2015
DOI: 10.1016/j.pocean.2015.03.003
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Migrant biomass and respiratory carbon flux by zooplankton and micronekton in the subtropical northeast Atlantic Ocean (Canary Islands)

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Cited by 80 publications
(66 citation statements)
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“…data), probably carnivore species, by Lobianchia species ( i.e. L. dofleini 43% of the diet: Ariza et al , ). Estimates of mesopelagic fish trophic levels indicated that these species feed through a continuum spanning the third trophic level, in general agreement with the findings of Cherel et al () and Flynn & Kloser (), limited to lanternfishes, from the Southern Ocean.…”
Section: Discussionmentioning
confidence: 97%
“…data), probably carnivore species, by Lobianchia species ( i.e. L. dofleini 43% of the diet: Ariza et al , ). Estimates of mesopelagic fish trophic levels indicated that these species feed through a continuum spanning the third trophic level, in general agreement with the findings of Cherel et al () and Flynn & Kloser (), limited to lanternfishes, from the Southern Ocean.…”
Section: Discussionmentioning
confidence: 97%
“…Oligotrophic waters dominate in the western sector [23] while upwelling near the North African coast and its interaction with the Canary Current and the islands favors the existence of diverse habitats in the transition from the highly productive shelf waters to the oceanic region [24,25]. Additional environmental variability is provided by the influence of diazotrophy (atmospheric nitrogen fixation) in the subtropical region, generally more important in the western waters but occasionally affecting also waters near Canary Islands [26][27][28][29][30]. Zooplankton composition and biomass in this region reflect the productivity of the surface waters (for example, References [21,25]) and previous studies on the vertical migrations of zooplankton [12,25] and mesopelagic fish [31] showed a measurable impact of these movements on carbon fluxes and export to deep ocean layers.…”
Section: Introductionmentioning
confidence: 99%
“…Nevertheless, they have been considered to play only a minor role in the global biogeochemical cycles in the oceans because their biomass is much smaller than that of bacteria and zooplankton (Conover, 1978;del Giorgio and Duarte, 2002). