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The Atlantic Ocean
Ocean
is the second largest of the world's oceans with a total area of about 106,460,000 square kilometers (41,100,000 square miles).[2][3] It covers approximately 20 percent of the Earth's surface and about 29 percent of its water surface area. It separates the "Old World" from the "New World". The Atlantic Ocean
Ocean
occupies an elongated, S-shaped basin extending longitudinally between Eurasia
Eurasia
and Africa to the east, and the Americas to the west. As one component of the interconnected global ocean, it is connected in the north to the Arctic
Arctic
Ocean, to the Pacific Ocean
Ocean
in the southwest, the Indian Ocean
Ocean
in the southeast, and the Southern Ocean
Southern Ocean
in the south (other definitions describe the Atlantic as extending southward to Antarctica). The Equatorial Counter Current subdivides it into the North Atlantic Ocean
Ocean
and the South Atlantic Ocean
Ocean
at about 8°N.[5] Scientific explorations of the Atlantic include the Challenger expedition, the German Meteor expedition, Columbia University's Lamont-Doherty Earth Observatory
Lamont-Doherty Earth Observatory
and the United States Navy Hydrographic Office.[5]

Contents

1 Etymology 2 Extent and data 3 Bathymetry

3.1 Mid-Atlantic Ridge 3.2 Ocean
Ocean
floor

4 Water characteristics

4.1 Salinity 4.2 Water masses 4.3 Gyres 4.4 Sargasso Sea

5 Climate

5.1 Natural hazards

6 Plate tectonics

6.1 Central Atlantic 6.2 Northern Atlantic 6.3 South Atlantic 6.4 Closure of the Atlantic

7 History

7.1 Human origin 7.2 Old World 7.3 New World 7.4 Atlantic World

8 Economy

8.1 Fisheries

9 Environmental issues 10 See also 11 References

11.1 Notes 11.2 Sources

12 Further reading 13 External links

Etymology[edit]

The Aethiopian Ocean
Aethiopian Ocean
in a 1710 French map of Africa

The oldest known mentions of an "Atlantic" sea come from Stesichorus around mid-sixth century BC (Sch. A. R. 1. 211):[6] Atlantikoi pelágei (Greek: Ἀτλαντικῷ πελάγει; English: 'the Atlantic sea'; etym. 'Sea of Atlantis') and in The Histories of Herodotus
Herodotus
around 450 BC (Hdt. 1.202.4): Atlantis
Atlantis
thalassa (Greek: Ἀτλαντὶς θάλασσα; English: 'Sea of Atlantis' or 'the Atlantis
Atlantis
sea'[7]) where the name refers to "the sea beyond the pillars of Heracles" which is said to be part of the ocean that surrounds all land.[8] Thus, on one hand, the name refers to Atlas, the Titan in Greek mythology, who supported the heavens and who later appeared as a frontispiece in Medieval maps and also lent his name to modern atlases.[9] On the other hand, to early Greek sailors and in Ancient Greek mythological literature such as the Iliad
Iliad
and the Odyssey, this all-encompassing ocean was instead known as Oceanus, the gigantic river that encircled the world; in contrast to the enclosed seas well-known to the Greeks: the Mediterranean and the Black Sea.[10] In contrast, the term "Atlantic" originally referred specifically to the Atlas Mountains
Atlas Mountains
in Morocco and the sea off the Strait of Gibraltar
Strait of Gibraltar
and the North African coast.[9] The Greek word thalassa has been reused by scientists for the huge Panthalassa
Panthalassa
ocean that surrounded the supercontinent Pangaea
Pangaea
hundreds of million years ago. The term "Aethiopian Ocean", derived from Ancient Ethiopia, was applied to the Southern Atlantic as late as the mid-19th century.[11] During the Age of Discovery, the Atlantic was also known to English cartographers as the Great Western Ocean.[12] Extent and data[edit] For complete lists of marginal seas and borders of the Atlantic, see List of seas
List of seas
§ Atlantic Ocean, and Borders of the oceans § Atlantic Ocean. For the extent of the Southern Ocean, see Southern Ocean § Definitions and use.

Extent of the Atlantic Ocean
Ocean
according to the 2002 IHO definition, excluding Arctic
Arctic
and Antarctic
Antarctic
regions

The International Hydrographic Organization
International Hydrographic Organization
(IHO) defined the limits of the oceans and seas in 1953,[13] but some of these definitions have been revised since then and some are not used by various authorities, institutions, and countries, see for example the CIA World Factbook. Correspondingly, the extent and number of oceans and seas varies. The Atlantic Ocean
Ocean
is bounded on the west by North and South America. It connects to the Arctic
Arctic
Ocean
Ocean
through the Denmark Strait, Greenland Sea, Norwegian Sea
Norwegian Sea
and Barents Sea. To the east, the boundaries of the ocean proper are Europe: the Strait of Gibraltar
Strait of Gibraltar
(where it connects with the Mediterranean Sea–one of its marginal seas–and, in turn, the Black Sea, both of which also touch upon Asia) and Africa. In the southeast, the Atlantic merges into the Indian Ocean. The 20° East meridian, running south from Cape Agulhas
Cape Agulhas
to Antarctica
Antarctica
defines its border. In the 1953 definition it extends south to Antarctica, while in later maps it is bounded at the 60° parallel by the Southern Ocean.[13] The Atlantic has irregular coasts indented by numerous bays, gulfs, and seas. These include the Baltic Sea, Black Sea, Caribbean Sea, Davis Strait, Denmark Strait, part of the Drake Passage, Gulf of Mexico, Labrador Sea, Mediterranean Sea, North Sea, Norwegian Sea, almost all of the Scotia Sea, and other tributary water bodies.[1] Including these marginal seas the coast line of the Atlantic measures 111,866 km (69,510 mi) compared to 135,663 km (84,297 mi) for the Pacific.[1][14] Including its marginal seas, the Atlantic covers an area of 106,460,000 km2 (41,100,000 sq mi) or 23.5% of the global ocean and has a volume of 310,410,900 km3 (74,471,500 cu mi) or 23.3% of the total volume of the earth's oceans. Excluding its marginal seas, the Atlantic covers 81,760,000 km2 (31,570,000 sq mi) and has a volume of 305,811,900 km3 (73,368,200 cu mi). The North Atlantic covers 41,490,000 km2 (16,020,000 sq mi) (11.5%) and the South Atlantic 40,270,000 km2 (15,550,000 sq mi) (11.1%).[4] The average depth is 3,646 m (11,962 ft) and the maximum depth, the Milwaukee Deep
Milwaukee Deep
in the Puerto Rico Trench, is 8,486 m (27,841 ft).[4][15] Bathymetry[edit]

