy diver in an atmospheric diving suit reached 2,000 feet (610 m) below sea level in 2006.[153]

Today, the American Global Positioning System (GPS) enables accurate navigation worldwide using over thirty satellites and message timing so exact as to involve general relativity.[147] Ongoing oceanographic research includes marine lifeforms, conservation, the marine environment, the chemistry of the ocean, the studying and modelling of climate dynamics, the air-sea boundary, weather patterns, ocean resources, renewable energy, waves and currents, and the design and development of new tools and technologies for investigating the deep.[154] Researchers make use of satellite-based remote sensing for surface waters, with research ships, moored observatories and autonomous underwater vehicles to study and monitor all parts of the sea.[155]


Map showing shipping routes
Shipping routes, showing relative density of commercial shipping around the world

Water-borne trade has been practiced since at least the dawn of civilization, when Sumeria was connected to Harappan India.[156] Buoyancy permits easy transport of bulk goods such as food and this has been an important factor in the placement of most the world's largest cities along the sea or along rivers navigable to the sea. The sea also permitted relatively safe transport of distant luxury items during times when brigandage was common. However, owing to the incompleteness of geographical knowledge, the difficulty of early navigation, and the limitations of shipbuilding technology, early trade was limited to coast-hugging cabotage, leaving it prey to piracy and local rulers requiring taxes or transshipment. The Indian Ocean trade, for instance, was carried out for centuries at the halfway points of Dilmun (modern Bahrain) and Aden in Yemen. At some point in the early millennia BC, though, the Indians and Arabs learned to harness the monsoon winds to sail swiftly and safely across the high seas once a year; a shipwrecked sailor then showed the Greek navigator Eudoxus this secret c. 117 BC, permitting centuries of direct and massive trade between Ptolemaic and, later, Roman Egypt and the ports of India.

Around 2000 BC, the Minoans of Crete established the earliest thalassocracy, a maritime empire heavily dependent upon its trade and naval power.[157] The city-states of the Phoenicians and Greeks then replaced them in the centuries after 1200 BC, ultimately establishing far-flung colonial empires which spread from the Sea of Azov to the Atlantic coast of Morocco.[158] Under the Romans, commerce continued to thrive. In the first centuries BC, steppe nomads' interruption of India's access to Siberian gold caused them to open up maritime routes to Malaysia and Indonesia,[159] exposing them first to Hindu and then Muslim traders. With the collapse of the Roman Empire, European trade dwindled but it continued to flourish elsewhere.[160] The Tamil Chola dynasty thrived on trade between Tang China, the Javanese Srivijaya Empire, and the Abbasid Caliphate in the west. Following further conquests, Arabians came to dominate maritime trade in the Indian Ocean, spreading Islam along the East African coast and, eventually, Southeast Asia.[161] A major effect of the Age of Discovery was the unification of the world's regional trade networks into a single world market, largely run by and for the European monarchs and the merchants of Amsterdam, London, and other Atlantic ports. From the 16th to the 19th centuries, about 13 million people were shipped across the Atlantic to be sold as slaves in the Americas.[162] The Hales Trophy was an award for the fastest commercial crossing of the Atlantic and was won by the SS United States in 1952 for a crossing that took three days, ten hours, and forty minutes.[163]

Nowadays, large quantities of goods are transported by sea, especially across the Atlantic and around the Pacific Rim. A major trade route passes through the Pillars of Hercules, across the Mediterranean and the Suez Canal to the Indian Ocean and through the Straits of Malacca; much trade also passes through the English Channel.[164] Shipping lanes are the routes on the open sea used by cargo vessels, traditionally making use of trade winds and currents. Over 60 percent of the world's container traffic is conveyed on the top twenty trade routes.[165] Increased melting of Arctic ice since 2007 enables ships to travel the Northwest Passage for some weeks in summer, avoiding the longer routes via the Suez Canal or the Panama Canal.[166] Shipping is supplemented by air freight, a more expensive process mostly used for particularly valuable or perishable cargoes. Seaborne trade carries more than US $4 trillion worth of goods each year.[167]

There are two main kinds of freight, London and first convened in 1959. Its objectives include developing and maintaining a regulatory framework for shipping, maritime safety, environmental concerns, legal matters, technical co-operation and maritime security.[172]


A Brixham Trawler by William Adolphus Knell. National Maritime Museum, Greenwich. Oil on board, 153 x 235 mm. 19th century.
19th-century Brixham trawlers at work.

A Brixham Trawler by William Adolphus Knell. National Maritime Museum, Greenwich. Oil on board, 153 x 235 mm. 19th century.

Humans in East Asia were consuming large amounts of freshwater fish around 40 000 years ago.[173] Spearfishing with barbed harpoons along the coast was widespread by the Palaeolithic.[174] Fish ponds surrounded Sumerian temples by 2 500 BC and a Chinese classical text credited to the 5th-century BC businessman Fan Li[175] is the earliest known work on fish farming.[176] A surviving fragment of Isidore of Charax's 1st-century Parthian itinerary describes locals freediving for pearls in the Persian Gulf,[177] and Oppian's 2nd-century Halieutics relates the four main Greek and Roman fishing methods as hook-and-line, netting, passive traps, and trident.[178] Traditional fishing boats operate in near-shore waters but, during the late Middle Ages and early Modern period, fishing on the open sea—particularly cod—became important to the economic and naval development of Northern Europe, New England, and Canada.[179] Overfishing along the coasts of the North Sea spurred the development of deep-sea fishers such as the Brixham[180] and otter trawlers, which might serve as motherships for longlining dories;[181] in the 19th century, advances such as rail transport, canning, and refrigeration allowed fishing to become a full-fledged industry. Improvements in sonar during the world wars were adapted as fishfinders and, during the 1950s, great factory ships caught and processed as many fish in an hour as earlier trawlers had in a season.[181] By the 1960s, the North Atlantic and North Pacific fisheries were close to maximal exploitation. After the catch from wild marine fisheries grew from 18 million metric tons (20 million tons) in 1950 to around 85 million metric tons (93½ million tons) by the late 1980s, it has remained essentially constant since.[182][9] Chinese economic reform led to massive growth of its fishing production, from 7% of the world total in 1961 to 35% by 2010.[182] Scientific studies of population dynamics and nationalization of formerly shared waters are both helping to cope with overexploitation but the success of modern commercial fishing has required major corrective actions: the collapse of the Grand Banks cod fishery to less than 1% of its historic levels required a complete moratorium by Canada in 1992[183] and China has enforced a zero-growth policy in its wild catch since 2000, redirecting its industry towards aquaculture;[184] its annual months-long bans on fishing in disputed areas of the South China Sea is enforced over the protest of neighboring states.[185]

The whale factory vessel Tonan Maru №2 was torpedoed four times but repaired or raised each time.[186] Built to Norwegian design, the Japanese whaling fleet provided half of the country's meat supply during its American occupation and remains the world's most active. Similar whalers in Europe inspired present-day fish processing ships.[181]

As of 2006, there were an estimated 43.5 million people involved in capturing or raising seafood, 85.5% of whom lived in Asia. About ¾ were fishers and the remainder fish farmers.[187] In 2012, total global production of fish, crustaceans, molluscs, and other aquatic animals was a record 158 million metric tons (174 million tons), of which 91.3 million metric tons (100 million tons) were caught in the wild.[188] This is also a record if ignoring the Peruvian anchovy,[188] whose population can vary dramatically with the El Niño cycle.[189][190] The overall trend remains increasing, but due to expanding aquaculture in inland waters and mariculture in the sea rather than higher catches in the wild. The exclusive economic zones around coastal countries under the UNCLOS regime have permitted states to institute quota and other management systems[191] over the most productive regions of the sea, accounting for around 87% of the annual harvest.[192] The results are sometimes dramatic—the lull in fishing over the course of the First World War saw the North Sea's 1919 catch double 1913's[181]—and sometimes much less so: two decades on, the levels of cod in the Grand Banks remain only 10% of their peak. At present, the species most frequently landed are herring, cod, anchovy, tuna, flounder, mullet, squid, and salmon. A number of these, as well as large predatory fish,[193] remain well below historical levels.[194]

A purse seiner hauling in around 360 metric tons (400 tons) of mackerel off Peru.

Over 3 million vessels are employed in sea fishing.[192] Modern fishing vessels include

  • National Oceanic and Atmospheric Administration—NOAA website
  • Oceans at DMOZ

External links

  • Cotterell, Arthur (ed.) (2000). World Mythology. Parragon.  
  • Illustrated Encyclopedia of the Ocean. Dorling Kindersley. 2011.  
  • Stow, Dorrik (2004). Encyclopedia of the Oceans. Oxford University Press.  

