List of submarine topographical features

Depiction of the abyssal zone in relation to other major oceanic zones.

List of submarine topographical features, oceanic landforms and topographic elements.

Abyssal plain

An abyssal plain is an underwater plain on the deep ocean floor, usually found at depths between 3,000 meters (9,800 ft) and 6,000 meters (20,000 ft). Lying generally between the foot of a continental rise and a mid-ocean ridge, abyssal plains are among the flattest, smoothest and least explored regions on Earth.^[1] Abyssal plains are key geologic elements of oceanic basins (the other elements being an elevated mid-ocean ridge and flanking abyssal hills). In addition to these elements, active oceanic basins (those that are associated with a moving plate tectonic boundary) also typically include an oceanic trench and a subduction zone. Though they cover more than 50% of the Earth’s surface,^[2][3] they are poorly preserved in the sedimentary record because they tend to be consumed by the subduction process.^[1]

The abyssal plain is formed when the lower oceanic crust is melted and forced upwards by the asthenosphere layer of the upper mantle. As this basaltic material reaches the surface at mid-ocean ridges, it forms new oceanic crust. Abyssal plains result from the blanketing of an originally uneven surface of oceanic crust by fine-grained sediments, mainly clay and silt. Much of this sediment is deposited from turbidity currents that have been channeled from the continental margins along submarine canyons down into deeper water. The remainder of the sediment is composed chiefly of pelagic sediments.

Use of a continuously recording fathometer enabled Tolstoy & Ewing in the summer of 1947 to identify and describe the first abyssal plain.^[1][4] This plain, located to the south of Newfoundland, is now known as the Sohm Abyssal Plain.^[4] Following this discovery many other examples were found in all the oceans.^{[5][6][7][8][9]}

List of abyssal plains and oceanic basins

Following is a list of named abyssal plains and oceanic basins:^[1][10][11]

Oceanic trenches

Oceanic trenches are long, narrow topographic depressions of the seabed. They are the deepest parts of the ocean floor, and they define one of the most important natural boundaries on the Earth's solid surface: the one between two lithospheric plates. Trenches are a distinctive morphological feature of plate boundaries.

There are three types of lithospheric plate boundaries: 1.) divergent (where lithosphere and oceanic crust is created at mid-ocean ridges), 2.) convergent (where one lithospheric plate sinks beneath another and returns to the mantle), and 3.) transform (where two lithospheric plates slide past each other).

An oceanic trench is a type of convergent boundary at which two oceanic lithospheric slabs meet; the older (and therefore denser) of these slabs flexes and subducts beneath the other slab. Oceanic lithosphere moves into trenches at a global rate of about a tenth of a square meter per second. Trenches are generally parallel to a volcanic island arc, and about 200 km from a volcanic arc. Oceanic trenches typically extend 3 to 4 km (1.9 to 2.5 mi) below the level of the surrounding oceanic floor. The greatest ocean depth to be sounded is in the Challenger Deep of the Mariana Trench, at a depth of 10,911 m (35,798 ft) below sea level.

List of oceanic trenches

Location of the Challenger Deep in the Mariana Trench

The following is a list of the deepest parts of the Earth's oceans and seas (all depths are measured from sea level):

• Entries marked with * are the deepest parts of their respective water bodies, but are not oceanic trenches.

Oceanic plateau

An oceanic plateau is a large, relatively flat submarine region that rises well above the level of the ambient seabed.^[46] While many oceanic plateaus are composed of continental crust, and often form a step interrupting the continental slope, some plateaus are undersea remnants of large igneous provinces. Continental crust has the highest amount of silicon (such rock is called felsic). Oceanic crust has a smaller amount of silicon (mafic rock).

The anomalous volcanism associated with the formation of oceanic plateaux at the time of the Cenomanian-Turonian boundary (90.4 million years) ago may have been responsible for the environmental disturbances that occurred at that time. The physical manifestations of this were elevated atmospheric and oceanic temperatures, a significant sea-level transgression, and a period of widespread anoxia, leading to the extinction of 26% of all genera.^[47] These eruptions would also have resulted in the emission of large quantities of carbon dioxide into the atmosphere, leading to global warming. Additionally, the emission of sulfur monoxide, hydrogen sulfide, carbon monoxide, and halogens into the oceans would have made seawater more acidic resulting in the dissolution of carbonate, and further release of CO2. This runaway greenhouse effect was probably put into reverse by the decline of the anomalous volcanic activity and by increased CO2-driven productivity in oceanic surface waters, leading to increased organic carbon burial, black shale deposition, anoxia and mass extinction in the ocean basins.^[47]

Map of the Zealandia microcontinent, showing Alpine Fault, Bounty Trough, Campbell Plateau, Challenger Plateau, Chatham Rise, Havre Trough, Hikurangi Plateau, Kermadec Trench, Lord Howe Rise, Louisville Ridge, New Caledonia Basin, Norfolk Ridge, South Fiji Basin, South West Pacific Basin, and Tasman Basin.

List of oceanic plateaus

• Campbell Plateau (South Pacific)
• Challenger Plateau (South Pacific)
• Agulhas Plateau^[48] (Southwest Indian)
• Caribbean-Colombian Plateau (Caribbean)
• Exmouth Plateau (Indian)
• Hikurangi Plateau (Southwest Pacific)
• Kerguelen Plateau (Indian)
• Manihiki Plateau (Southwest Pacific)
• Marquesas Plateau (Southwest Pacific)
• Mascarene Plateau (Indian)
• Naturaliste Plateau (Indian)
• Ontong Java Plateau (Southwest Pacific)
• Shatsky Rise (North Pacific)
• Vøring Plateau (North Atlantic)
• Wrangellia Terrane (Northeast Pacific)
• Yermak Plateau (Arctic)

Mid-ocean ridges

A mid-ocean ridge is a general term for an underwater mountain system that consists of various mountain ranges (chains), typically having a valley known as a rift running along its spine, formed by plate tectonics. This type of oceanic ridge is characteristic of what is known as an oceanic spreading center, which is responsible for seafloor spreading.

List of mid-ocean ridges

• Aden Ridge
• American-Antarctic Ridge
• Carlsberg Ridge
• Central Indian Ridge
• Chile Rise
• Cocos Ridge
• East Pacific Rise
• East Scotia Ridge
• Explorer Ridge
• Gakkel Ridge (Mid-Arctic Ridge)
• Gorda Ridge
• Juan de Fuca Ridge
• Knipovich Ridge (between Greenland and Spitsbergen)
• Kolbeinsey Ridge (North of Iceland)
• Mid-Atlantic Ridge
• Mohns Ridge
• Norfolk Ridge
• Pacific-Antarctic Ridge
• Palau-Kyushu Ridge
• Reykjanes Ridge (South of Iceland)
• Southeast Indian Ridge
• Southwest Indian Ridge
• West Mariana Ridge

See also

• Physical oceanography
• Bathymetry
• Challenger Deep
• Hadal zone
• List of oceanic landforms
• Seamount

References

Further reading

• Böggemann M. & Purschke G. (2005). "Abyssal benthic Syllidae (Annelida: Polychaeta) from the Angola Basin". Organisms, Diversity & Evolution 5 (Supplement 1): 221–226. doi:10.1016/j.ode.2004.11.006. 

• Bohn, J.M. (2005). "On two rare abyssal Myriotrochidae (Echinodermata: Holothuroidea: Apodida) new to the South Atlantic: Siniotrochus myriodontus Gage and Billet, 1986 and Lepidotrochus parvidiscus angolensis subsp. nov". Organisms, Diversity & Evolution 5 (Supplement 1): 231–238. doi:10.1016/j.ode.2004.11.008. 

• Brandt A., Brenke N., Andres H.-G., Brix S., Guerrero-Kommritz J., Mühlenhardt-Siegel U., & Wägele J.-W. (2005). "Diversity of peracarid crustaceans (Malacostraca) from the abyssal plain of the Angola Basin". Organisms, Diversity and Evolution 5: 105–112. doi:10.1016/j.ode.2004.10.007. 

• Gad G. (2005). "Giant Higgins-larvae with paedogenetic reproduction from the deep sea of the Angola Basin- evidence for a new life cycle and for abyssal gigantism in Loricifera?". Organisms, Diversity & Evolution 5 (Supplement 1): 59–76. doi:10.1016/j.ode.2004.10.005. 

• Gill Adrian E. (1982). Atmosphere-Ocean Dynamics. San Diego: Academic Press. ISBN 0-12-283520-4. 

• Gooday A.J., Nomaki H., & Kitazato H. (2008). "Modern deep-sea benthic foraminifera: a brief review of their morphology-based biodiversity and trophic diversity". Geological Society (Special Publications 303): 97–119. 