False color
False color
map of ocean depth in the Atlantic basin

The bathymetry of the Atlantic is dominated by a submarine mountain range called the Mid-Atlantic Ridge
Mid-Atlantic Ridge
(MAR). It runs from 87°N or 300 km (190 mi) south of the North Pole
North Pole
to the subantarctic Bouvet Island
Bouvet Island
at 42°S.[16] Mid-Atlantic Ridge[edit] Main article: Mid-Atlantic Ridge The MAR divides the Atlantic longitudinally into two halves, in each of which a series of basins are delimited by secondary, transverse ridges. The MAR reaches above 2,000 m (6,600 ft) along most of its length, but is interrupted by larger transform faults at two places: the Romanche Trench
Romanche Trench
near the Equator and the Gibbs Fracture Zone at 53°N. The MAR is a barrier for bottom water, but at these two transform faults deep water currents can pass from one side to the other.[17] The MAR rises 2–3 km (1.2–1.9 mi) above the surrounding ocean floor and its rift valley is the divergent boundary between the North American and Eurasian plates in the North Atlantic and the South American and African plates in the South Atlantic. The MAR produces basaltic volcanoes in Eyjafjallajökull, Iceland, and pillow lava on the ocean floor.[18] The depth of water at the apex of the ridge is less than 2,700 m (1,500 fathoms; 8,900 ft) in most places, while the bottom of the ridge is three times as deep.[19] The MAR is intersected by two perpendicular ridges: the Azores–Gibraltar Transform Fault, the boundary between the Nubian and Eurasian plates, intersects the MAR at the Azores Triple Junction, on either side of the Azores microplate, near the 40°N.[20] A much vaguer, nameless boundary, between the North American and South American plates, intersects the MAR near or just north of the Fifteen-Twenty Fracture Zone, approximately at 16°N.[21] In the 1870s, the Challenger expedition
Challenger expedition
discovered parts of what is now known as the Mid-Atlantic Ridge, or:

An elevated ridge rising to an average height of about 1,900 fathoms [3,500 m; 11,400 ft] below the surface traverses the basins of the North and South Atlantic in a meridianal direction from Cape Farewell, probably its far south at least as Gough Island, following roughly the outlines of the coasts of the Old and the New Worlds.[22]

The remainder of the ridge was discovered in the 1920s by the German Meteor expedition using echo-sounding equipment.[23] The exploration of the MAR in the 1950s led to the general acceptance of seafloor spreading and plate tectonics.[16] Most of the MAR runs under water but where it reaches the surfaces it has produced volcanic islands. While nine of these have collectively been nominated a World Heritage Site
World Heritage Site
for their geological value, four of them are considered of "Outstanding Universal Value" based on their cultural and natural criteria: Þingvellir, Iceland; Landscape of the Pico Island Vineyard Culture, Portugal; Gough and Inaccessible Islands, United Kingdom; and Brazilian Atlantic Islands: Fernando de Noronha and Atol das Rocas Reserves, Brazil.[16] Ocean
Ocean
floor[edit] For a list of fracture zones in the Atlantic, see List of fracture zones § Atlantic Ocean. Continental shelves in the Atlantic are wide off Newfoundland, southern-most South America, and north-eastern Europe. In the western Atlantic carbonate platforms dominate large areas, for example the Blake Plateau
Blake Plateau
and Bermuda
Bermuda
Rise. The Atlantic is surrounded by passive margins except at a few locations where active margins form deep trenches: the Puerto Rico Trench
Puerto Rico Trench
(8,414 m or 27,605 ft maximum depth) in the western Pacific and South Sandwich Trench (8,264 m or 27,113 ft) in the South Atlantic. There are numerous submarine canyons off north-eastern North America, western Europe, and north-western Africa. Some of these canyons extend along the continental rises and farther into the abyssal plains as deep-sea channels.[17] In 1922 a historic moment in cartography and oceanography occurred. The USS Stewart used a Navy Sonic Depth Finder to draw a continuous map across the bed of the Atlantic. This involved little guesswork because the idea of sonar is straight forward with pulses being sent from the vessel, which bounce off the ocean floor, then return to the vessel.[24] The deep ocean floor is thought to be fairly flat with occasional deeps, abyssal plains, trenches, seamounts, basins, plateaus, canyons, and some guyots. Various shelves along the margins of the continents constitute about 11% of the bottom topography with few deep channels cut across the continental rise. The mean depth between 60°N and 60°S is 3,730 m (12,240 ft), or close to the average for the global ocean, with a modal depth between 4,000 and 5,000 m (13,000 and 16,000 ft).[17] In the South Atlantic the Walvis Ridge
Walvis Ridge
and Rio Grande Rise
Rio Grande Rise
form barriers to ocean currents. The Laurentian Abyss is found off the eastern coast of Canada. Water characteristics[edit]

As the Gulf Stream
Gulf Stream
meanders across the North Atlantic from the North American east coast to Western Europe its temperature drops by 20 °C (36 °F).

Path of the thermohaline circulation. Purple paths represent deep-water currents, while blue paths represent surface currents.

Surface water temperatures, which vary with latitude, current systems, and season and reflect the latitudinal distribution of solar energy, range from below −2 °C (28 °F) to over 30 °C (86 °F). Maximum temperatures occur north of the equator, and minimum values are found in the polar regions. In the middle latitudes, the area of maximum temperature variations, values may vary by 7–8 °C (13–14 °F).[5] From October to June the surface is usually covered with sea ice in the Labrador Sea, Denmark Strait, and Baltic Sea.[5] The Coriolis effect
Coriolis effect
circulates North Atlantic water in a clockwise direction, whereas South Atlantic water circulates counter-clockwise. The south tides in the Atlantic Ocean
Ocean
are semi-diurnal; that is, two high tides occur during each 24 lunar hours. In latitudes above 40° North some east-west oscillation, known as the North Atlantic oscillation, occurs.[5] Salinity[edit] On average, the Atlantic is the saltiest major ocean; surface water salinity in the open ocean ranges from 33 to 37 parts per thousand (3.3 – 3.7%) by mass and varies with latitude and season. Evaporation, precipitation, river inflow and sea ice melting influence surface salinity values. Although the lowest salinity values are just north of the equator (because of heavy tropical rainfall), in general the lowest values are in the high latitudes and along coasts where large rivers enter. Maximum salinity values occur at about 25° north and south, in subtropical regions with low rainfall and high evaporation.[5] The high surface salinity in the Atlantic, on which the Atlantic thermohaline circulation is dependent, is maintained by two processes: the Agulhas Leakage/Rings, which brings salty Indian Ocean
Ocean
waters into the South Atlantic, and the "Atmospheric Bridge", which evaporates subtropical Atlantic waters and exports it to the Pacific.[25]

Water masses[edit]

Temperature-salinity characteristics for Atlantic water masses[26]

Water mass Temperature Salinity

Upper waters (0–500 m or 0–1,600 ft)

Atlantic Subarctic Upper Water (ASUW) 0.0–4.0 °C 34.0–35.0

Western North Atlantic Central Water (WNACW) 7.0–20 °C 35.0–36.7

Eastern North Atlantic Central Water (ENACW) 8.0–18.0 °C 35.2–36.7

South Atlantic Central Water (SACW) 5.0–18.0 °C 34.3–35.8

Intermediate waters (500–1,500 m or 1,600–4,900 ft)

Western Atlantic Subarctic Intermediate Water (WASIW) 3.0–9.0 °C 34.0–35.1

Eastern Atlantic Subarctic Intermediate Water (EASIW) 3.0–9.0 °C 34.4–35.3

Mediterranean Water (MW) 2.6–11.0 °C 35.0–36.2

Arctic
Arctic
Intermediate Water (AIW) −1.5–3.0 °C 34.7–34.9

Deep and abyssal waters (1,500 m–bottom or 4,900 ft–bottom)

North Atlantic Deep Water (NADW) 1.5–4.0 °C 34.8–35.0

Antarctic
Antarctic
Bottom Water (AABW) −0.9–1.7 °C 34.64–34.72

Arctic
Arctic
Bottom Water (ABW) −1.8 to −0.5 °C 34.85–34.94

The Atlantic Ocean
Ocean
consists of four major, upper water masses with distinct temperature and salinity. The Atlantic Subarctic Upper Water in the northern-most North Atlantic is the source for Subarctic Intermediate Water and North Atlantic Intermediate Water. North Atlantic Central Water can be divided into the Eastern and Western North Atlantic central Water since the western part is strongly affected by the Gulf Stream
Gulf Stream
and therefore the upper layer is closer to underlying fresher subpolar intermediate water. The eastern water is saltier because of its proximity to Mediterranean Water. North Atlantic Central Water flows into South Atlantic Central Water at 15°N.[27] There are five intermediate waters: four low-salinity waters formed at subpolar latitudes and one high-salinity formed through evaporation. Arctic
Arctic
Intermediate Water, flows from north to become the source for North Atlantic Deep Water
North Atlantic Deep Water
south of the Greenland-Scotland sill. These two intermediate waters have different salinity in the western and eastern basins. The wide range of salinities in the North Atlantic is caused by the asymmetry of the northern subtropical gyre and the large number of contributions from a wide range of sources: Labrador Sea, Norwegian- Greenland
Greenland
Sea, Mediterranean, and South Atlantic Intermediate Water.[27] The North Atlantic Deep Water
North Atlantic Deep Water
(NADW) is a complex of four water masses, two that form by deep convection in the open ocean — Classical and Upper Labrador Sea
Labrador Sea
Water — and two that form from the inflow of dense water across the Greenland-Iceland-Scotland sill — Denmark Strait
Denmark Strait
and Iceland-Scotland Overflow Water. Along its path across Earth
Earth
the composition of the NADW is affected by other water masses, especially Antarctic
Antarctic
Bottom Water and Mediterranean Overflow Water.[28] The NADW is fed by a flow of warm shallow water into the northern North Atlantic which is responsible for the anomalous warm climate in Europe. Changes in the formation of NADW have been linked to global climate changes in the past. Since man-made substances were introduced into the environment, the path of the NADW can be traced throughout its course by measuring tritium and radiocarbon from nuclear weapon tests in the 1960s and CFCs.[29]

Gyres[edit]

Map of the five major ocean gyres

The clockwise warm-water North Atlantic Gyre
North Atlantic Gyre
occupies the northern Atlantic, and the counter-clockwise warm-water South Atlantic Gyre appears in the southern Atlantic.[5] In the North Atlantic, surface circulation is dominated by three inter-connected currents: the Gulf Stream
Gulf Stream
which flows north-east from the North American coast at Cape Hatteras; the North Atlantic Current, a branch of the Gulf Stream
Gulf Stream
which flows northward from the Grand Banks; and the Subpolar Front, an extension of the North Atlantic Current, a wide, vaguely defined region separating the subtropical gyre from the subpolar gyre. This system of currents transport warm water into the North Atlantic, without which temperatures in the North Atlantic and Europe would plunge dramatically.[30]

In the subpolar gyre of the North Atlantic warm subtropical waters are transformed into colder subpolar and polar waters. In the Labrador Sea this water flows back to the subtropical gyre.

North of the North Atlantic Gyre, the cyclonic North Atlantic Subpolar Gyre plays a key role in climate variability. It is governed by ocean currents from marginal seas and regional topography, rather than being steered by wind, both in the deep ocean and at sea level.[31] The subpolar gyre forms an important part of the global thermohaline circulation. Its eastern portion includes eddying branches of the North Atlantic Current
North Atlantic Current
which transport warm, saline waters from the subtropics to the north-eastern Atlantic. There this water is cooled during winter and forms return currents that merge along the eastern continental slope of Greenland
Greenland
where they form an intense (40–50 Sv) current which flows around the continental margins of the Labrador Sea. A third of this water become parts of the deep portion of the North Atlantic Deep Water
North Atlantic Deep Water
(NADW). The NADW, in its turn, feed the meridional overturning circulation (MOC), the northward heat transport of which is threatened by anthropogenic climate change. Large variations in the subpolar gyre on a decade-century scale, associated with the North Atlantic oscillation, are especially pronounced in Labrador Sea
Labrador Sea
Water, the upper layers of the MOC.[32] The South Atlantic is dominated by the anti-cyclonic southern subtropical gyre. The South Atlantic Central Water originates in this gyre, while Antarctic
Antarctic
Intermediate Water originates in the upper layers of the circumpolar region, near the Drake Passage
Drake Passage
and Falkland Islands. Both these currents receive some contribution from the Indian Ocean. On the African east coast the small cyclonic Angola Gyre lies embedded in the large subtropical gyre.[33] The southern subtropical gyre is partly masked by a wind-induced Ekman layer. The residence time of the gyre is 4.4–8.5 years. North Atlantic Deep Water flows southerward below the thermocline of the subtropical gyre.[34] Sargasso Sea[edit] Main article: Sargasso Sea

Approximate extent of the Sargasso Sea

The Sargasso Sea
Sargasso Sea
in the western North Atlantic can be defined as the area where two species of Sargassum
Sargassum
(S. fluitans and natans) float, an area 4,000 km (2,500 mi) wide and encircled by the Gulf Stream, North Atlantic Drift, and North Equatorial Current. This population of seaweed probably originated from Tertiary ancestors on the European shores of the former Tethys Ocean
Tethys Ocean
and has, if so, maintained itself by vegetative growth, floating in the ocean for millions of years.[35]

Sargassum
Sargassum
fish (Histrio histrio)

Other species endemic to the Sargasso Sea
Sargasso Sea
include the sargassum fish, a predator with algae-like appendages who hovers motionless among the Sargassum. Fossils of similar fishes have been found in fossil bays of the former Tethys Ocean, in what is now the Carpathian region, that were similar to the Sargasso Sea. It is possible that the population in the Sargasso Sea
Sargasso Sea
migrated to the Atlantic as the Tethys closed at the end of the Miocene around 17 Ma.[35] The origin of the Sargasso fauna and flora remained enigmatic for centuries. The fossils found in the Carpathians in the mid-20th century, often called the "quasi-Sargasso assemblage", finally showed that this assemblage originated in the Carpathian Basin
Carpathian Basin
from were it migrated over Sicily to the Central Atlantic where it evolved into modern species of the Sargasso Sea.[36] The location of the spawning ground for European eels remained unknown for decades. In the early 19th century it was discovered that the southern Sargasso Sea
Sargasso Sea
is the spawning ground for both the European and American eel
American eel
and that the former migrate more than 5,000 km (3,100 mi) and the latter 2,000 km (1,200 mi). Ocean currents such as the Gulf Stream
Gulf Stream
transport eel larvae from the Sargasso Sea
Sargasso Sea
to foraging areas in North America, Europe, and Northern Africa.[37] Recent but disputed research suggests that eels possibly use Earth's magnetic field
Earth's magnetic field
to navigate through the ocean both as larvae and as adults.[38] Climate[edit]

Waves in the trade winds in the Atlantic Ocean—areas of converging winds that move along the same track as the prevailing wind—create instabilities in the atmosphere that may lead to the formation of hurricanes.

Climate is influenced by the temperatures of the surface waters and water currents as well as winds. Because of the ocean's great capacity to store and release heat, maritime climates are more moderate and have less extreme seasonal variations than inland climates. Precipitation can be approximated from coastal weather data and air temperature from water temperatures.[5] The oceans are the major source of the atmospheric moisture that is obtained through evaporation. Climatic zones vary with latitude; the warmest zones stretch across the Atlantic north of the equator. The coldest zones are in high latitudes, with the coldest regions corresponding to the areas covered by sea ice. Ocean
Ocean
currents influence climate by transporting warm and cold waters to other regions. The winds that are cooled or warmed when blowing over these currents influence adjacent land areas.[5] The Gulf Stream
Gulf Stream
and its northern extension towards Europe, the North Atlantic Drift is thought to have at least some influence on climate. For example, the Gulf Stream
Gulf Stream
helps moderate winter temperatures along the coastline of southeastern North America, keeping it warmer in winter along the coast than inland areas. The Gulf Stream
Gulf Stream
also keeps extreme temperatures from occurring on the Florida Peninsula. In the higher latitudes, the North Atlantic Drift, warms the atmosphere over the oceans, keeping the British Isles and north-western Europe mild and cloudy, and not severely cold in winter like other locations at the same high latitude. The cold water currents contribute to heavy fog off the coast of eastern Canada (the Grand Banks of Newfoundland area) and Africa's north-western coast. In general, winds transport moisture and air over land areas.[5] Natural hazards[edit]

Iceberg
Iceberg
A22A in the South Atlantic Ocean

Icebergs are common from February to August in the Davis Strait, Denmark Strait, and the northwestern Atlantic and have been spotted as far south as Bermuda
Bermuda
and Madeira. Ships are subject to superstructure icing in the extreme north from October to May. Persistent fog can be a maritime hazard from May to September, as can hurricanes north of the equator (May to December). The United States' southeast coast, especially the Virginia and North Carolina coasts, has a long history of shipwrecks due to its many shoals and reefs. The Bermuda
Bermuda
Triangle is popularly believed to be the site of numerous aviation and shipping incidents because of unexplained and supposedly mysterious causes, but Coast Guard
Coast Guard
records do not support this belief. Hurricanes
Hurricanes
are also a natural hazard in the Atlantic, but mainly in the northern part of the ocean, rarely tropical cyclones form in the southern parts. Hurricanes
Hurricanes
usually form annually between June and November. Plate tectonics[edit]

The break-up of Pangaea
Pangaea
resulted in the opening of the Atlantic Ocean in three stages

Central Atlantic[edit]

Opening of the Central Atlantic 200-170 Ma

The break-up of Pangaea
Pangaea
began in the Central Atlantic, between North America and Northwest Africa, where rift basins opened during the Late Triassic and Early Jurassic. This period also saw the first stages of the uplift of the Atlas Mountains. The exact timing is controversial with estimates ranging from 200 to 170 Ma.[39] The opening of the Atlantic Ocean
Ocean
coincided with the initial break-up of the supercontinent Pangaea, both of which were initiated by the eruption of the Central Atlantic Magmatic Province
Central Atlantic Magmatic Province
(CAMP), one of the most extensive and voluminous large igneous provinces in Earth's history associated with the Triassic–Jurassic extinction event, one of Earth's major extinction events.[40] Theoliitic dikes, sills, and lava flows from the CAMP eruption at 200 Ma have been found in West Africa, eastern North America, and northern South America. The extent of the volcanism has been estimated to 4.5×106 km2 (1.7×106 sq mi) of which 2.5×106 km2 (9.7×105 sq mi) covered what is now northern and central Brazil.[41] The formation of the Central American Isthmus
Central American Isthmus
closed the Central American Seaway at the end of the Pliocene 2.8 Ma ago. The formation of the isthmus resulted in the migration and extinction of many land-living animals, known as the Great American Interchange, but the closure of the seaway resulted in a "Great American Schism" as it affected ocean currents, salinity, and temperatures in both the Atlantic and Pacific. Marine organisms on both sides of the isthmus became isolated and either diverged or went extinct.[42] Northern Atlantic[edit] Main article: Opening of the North Atlantic Ocean Geologically the Northern Atlantic is the area delimited to the south by two conjugate margins, Newfoundland and Iberia, and to the north by the Arctic
Arctic
Eurasian Basin. The opening of the Northern Atlantic closely followed the margins of its predecessor, the Iapetus Ocean, and spread from the Central Atlantic in six stages: Iberia–Newfoundland, Porcupine–North America, Eurasia–Greenland, Eurasia–North America. Active and inactive spreading systems in this area are marked by the interaction with the Iceland
Iceland
hotspot.[43] South Atlantic[edit]

