Life in the World's Oceans 2010
DOI: 10.1002/9781444325508.ch8
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Diversity of Abyssal Marine Life

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Cited by 26 publications
(24 citation statements)
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“…This is not surprising; deep-sea biology is a fairly young discipline. Only a decade ago a typical survey of the abyssal plains and basins (54% of Earth's surface) would typically find that 90% of the infaunal species collected were new to science (Ebbe et al, 2010). This staggering figure has changed little for groups like nematodes, isopods, and copepods (Seifried, 2004;Ebbe et al, 2010), some of the most abundant components of deep-sea benthic diversity.…”
Section: Discussionmentioning
confidence: 99%
“…This is not surprising; deep-sea biology is a fairly young discipline. Only a decade ago a typical survey of the abyssal plains and basins (54% of Earth's surface) would typically find that 90% of the infaunal species collected were new to science (Ebbe et al, 2010). This staggering figure has changed little for groups like nematodes, isopods, and copepods (Seifried, 2004;Ebbe et al, 2010), some of the most abundant components of deep-sea benthic diversity.…”
Section: Discussionmentioning
confidence: 99%
“…The regions of ocean crust where slopes and ridge flanks flatten out represent perhaps the single largest contiguous feature of our planet and also the least explored: the extensive abyssal plains (Smith et al, 2008;Ebbe et al, 2010). Abyssal sediments consist of terrigenous particles derived from rock weathering on land as well as biological particles produced in the surface layers by plancktonic organisms.…”
Section: The Great Expanse: Abyssal Plainsmentioning
confidence: 99%
“…The Clarion-Clipperton fracture zone (CCZ) in the equatorial North Pacific is a focal area for mining interests, and mining operations are expected to be initiated in the CCZ by 2025 [10]. The CCZ is estimated to contain 340 million tonnes of nickel and 265 million tonnes of copper [8]. Mining of abyssal manganese nodules will affect large areas of the seafloor owing to direct mining disturbance (estimated scales of 300-600 km 2 per year) and re-deposition from sediment plumes (over scales of 10-100 km from the mining site; see [11][12][13][14]).…”
Section: Introductionmentioning
confidence: 99%
“…The seabed is characterized by a number of unique habitats and ecosystem types, including abyssal plains, seamounts, hydrothermal vents and cold seeps [1,5,6]. In addition, commercially valuable mineral resources, including nickel-and copper-rich manganese nodules and cobalt-rich crusts, are also present in these environments [7,8]. Recent advances in technological capabilities have led to competing spatial demands between conservation of the unique deep-sea ecosystems and economic mining interests.…”
Section: Introductionmentioning
confidence: 99%