• Gooday A.J., Kamenskaya O.E. & Cedhagen T. (2007). "New and little-known Komokiacea (Foraminifera) from the bathyal and abyssal Weddell Sea and adjacent areas". Zoological Journal of the Linnean Society 151 (2): 219–251. doi:10.1111/j.1096-3642.2007.00326.x. 

• Gooday A.J. & Malzone G. (2004). "Hyperammina micaceus sp. nov.: a new foraminiferan species (Protista) from the Porcupine Abyssal Plain, Northeast Atlantic". Journal of Micropalaeontology 23 (2): 171–179. doi:10.1144/jm.23.2.171. 

• Janussen D. & Tendal O.S. (2007). "Diversity and distribution of Porifera in the bathyal and abyssal Weddell Sea and adjacent areas". Deep-Sea Research II 54 (16–17): 1864–1875. Bibcode:2007DSR....54.1864J. doi:10.1016/j.dsr2.2007.07.012. 

• Markhaseva E.L. & Schulz K. (2006). "Sensiava longiseta (Copepoda, calanoidea): a new genus and species from the abyssal of the Weddell Sea". Zootaxa (1368): 1–18. 

• Mühlenhardt-Siegel U. (2008). "Phalloleucon abyssalis, a new cumacean genus and species (Crustacea: Peracarida: Leuconidae) from the Peru Basin". Zootaxa (1829). pp. 61–68.  |accessdate= requires |url= (help)

• Nozawa F., Kitazato H., Tsuchiya M. & Gooday A.J. (2006). "'Live' benthic foraminifera at an abyssal site in the equatorial Pacific nodule province: abundance, diversity and taxonomic composition". Deep-Sea Research I 53 (8): 1406–1422. Bibcode:2006DSRI...53.1406N. doi:10.1016/j.dsr.2006.06.001. 

• Sabbatini A., Morigi C., Negri A., & Gooday A.J. (2007). "DISTRIBUTION AND BIODIVERSITY OF STAINED MONOTHALAMOUS FORAMINIFERA FROM TEMPELFJORD, SVALBARD". Journal of Foraminiferal Research 37 (2): 93–106. doi:10.2113/gsjfr.37.2.93. 

• Schrödl M., Linse K. & Schwabe E. (2006). "Review on the distribution and biology of Antarctic Monoplacophora, with first abyssal record of Laevipilina antarctica". Polar Biology 29 (9): 721–727. doi:10.1007/s00300-006-0132-7. 

• Schwabe E., Bohn J.M., Engl W., Linse K. & Schrödl M. (2007). "Rich and rare - first insights into species diversity and abundance of Antarctic abyssal Gastropoda (Mollusca)". Deep-Sea Research II 54 (16–17): 1831–1847. Bibcode:2007DSR....54.1831S. doi:10.1016/j.dsr2.2007.07.010. 

• Sebastian S., Raes M., De Mesel I. & Vanreusel A. (2007). "Comparison of the nematode fauna from the Weddell Sea Abyssal Plain with two North Atlantic abyssal sites". Deep-Sea Research II 54 (16–17): 1727–1736. Bibcode:2007DSR....54.1727S. doi:10.1016/j.dsr2.2007.07.004. 

• Seifried S., Plum Ch. & Schulz M. (2007). "A new species of Parabradya Lang, 1944 (Copepoda: Harpacticoida: Ectinosomatidae) from the abyssal plain of the Angola Basin". Zootaxa (1432): 1–21. 

• Robert H. Stewart (2007). Introduction to Physical Oceanography (PDF). College Station: Texas A&M University. ISBN 1-61610-045-1. OCLC 169907785. 

• Willen E. (2005). "A new species of Paranannopus Lang, 1936 (Copepoda, Harpacticoida, Pseudotachidiidae) with atrophic mouthparts from the abyssal of the Angola Basin". Organisms, Diversity & Evolution 5 (Supplement 1): 19–27. doi:10.1016/j.ode.2004.10.002. 

• Yasuhara M., Cronin T.M. & Martinez Arbizu P. (2008). "Abyssal ostracods from the South and Equatorial Atlantic Ocean: biological and paleoceanographic implications". Deep-Sea Research I 55 (4): 490–497. Bibcode:2008DSRI...55..490Y. doi:10.1016/j.dsr.2008.01.004. 

External links

• Monterey Bay Aquarium Research Institute (3 November 2009). "Deep-sea Ecosystems Affected By Climate Change". ScienceDaily. Retrieved 27 June 2010. 

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