The opening of the South Atlantic

West Gondwana (South America and Africa) broke up in the Early Cretaceous to form the South Atlantic. The apparent fit between the coastlines of the two continents was noted on the first maps that included the South Atlantic and it was also the subject of the first computer-assisted plate tectonic reconstructions in 1965.[44][45] This magnificent fit, however, has since then proven problematic and later reconstructions have introduced various deformation zones along the shorelines to accommodate the northward-propagating break-up.[44] Intra-continental rifts and deformations have also been introduced to subdivide both continental plates into sub-plates.[46] Geologically the South Atlantic can be divided into four segments: Equatorial segment, from 10°N to the Romanche Fracture Zone (RFZ);; Central segment, from RFZ to Florianopolis Fracture Zone (FFZ, north of Walvis Ridge
Walvis Ridge
and Rio Grande Rise); Southern segment, from FFZ to the Agulhas-Falkland Fracture Zone (AFFZ); and Falkland segment, south of AFFZ.[47] In the southern segment the Early Cretaceous (133–130 Ma) intensive magmatism of the Paraná–Etendeka Large Igneous Province produced by the Tristan hotspot
Tristan hotspot
resulted in an estimated volume of 1.5×106 to 2.0×106 km3 (3.6×105 to 4.8×105 cu mi). It covered an area of 1.2×106 to 1.6×106 km2 (4.6×105 to 6.2×105 sq mi) in Brazil, Paraguay, and Uruguay and 0.8×105 km2 (3.1×104 sq mi) in Africa. Dyke swarms in Brazil, Angola, eastern Paraguay, and Namibia, however, suggest the LIP originally covered a much larger area and also indicate failed rifts in all these areas. Associated offshore basaltic flows reach as far south as the Falkland Islands and South Africa. Traces of magmatism in both offshore and onshore basins in the central and southern segments have been dated to 147–49 Ma with two peaks between 143–121 Ma and 90–60 Ma.[47] In the Falkland segment rifting began with dextral movements between the Patagonia and Colorado sub-plates between the Early Jurassic (190 Ma) and the Early Cretaceous (126.7 Ma). Around 150 Ma sea-floor spreading propagated northward into the southern segment. No later than 130 Ma rifting had reached the Walvis Ridge–Rio Grande Rise.[46] In the central segment rifting started to break Africa in two by opening the Benue Trough
Benue Trough
around 118 Ma. Rifting in the central segment, however, coincided with the Cretaceous Normal Superchron (also known as the Cretaceous quiet period), a 40 Ma period without magnetic reversals, which makes it difficult to date sea-floor spreading in this segment.[46] The equatorial segment is the last phase of the break-up, but, because it is located on the Equator, magnetic anomalies cannot be used for dating. Various estimates date the propagation of sea-floor spreading in this segment to the period 120–96 Ma. This final stage, nevertheless, coincided with or resulted in the end of continental extension in Africa.[46] About 50 Ma the opening of the Drake Passage
Drake Passage
resulted from a change in the motions and separation rate of the South American and Antarctic
Antarctic
plates. First small ocean basins opened and a shallow gateway appeared during the Middle Eocene. 34–30 Ma a deeper seaway developed, followed by an Eocene–Oligocene climatic deterioration and the growth of the Antarctic
Antarctic
ice sheet.[48] Closure of the Atlantic[edit] See also: Pangaea
Pangaea
Ultima An embryonic subduction margin is potentially developing west of Gibraltar. The Gibraltar Arc
Gibraltar Arc
in the western Mediterranean is migrating westward into the Central Atlantic where it joins the converging African and Eurasian plates. Together these three tectonic forces are slowly developing into a new subduction system in the eastern Atlantic Basin. Meanwhile, the Scotia Arc
Scotia Arc
and Caribbean Plate
Caribbean Plate
in the western Atlantic Basin are eastward-propagating subduction systems that might, together with the Gibraltar system, represent the beginning of the closure of the Atlantic Ocean
Ocean
and the final stage of the Atlantic Wilson Cycle.[49] History[edit] Main category: History of the Atlantic Ocean Human origin[edit] Humans evolved in Africa; first by diverging from other apes around 7 Ma; then developing stone tools around 2.6 Ma; to finally evolve as modern humans around 100 kya. The earliest evidences for the complex behavior associated with this behavioral modernity has been found in the Greater Cape Floristic Region
Cape Floristic Region
(GCFR) along the coast of South Africa. During the latest glacial stages the now-submerged plains of the Agulhas Bank
Agulhas Bank
were exposed above sea level, extending the South African coastline farther south by hundreds of kilometers. A small population of modern humans — probably fewer than a thousand reproducing individuals — survived glacial maxima by exploring the high diversity offered by these Palaeo-Agulhas plains. The GCFR is delimited to the north by the Cape Fold Belt
Cape Fold Belt
and the limited space south of it resulted in the development of social networks out of which complex Stone Age technologies emerged.[50] Human history thus begins on the coasts of South Africa where the Atlantic Benguela Upwelling and Indian Ocean
Ocean
Agulhas Current
Agulhas Current
meet to produce an intertidal zone on which shellfish, fur seal, fishes and sea birds provided the necessary protein sources.[51] The African origin of this modern behaviour is evidenced by 70,000 years-old engravings from Blombos Cave, South Africa.[52] Old World[edit] Mitochondrial DNA
Mitochondrial DNA
(mtDNA) studies indicate that 80–60,000 years ago a major demographic expansion within Africa, derived from a single, small population, coincided with the emergence of behavioral complexity and the rapid MIS 5–4 environmental changes. This group of people not only expanded over the whole of Africa, but also started to disperse out of Africa into Asia, Europe, and Australasia around 65,000 years ago and quickly replaced the archaic humans in these regions.[53] During the Last Glacial Maximum
Last Glacial Maximum
(LGM) 20,000 years ago humans had to abandon their initial settlements along the European North Atlantic coast and retreat to the Mediterranean. Following rapid climate changes at the end of the LGM this region was repopulated by Magdalenian
Magdalenian
culture. Other hunter-gatherers followed in waves interrupted by large-scale hazards such as the Laacher See
Laacher See
volcanic eruption, the inundation of Doggerland
Doggerland
(now the North Sea), and the formation of the Baltic Sea.[54] The European coasts of the North Atlantic were permanently populated about 9–8.5 thousand years ago.[55] This human dispersal left abundant traces along the coasts of the Atlantic Ocean. 50 ka-old, deeply stratified shell middens found in Ysterfontein on the western coast of South Africa are associated with the Middle Stone Age (MSA). The MSA population was small and dispersed and the rate of their reproduction and exploitation was less intense than those of later generations. While their middens resemble 12–11 ka-old Late Stone Age (LSA) middens found on every inhabited continent, the 50–45 ka-old Enkapune Ya Muto
Enkapune Ya Muto
in Kenya probably represents the oldest traces of the first modern humans to disperse out of Africa.[56]

Excavation of the Ertebølle middens in 1880

The same development can be seen in Europe. In La Riera Cave (23–13 ka) in Asturias, Spain, only some 26,600 molluscs were deposited over 10 ka. In contrast, 8–7 ka-old shell middens in Portugal, Denmark, and Brazil generated thousands of tons of debris and artefacts. The Ertebølle middens in Denmark, for example, accumulated 2,000 m3 (71,000 cu ft) of shell deposits representing some 50 million molluscs over only a thousand years. This intensification in the exploitation of marine resources has been described as accompanied by new technologies — such as boats, harpoons, and fish-hooks — because many caves found in the Mediterranean and on the European Atlantic coast have increased quantities of marine shells in their upper levels and reduced quantities in their lower. The earliest exploitation, however, took place on the now submerged shelves, and most settlements now excavated were then located several kilometers from these shelves. The reduced quantities of shells in the lower levels can represent the few shells that were exported inland.[57] New World[edit] During the LGM the Laurentide Ice Sheet
Laurentide Ice Sheet
covered most of northern North America while Beringia
Beringia
connected Siberia to Alaska. In 1973 late U.S. geoscientist Paul S. Martin
Paul S. Martin
proposed a "blitzkrieg" colonization of America by which Clovis hunters migrated into North America around 13,000 years ago in a single wave through an ice-free corridor in the ice sheet and "spread southward explosively, briefly attaining a density sufficiently large to overkill much of their prey."[58] Others later proposed a "three-wave" migration over the Bering Land Bridge.[59] These hypotheses remained the long-held view regarding the settlement of the Americas, a view challenged by more recent archaeological discoveries: the oldest archaeological sites in the Americas have been found in South America; sites in north-east Siberia report virtually no human presence there during the LGM; and most Clovis artefacts have been found in eastern North America along the Atlantic coast.[60] Furthermore, colonisation models based on mtDNA, yDNA, and atDNA data respectively support neither the "blitzkrieg" nor the "three-wave" hypotheses but they also deliver mutually ambiguous results. Contradictory data from archaeology and genetics will most likely deliver future hypotheses that will, eventually, confirm each other.[61] A proposed route across the Pacific to South America could explain early South American finds and another hypothesis proposes a northern path, through the Canadian Arctic
Arctic
and down the North American Atlantic coast.[62] Early settlements across the Atlantic have been suggested by alternative theories, ranging from purely hypothetical to mostly disputed, including the Solutrean hypothesis
Solutrean hypothesis
and some of the Pre-Columbian trans-oceanic contact theories.

Based on the medieval Íslendingasögur sagas, including the Grœnlendinga saga, this interpretative map of the "Norse World" shows that Norse knowledge of America and the Atlantic remained limited.

The Norse settlement of the Faroe Islands
Faroe Islands
and Iceland
Iceland
began during the 9th and 10th centuries. A settlement on Greenland
Greenland
was established before 1000 CE, but contact with it was lost in 1409 and it was finally abandoned during the early Little Ice Age. This setback was caused by a range of factors: an unsustainable economy resulted in erosion and denudation, while conflicts with the local Inuit
Inuit
resulted in the failure to adapt their Arctic
Arctic
technologies; a colder climate resulted in starvation; and the colony got economically marginalized as the Great Plague
Great Plague
and Barbary pirates
Barbary pirates
harvested its victims on Iceland
Iceland
in the 15th century.[63] Iceland
Iceland
was initially settled 865–930 CE following a warm period when winter temperatures hovered around 2 °C (36 °F) which made farming favorable at high latitudes. This did not last, however, and temperatures quickly dropped; at 1080 CE summer temperatures had reached a maximum of 5 °C (41 °F). The Landnámabók ( Book
Book
of Settlement) records disastrous famines during the first century of settlement — "men ate foxes and ravens" and "the old and helpless were killed and thrown over cliffs" — and by the early 1200s hay had to be abandoned for short-season crops such as barley.[64] See also: Brendan § Possible link to North America Atlantic World[edit] Main articles: Atlantic world and Atlantic history

A century after Columbus' first voyage, large parts of the New World had been included into the Spanish Empire.

Christopher Columbus
Christopher Columbus
discovered the Americas in 1492 under Spanish flag.[65] Six years later Vasco da Gama
Vasco da Gama
reached India under Portuguese flag, by navigating south around the Cape of Good Hope, thus proving that the Atlantic and Indian Oceans are connected. In 1500, in his voyage to India following Vasco da Gama, Pedro Alvares Cabral
Pedro Alvares Cabral
reached Brazil, taken by the currents of the South Atlantic Gyre. Following these explorations, Spain and Portugal quickly conquered and colonized large territories in the New World
New World
and forced the Native American population into slavery in order to explore the vast quantities of silver and gold they found. Spain and Portugal monopolized this trade in order to keep other European nations out, but conflicting interests nevertheless led to a series of Spanish-Portuguese wars. A peace treaty mediated by the Pope divided the conquered territories into Spanish and Portuguese sectors while keeping other colonial powers away. England, France, and the Dutch Republic enviously watched the Spanish and Portuguese wealth grow and allied themselves with pirates such as Henry Mainwaring and Alexandre Exquemelin. They could explore the convoys leaving America because prevailing winds and currents made the transport of heavy metals slow and predictable.[65]

Embarked and disembarked slaves in the Atlantic slave trade 1525–1863 (first and last slave voyages)