Cited texts

  1. ^ Pidwirny, Michael. "Introduction to the Hydrosphere"Ch. 8:, 2nd ed., Fundamentals of Physical Geography. University of British Columbia (Okanagan), 2006. Accessed 26 Nov 2007.
  2. ^ National Oceanic and Atmospheric Administration. Expedition and the 'Mountains in the Sea' Expedition"Challenger"Then and Now: The HMS at Ocean Explorer. Accessed 2 Jan 2012.
  3. ^ a b c Reddy, M.P.M. p. 112, Descriptive Physical Oceanography. A.A. Balkema (Leiden), 2001. ISBN 90-5410-706-5. Accessed 6 Aug 2014.
  4. ^ a b Monte Carlo), 1953. Retrieved 7 February 2010.
  5. ^ a b Oxford English Dictionary, 1st ed. "sea, n." Oxford University Press (Oxford), 1911.
  6. ^ a b c d e f g h i j k l m n o p q r s t Stow, Dorrik (2004). Encyclopedia of the Oceans. Oxford University Press.  
  7. ^ National Oceanic and Atmospheric Administration. "What's the Difference between an Ocean and a Sea?" in Ocean Facts. Accessed 19 Apr 2013.
  8. ^ Nishri, A.; Stiller, M; Rimmer, A.; Geifman, Y.; Krom, M. (1999). "Lake Kinneret (The Sea of Galilee): the effects of diversion of external salinity sources and the probable chemical composition of the internal salinity sources". Chemical Geology 158 (1–2): 37–52.  
  9. ^ American Society of Civil Engineers. p. 365, The Glossary of the Mapping Sciences. ASCE Publications, 1994. ISBN 0-7844-7570-9.
  10. ^ Karleskint, George & al. p. 47, Introduction to Marine Biology Cengage Learning, 2009. ISBN 978-0-495-56197-2.
  11. ^ Conforti, B. & al. .p. 237, Vol. 14, The Italian Yearbook of International Law Martinus Nijhoff, 2005. ISBN 978-90-04-15027-0.
  12. ^ Vukas, B. p. 271, The Law of the Sea: Selected Writings. Martinus Nijhoff, 2004. ISBN 978-90-04-13863-6.
  13. ^ Gokay, Bulent (2001). "The Politics of Caspian Oil". Palgrave Macmillan. p. 74.  
  14. ^ Ravilious, Kate. "Most Earthlike Planet Yet Found May Have Liquid Oceans" in National Geographic. 21 Apr 2009. Accessed 10 Sept 2013.
  15. ^ Platnick, Steven. "Visible Earth". NASA. Accessed 22 Apr 2013.
  16. ^ a b NOAA. "Lesson 7: The Water Cycle" in Ocean Explorer. Accessed 19 Apr 2013.
  17. ^ Oskin, Becky. "Rare Diamond Confirms that Earth's Mantle Holds an Ocean's Worth of Water" in Scientific American. 12 Mar 2014. Accessed 13 Mar 2014.
  18. ^ Schmandt, Brandon & al. "Dehydration Melting at the Top of the Lower Mantle" in Science, Vol. 344, No. 6189, pp. 1265–68. 13 Jun 2014. DOI 10.1126/science.1253358. Accessed 13 Jun 2014.
  19. ^ Harder, Ben. "Inner Earth May Hold More Water Than the Seas" in National Geographic. 7 Mar 2002. Accessed 14 Nov 2013.
  20. ^ Murakami, Motohiko & al. "Water in Earth's Lower Mantle" in Science, Vol. 295, No. 5561, pp. 1885–87. 8 Mar 2002. Accessed 8 Aug 2014.
  21. ^ Lee, Sidney (ed.) "Rennell, James" in the Dictionary of National Biography, Vol. 48. Smith, Elder, & Co. (London), 1896. Hosted at Wikisource.
  22. ^ a b c Monkhouse, F.J. Principles of Physical Geography, pp. 327–328. Hodder & Stoughton, 1975. ISBN 978-0-340-04944-0.
  23. ^ Russell, S.F. & al. The Seas: Our Knowledge of Life in the Sea and How It is Gained, pp. 8 ff. Frederick Warne, 1963. JSTOR 1785367.
  24. ^ Stewart, Robert H. pp. 2–3, Introduction To Physical Oceanography. Texas A & M University, 2008. Accessed 15 Sept. 2013.
  25. ^ a b Millero, Frank & al. "The Composition of Standard Seawater and the Definition of the Reference-Composition Salinity Scale" in Deep Sea Research, Part I: Oceanographic Research Papers, Vol. 55, No. 1, pp. 50–72. Jan 2008. DOI 10.1016/j.dsr.2007.10.001. Bibcode: 2008DSRI...55...50M.
  26. ^ Pond, Stephen & al. Introductory Dynamic Oceanography, p. 5. Pergamon Press, 1978.
  27. ^ Pinet, Paul. Invitation to Oceanography. West Publishing Co. (St. Paul), 1996. ISBN 978-0-314-06339-7.
  28. ^ Swenson, Herbert. "Why is the Ocean Salty?" US Geological Survey. Accessed 17 April 2013.
  29. ^ a b US Army. , Chapter 6: "Water Procurement"Survival: FM 21-76. June 1992. Accessed 1 Aug 2014.
  30. ^ NOAA. "Drinking Seawater Can Be Deadly to Humans". 11 Jan 2013. Accessed 16 Sept 2013.
  31. ^ Thulin, Jan & al. "Religion, Science, and the Environment Symposium V on the Baltic Sea". 2003. Hosted at, 6 Jun 2007. Accessed 16 Apr 2013.
  32. ^ Thunell, Robert C.; Locke, Sharon M.; Williams, Douglas F. (1988). "Glacio-eustatic sea-level control on Red Sea salinity". Nature 334 (6183): 601–604.  
  33. ^ Gordon, Arnold. The Climate System"Ocean Circulation" in . Columbia University (New York), 2004. Accessed 6 July 2013.
  34. ^ Jeffries, Martin. .Encyclopædia Britannica Online"Sea ice" in the Britannica Online, 2012. Accessed 21 April 2013.
  35. ^ a b Russell, F.S. & al. The Seas, pp. 225–227. Frederick Warne, 1928.
  36. ^ Swedish Meteorological and Hydrological Institute. "Oxygen in the Sea". 2010. Accessed 6 Jul 2013.
  37. ^ United States Environmental Protection Agency. , 5.2: "Dissolved Oxygen and Biochemical Oxygen Demand"Water Monitoring & Assessment. 2012. Accessed Aug 7 2014.
  38. ^ Shaffer, Gary & al. "Long-term Ocean Oxygen Depletion in Response to Carbon Dioxide Emissions from Fossil Fuels" in Nature Geoscience, Vol. 2, No. 2, pp. 105–109. 2009. DOI 10.1038/ngeo420. Bibcode 2009NatGe...2..105S.
  39. ^ a b c National Oceanic and Atmospheric Administration. "Ocean Waves" in the Ocean Explorer. Accessed 17 April 2013.
  40. ^ Young, I.R. Wind Generated Ocean Waves, p. 83. Elsevier, 1999. ISBN 0-08-043317-0.
  41. ^ a b c Garrison, Tom. pp. 204 ff., 6th ed., Essentials of Oceanography Brooks/Cole (Belmont), 2012. ISBN 0321814053.
  42. ^ National Meteorological Library and Archive. "Fact Sheet 6—The Beaufort Scale". Met Office (Devon), 2010. Accessed 7 Aug 2014.
  43. ^ Goda, Y. Random Seas and Design of Maritime Structures, pp. 421–22. World Scientific, 2000. ISBN 978-981-02-3256-6.
  44. ^ Holliday, N.P. & al. "Were extreme waves in the Rockall Trough the largest ever recorded?" in Geophysical Research Letters, Vol. 33. 2006. L05613.
  45. ^ Laird, Anne. "Observed Statistics of Extreme Waves". Naval Postgraduate School (Monterey), 2006. Accessed 7 Aug 2014.
  46. ^ United States Geological Survey. "Summary". Accessed 12 Aug 2010.
  47. ^ a b c "Life of a Tsunami". Tsunamis & Earthquakes. US Geological Survey. Retrieved 18 April 2013. 
  48. ^ a b "Physics of Tsunamis".  
  49. ^ a b c "The Physics of Tsunamis". Earth and Space Sciences. University of Washington. Retrieved 21 September 2013. 
  50. ^ "Tsunami warning system". 28 June 2009. Retrieved 4 October 2013. 
  51. ^ "Tsunami Programme: About Us". Intergovernmental Oceanographic Commission. Retrieved 4 October 2013. 
  52. ^ Our Amazing Planet staff (12 March 2012). "Deep Ocean Floor Can Focus Tsunami Waves". Livescience. Retrieved 4 October 2013. 
  53. ^ Berry, M. V. (2007). "Focused tsunami waves". Proceedings of the Royal Society: A 463 (2087): 3055.  
  54. ^ Bureau of Meteorology of the Australian Government. "Tsunami Facts and Information". Accessed 3 October 2013.
  55. ^ a b c "Tides and Water Levels". NOAA Oceans and Coasts. NOAA Ocean Service Education. Retrieved 20 April 2013. 
  56. ^ "Tidal amplitudes". University of Guelph. Retrieved 12 September 2013. 
  57. ^ a b "Tides". Ocean Explorer. National Oceanic and Atmospheric Administration. Retrieved 20 April 2013. 
  58. ^ Eginitis, D. (1929). "The problem of the tide of Euripus". Astronomische Nachrichten 236 (19–20): 321–328.  
  59. ^ "Evia Island". Chalkis. Retrieved 29 June 2013. 
  60. ^ Cline, Isaac M. (4 February 2004). "Galveston Storm of 1900". National Oceanic and Atmospheric Administration. Retrieved 21 April 2013. 
  61. ^ Ahrens, C. Donald; Jackson, Peter Lawrence; Jackson, Christine E. J.; Jackson, Christine E. O. (2012). Meteorology Today: An Introduction to Weather, Climate, and the Environment. Cengage Learning. p. 283.  
  62. ^ a b c d "Ocean Currents". Ocean Explorer. National Oceanic and Atmospheric Administration. Retrieved 19 April 2013. 
  63. ^ Pope, Vicky (2 February 2007). "'"Models 'key to climate forecasts. BBC. Retrieved 8 September 2013. 
  64. ^ Cushman-Roisin, Benoit; Beckers, Jean-Marie (2011). Introduction to Geophysical Fluid Dynamics: Physical and Numerical Aspects. Academic Press.  
  65. ^ Wunsch, Carl (2002). "What is the thermohaline circulation?". Science 298 (5596): 1179–1181.  
  66. ^ "Long-shore currents". Orange County Lifeguards. 2007. Retrieved 19 April 2013. 
  67. ^ "Rip current characteristics". Rip currents. University of Delaware Sea Grant College Program. Retrieved 19 April 2013. 
  68. ^ "Marine and Coastal: Bathymetry". Geoscience Australia. Retrieved 25 September 2013. 
  69. ^ Pidwirny, Michael (28 March 2013). "Structure of the Earth". The Encyclopedia of Earth. Retrieved 20 September 2013. 
  70. ^ Pidwirny, Michael (28 March 2013). "Plate tectonics". The Encyclopedia of Earth. Retrieved 20 September 2013. 
  71. ^ "Plate Tectonics: The Mechanism". University of California Museum of Paleontology. Retrieved 20 September 2013. 
  72. ^ "Scientists map Mariana Trench, deepest known section of ocean in the world". The Telegraph. 7 December 2011. Retrieved 24 September 2013. 
  73. ^ "Peru-Chile Trench". Encyclopedia Britannica. Britannica Online Encyclopedia. Retrieved 24 September 2013. 
  74. ^ a b c Monkhouse, F. J. (1975). Principles of Physical Geography. Hodder & Stoughton. pp. 280–291.  
  75. ^ Whittow, John B. (1984). The Penguin Dictionary of Physical Geography. Penguin Books. pp. 29, 80, 246.  
  76. ^ "Thames Barrier engineer says second defence needed". BBC News. 5 January 2013. Retrieved 18 September 2013. 
  77. ^ Plant, G.W.; Covil, C.S; Hughes, R.A.; Airport Authority Hong Kong (1998). Site Preparation for the New Hong Kong International Airport. Thomas Telford. pp. 1–4, 43.  
  78. ^ a b United Nations Office of Legal Affairs. "United Nations Convention on the Law of the Sea of 10 December 1982" at Oceans & Law of the Sea. United Nations Division for Ocean Affairs and the Law of the Sea (New York), 22 Aug 2013. Accessed 10 Aug 2014.
  79. ^ Müller, R. Dietmar; Sdrolias, Maria; Gaina, Carmen; Steinberger, Bernhard; Heine, Christian (2008). "Long-term sea-level fluctuations driven by ocean basin dynamics". Science 319 (5868): 1357–1362.  
  80. ^ Bruce C. Douglas (1997). "Global sea rise: a redetermination". Surveys in Geophysics 18 (2/3): 279–292.  
  81. ^ Bindoff, N. L.; Willebrand, J.; Artale, V.; Cazenave, A.; Gregory, J.; Gulev, S.; Hanawa, K.; Le Quéré, C.; Levitus, S.; Nojiri, Y.; Shum, A.; Talley, L. D.; Unnikrishnan, A. S.; Josey, S. A.; Tamisiea, M.; Tsimplis, M.; Woodworth, P. (2007). Observations: Oceanic Climate Change and Sea Level. Cambridge University Press. pp. 385–428.  
  82. ^ Meeh, Gerald A.; Washington, Warren M.; Collins, William D.; Arblaster, Julie M.; Hu, Aixue; Buja, Lawrence E.; Strand, Warren G.; Teng, Haiyan (2005). "How much more global warming and sea level rise?". Science 307 (5716): 1769–1772.  
  83. ^ "The Water Cycle: The Oceans". US Geological Survey. Retrieved 12 September 2013. 
  84. ^ Vesilind, Priit J. (2003). "The Driest Place on Earth". National Geographic. Retrieved 12 September 2013. 
  85. ^ "Endorheic Lakes: Waterbodies That Don't Flow to the Sea". The Watershed: Water from the Mountains into the Sea. United Nations Environment Programme. Retrieved 16 September 2013. 
  86. ^ a b Falkowski, P.; Scholes, R. J.; Boyle, E.; Canadell, J.; Canfield, D.; Elser, J.; Gruber, N.; Hibbard, K.; Högberg, P.; Linder, S.; MacKenzie, F. T.; Moore b, 3.; Pedersen, T.; Rosenthal, Y.; Seitzinger, S.; Smetacek, V.; Steffen, W. (2000). "The Global Carbon Cycle: A Test of Our Knowledge of Earth as a System". Science 290 (5490): 291–296.  
  87. ^ Sarmiento, J. L.; Gruber, N. (2006). Ocean Biogeochemical Dynamics. Princeton University Press. 
  88. ^ a b Prentice, I. C. (2001). "The carbon cycle and atmospheric carbon dioxide". Climate change 2001: the scientific basis: contribution of Working Group I to the Third Assessment Report of the Intergouvernmental Panel on Climate Change / Houghton, J. T. [ed.] Retrieved 26 September 2012. 
  89. ^ "Ocean Acidity". U.S. EPA climate change web site.  
  90. ^ Feely, R. A.; et al. (July 2004). System in the Oceans"3 on the CaCO2"Impact of Anthropogenic CO. Science 305 (5682): 362–366.  
  91. ^ Zeebe, R. E.; Zachos, J. C.; Caldeira, K.; Tyrrell, T. (4 July 2008). "OCEANS: Carbon Emissions and Acidification". Science 321 (5885): 51–52.  
  92. ^ Gattuso, J.-P.; Hansson, L. (15 September 2011). Ocean Acidification. Oxford University Press.  
  93. ^ a b "Ocean acidification". Department of Sustainability, Environment, Water, Population & Communities: Australian Antarctic Division. 28 September 2007. Retrieved 17 April 2013. 
  94. ^ Tanner, G. A. (18 January 2012). "Acid-Base Homeostasis". In Rhoades, R. A.; Bell, D. R. Medical Physiology: Principles for Clinical Medicine. Lippincott Williams & Wilkins.  
  95. ^ Pinet, Paul R. (1996). Invitation to Oceanography. West Publishing Company. pp. 126, 134–135.  
  96. ^ "What is Ocean Acidification?". NOAA PMEL Carbon Program. Retrieved 15 September 2013. 
  97. ^ Orr, James C.; et al. (2005). "Anthropogenic ocean acidification over the twenty-first century and its impact on calcifying organisms".  
  98. ^ Cohen, A.; Holcomb, M. (2009). "Why Corals Care About Ocean Acidification: Uncovering the Mechanism". Oceanography 24 (4): 118–127.  
  99. ^ Hönisch, Bärbel; Ridgwell, Andy; Schmidt, Daniela N.; Thomas, E.; Gibbs, S. J.; Sluijs, A.; Zeebe, R.; Kump, L.; Martindale, R. C.; Greene, S. E.; Kiessling, W.; Ries, J.; Zachos, J. C.; Royer, D. L.; Barker, S.; Marchitto, T. M.; Moyer, R.; Pelejero, C.; Ziveri, P.; Foster, G. L.; Williams, B. (2012). "The Geological Record of Ocean Acidification".  
  100. ^ Gruber, N. (18 April 2011). "Warming up, turning sour, losing breath: ocean biogeochemistry under global change". Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 369 (1943): 1980–1996.  
  101. ^ "Profile". Department of Natural Environmental Studies: University of Tokyo. Retrieved 26 September 2013. 
  102. ^ Mann, Nicholas H. (2005). "The third age of phage". PLoS Biology 3 (5): 753–755.  
  103. ^ Levinton, Jeffrey S. (2010). "18. Fisheries and Food from the Sea". Marine Biology: International Edition: Function, Biodiversity, Ecology. Oxford University Press.  
  104. ^ a b Kindersley, Dorling (2011). Illustrated Encyclopedia of the Ocean. Dorling Kindersley.  
  105. ^ Spalding MD and Grenfell AM (1997). "New estimates of global and regional coral reef areas". Coral Reefs 16 (4): 225.  
  106. ^ Neulinger, Sven (2008–2009). "Cold-water reefs". Retrieved 22 April 2013. 
  107. ^ Yool, Andrew; Tyrrell, Toby (2003). "Role of diatoms in regulating the ocean's silicon cycle". Global Biogeochemical Cycles 17 (4): 1103–1124.  
  108. ^ van der Heide, T.; van Nes, E. H.; van Katwijk, M. M.; Olff, H.; Smolders, A. J. P. (2011). Romanuk, Tamara, ed. "Positive feedbacks in seagrass ecosystems: evidence from large-scale empirical data". PLoS ONE 6 (1): e16504.  
  109. ^ "Mangal (Mangrove)". Mildred E. Mathias Botanical Garden. Retrieved 11 July 2013. 
  110. ^ "Coastal Salt Marsh". Mildred E. Mathias Botanical Garden. Retrieved 11 July 2013. 
  111. ^ "Facts and figures on marine biodiversity". Marine biodiversity. UNESCO. 2012. Retrieved 11 July 2013. 
  112. ^ Voss, Maren; Bange, Hermann W.; Dippner, Joachim W.; Middelburg, Jack J.; Montoya, Joseph P.; Ward, Bess (2013). "The marine nitrogen cycle: recent discoveries, uncertainties and the potential relevance of climate change". Philosophical Transactions of the Royal Society B 368 (1621): 20130121.  
  113. ^ a b Thorne-Miller, Boyce (1999). The Living Ocean: Understanding and Protecting Marine Biodiversity. Island Press. p. 2.  
  114. ^ Thorne-Miller, Boyce (1999). The Living Ocean: Understanding and Protecting Marine Biodiversity. Island Press. p. 88.  
  115. ^ Kingsford, Michael John. "Marine ecosystem: Plankton". Encyclopedia Britannica. Britannica Online Encyclopedia. Retrieved 14 July 2013. 
  116. ^ Walrond, Carl. "Oceanic Fish". The Encyclopedia of New Zealand. New Zealand Government. Retrieved 14 July 2013. 
  117. ^ Steele, John H.; Thorpe, Steve A.; Turekian, Karl K. (eds.) (2010). Marine Ecological Processes: A Derivative of the Encyclopedia of Ocean Sciences. Academic Press. p. 316.  
  118. ^ "Invasive species". Water: Habitat Protection. Environmental Protection Agency. 6 March 2012. Retrieved 17 September 2013. 
  119. ^ Sedberry, G. R.; Musick, J. A. (1978). "Feeding strategies of some demersal fishes of the continental slope and rise off the Mid-Atlantic Coast of the USA". Marine Biology 44 (44): 357–375.  
  120. ^ Committee on Biological Diversity in Marine Systems, National Research Council (1995). "Waiting for a whale: human hunting and deep-sea biodiversity". Understanding Marine Biodiversity. National Academies Press.  
  121. ^ University of Wollongong. "Skeleton Reveals Lost World Of 'Little People'". Hosted at ScienceDaily. 28 October 2004. Accessed 29 July 2014.
  122. ^ a b Cane, Scott. First Footprints—The Epic Story of the First Australians, pp. 25 f. Allen & Unwin, 2013. ISBN 978 1 74331 493 7.
  123. ^ Lourandos, H. Continent of Hunter-Gatherers: New Perspectives in Australian Prehistory, pp. 80 f. Cambridge University Press (Cambridge), 1997.
  124. ^ Gerritsen, Rupert. Beyond the Frontier: Explorations in Ethnohistory, pp. 70 ff. Batavia Online Publishing (Canberra), 2011. ISBN 978-0-9872141-4-0.
  125. ^ Carter, Robert. pp. 347 ff., Ch. 19: "Watercraft", A Companion to the Archaeology of the Ancient Near East Wiley-Blackwell (Chichester), 2012. ISBN 978-1-4051-8988-0. Accessed 8 Feb 2014.
  126. ^ Rao, S.R. Lothal in the Archaeological Survey of India, pp. 27 f. 1985.
  127. ^ Hage, P.; Marck, J. (2003). "Matrilineality and Melanesian Origin of Polynesian Y Chromosomes". Current Anthropology 44 (S5): S121.  
  128. ^ Kayser, M.; Brauer, S.; Cordaux, R.; Casto, A.; Lao, O.; Zhivotovsky, L. A.; Moyse-Faurie, C.; Rutledge, R. B.; Schiefenhoevel, W.; Gil, D.; Lin, AA; Underhill, PA; Oefner, PJ; Trent, RJ; Stoneking, M. (2006). "Melanesian and Asian origins of Polynesians: mtDNA and Y chromosome gradients across the Pacific". Molecular Biology and Evolution 23 (11): 2234–2244.  
  129. ^ Su, B.; Jin, L.; Underhill, P.; Martinson, J.; Saha, N.; McGarvey, S. T.; Shriver, M. D.; Chu, J.; Oefner, P.; Chakraborty, R.; Deka, R. (2000). "Polynesian origins: Insights from the Y chromosome".  
  130. ^ Bellwood, Peter (1987). The Polynesians – Prehistory of an Island People. Thames and Hudson. pp. 45–65.  
  131. ^ Clark, Liesl (15 February 2000). "Polynesia's Genius Navigators". NOVA. Retrieved 10 May 2013. 
  132. ^ Kirch, Patrick. Hawaiki, p. 80. Cambridge University Press (Cambridge), 2001. ISBN 978-0-521-78309-5.
  133. ^ Hunt, Terry & al. The Statues that Walked: Unraveling the Mystery of Easter Island. Free Press, 2011. ISBN 1-4391-5031-1.
  134. ^ Lowe, David. p. 142"Polynesian settlement of New Zealand and the Impacts of Volcanism on Early Maori Society: an Update", , in Guidebook for Pre-conference North Island Field Trip A1 ‘Ashes and Issues’. Nov 2008. ISBN 978-0-473-14476-0. Accessed 18 Jan 2010.
  135. ^ Herodotus. Ἱστορίαι [The Histories], IV.42. c. 420 BC. (Ancient Greek)
  136. ^ Tozer, Henry F. (1997). pp. 189 f., History of Ancient Geography Biblo & Tannen, 1997. ISBN 0-8196-0138-1.
  137. ^ Harden, Donald. The Phoenicians, p. 168. Penguin (Harmondsworth), 1962. Reprinted 1971.
  138. ^ Warmington, Brian H. Carthage, p. 79. Penguin (Harmondsworth), 1960. Reprinted 1964.
  139. ^ Mckenzie, Judith (2007). Architecture of Alexandria and Egypt 300 B.C A.D 700. Yale University Press. p. 41.  
  140. ^ Jenkins, Simon (1992). "Four Cheers for Geography". Geography 77 (3): 193–197.  
  141. ^ Sobel, Dava. Longitude: The True Story of a Lone Genius Who Solved the Greatest Scientific Problem of His Time. Walker, 1995.
  142. ^ U.S. Antarctic Program External Panel. "Antarctica —past and present".  
  143. ^ Guy G. Guthridge. "Nathaniel Brown Palmer".  
  144. ^ Palmer Station.
  145. ^ Sverdlov, Leonid (27 November 1996). "Russian naval officers and geographic exploration in Northern Russia (18th through 20th centuries)". Arctic Voice No. 11. Retrieved 12 September 2013. 
  146. ^ Зацепились за Моржовец (in Russian). Русское географическое общество. 2012. Retrieved 5 March 2012. 
  147. ^ a b BBC. "A History of Navigation". Accessed 13 Sept 2013.
  148. ^ Rozwadowski, Helen. pp. 141 ff., Fathoming the Ocean: The Discovery and Education of the Deep Sea Harvard University Press (Cambridge), 2005. Accessed 9 Aug 2014.
  149. ^ Rozwadowski (2005), }
  150. ^ International Hydrographic Organization. Official website. 15 March 2013. Accessed 14 Sept 2013.
  151. ^ "Underwater Exploration—History, Oceanography, Instrumentation, Diving Tools and Techniques, Deep-sea Submersible Vessels, Key Findings in Underwater Exploration, Deep-sea Pioneers" in the Science Encyclopedia. Net Industries. Accessed 15 Sept 2013.
  152. ^ "Jacques Piccard: Oceanographer and pioneer of deep-sea exploration". The Independent. 5 November 2008. Retrieved 15 September 2013. 
  153. ^ Logico, Mark G. (8 April 2006). "Navy Chief Submerges 2,000 Feet, Sets Record". America's Navy. United States Navy. Retrieved 12 September 2013. 
  154. ^ "Research topics". Scripps Institution of Oceanography. Retrieved 16 September 2013. 
  155. ^ "Research at Sea". National Oceanography Centre. 2013. Retrieved 20 September 2013. 
  156. ^ Gosch, Stephen S. & al. Premodern Travel in World History. Taylor & Francis, 2007. ISBN 0-203-92695-1.
  157. ^ Hägg, R. & al. The Minoan Thalassocracy: Myth and Reality. (Stockholm), 1994.
  158. ^ Greer, Thomas & al. , p. 63A Brief History of the Western World. Thomson Wadsworth, 2004. ISBN 978-0-534-64236-5.
  159. ^ Shaffer, Lynda. "Southernization" in Agricultural and Pastoral Societies in Ancient and Classical History. Temple University Press, 2001. ISBN 1-56639-832-0.
  160. ^ Curtin, Philip D. (1984). Cross-Cultural Trade in World History. Cambridge University Press. pp. 88–104.  
  161. ^ Tibbets, Gerald Randall (1979). A Comparison of Medieval Arab Methods of Navigation with Those of the Pacific Islands. Coimbra. 
  162. ^ Kubetzek, Kathrin; Kant, Karo (2012). The Atlantic Slave Trade: Effects on Africa. GRIN Verlag. p. 1.  
  163. ^ Smith, Jack (1985). succumbs to the sea"Challenger remains at King's Point as SS United States"Hales Trophy, won in 1952 by . Yachting (November): 121. 
  164. ^ Halpern, Benjamin S.; Walbridge, Shaun; Selkoe, Kimberly A.; Kappel, Carrie V.; Micheli, Fiorenza; D'Agrosa, Caterina; Bruno, John F.; Casey, Kenneth S.; Ebert, Colin; Fox, Helen E.; Fujita, Rod; Heinemann, Dennis; Lenihan, Hunter S.; Madin, Elizabeth M. P.; Perry, Matthew T.; Selig, Elizabeth R.; Spalding, Mark; Steneck, Robert; Watson, Reg (2008). "A global map of human impact on marine ecosystems". Science 319 (5865): 948–952.  
  165. ^ "Trade routes". World Shipping Council. Retrieved 25 April 2013. 
  166. ^ Roach, John (17 September 2007). "Arctic Melt Opens Northwest Passage". National Geographic. Retrieved 17 September 2013. 
  167. ^ "Global trade". World Shipping Council. Retrieved 25 April 2013. 
  168. ^  
  169. ^ Reed Business Information (22 May 1958). "News and Comments". The New Scientist 4 (79): 10. 
  170. ^ a b Sauerbier, Charles L.; Meurn, Robert J. (2004). Marine Cargo Operations: a guide to stowage. Cambridge, Md: Cornell Maritime Press. pp. 1–16.  
  171. ^ "Freight forwarder". Random House Unabridged Dictionary. Random House. 1997. Retrieved 24 April 2013. 
  172. ^ "Introduction to IMO". International Maritime Organization. 2013. Retrieved 14 September 2013. 
  173. ^ Hu, Y. & al. "Stable Isotope Dietary Analysis of the Tianyuan 1 Early Modern Human" in Proceedings of the National Academy of Sciences, Vol. 106, No. 27, pp. 10 971–10 974. Jul 2009. Bibcode 2009PNAS..10610971H. DOI 10.1073/pnas.0904826106. ISSN 0027-8424. PMC 2706269. PMID 19581579.
  174. ^ Guthrie, Dale. p. 298, The Nature of Paleolithic Art. University of Chicago Press (Chicago), 2005. ISBN 0-226-31126-0.
  175. ^ 范蠡 [Fan Li]. 《養魚經》 or 《养鱼经》 [Yǎngyú Jīng, "The Fish-Breeding Classic"]. c. 475 BC. (Chinese)
  176. ^ Nash, Colin. pp. 26 ff., The History of Aquaculture Blackwell Publishing (Danvers), 2011. Accessed 12 Aug 2014.
  177. ^ Ἰσίδωρος Χαρακηνός [Isidore of Charax]. Τὸ τῆς Παρθίας Περιηγητικόν [Tò tēs Parthías Periēgētikón, A Journey around Parthia]. c. 1st century AD (Ancient Greek) in Ἀθήναιος [Athenaeus]. Δειπνοσοφισταί [Deipnosophistaí, The Dinner Experts], Book III, 93E. c. 3rd century (Ancient Greek) Trans. Charles Burton Gulick as p. 403. Vol. I,, Athenaeus Harvard University Press (Cambridge), 1927. Accessed 13 Aug 2014.
  178. ^ Ὀππιανός [Oppian]. Ἁλιευτικά [Halieutiká, The Halieutics]. c. 180. Trans. John Jones as Oppian's Halieuticks, Part II: "Of the Fishing of the Ancients", Book III, ll. 103–132. Rob. Shippen (Oxford), 1722.
  179. ^ Kurlansky, Mark. Cod: A Biography of the Fish That Changed the World. Walker (New York), 1997. ISBN 0-8027-1326-2.
  180. ^ Trinity Sailing Foundation. Sailing Trawlers. Issuu (Brixham), 2014. Accessed 12 Aug 2014.
  181. ^ a b c d Kunzig, Robert. "Twilight of the Cod" in Discover, Vol. 52. April 1995. Accessed 1 May 2012.
  182. ^ a b c Granger, R. & al. pp. 3 ff., The State of World Fisheries and Aquaculture FAO Fisheries and Aquaculture Department (Rome), 2012. ISBN 978-92-5-107225-7. ISSN 1020-5489. Accessed 12 Aug 2014.
  183. ^ Hamilton, Lawrence & al. "Outport Adaptations: Social Indicators through Newfoundland's Cod Crisis" in Human Ecology Review, Vol. 8, No. 2, 1–11. 2001.
  184. ^ "Fishery Country Profile: The People's Republic of China". FAO Fisheries and Aquaculture Department (Rome), 2001. Accessed 13 Aug 2014.
  185. ^ Hou Qiang. "China starts annual South China Sea fishing ban". Xinhua (Beijing), 16 May 2013. Accessed 13 Aug 2014.
  186. ^ Hackett, Bob & al. "Tonan Maru No. 2: Tabular Record of Movement" at Yusosen! Stories and Battle Histories of the IJN's Oilers & Tanker Fleet. 2014. Accessed 13 Aug 2014.
  187. ^ Farmer, Tina. "[ Topics Fact Sheet: Fishing People]". FAO Fisheries and Aquaculture Department (Rome), 2014. Accessed 10 Aug 2014.
  188. ^ a b Statistics and Information Service. "Overview: Major Trends and Issues". FAO Fisheries and Aquaculture Department (Rome), 2012. Accessed 10 Aug 2014.
  189. ^ Watson, Reg & al. "Systematic Distortions in World Fisheries Catch Trends", Figure 1, in Nature, Vol. 414, No. 6863, pp. 534–536. 29 Nov 2001. DOI 10.1038/35107050. Accessed 10 Aug 2014.
  190. ^ "[ Peruvian Fisheries' Production Up Dramatically]" in Peru This Week. 17 Jan 2014. Accessed 13 Aug 2014.
  191. ^ Evans, Michael. "Fishing" at Earth Times. 3 June 2011. Accessed 23 April 2013.
  192. ^ a b "Fisheries: Latest data". GreenFacts. Retrieved 23 April 2013. 
  193. ^ Myers, R. A.; Worm, B. (2003). "Rapid worldwide depletion of predatory fish communities". Nature 423 (6937): 280–283.  
  194. ^ Charles Clover (2008). The End of the Line: How Overfishing is Changing the World and what We Eat. University of California Press.  
  195. ^ Béné, C.; Macfadyen, G.; Allison, E. H. (2007). Increasing the contribution of small-scale fisheries to poverty alleviation and food security. Fisheries Technical Paper. No. 481 (FAO).  
  196. ^ The State of World Fisheries and Aquaculture 2012. FAO Fisheries and Aquaculture Department. 2012.  
  197. ^ Soto, D. (ed.) (2009). Integrated mariculture. Fisheries and Aquaculture Technical Paper. No. 529 (FAO).  
