Census of Diversity of Abyssal Marine Life

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Census of Diversity of Abyssal Marine Life
AbbreviationCeDAMar
Formation2003 (2003)
TypeBiological census
Headquarters Naturmuseum Senckenberg
Region served
Abyssal plain
Leader
  • Dr. Pedro Martinez Arbizu
  • Dr. Craig Smith
Parent organization
Census of Marine Life
Website www.cedamar.org

The Census of Diversity of Abyssal Marine Life (CeDAMar) is a field project of the Census of Marine Life that studies the species diversity of one of the largest and most inaccessible environments on the planet, the abyssal plain. CeDAMar uses data to create an estimation of global species diversity and provide a better understanding of the history of deep-sea fauna, including its present diversity and dependence on environmental parameters. CeDAMar initiatives aim to identify centers of high biodiversity useful for planning both commercial and conservation efforts, and are able to be used in future studies on the effects of climate change on the deep sea. [1]

As of May 2009, participation by upwards of 56 institutions [2] in 17 countries has resulted in the publication of nearly 300 papers. [3] Results of CeDAMar-related research were also published in a 2010 textbook on deep-sea biodiversity by Michael Rex and Ron Etter, members of CeDAMar's Scientific Steering Committee.( ISBN   978-0674036079)

CeDAMar is led by Dr. Pedro Martinez Arbizu of Germany and Dr. Craig Smith, USA.

Related Research Articles

Biodiversity Variety and variability of life forms

Biodiversity or biological diversity is the variety and variability of life on Earth. Biodiversity is a measure of variation at the genetic, species, and ecosystem level.

Gastropoda Class of molluscs

The gastropods, commonly known as snails and slugs, belong to a large taxonomic class of invertebrates within the phylum Mollusca called Gastropoda.

Benthic zone Ecological region at the lowest level of a body of water

The benthic zone is the ecological region at the lowest level of a body of water such as an ocean, lake, or stream, including the sediment surface and some sub-surface layers. The name comes from ancient Greek, βένθος (bénthos), meaning "the depths." Organisms living in this zone are called benthos and include microorganisms as well as larger invertebrates, such as crustaceans and polychaetes. Organisms here generally live in close relationship with the substrate and many are permanently attached to the bottom. The benthic boundary layer, which includes the bottom layer of water and the uppermost layer of sediment directly influenced by the overlying water, is an integral part of the benthic zone, as it greatly influences the biological activity that takes place there. Examples of contact soil layers include sand bottoms, rocky outcrops, coral, and bay mud.

Abyssal plain Flat area on the deep ocean floor

An abyssal plain is an underwater plain on the deep ocean floor, usually found at depths between 3,000 metres (9,800 ft) and 6,000 metres (20,000 ft). Lying generally between the foot of a continental rise and a mid-ocean ridge, abyssal plains cover more than 50% of the Earth's surface. They are among the flattest, smoothest, and least explored regions on Earth. Abyssal plains are key geologic elements of oceanic basins.

Seabed The bottom of the ocean

The seabed is the bottom of the ocean. All floors of the ocean are known as 'seabeds'.

Whale fall Whale carcass falling to the ocean floor

A whale fall occurs when the carcass of a whale has fallen onto the ocean floor at a depth greater than 1,000 m (3,300 ft), in the bathyal or abyssal zones. On the sea floor, these carcasses can create complex localized ecosystems that supply sustenance to deep-sea organisms for decades. This is unlike in shallower waters, where a whale carcass will be consumed by scavengers over a relatively short period of time. Whale falls were first observed in the late 1970s with the development of deep-sea robotic exploration. Since then, several natural and experimental whale falls have been monitored through the use of observations from submersibles and remotely operated underwater vehicles (ROVs) in order to understand patterns of ecological succession on the deep seafloor.

The hadal zone, also known as the hadopelagic zone, is the deepest region of the ocean, lying within oceanic trenches. The hadal zone ranges from around 6 to 11 km below sea level, and exists in long, narrow, topographic V-shaped depressions.

The deep sea or deep layer is the lowest layer in the ocean, existing below the thermocline and above the seabed, at a depth of 1,000 fathoms or more. Little or no light penetrates this part of the ocean, and most of the organisms that live there rely for subsistence on falling organic matter produced in the photic zone. For this reason, scientists once assumed that life would be sparse in the deep ocean, but virtually every probe has revealed that, on the contrary, life is abundant in the deep ocean.

Census of Marine Life

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Philippe Bouchet French biologist

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Angelika Brandt German deep-sea biologist

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Katrin Linse British zoologist

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J. Frederick Grassle American oceanographer and academic

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Imants Priede

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References

  1. "CeDAMar on COML". Archived from the original on 2010-09-26. Retrieved 2010-09-24.
  2. "Census of the Diversity of Abyssal Marine Life (CeDAMar) - Welcome to the deep sea! - Participating Institutes". Archived from the original on 2011-04-25. Retrieved 2010-09-24.
  3. "CeDAMar". Archived from the original on 2010-09-14. Retrieved 2010-09-24.