In the American colonies depredation, disease, and slavery quickly reduced the indigenous American population to the extent that the Atlantic slave trade
Atlantic slave trade
had to be introduced to replace them — a trade that became norm and an integral part of the colonization. Between the 15th century and 1888, when Brazil became the last part of America to end slave trade, an estimated ten million Africans were exported as slaves, most of them destined for agricultural labour. The slave trade was officially abolished in the British Empire and the United States in 1808, and slavery itself was abolished in the British Empire in 1838 and in the U.S. in 1865 after the Civil War.[66][67] From Columbus to the Industrial Revolution
Industrial Revolution
Trans-Atlantic trade, including colonialism and slavery, became crucial for Western Europe. For European countries with a direct access to the Atlantic (including Britain, France, the Netherlands, Portugal, and Spain) 1500–1800 was a period of sustained growth during which these countries grew richer than those in Eastern Europe and Asia. Colonialism evolved as part of the Trans-Atlantic trade, but this trade also strengthened the position of merchant groups at the expense of monarchs. Growth was more rapid in non-absolutist countries, such as Britain and the Netherlands, and more limited in absolutist monarchies, such as Portugal, Spain, and France, where profit mostly or exclusively benefited the monarchy and its allies.[68] Trans-Atlantic trade also resulted in an increasing urbanization: in European countries facing the Atlantic urbanization grew from 8% in 1300, 10.1% in 1500, to 24.5% in 1850; in other European countries from 10% in 1300, 11.4% in 1500, to 17% in 1850. Likewise, GDP doubled in Atlantic countries but rose by only 30% in the rest of Europe. By end of the 17th century the volume of the Trans-Atlantic trade had surpassed that of the Mediterranean trade.[68] See also: List of notable crossings of the Atlantic Ocean Economy[edit] The Atlantic has contributed significantly to the development and economy of surrounding countries. Besides major transatlantic transportation and communication routes, the Atlantic offers abundant petroleum deposits in the sedimentary rocks of the continental shelves.[5] The Atlantic harbors petroleum and gas fields, fish, marine mammals (seals and whales), sand and gravel aggregates, placer deposits, polymetallic nodules, and precious stones.[69] Gold deposits are a mile or two under water on the ocean floor, however the deposits are also encased in rock that must be mined through. Currently, there is no cost-effective way to mine or extract gold from the ocean to make a profit.[70] Various international treaties attempt to reduce pollution caused by environmental threats such as oil spills, marine debris, and the incineration of toxic wastes at sea.[5] Fisheries[edit] The shelves of the Atlantic hosts one of the world's richest fishing resources. The most productive areas include the Grand Banks of Newfoundland, the Scotian Shelf, Georges Bank
Georges Bank
off Cape Cod, the Bahama Banks, the waters around Iceland, the Irish Sea, the Bay of Fundy, the Dogger Bank
Dogger Bank
of the North Sea, and the Falkland Banks.[5] Fisheries have, however, undergone significant changes since the 1950s and global catches can now be divided into three groups of which only two are observed in the Atlantic: fisheries in the Eastern Central and South-West Atlantic oscillate around a globally stable value, the rest of the Atlantic is in overall decline following historical peaks. The third group, "continuously increasing trend since 1950", is only found in the Indian Ocean
Ocean
and Western Pacific.[71]

Banks of the North-East Atlantic

In the North-East Atlantic total catches decreased between the mid-1970s and the 1990s and reached 8.7 million tons in 2013. Blue whiting reached a 2.4 million tons peak in 2004 but was down to 628,000 tons in 2013. Recovery plans for cod, sole, and plaice have reduced mortality in these species. Arctic
Arctic
cod reached its lowest levels in the 1960s–1980s but is now recovered. Arctic
Arctic
saithe and haddock are considered fully fished; Sand
Sand
eel is overfished as was capelin which has now recovered to fully fished. Limited data makes the state of redfishes and deep-water species difficult to assess but most likely they remain vulnerable to overfishing. Stocks of northern shrimp and Norwegian lobster
Norwegian lobster
are in good condition. In the North-East Atlantic 21% of stocks are considered overfished.[71]

Banks of the North-West Atlantic

In the North-West Atlantic landings have decreased from 4.2 million tons in the early 1970s to 1.9 million tons in 2013. During the 21th century some species have shown weak signs of recovery, including Greenland
Greenland
halibut, yellowtail flounder, Atlantic halibut, haddock, spiny dogfish, while other stocks shown no such signs, including cod, witch flounder, and redfish. Stocks of invertebrates, in contrast, remain at record levels of abundance. 31% of stocks are overfished in the North-west Atlantic.[71]

Capture of Atlantic north-west cod in million tons

In 1497 John Cabot
John Cabot
became the first to explore mainland North America and one of his major discoveries was the abundant resources of Atlantic cod
Atlantic cod
off Newfoundland. Referred to as "Newfoundland Currency" this discovery supplied mankind with some 200 million tons of fish over five centuries. In the late 19th and early 20th centuries new fisheries started to exploit haddock, mackerel, and lobster. From the 1950s to the 1970s the introduction of European and Asian distant-water fleets in the area dramatically increased the fishing capacity and number of exploited species. It also expanded the exploited areas from near-shore to the open sea and to great depths to include deep-water species such as redfish, Greenland
Greenland
halibut, witch flounder, and grenadiers. Overfishing
Overfishing
in the area was recognised as early as the 1960s but, because this was occurring on international waters, it took until the late 1970s before any attempts to regulate was made. In the early 1990s this finally resulted in the collapse of the Atlantic northwest cod fishery. The population of a number of deep-sea fishes also collapsed in the process, including American plaice, redfish, and Greenland
Greenland
halibut, together with flounder and grenadier.[72] In the Eastern Central Atlantic small pelagic fishes constitute about 50% of landings with sardine reaching 0.6–1.0 million tons per year. Pelagic fish
Pelagic fish
stocks are considered fully fishes or overfished, with sardines south of Cape Bojador
Cape Bojador
the notable exception. Almost half of stocks are fished at biologically unsustainable levels. Total catches have been fluctuating since the 1970s; reaching 3.9 million tons in 2013 or slightly less than the peak production in 2010.[71]

Bahama Banks

In the Western Central Atlantic catches have been decreasing since 2000 and reached 1.3 million tons in 2013. The most important species in the area, Gulf menhaden, reached a million tons in the mid-1980s but only half a million tons in 2013 and is now considered fully fished. Round sardinella
Round sardinella
was an important species in the 1990s but is now considered overfished. Groupers and snappers are overfished and northern brown shrimp and American cupped oyster are considered fully fished approaching overfished. 44% of stocks are being fished at unsustainable levels.[71]

Agulhas Bank

In the South-East Atlantic catches have decreased from 3.3 million tons in the early 1970s to 1.3 million tons in 2013. Horse mackerel and hake are the most important species, together representing almost half of the landings. Off South Africa and Namibia deep-water hake and shallow-water Cape hake have recovered to sustainable levels since regulations were introduced in 2006 and the states of Southern African pilchard and anchovy have improved to fully fished in 2013.[71] In the South-West Atlantic a peak was reached in the mid-1980s and catches now fluctuate between 1.7 and 2.6 million tons. The most important species, the Argentine shortfin squid, which reached half a million tons in 2013 or half the peak value, is considered fully fished to overfished. Another important species was the Brazilian sardinella, with a production of 100,000 tons in 2013 it is now considered overfished. Half the stocks in this area are being fished at unsustainable levels: Whitehead’s round herring has not yet reached fully fished but Cunene horse mackerel
Cunene horse mackerel
is overfished. The sea snail perlemoen abalone is targeted by illegal fishing and remain overfished.[71] See also: Ocean
Ocean
fisheries § Atlantic Ocean, and Fishing down the food web Environmental issues[edit]