  198. ^ "About shrimp farming". Shrimp News International. Archived from the original on 1 February 2010. Retrieved 25 April 2013. 
  199. ^ "Sea cucumber ranching improves livelihoods". WorldFish. Retrieved 25 April 2013. 
  200. ^ Anderson, Genny (15 June 2009). "Lobster mariculture". Marine Science. Retrieved 25 April 2013. 
  201. ^ Winterman, Denise (30 July 2012). "Future foods: What will we be eating in 20 years' time?". BBC. Retrieved 24 April 2013. 
  202. ^ "Samphire". BBC: Good Food. Retrieved 24 April 2013. 
  203. ^ "An Overview of China's Aquaculture", p. 6. Netherlands Business Support Office (Dalien), 2010. Accessed 13 Aug 2014.
  204. ^ Black, K.D. "Environmental, economic and social impacts of mariculture" in Encyclopedia of Ocean Sciences, pp. 1578-1584. Academic Press, 2001.
  205. ^ Jefferson, Thomas & al. "A Declaration by the Representatives of the United States of America, in General Congress Assembled". John Dunlap (Philadelphia), 1776.
  206. ^ The section admonishing Trial by Jury"[205] referred to the enforcement of the Stamp Act by the courts of admiralty, considered more likely to secure a conviction than a colonial jury.
  207. ^ Grotius, Hugo. Mare Liberum ["The Free Sea"]. 1609. (Latin)
  208. ^ Bynkershoek, Cornelius. De dominio maris ["On the Dominion of the Sea"]. 1702. (Latin)
  209. ^ a b c United Nations Office of Legal Affairs. "The United Nations Convention on the Law of the Sea (A historical perspective)" at Oceans & Law of the Sea. United Nations Division for Ocean Affairs and the Law of the Sea (New York), 2012. Accessed 10 Aug 2014.
  210. ^ Truman, Harry. : Policy of the United States with Respect to the Natural Resources of the Subsoil of the Sea Bed and the Continental ShelfNo. 2667Presidential Proclamation . (Washington), 28 Sept 1945. Hosted at the National University of Singapore. Accessed 14 Aug 2014.
  211. ^ United Nations Convention on the Law of the Sea (1982), §87(1).
  212. ^ Dutton, Benjamin (2004). Dutton's Nautical Navigation (15 ed.). Naval Institute Press. pp. 260–265. 
  213. ^ Grant, R.G. Battle at Sea: 3,000 Years of Naval Warfare. 2008. Accessed 10 Aug 2010.
  214. ^ Drews, Robert. The End of the Bronze Age: Changes in Warfare and the Catastrophe ca. 1200 B.C.. 1993.
  215. ^ Strauss, Barry. The Battle of Salamis: The Naval Encounter that Saved Greece—and Western Civilization, p. 26. Simon & Schuster, 2004. ISBN 0-7432-4450-8.
  216. ^ Herodotus. Ἱστορίαι [The Histories], VIII. 97. c. 420 BC. (Ancient Greek)
  217. ^ Fremont-Barnes, Gregory; Hook, Christa (2005). Trafalgar 1805: Nelson's Crowning Victory. Osprey Publishing. p. 1.  
  218. ^ Sterling, Christopher. .p. 459, Military Communications: From Ancient Times to the 21st Century ABC-CLIO, 2008. ISBN 1-85109-732-5.
  219. ^ "The naval battle of Tsushima, the ultimate contest of the 1904–1905 Russo-Japanese War, was one of the most decisive sea battles in history."[218]
  220. ^ Campbell, John. Jutland: An Analysis of the Fighting, p. 2. Lyons Press, 1998. ISBN 1-55821-759-2.
  221. ^ Helgason, Guðmundur. "Finale" at Accessed 13 Sept 2013.
  222. ^ Bennett, William. America: The Last Best Hope, Vol. 2: From a World at War to the Triumph of Freedom 1914—1989, p. 301. Nelson Current, 2007. ISBN 978-1-59555-057-6.
  223. ^ BBC. "Q&A: Trident Replacement". 22 Sept 2010. Accessed 15 Sept 2013.
  224. ^ California Center for Military History. "Submarines of the Cold War". Accessed 15 Sept 2013.
  225. ^ Simpson, Michael. A Life of Admiral of the Fleet Andrew Cunningham: A Twentieth-Century Naval Leader, p. 74. Routledge, 2004. ISBN 978-0-7146-5197-2.
  226. ^ Crocker, H.W. III. Don't Tread on Me: A 400-Year History of America at War, pp. 294 ff. Three Rivers Press, 2006. ISBN 978-1-4000-5364-3.
  227. ^ Thomas, Evan. Sea of Thunder, pp. 3 f. Simon & Schuster, 2007. ISBN 0-7432-5222-5.
  228. ^ Lickorish, Leonard & al. .p. 16, Introduction to Tourism Butterworth–Heinemann (Oxford), 1997. Accessed 8 Aug 2014.
  229. ^ Hazbun, Waleed. p. 5,"The East as an Exhibit: Thomas Cook & Son and the Origins of the International Tourism Industry in Egypt", in The Business of Tourism: Place, Faith, and History. University of Pennsylvania Press (Philadelphia), 2007. Accessed 8 Aug 2014.
  230. ^ Newman, Jeff. "The Blue Riband of the North Atlantic" at Great Ships. Accessed 11 Sept 2013.
  231. ^ Norris, Gregory. "Evolution of Cruising" in Cruise Travel, p. 28. Dec 1981.
  232. ^ "No evidence to support Foreign Minister Bob Carr's economic migrants claims". ABC News. 15 August 2013. Retrieved 21 August 2013. 
  233. ^ "The voice of the recreational marine industry worldwide". International Council of Marine Industry Associations. 2013. Retrieved 25 April 2013. 
  234. ^ "Yachting". Retrieved 17 September 2013. 
  235. ^ Aas, Øystein (ed.) (2008). Global Challenges in Recreational Fisheries. John Wiley and Sons. p. 5.  
  236. ^ Dowling, Ross Kingston (ed.) (2006). Cruise Ship Tourism. CABI. p. 3.  
  237. ^ Cater, Carl; Cater, Erlet (2007). Marine Ecotourism: Between the Devil and the Deep Blue Sea. CABI. p. 8.  
  238. ^ "Health Benefits of Sea Bathing". MedClick. Retrieved 4 July 2013. 
  239. ^ Nickel, Christoph; Zernial, Oliver; Musahl, Volker; Hansen, Ute; Zantop, Thore; Petersen, Wolf (2004). "A prospective study of kitesurfing injuries". American Journal of Sports Medicine 32 (4): 921–927.  
  240. ^ "The disciplines of windsurfing". World of Windsurfing. 15 April 2013. Retrieved 4 July 2013. 
  241. ^ "Water skiing disciplines". ABC of Skiing. Retrieved 4 July 2013. 
  242. ^ Catelle, W. R. (1907). "Methods of Fishing". The Pearl: Its Story, Its Charm, and Its Value. J. B. Lippincott. p. 171. 
  243. ^ a b US Navy Diving Manual, 6th revision. US Naval Sea Systems Command. 2006. Retrieved 4 May 2013. 
  244. ^ Ovdak, Alla & al. "Offshore Wind Energy in France". Oct 2013. Accessed 31 July 2014.
  245. ^ a b "Ocean Energy". Ocean Energy Systems. 2011. Retrieved 5 July 2013. 
  246. ^ Cruz, João (2008). Ocean Wave Energy – Current Status and Future Perspectives. Springer. p. 2.  
  247. ^ US Department of the Interior (May 2006). "Ocean Current Energy Potential on the U.S. Outer Continental Shelf". Retrieved 8 May 2013. 
  248. ^ Ponta, F. L.; Jacovkis, P. M. (2008). "Marine-current power generation by diffuser-augmented floating hydro-turbines". Renewable Energy 33 (4): 665–673.  
  249. ^ "Offshore Wind Power 2010". BTM Consult. 22 November 2010. Retrieved 25 April 2013. 
  250. ^  
  251. ^ Tillessen, Teena (2010). "High demand for wind farm installation vessels". Hansa International Maritime Journal 147 (8): 170–171. 
  252. ^ "Cooling power plants". World Nuclear Association. 1 September 2013. Retrieved 14 September 2013. 
  253. ^ Lamb, Robert (2011). "How offshore drilling works". HowStuffWorks. Retrieved 6 May 2013. 
  254. ^ Nixon, Robin (25 June 2008). "Oil Drilling: Risks and Rewards". LiveScience. Retrieved 30 November 2014. 
  255. ^ Horton, Jennifer (2011). "Effects of offshore drilling: energy vs. environment". HowStuffWorks. Retrieved 6 May 2013. 
  256. ^ "Chemistry: Mining the Sea". Time. 15 May 1964. Retrieved 25 April 2013. 
  257. ^ Al-Weshah, Radwan A. (2000). "The water balance of the Dead Sea: an integrated approach". Hydrological Processes 14 (1): 145–154.  
  258. ^ Nurok, G. A.; Bubis, I. V. (1970–1979). "Mining, Undersea". The Great Soviet Encyclopedia, 3rd Edition. Retrieved 6 May 2013. 
  259. ^ Kohl, Keith (2013). "Underwater Mining Companies". Wealth Daily. Retrieved 6 May 2013. 
  260. ^ Miner, Meghan (1 February 2013). "Will Deep-sea Mining Yield an Underwater Gold Rush?". National Geographic. Retrieved 6 May 2013. 
  261. ^ Hamed, Osman A. (2005). "Overview of hybrid desalination systems – current status and future prospects". Desalination 186: 207–214.  
  262. ^ Milkov, A. V. (2004). "Global estimates of hydrate-bound gas in marine sediments: how much is really out there?". Earth-Science Review 66 (3–4): 183–197.  
  263. ^ Achurra, L. E.; Lacassie, J. P.; Le Roux, J. P.; Marquardt, C.; Belmar, M.; Ruiz-del-solar, J.; Ishman, S. E. (2009). "Manganese nodules in the Miocene Bahía Inglesa Formation, north-central Chile: petrography, geochemistry, genesis and palaeoceanographic significance". Sedimentary Geology 217 (1–4): 128–130.  
  264. ^ "Diamonds". Geological Survey of Namibia. Ministry of Mines and Energy. 2006. Retrieved 26 September 2013. 
  265. ^ "Toxic Pollution". Ocean Briefing Book. SeaWeb. Retrieved 23 April 2013. 
  266. ^ Ansari, T. M.; Marr, L. L.; Tariq, N. (2004). "Heavy metals in marine pollution perspective: a mini review". Journal of Applied Sciences 4 (1): 1–20.  
  267. ^ a b "Marine problems: Pollution". World Wildlife Fund. Retrieved 21 April 2013. 
  268. ^ Dell'Amore, Christine (12 April 2013). "New Diseases, Toxins Harming Marine Life". National Geographic Daily News. National Geographic. Retrieved 23 April 2013. 
  269. ^ Jefferies, D. F.; Preston, A.; Steele, A. K. (1973). "Distribution of caesium-137 in British coastal waters". Marine Pollution Bulletin 4 (8): 118–122.  
  270. ^ Tsumunea, Daisuke; Tsubonoa, Takaki; Aoyamab, Michio; Hirosec, Katsumi (2012). "Distribution of oceanic 137–Cs from the Fukushima Dai-ichi Nuclear Power Plant simulated numerically by a regional ocean model". Journal of Environmental Radioactivity 111: 100–108.  
  271. ^ "London Convention and Protocol". International Maritime Organization. Retrieved 15 September 2012. 
  272. ^ "International Convention for the Prevention of Pollution from Ships (MARPOL 73/78)". International Maritime Organization. Retrieved 15 September 2012. 
  273. ^ Barnes, D. K. A.; Galgani, Francois; Thompson, Richard C.; Barlaz, Morton (2009). "Accumulation and fragmentation of plastic debris in global environments". Philosophical Transactions of the Royal Society 364 (1526): 1985–1998.  
  274. ^ Karl, David M. (199). "A sea of change: biogeochemical variability in the North Pacific subtropical gyre". Ecosystems 2 (3): 181–214.  
  275. ^ Lovett, Richard A. (2 March 2010). "Huge Garbage Patch Found in Atlantic too". National Geographic. Retrieved 10 July 2013. 
  276. ^ Moore, Charles James (2008). "Synthetic polymers in the marine environment: a rapidly increasing, long-term threat". Environmental Research 108 (2): 131–139.  
  277. ^ "How Does the BP Oil Spill Impact Wildlife and Habitat?". National Wildlife Federation. Retrieved 22 April 2013. 
  278. ^ American Chemical Society (9 April 2013). "Gulf of Mexico Has Greater-Than-Believed Ability to Self-Cleanse Oil Spills". Science Daily. Retrieved 22 April 2013. 
  279. ^ "Environmental, social and cultural settings of the Surin Islands". Sustainable Development in Coastal Regions and Small Islands. UNESCO. Retrieved 7 September 2013. 
  280. ^ "Samal – Orientation". Countries and Their Cultures. Retrieved 7 September 2013. 
  281. ^ Langenheim, Johnny (18 September 2010). "The last of the sea nomads". The Guardian. Retrieved 7 September 2013. 
  282. ^ Ivanoff, Jacques (1 April 2005). "Sea Gypsies of Myanmar". National Geographic. Retrieved 7 September 2013. 
  283. ^ Hovelsrud, Grete K; McKenna, Meghan; Huntington, Henry P (March 2008). "Marine Mammal Harvests and Other Interactions with Humans". Ecological Applications 18 (2): S135–S147.  
  284. ^ "Traditional Owners of the Great Barrier Reef". Great Barrier Reef Marine Park Authority. Retrieved 16 September 2013. 
  285. ^ Westerdahl, Christer (1994). "Maritime cultures and ship types: brief comments on the significance of maritime archaeology". International Journal of Nautical Archaeology 23 (4): 265–270.  
  286. ^ The Bible (King James Version). 1611. pp. Job 41: 1–34. 
  287. ^ Kerenyi, C. (1974). The Gods of the Greeks. Thames and Hudson. pp. 37–40.  
  288. ^ Shunsen, Takehara (1841). Ehon Hyaku Monogatari (絵本百物語, "Picture Book of a Hundred Stories") (in Japanese). Kyoto: Ryûsuiken. 
  289. ^ Pontoppidan, Erich (1839). The Naturalist's Library, Volume 8: The Kraken. W. H. Lizars. pp. 327–336. 
  290. ^ Cotterell, Arthur (ed.) (2000). World Mythology. Parragon.  
  291. ^ Slive, Seymour (1995). Dutch Painting, 1600–1800. Yale University Press. pp. 213–216.  
  292. ^ Johnson, Ken (30 July 2009). "When Galleons Ruled the Waves". New York Times. Retrieved 19 September 2013. 
  293. ^ Tymieniecka, Anna–Teresa (ed.) (1985). Poetics of the Elements in the Human Condition: Part I – The Sea: From Elemental Stirrings to the Symbolic Inspiration, Language, and Life-Significance in Literary Interpretation and Theory. Springer. pp. 4–8.  
  294. ^ Wagner, Richard (1843). "An Autobiographical Sketch". The Wagner Library. Retrieved 24 April 2013. 
  295. ^ Potter, Caroline; Trezise, Simon (ed.) (1994). "Debussy and Nature". The Cambridge Companion to Debussy. Cambridge University Press. p. 149.  
  296. ^ Schwartz, Elliot S. (1964). The Symphonies of Ralph Vaughan Williams. University of Massachusetts Press.  
  297. ^ Tymieniecka, Anna–Teresa (ed.) (1985). Poetics of the Elements in the Human Condition: Part I – The Sea: From Elemental Stirrings to the Symbolic Inspiration, Language, and Life-Significance in Literary Interpretation and Theory. Springer. p. 45.  
  298. ^ Homer (translation by Rieu, D. C. H.) (2003). The Odyssey. Penguin. pp. xi.  
  299. ^ Porter, John (8 May 2006). "Plot Outline for Homer's Odyssey". University of Saskatchewan. Retrieved 10 September 2013. 
  300. ^ Basho, Matsuo. "A Selection of Matsuo Basho's Haiku". Greenleaf. Retrieved 27 April 2013. 
  301. ^  
  302. ^ Najder, Zdzisław (2007). Joseph Conrad: A Life. Camden House. p. 187. 
  303. ^ "The Caine Mutiny". Pulitzer Prize First Edition Guide. 2006. Retrieved 25 May 2013. 
  304. ^ Jung, Carl Gustav (1985). Dreams. Translated by Hull, R.F.C. Ark Paperbacks. pp. 122, 192.  
  305. ^ Lal, Ashwini Kumar (2008). "Origin of Life". Astrophysics and Space Science 317 (3–4): 267–278.  
  306. ^  


  1. ^ One definition is that a sea is a sub-division of an ocean, although presently the [4] which are taken as customary and essentially arbitrary.[9] Another states that "sea" is a convenient name for a largely "land-locked" body of water,[10] which would exclude the Sargasso Sea. A third requires that seas possess a floor formed of oceanic crust, which would accept the Caspian since it was once part of an ancient ocean.[11]
  2. ^ Accordingly, the Convention does not apply to the Caspian, which is instead an "international lake" for most legal purposes.[13]
  3. ^ Hydrous ringwoodite recovered from volcanic eruptions suggests that the transition zone between the lower and upper mantle holds between one[17] and three[18] times as much water as all of the world's surface oceans combined. Experiments to recreate the conditions of the lower mantle suggest it may contain still more water as well, as much as five times the mass of water present in the world's oceans.[19][20]
  4. ^ Human kidneys excrete urine that is around 2% saline,[29] so that drinking one liter of most forms of seawater will require drinking at least another liter of freshwater to prevent harmful excesses of sodium. Without this additional water, increased urination to remove the salt produces dehydration.[30]
  5. ^ "As the waves leave the region where they were generated, the longer ones outpace the shorter because their velocity is greater. Gradually, they fall in with other waves travelling at similar speed—where different waves are in phase they reinforce each other, and where out of phase they are reduced. Eventually, a regular pattern of high and low waves (or swell) is developed that remains constant as it travels out across the ocean."[6](pp83–84)
  6. ^ To help put a change of this magnitude into perspective, when the pH of human blood plasma is raised from its normal 7.4 to a value above 7.8, or lowered to a value below 6.8, death ensues.[94]
  7. ^ Given that the most likely landfall regions have been under 50 meters (160 ft) of water since the end of the last ice age, it is unlikely that the timing will ever be established with certainty.[122] Two common theories are a crossing from Timor to the northwest Australian mainland around 70,000 years ago and a crossing from Sulawesi to New Guinea around 50,000 years ago,[122][123] possibly assisted by a tsunami.[124]
  8. ^ The Greek navigator Eudoxus was later reported by Strabo to have accidentally discovered a wrecked ship from Gades on the northeast coast of Africa and to have then attempted two (failed) circumnavigations of Africa around 116 BC.[136]
  9. ^ Capture of seafood from inland waters has grown constantly, from less than 3 million metric tons per year in 1950 to more than 11 million by 2010, but remains less than 10% of the total capture.[182]


See also

As a symbol, the sea has for centuries played a role in literature and poetry. Sometimes, it is there just as a gentle background but often it introduces such themes as storm, shipwreck, battle, hardship, disaster, the dashing of hopes, or death.[297] In his epic poem the Odyssey, written in the 8th century BC,[298] Homer describes the ten-year voyage of the Greek hero Odysseus who struggles to return home across the sea's many hazards after the war described in the Iliad.[299] The sea is a recurring theme in the Haiku poems of the Japanese poet Matsuo Bashō (1644–1694).[300] In modern literature, sea-inspired novels have been written by the sailors Herman Melville,[301] Joseph Conrad,[302] and Herman Wouk.[303] The psychiatrist Carl Jung argued that, in dream interpretation, the sea symbolizes the personal and the collective unconscious.[304] Although the origin of life on Earth is still a matter of debate,[305] naturalist Rachel Carson wrote in The Sea Around Us that "it is a curious situation that the sea, from which life first arose, should now be threatened by the activities of one form of that life. But the sea, though changed in a sinister way, will continue to exist: the threat is rather to life itself."[306]

Music too has been inspired by the ocean. Sea shanties were chanted by mariners to help coordinate arduous tasks and impressions in music have been created of calm waters, crashing waves, and storms at sea.[293] Classical sea-related music includes Richard Wagner's The Flying Dutchman,[294] Claude Debussy's La mer (1903–05),[295] Charles Villiers Stanford's Songs of the Sea (1904) and Songs of the Fleet (1910), Edward Elgar's Sea Pictures (1899), and Ralph Vaughan Williams's A Sea Symphony (1903–1909).[296]

The sea, its life, and its ships have been depicted in art ranging from the simple drawings on the walls of caves outside Les Eyzies, France, to the early Christian ichthys to the Dutch Hendrik Vroom to Hokusai's ukiyo-e to seascapes by Winslow Homer. During the Golden Age of the Netherlands, artists such as Jan Porcellis, Hendrick Dubbels, Willem van de Velde the Elder and his son, and Ludolf Bakhuizen celebrated the sea and the Dutch navy at the peak of its military prowess.[291][292]

The sea appears in human culture in contradictory ways, as both powerful but serene and as beautiful but dangerous.[6](p10) It has its place in mythology and religion, literature, art, poetry, film, theater, and music.[285] The Ancients personified it, believing it to be under the control of a being who needed to be appeased. It has been populated by fantastic creatures: the Leviathan of the Bible,[286] Scylla in Greek mythology,[287] Isonade in Japanese mythology,[288] and the kraken of late Norse mythology.[289][290](pp206–208) The sea is especially common in Christian imagery, where several of Jesus's disciples were said to have been fishermen on the Sea of Galilee.

WA 124772: An Assyrian warship carved into stone (700–692 BC) from the reign of Sennacherib. Ninevah, South-West Palace, Room VII, Panel 11. British Museum.
An Assyrian relief from c. 700 BC showing fish and a crab swimming around a bireme.

In culture

The indigenous peoples of the Arctic such as the Chukchi, Inuit, Inuvialuit, and Yupik hunt marine mammals including seals and whales[283] and the Torres Strait Islanders claim ownership of the Great Barrier Reef. They live a traditional life on the islands involving hunting, fishing, gardening, and trading with neighboring peoples in Papua New Guinea and Australia.[284]

Several nomadic indigenous groups in Maritime Southeast Asia live in boats and derive nearly all they need from the sea. The Moken people live on the coasts of Thailand and Burma and islands in the Andaman Sea.[279] The Bajau people are originally from the Sulu Archipelago, Mindanao, and northern Borneo.[280] Some Sea Gypsies are accomplished free-divers, able to descend to depths of 30 m (98 ft), though many are adopting a more settled, land-based way of life.[281][282]

Indigenous sea peoples

Most oil pollution in the sea comes from cities and industry.[267] Oil is dangerous for marine animals. It can clog the feathers of sea birds, reducing their insulating effect and the birds' buoyancy, or be ingested when they preen themselves in an attempt to remove the contaminant. Marine mammals are less seriously affected but may be chilled through the removal of their insulation, blinded, dehydrated, or poisoned. Benthic invertebrates are swamped when the oil sinks, fish are poisoned, and the food chain is disrupted. In the short term, oil spills result in wildlife populations being decreased and unbalanced, leisure activities being affected, and the livelihoods of people dependent on the sea being devastated.[277] The marine environment has self-cleansing properties and naturally-occurring bacteria will act over time to remove oil from the sea. In the Gulf of Mexico, where oil-eating bacteria are already present, they take only a few days to consume spilt oil.[278]

Much floating plastic trash does not biodegrade, instead disintegrating over time and eventually breaking down to the molecular level. Rigid plastics may float for years.[273] In the center of the Pacific gyre, there is a permanent floating accumulation of mostly plastic waste[274] and there is a similar garbage patch in the Atlantic.[275] Foraging sea birds such as the albatross and petrel may mistake debris for food and accumulate indigestible plastic in their digestive systems. Turtles and whales have been found with plastic bags and fishing line in their stomachs. Microplastics may sink, threatening filter feeders on the seabed.[276]

The dumping of waste (including oil, noxious liquids, sewage, and garbage) at sea is governed by international law. The London Convention (1972) is a United Nations agreement to control ocean dumping which had been ratified by 89 countries by 8 June 2012.[271] MARPOL 73/78 is a convention to minimize pollution of the seas by ships. By May 2013, 152 maritime nations had ratified MARPOL.[272]

Run-off of fertilizers from agricultural land is a major source of pollution in some areas and the discharge of raw sewage has a similar effect. The extra nutrients provided by these sources can cause excessive plant growth. Nitrogen is often the limiting factor in marine systems and the addition of nitrogen sparks algal blooms and red tides, which then may lower the oxygen level of the water to the point where it kills marine animals. Such events have created dead zones in the Baltic Sea and the Gulf of Mexico.[267] Some algal blooms are caused by cyanobacteria that make shellfish that filter feed on them toxic, harming animals like sea otters.[268] Nuclear facilities too can pollute. The Irish Sea was contaminated by radioactive caesium-137 from the former Sellafield nuclear fuel processing plant[269] and nuclear accidents sometimes cause radioactive material to seep into the sea, as at the Fukushima in 2011.[270]

Many substances enter the sea as a result of human activities. Combustion products are transported in the air and deposited through precipitation. Agricultural, industrial, and sewage outflows contribute heavy metals, pesticides, PCBs, disinfectants, cleaning products, and other synthetic chemicals. These become concentrated in the surface film and in marine sediment, especially estuarine mud. The result of all this contamination is largely unknown because of the large number of substances involved and the lack of information on their biological effects.[265] The heavy metals of greatest concern are copper, lead, mercury, cadmium, and zinc which may be accumulated by marine invertebrates. They are then passed up the food chain.[266]


Large quantities of methane clathrate exist on the seabed and in ocean sediment at a temperature of around 2 °C (36 °F) and these are of interest as a potential energy source. Some estimates put the amount available at between one and 5 million cubic kilometers (0.24 to 1.2 million cubic miles).[262] Also on the seabed are manganese nodules formed of layers of iron, manganese, and other hydroxides around a core. In the Pacific these may cover up to 30 percent of the deep ocean floor. The minerals precipitate from seawater and grow very slowly. Their commercial extraction for nickel was investigated in the 1970s but abandoned in favour of more convenient sources.[263] In suitable locations, diamonds are gathered from the seafloor using suction hoses to bring gravel ashore. In deeper waters, mobile seafloor crawlers are used and the deposits are pumped to a vessel above. In Namibia, more diamonds are now collected from marine sources than by conventional methods on land.[264]

Desalination is the technique of removing salts from seawater to leave fresh water suitable for drinking or irrigation. The two main processing methods, vacuum distillation and reverse osmosis, use large quantities of energy. Desalination is normally only undertaken where fresh water from other sources is in short supply or energy is plentiful, as in the excess heat generated by power stations. The brine produced as a by-product contains some toxic materials and is returned to the sea.[261]

The sea holds enormous quantities of valuable dissolved minerals.[256] The most important, Salt for table and industrial use has been harvested by solar evaporation from shallow ponds since prehistoric times. Bromine, accumulated after being leached from the land, is economically recovered from the Dead Sea, where it occurs at 55,000 parts per million (ppm).[257] Other minerals on or within the seabed can be exploited by dredging. This has advantages over land-based mining in that equipment can be built at specialized shipyards and infrastructure costs are lower. Disadvantages include problems caused by waves and tides, the tendency for excavations to silt up, and the washing away of spoil heaps. There is a risk of coastal erosion and environmental damage.[258] Sulphide deposits are potential sources of silver, gold, copper, lead, zinc, and trace metals which were only discovered in the 1960s. They form when geothermally superheated water is emitted from deep sea hydrothermal vents known as "black smokers": in contact with the cold waters of the deep ocean, the minerals precipitate and settle around the vent. The ores are of high quality but currently very costly to extract.[259] Small scale mining of the deep sea floor is being developed off the coast of Papua New Guinea using robotic techniques, but the obstacles are formidable.[260]

A hydrothermal vent in the Atlantic Ocean
A black smoker releasing dissolved sulfides and other minerals amid its superheated jets of water.

There are large deposits of petroleum (as oil and natural gas) in rocks beneath the seabed. Offshore platforms and drilling rigs extract the oil or gas and store it for transport to land. Offshore oil and gas production can be difficult due to the remote, harsh environment.[253] Drilling for oil in the sea has environmental impacts. Animals may be disorientated by seismic waves used to locate deposits, probably causing the beaching of whales.[254] Toxic substances such as mercury, lead, and arsenic may be released. The infrastructure may cause damage and oil may be spilt.[255]

Extractive industries

Electricity power stations are often located on the coast or beside an estuary so that the sea can be used as a heat sink. A colder heat sink enables more efficient power generation, which is important for expensive nuclear power plants in particular.[252]

Offshore wind power is captured by wind turbines placed out at sea; it has the advantage that wind speeds are higher than on land, though wind farms are more costly to construct offshore.[249] The first offshore wind farm was installed in Denmark in 1991,[250] and the installed capacity of European offshore wind farms reached 3 GW in 2010.[251]

The large and highly variable energy of waves gives them enormous destructive capability, making affordable and reliable wave machines problematic to develop. A small 2 MW commercial wave power plant, "Osprey", was built in Northern Scotland in 1995 about 300 meters (1000 ft) offshore. It was soon damaged by waves, then destroyed by a storm.[6](p112) Marine current power could provide populated areas close to the sea with a significant part of their energy needs.[247] In principle, it could be harnessed by open-flow turbines; sea bed systems are available, but limited to a depth of about 40 m (130 ft).[248]

Tidal power uses generators to produce electricity from tidal flows, sometimes by using a dam to store and then release seawater. The Rance barrage, 1 kilometer (0.62 mi) long, near St Malo in Brittany opened in 1967; it generates about 0.5 GW, but it has been followed by few similar schemes.[6](pp111–112)

The sea offers a very large supply of energy carried by ocean waves, tides, salinity differences, and ocean temperature differences which can be harnessed to generate electricity.[245] Forms of 'green' marine energy include tidal power, marine current power, osmotic power, ocean thermal energy and wave power.[245][246]

The Rance Tidal Power Station in France
The first tidal power station in the world: the kilometer-long Rance Tidal Power Station, which produces around 540 GWh per year, around 3% of Brittany's total electrical consumption (2011).[244]

Power generation

Beneath the surface, freediving is necessarily restricted to shallow descents. Pearl divers have traditionally greased their skins, put cotton in their ears and clips on their noses, and dived to 40 ft (12 m) with baskets in order to collect pearl oysters.[242] Human eyes are not adapted for use underwater, but vision can be improved by wearing a diving mask. Other useful equipment includes fins and snorkels. Scuba equipment allows underwater breathing, permitting hours of time beneath the surface.[243] The depths that can be reached by divers and the length of time they can stay underwater is limited by the increase of pressure they experience as they descend and the need to prevent decompression sickness as they return to the surface. Recreational divers are advised to restrict themselves to depths of under 100 feet (30 m) beyond which the danger of nitrogen narcosis increases. Deeper dives can be made with specialized equipment and training.[243]

