2010
DOI: 10.1016/j.dsr2.2010.02.018
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Mesopelagic zone ecology and biogeochemistry – a synthesis

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Cited by 272 publications
(215 citation statements)
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References 195 publications
(246 reference statements)
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“…The deep-scattering layer is a mid-water (200-1,000 m) mass of small fishes, cephalopods, crustaceans and zooplankton that provides a rich source and variety of prey items [28][29][30] . It should be possible for C. rupestris to feed there at a relatively high trophic level (and some data are consistent with this 31 ; Supplementary Fig.…”
Section: Nature Ecology and Evolutionmentioning
confidence: 99%
“…The deep-scattering layer is a mid-water (200-1,000 m) mass of small fishes, cephalopods, crustaceans and zooplankton that provides a rich source and variety of prey items [28][29][30] . It should be possible for C. rupestris to feed there at a relatively high trophic level (and some data are consistent with this 31 ; Supplementary Fig.…”
Section: Nature Ecology and Evolutionmentioning
confidence: 99%
“…This results in high bacterial growth at depth as a result of the decomposition of organic carbon in sinking particulate matter, yielding very low oxygen concentrations [19]. While species from many taxa (including copepods, euphausiids, cnidarians, ctenophores, fish and squid) live entirely or part of the time (during diel or ontogenetic vertical migrations) within the most pronounced OMZs [20,21], many organisms are stressed or die under hypoxic conditions [22], and overall abundance and species diversity are reduced. OMZs have dramatic effects on the spatial distribution patterns of animals in the water column, and zones of enhanced biological and biogeochemical activity exist at the OMZ's upper and lower boundaries [23,24].…”
Section: Introductionmentioning
confidence: 99%
“…The mesopelagic (200-1000 m) and bathypelagic (1000-4000 m) zones contain 470% of marine microbial biomass (Arıstegui et al, 2009) and these organisms have vital roles in global cycling of carbon, nitrogen and other biogeochemical processes (Nagata et al, 2010;Robinson et al, 2010). In addition to microorganisms necessarily being adapted to cold and increased pressure there, the deep sea also contains more recalcitrant forms of carbon than at the surface (Arıstegui et al, 2009;Nagata et al, 2010;Robinson et al, 2010).…”
Section: Introductionmentioning
confidence: 99%
“…The mesopelagic (200-1000 m) and bathypelagic (1000-4000 m) zones contain 470% of marine microbial biomass (Arıstegui et al, 2009) and these organisms have vital roles in global cycling of carbon, nitrogen and other biogeochemical processes (Nagata et al, 2010;Robinson et al, 2010). In addition to microorganisms necessarily being adapted to cold and increased pressure there, the deep sea also contains more recalcitrant forms of carbon than at the surface (Arıstegui et al, 2009;Nagata et al, 2010;Robinson et al, 2010). Cultivated isolates have revealed some microbial adaptations associated with life at depth, including increased intergenic spacer regions, rRNA gene indels and higher abundances of membrane polyunsaturated fatty acids and surface-adhesion/ motility genes (Simonato et al, 2006;Lauro and Bartlett, 2008;Wang et al, 2008;Nagata et al, 2010).…”
Section: Introductionmentioning
confidence: 99%