Marine debris
Marine debris
strewn over the beaches of the South Atlantic Inaccessible Island

Endangered marine species include the manatee, seals, sea lions, turtles, and whales. Drift net
Drift net
fishing can kill dolphins, albatrosses and other seabirds (petrels, auks), hastening the fish stock decline and contributing to international disputes.[73] Municipal pollution comes from the eastern United States, southern Brazil, and eastern Argentina; oil pollution in the Caribbean Sea, Gulf of Mexico, Lake Maracaibo, Mediterranean Sea, and North Sea; and industrial waste and municipal sewage pollution in the Baltic Sea, North Sea, and Mediterranean Sea. North Atlantic hurricane activity has increased over past decades because of increased sea surface temperature (SST) at tropical latitudes, changes that can be attributed to either the natural Atlantic Multidecadal Oscillation
Atlantic Multidecadal Oscillation
(AMO) or to anthropogenic climate change.[74] A 2005 report indicated that the Atlantic meridional overturning circulation (AMOC) slowed down by 30% between 1957 and 2004.[75] If the AMO were responsible for SST variability, the AMOC would have increased in strength, which is apparently not the case. Furthermore, it is clear from statistical analyses of annual tropical cyclones that these changes do not display multidecadal cyclicity.[74] Therefore, these changes in SST must be caused by human activities.[76] The ocean mixed layer plays an important role heat storage over seasonal and decadal time-scales, whereas deeper layers are affected over millennia and has a heat capacity about 50 times that of the mixed layer. This heat uptake provides a time-lag for climate change but it also results in a thermal expansion of the oceans which contribute to sea-level rise. 21st century global warming will probably result in an equilibrium sea-level rise five times greater than today, whilst melting of glaciers, including that of the Greenland
Greenland
ice-sheet, expected to have virtually no effect during the 21st century, will probably result in a sea-level rise of 3–6 m over a millennium.[77] On 7 June 2006, Florida's wildlife commission voted to take the manatee off the state's endangered species list. Some environmentalists worry that this could erode safeguards for the popular sea creature. Marine pollution
Marine pollution
is a generic term for the entry into the ocean of potentially hazardous chemicals or particles. The biggest culprits are rivers and with them many agriculture fertilizer chemicals as well as livestock and human waste. The excess of oxygen-depleting chemicals leads to hypoxia and the creation of a dead zone.[78] Marine debris, which is also known as marine litter, describes human-created waste floating in a body of water. Oceanic debris tends to accumulate at the center of gyres and coastlines, frequently washing aground where it is known as beach litter. See also: Environmental impact of shipping
Environmental impact of shipping
and Shutdown of thermohaline circulation See also[edit]

Environment portal Ecology portal Geography portal Weather portal

List of countries and territories bordering the Atlantic Ocean Seven Seas Gulf Stream
Gulf Stream
shutdown Shipwrecks in the Atlantic Ocean Atlantic hurricanes Transatlantic crossing

References[edit] Notes[edit]

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Further reading[edit]

Winchester, Simon (2010). Atlantic: A Vast Ocean
Ocean
of a Million Stories. HarperCollins UK. ISBN 978-0-00-734137-5. 

External links[edit]

Find more aboutAtlantic Oceanat's sister projects

Definitions from Wiktionary Media from Wikimedia Commons Texts from Wikisource Travel guide from Wikivoyage

Atlantic Ocean. Cartage.org.lb. "Map of Atlantic Coast of North America from the Chesapeake Bay to Florida" from 1639 via the World Digital Library

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Amundsen Gulf Barents Sea Beaufort Sea Chukchi Sea East Siberian Sea Greenland
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Atlantic Ocean

Adriatic Sea Aegean Sea Alboran Sea Archipelago Sea Argentine Sea Baffin Bay Balearic Sea Baltic Sea Bay of Biscay Bay of Bothnia Bay of Campeche Bay of Fundy Black Sea Bothnian Sea Caribbean Sea Celtic Sea English Channel Foxe Basin Greenland
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Indian Ocean

Andaman Sea Arabian Sea Bali Sea Bay of Bengal Flores Sea Great Australian Bight Gulf of Aden Gulf of Aqaba Gulf of Khambhat Gulf of Kutch Gulf of Oman Gulf of Suez Java Sea Laccadive Sea Mozambique Channel Persian Gulf Red Sea Timor Sea

Pacific Ocean

Arafura Sea Banda Sea Bering Sea Bismarck Sea Bohai Sea Bohol Sea Camotes Sea Celebes Sea Ceram Sea Chilean Sea Coral Sea East China Sea Gulf of Alaska Gulf of Anadyr Gulf of California Gulf of Carpentaria Gulf of Fonseca Gulf of Panama Gulf of Thailand Gulf of Tonkin Halmahera Sea Koro Sea Mar de Grau Molucca Sea Moro Gulf Philippine Sea Salish Sea Savu Sea Sea of Japan Sea of Okhotsk Seto Inland Sea Shantar Sea Sibuyan Sea Solomon Sea South China Sea Sulu Sea Tasman Sea Visayan Sea Yellow Sea

Southern Ocean

Amundsen Sea Bellingshausen Sea Cooperation Sea Cosmonauts Sea Davis Sea D'Urville Sea King Haakon VII Sea Lazarev Sea Mawson Sea Riiser-Larsen Sea Ross Sea Scotia Sea Somov Sea Weddell Sea

Landlocked seas

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  Book   Category

v t e

Ocean
Ocean
currents and gyres

Currents

Arctic
Arctic
Ocean

East Greenland North Icelandic Norwegian Transpolar Drift Stream

Atlantic Ocean

Angola Antilles Azores Baffin Island Benguela Brazil Canary Cape Horn Caribbean East Greenland East Iceland Falkland Florida Guinea Gulf Stream Irminger Labrador Lomonosov Loop North Atlantic North Brazil North Equatorial Norwegian Portugal Slope Jet South Atlantic South Equatorial West Greenland West Spitsbergen

Indian Ocean

Agulhas Agulhas Return East Madagascar Equatorial Counter Indian Monsoon Indonesian Throughflow Leeuwin Madagascar Mozambique North Madagascar Somali South Australian South Equatorial West Australian

Pacific Ocean

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WorldCat Identities VIAF: 152295726 GND: 40033

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