Many humans enjoy venturing into the sea: children paddle and splash in the shallows, while others swim or relax on the beach. This was not always the case, with sea bathing becoming the vogue in Europe in the 18th century after Dr. William Buchan advocated the practice for health reasons.[238] Surfing is a sport in which a wave is ridden by a surfer, with or without a surfboard. Other water sports include kite surfing, where a power kite propels a manned board across the water;[239] windsurfing, where the power is provided by a fixed, maneuverable sail;[240] and water skiing, where a powerboat is used to pull a skier.[241]

Scuba diver
Scuba diver with face mask, fins, and underwater breathing apparatus

Use of the sea for leisure developed in the nineteenth century and became a significant industry in the twentieth century.[233] Maritime leisure activities are varied and include self-organized trips cruise ships;[236] and trips on smaller vessels for ecotourism such as whale watching and coastal birdwatching.[237]


The sea still remains a venue for recreational boating and large cruise ships. It is also a route for refugees and economic migrants, some traveling in small unseaworthy craft and others smuggled into shipping vessels. Some flee persecution while many are economic migrants attempting to reach countries where they believe their prospects are brighter.[232]

Although the use of small private vessels for personal transport undoubtably extends back into prehistory, large ships capable of braving the open ocean were typically dedicated to trade or fishing for most of human history. Even military campaigns would often simply hire or commandeer these private fleets to serve as troop transports, as did the traders, pilgrims, and wealthy tourists of antiquity and the Middle Ages. The voyages of exploration and colonization were often provided for by the crown out of naval funds; where they were not, they were usually chartered or else purchased and then used for shipping supplies after the initial settlement. Dedicated and scheduled local passenger services came to be offered in the 16th and 17th centuries, but the 1817 Black Ball was the first trans-Atlantic passenger line. In the Age of Sail, the duration of such passages depended much on the prevailing winds and the weather. The 18th-century coastal Margate hoys began the popularization of leisure travel in Britain[228] that later gathered steam with Thomas Cook's package tours in the next century.[229] During the 19th century, steam-powered ocean liners connected the railroad networks of the world. By 1900, the Atlantic crossing took about five days and the passenger lines competed to win the Blue Riband, an unofficial accolade accorded to the fastest liner in regular service. For twenty years from 1909, the prize went to the RMS Mauretania for its average speed of 26.06 knots (48.26 km/h).[230] This era waned as cheaper and faster intercontinental flights became available, most importantly the 1958 New YorkParis route.[231]


With steam, mass-produced steel plate, and exploding shells, European gunships permitted the New Imperialism of the 19th century, forcing open access to Africa, China, Korea, and Japan for their merchants on favorable terms. Although internal politics hampered Chinese modernization, American naval power produced a major reform in Japan which bore fruit during the 1905 Battle of Tsushima when the Japanese were able to decisively defeat Russia.[219] The great navies initially focused their efforts on constructing great dreadnoughts and battleships, but these fought inconclusively in the First World War.[220] By contrast, the much cheaper German U-boats showed that submarines could cripple shipping even in waters nominally controlled by the enemy.[221] Convoys, intelligence, and airborne ASW won a hard-fought victory in the Second World War's Battle of the Atlantic,[222] but developments in applied physics meant that by the 1960s nuclear-powered ballistic missile submarines were being maintained on constant patrol as a second-strike force[223][224] along with a second set of hunters intended to counter them. Meanwhile, the battles of the Mediterranean[225] and Pacific[226][227] theaters of the war had shown that air power was capable of overcoming the strongest warships. Initial planning to permanently reduce naval size, however, was undone by the Korean War, which showed a continuing need to transport men and materiel overseas, as well as the means to protect them. At present, only the United States, Great Britain, and France are considered to possess true blue-water navies capable of projecting force into an enemy's littoral, Russia having lost the ability during the collapse of the Soviet Union and China rising rapidly.

In the ancient world, in addition to Salamis, major naval engagements included the Battle of Actium, which permitted the establishment of Augustus's empire. In the modern era, important naval battles include the English victories against the Armada in 1588 and at Trafalgar in 1805,[217] which broke the threats of invasion by the superior land forces of the Spanish and French empires. (Some of the most important battles of Chinese history—including the battles of Red Cliffs, Caishi, and Lake Poyang which respectively determined the fate of the Three Kingdoms and the Song and Ming empires—were also naval but all were riverine rather than maritime.)

A photograph by an airplane of the Imperial Japanese Navy, facing east over Battleship Row. 7 November 1941.
Modern naval warfare: a torpedo strikes the USS West Virginia during the Japanese attack on Pearl Harbor.

Elizabeth I and the Spanish Armada. Anonymous. Oil on canvas, 121.3 × 284.5 cm (47¾ × 112 in). Early 17th century.
Naval warfare in the Age of Sail: a painting by contemporaries of the 1588 Battle of Gravelines, which along with the subsequent Protestant Wind dispersed the Spanish Armada.

Elizabeth I and the Spanish Armada. Anonymous. Oil on canvas, 121.3 × 284.5 cm (47¾ × 112 in). Early 17th century.

Piracy—both illicit in ancient Cilicia and China and state-supported among the Cretans, Vikings, Japanese, English, and Berbers—has remained a problem into the present day, given the expense involved in securely protecting every merchant vessel or in policing extensive coastlines. At times, China reacted against its domestic and Japanese pirates by imposing the haijin, blanket prohibitions on foreign trade and coastal settlement; other states—including Rome, Britain, and the United States—have at times taken it upon themselves to secure internal and international trade lanes against pirates, permitting inspections of foreign vessels and punitive actions (or invasions) against pirate states. Similar interventions were undertaken following the abolition of the slave trade.

Since the development of coordinated fleets of ships capable of landing an invasion force, naval warfare has been an important aspect in the defense (or conquest) of maritime states. The first naval battle in recorded history saw Suppiluliuma II of the Hittites burn a Cypriot fleet at sea in 1210 BC.[213] Shortly after, the fleets of the Sea Peoples disrupted the entire Eastern Mediterranean: over a period of about 50 years, raids and invasions violently destroyed nearly every coastal city between Pylos and Gaza.[214] As empires grew and their armies became too large to live off the lands through which they passed, disruption of their supply fleets also became a powerful tactic. The 480 BC Battle of Salamis largely determined the course of the Persian Wars[215] not because of its inherent damage (however considerable) but because Themistocles's deception and superior strategy left the Athenians capable of disrupting sea-borne supplies at will and potentially striking at the pontoon bridges across the Hellespont, cutting off the Persians' line of retreat.[216] During the age of wooden ships, however, great fleets were burdensome to maintain and always liable to destruction by contrary weather, most famously in the case of the two kamikaze typhoons that destroyed the Mongol invasions of Japan in AD 1274 and 1281. The unpleasantness of naval service long connected it with slavery, penal servitude, and impressment openly encouraged by various states and Shanghaiing carried out by unscrupulous merchants.

A Byzantine galley using Greek fire against rebel ships in the 9th century.


Ships may cross numerous time zones on a voyage, so nautical time, introduced in the 1920s, is used in international waters. Each such zone is uniformly 15 degrees of longitude wide, the ship's clock going forward one hour per zone when travelling eastwards.[212]

The present Convention on the Law of the Sea (UNCLOS) was drafted in 1982 and came into force in 1994.[78] It states that "the high seas are open to all states, whether coastal or land-locked" and provides a non-exhaustive list of freedoms including navigation, overflight, the laying of submarine cables, the building of artificial islands, fishing, and scientific research.[211] It extended territorial waters up to 12 nautical miles (22.2 km or 13.8 mi) from a baseline (sea) generally (but not always) equivalent to the low-water line; this area is subject to national laws but free to both innocent and transit passage. (The "internal waters" landward of the baseline are solely under national control.) A "contiguous zone" of a further 12 nmi are permitted for hot pursuit of vessels charged with violating customs, taxation, immigration, or pollution laws in the territorial waters. An "exclusive economic zone" or EEZ places all exploitation of marine life and minerals within 200 nmi (370 km or 230 mi) of the baseline under national supervision. For legal purposes, the "continental shelf" is considered to be the actual continental shelf (to a depth of 200 m or 660 ft) contiguous to the baseline or 200 nmi, whichever is greater; the marine life and minerals "attached to" (or below) the seabed within this area also fall under national supervision.[209]

The Law of the Sea is the particular body international law applied to maritime questions and offenses. Empires such as Rome and China long claimed universal jurisdiction; during the Middle Ages, Italian maritime republics such as Venice and Genoa recognized the existence of rival states but claimed the right to close the seas to their traffic. Portuguese and Spanish pursuit of similar rights over new seas and lands during the Age of Discovery and papal support of their claims was a factor in the Wars of Religion; in 1609, a jurist hired to defend a lucrative act of piracy by the Dutch East India Company penned Mare Liberum,[207] an argument in favor of freedom of the seas that ultimately produced the compromise[208] that territory extended as far as land-based cannonshot could reach, standardized to 3 nautical miles (5,556 m or 18,228 ft), and that everything beyond was international waters.[209] President Woodrow Wilson argued this principle as part of America's entrance into World War I and as one of his Fourteen Points afterwards; nonetheless, President Truman's unilateral claim of jurisdiction over the oil reserves of America's continental shelf in 1945[210] directly led to the end of the regime.[209] The three rounds of the United Nations' conferences on the Law of the Sea eventually reshaped international maritime law but the United States has not ratified the present treaty but instead adopted its policies piecemeal via presidential proclamations.

Admiralty law is the particular body of national laws applied to maritime questions and offenses, as the uncertainty of sea voyages has caused the sea to be viewed as a unique jurisdiction since antiquity. Rhodian, Roman, Byzantine, Trani, and Amalfian laws were important influences on the French, Genovese, and Hanseatic codes which established the first English courts of admiralty. Unlike the usual English common law system, the courts of admiralty hewed closer to Continental practice, leaving it open for abuse that contributed to the American Revolution.[206] The adoption of the present constitution reintroduced admiralty law to the United States, but with a relatively larger sphere for trials by jury.


As well as the wild stock, about 79 million metric tons (87 million tons) of food and non-food products were produced by sea farming in 2010, an all time high. About six hundred species of plants and animals were cultured, some for use in seeding wild populations. The animals raised included finfish, aquatic reptiles, crustaceans, molluscs, sea cucumbers, sea urchins, sea squirts, and jellyfish.[196] Integrated mariculture has the advantage that there is a readily-available supply of planktonic food and waste is removed naturally;[197] in cases where the waste would otherwise be harmful, multi-species techniques can used to, e.g., feed farmed shellfish from the waste being produced by farmed salmon. Various methods are employed. Mesh enclosures for finfish can be suspended in the open seas, cages can be used in more sheltered waters, or ponds can be refreshed with water at each high tide. Shrimps can be reared in shallow ponds connected to the open sea.[198] Ropes can be hung in water to grow algae, oysters, and mussels. Oysters can be reared on trays or in mesh tubes. Sea cucumbers can be ranched on the seabed.[199] Captive breeding programmes have raised lobster larvae for release of juveniles into the wild resulting in an increased lobster harvest in Maine.[200] At least 145 species of seaweed—red, green, and brown algae—are eaten worldwide, some long farmed in Japan and other Asian countries; there is great potential for additional algaculture.[201] Few maritime flowering plants are widely used for food but one example is marsh samphire, which is eaten both raw and cooked.[202] A major difficulty for aquaculture is the tendency towards monoculture and the associated risk of widespread disease. In the 1990s, disease wiped out China's farmed Farrer's scallop and white shrimp and required their replacement by other species.[203] Shrimp farming has also caused the destruction of important mangrove forests throughout southeast Asia.[204]

Salmon pens off Vestmanna in the Faroes.

Fishing vessels are increasingly venturing further afield to exploit stocks in international waters. However, industrial fishing has depleted native stocks and developing regions such as Africa see falling harvests, forcing them to import increasing amounts of seafood from developed nations. [195] In the 20th century, the

Meanwhile, the determination of longitude continued to involve approximations and guesswork: its true calculation required an accurate clock which permitted comparison between noon aboard ship and the exact time at a fixed point such as Royal Observatory in Greenwich. Britain's Longitude prize was effectively awarded in 1773 to the self-educated John Harrison for his 1761 sea watch. James Cook used a copy on his second and third voyages, which studied the Pacific[147] and inspired studies from Russia, France, the Netherlands, and the United States.[6](p15) The completion of a submarine telegraphic cable across the English Channel in 1850 and subsequent links of the All Red Line led to greater interest in the deep sea. Earlier ideas that no life could exist below 300 fathoms (550 meters or 1,800 feet) were disproved in 1860 when a Mediterranean line failed and was pulled up from depths four times lower, completely encrusted with marine life.[148] Michael Sars's discovery of "living fossils" deep in Norway's fjords helped spur British efforts including HMS Challenger’s expedition during the 1870s[149] that effectively created modern oceanography.[6](p15) From 1878 to 1880, the SS Vega successfully completed the Northeast Passage and went on to circumnavigate Eurasia for the first time. During the mid-1890s, Fridtjof Nansen used a specially-designed ship to drift through the northern pack ice, establishing that the Arctic was an open sea. In 1898 & 1899, Carl Chun raised and studied many new life forms from over 4,000 m (13,000 ft) below the surface of the South Atlantic.

In the 15th century, West European mariners—beginning with Portugal—started making still longer voyages of exploration, using improvements on translated Islamic star charts and a variation on African fishing boats called the caravel. In 1473, Lopes Gonçalves crossed the equator and disproved the Aristotlean notion that a ring of fire would bar exploration of the southern hemisphere. Bartolomeu Dias rounded the Cape of Good Hope in 1487; in 1498, Vasco da Gama reached Malindi, where a local pilot showed him how to follow the monsoon to India. In 1492, relying on incorrect estimates of the circumference of the Earth, the Genovese Christopher Columbus sailed from Cadiz to the Canaries and thence into the open Atlantic in a Spanish attempt to reach the Orient. Instead, he made landfall on an island in the Caribbean Sea. The resulting Columbian Exchange introduced potatoes, corn, and chili peppers to the Old World while smallpox epidemics devastated the indigenous peoples of the Americas. This disruption and depopulation permitted rapid Spanish conquests and led to the widespread adoption of African slavery to man lucrative tobacco, sugar, indigo, and cotton plantations. In 1519, Juan Sebastián Elcano completed Magellan's Spanish expedition to sail around the world.[6](pp12–13) These and other voyages permitted European maps to attain a previously impossible degree of accuracy. In 1538, Gerardus Mercator devised a map projection conveniently making constant bearings (rhumb lines) straight.[6](pp12–13) In the Arctic, in 1594, the Dutch captain Willem Barentsz reached Svalbard and the Barents Sea while, in the south, Anthony de la Roché crossed the Antarctic Convergence in 1675 and three separate expeditions—one British, one American, and one Russian—all claimed to have discovered Antarctica in 1820.[142][143][144] Not all voyages of discovery originated in Western Europe. Although accurate charting of the coasts of Russia only began in the 18th century and the archipelago of Severnaya Zemlya was not discovered until 1910,[145] Novgorodians had been sailing the White Sea since at least the 13th century.[146] Despite a long-standing preference for autarky, China briefly opened up under the Song and Mongol Yuan dynasties. In the early 15th century, Zheng He's fleet of treasure ships repeatedly sailed from Ming China with 37,000 men aboard 317 ships, reaching as far as the African coast.[6](pp12–13) Chinese exploration, however, was soon curtailed again and finally outlawed. The peoples of East Asia were introduced to the true shape of the other continents from the maps of Matteo Ricci.

Mercator's map of the world
Gerardus Mercator's world map of 1569. The coastline of the Old World is quite accurately depicted, despite the great distortions of this projection in the polar regions and the uncertain information about the Americas.

In the Mediaeval era, the Vikings used clinker-built ships to colonize Iceland, Greenland, Canada, and Russia.[6](pp12–13) A compass showing magnetic north is first attested—in the form of a "south-pointing spoon"—in the 1st-century Chinese Lunheng. The first evidence of its use in Chinese maritime navigation, however, dates to Zhu Yu's c. 1115 Pingzhou Table Talks. Alexander of Neckham's De naturis rerum, the first European mention of a magnetized needle, dates to 1190 and immediately notes its use among sailors. Latitude (the ship's position ranging from 0° at the equator to 90° north and south) could be determined by inclinometers—including the astrolabe, sextant, and Jacob's staff—measuring the angle between the horizon and heavenly bodies like the sun or moon. Accurately determining longitude (the ship's position east or west of some fixed point) proved much harder.[141]

The hunter-gatherer Ortoiroid people began spreading through the Caribbean from Venezuela's Orinoco valley by at least the 6th millennium BC. Around the same time, Mesopotamians were using bitumen to caulk their reed boats and, a little later, masted sails.[125] Lothal in India boasted the earliest known dock around 2400 BC.[126] By c. 2000 BC, Austronesians on Taiwan had begun spreading into maritime Southeast Asia.[127][128][129] From 1300 to 900 BC, the Austronesian "Lapita" peoples displayed great feats of navigation, reaching out from the Bismarck Archipelago to as far away as Fiji, Tonga, and Samoa.[130] Their descendants continued to travel thousands of miles between tiny islands on outrigger canoes:[131] the Austronesians of the Sunda Islands settled Madagascar off southeast Africa before AD 500 and the Polynesians settled the Hawaiis before 800,[132] Easter Island before 1200,[133] and New Zealand shortly after.[134] The Egyptian pharaoh Necho II initiated construction on a canal which eventually linked the Mediterranean and Red Seas around 600 BC. Herodotus records Egyptian claims that he also commissioned a 3-year-long expedition which circumnavigated Africa from the Red Sea to the Nile delta.[135][8] Around 500 BC, the Carthaginian navigator Hanno left a detailed periplus of an Atlantic journey that reached at least Senegal and possibly Mount Cameroon;[137][138] and the Greek Pytheas left another exploring the seas around Great Britain around 325 BC. The massive 3rd-century BC Lighthouse of Alexandria was considered one of the Seven Wonders of the World.[139] In the 2nd century, the Alexandrian Ptolemy mapped the known world, using the "Fortunate Isles" as his prime meridian and including details as distant as the Gulf of Thailand. A modified form was used by Columbus for his voyages.[140]

Humans have travelled the sea since prehistoric times, originally on rafts and in dugout, reed, and bark canoes. Most of the early human migrations occurred over land: even areas now separated by open sea such as the Americas, Japan, and Britain were accessible by land bridges or fast ice during the last ice age. However, the dwarf Flores man probably needed to cross a 19-kilometer (12 mi) wide strait from Sundaland to reach Komodo[121] and, although the exact details remain uncertain, the ancestors of Australia's Aborigines must have crossed the broader deep-sea Wallace Line to Near Oceania tens of thousands of years ago.[7] Despite earlier theories, modern bathymetric soundings now suggest that even the earliest settlement of the Philippines required crossing deep water at the Mindoro Strait or the Sibutu Passage.

Navigation and exploration

A 19th-century illustration of Columbus's 'discovery' of the Americas on 12 October 1492, displaying how even historical explorers could be mythologized both at home and abroad.

Humans and the sea

[120] The demersal zone supports many animals that feed on benthic organisms or seek protection from predators. The seabed provides a range of habitats on or under the surface of the

The pelagic zone contains fouling community on the hulls of vessels.[118]

There is a broader spectrum of higher animal taxa in the sea than on land, many marine species have yet to be discovered, and the number known to science is expanding annually.[113] Some vertebrates such as seabirds, seals, and sea turtles return to the land to breed but fish, cetaceans, and sea snakes have a completely aquatic lifestyle and many invertebrate phyla are entirely marine. In fact, the oceans teem with life and provide many varying microhabitats.[113] One of these is the surface film which—despite being tossed about by the movement of waves—provides a rich environment and is home to bacteria, fungi, microalgae, protozoa, fish eggs, and various larvae.[114]

Marine habitats such as coral reefs hold a diversity of species including starfish, corals and fish.

Animals and other life

Light is only able to penetrate the top 200 m (660 ft) so this is the only part of the sea where plants can grow.[35] The surface layers are often deficient in biologically-active nitrogen compounds. The marine nitrogen cycle consists of complex microbial transformations which include the fixation of nitrogen, its assimilation, nitrification, anammox, and denitrification.[112] Some of these processes take place in deep water so that where there is an upwelling of cold waters or near estuaries where land-sourced nutrients are present, plant growth is higher. This means that the most productive areas, rich in plankton and therefore also in fish, are mainly coastal.[6](pp160–163)

Marine photosynthetic algae, phytoplankton, contribute a larger proportion of the world's photosynthetic output than all the terrestrial forests combined. About 45 percent of the sea's primary production of living material is contributed by diatoms.[107] Much larger algae, commonly known as seaweeds, are important locally; Sargassum forms floating drifts, while kelp form seabed forests.[104](pp246–255) Flowering plants in the form of seagrasses grow in "meadows" in sandy shallows,[108] mangroves line the coast in tropical and subtropical regions,[109] and salt-tolerant plants thrive in regularly inundated salt marshes.[110] All of these habitats are able to sequester large quantities of carbon and support a biodiverse range of larger and smaller animal life.[111]

Algae and plants

Coral reefs, the so-called "rainforests of the sea", occupy less than 0.1 percent of the world's ocean surface, yet their ecosystems include 25 percent of all marine species.[105] The best-known are tropical coral reefs such as Australia's Great Barrier Reef, but cold water reefs harbor a wide array of species including corals (only six of which contribute to reef formation).[6](pp204–207)[106]

Marine habitats can be divided horizontally into coastal and open ocean habitats. Coastal habitats extend from the shoreline to the edge of the continental shelf. Most marine life is found in coastal habitats, even though the shelf area occupies only 7 percent of the total ocean area. Open ocean habitats are found in the deep ocean beyond the edge of the continental shelf. Alternatively, marine habitats can be divided vertically into pelagic (open water), demersal (just above the seabed), and benthic (sea bottom) habitats. A third division is by latitude: from tropical to temperate to polar waters.[6](pp150–151)


Life may have originated in the sea and all the major groups of animals are represented there. Scientists differ as to precisely where in the sea life arose: the Miller-Urey experiments suggested a dilute chemical "soup" in open water, but more recent suggestions include volcanic hot springs, fine-grained clay sediments, or deep-sea "black smoker" vents, all of which would have provided protection from damaging ultraviolet radiation which was not blocked by the early earth's atmosphere.[6](pp138–140)

The oceans are home to a diverse collection of life forms that use it as a habitat. Since sunlight illuminates only the upper layers, the major part of the ocean exists in permanent darkness. As the different depth and temperature zones each provide habitat for a unique set of species, the marine environment as a whole encompasses an immense diversity of life.[101] Marine habitats range from surface water to the deepest fish for use as food.[103][104](pp204–229)

A map of mean surface chlorophyll for the period 1998-2006. NASA SeaWiFS.
A map of mean surface chlorophyll a (1998–2006), from 0.03 (light violet) to 30 mg chl per (dark red) on a logarithmic scale.

Marine life

The current rate of ocean chemistry change appears to be without precedent in Earth's geological history, making it unclear how well marine ecosystems will be able to adapt to the shifting conditions of the near future.[99] Of particular concern is the manner in which the combination of acidification with the expected additional stressors of higher temperatures and lower oxygen levels will impact the seas.[100]

One important element for the formation of pteropods, and single-celled algae called coccolithophorids and foraminifera. All of these are important parts of the food chain and a diminution in their numbers will have significant consequences. In tropical regions, corals are likely to be severely affected as it becomes more difficult to build their calcium carbonate skeletons,[98] in turn adversely impacting other reef dwellers.[93]

Seawater is slightly alkaline and had a preindustrial pH of about 8.2. More recently, anthropogenic activities have steadily increased the carbon dioxide content of the atmosphere; about 30–40% of the added CO2 is absorbed by the oceans, forming carbonic acid and lowering the pH (now below 8.1[89]) through a process called ocean acidification.[90][91][92] The pH is expected to reach 7.7 (representing a 3-fold increase in hydrogen ion concentration) by the year 2100, which is a significant change in a century.[93][6]


It can also enter as dissolved organic carbon through rivers and is converted by photosynthetic organisms into organic carbon. This can either be exchanged throughout the food chain or precipitated into the deeper, more carbon-rich layers as dead soft tissue or in shells and bones as calcium carbonate. It circulates in this layer for long periods of time before either being deposited as sediment or being returned to surface waters through thermohaline circulation.[88]

Carbon enters the ocean as atmospheric carbon dioxide dissolves into the surface layers and is converted into carbonic acid, carbonate, and bicarbonate: CO2 (aq) + H2O \rightleftharpoons H2CO3 \rightleftharpoons HCO3 + H+ \rightleftharpoons CO32− + 2 H+. The process liberates hydrogen ions (H+
), decreasing ocean pH and increasing its acidity.

[86] exchanges carbon between these two layers.Thermohaline circulation [88] and it remains there for much longer periods of time.[87]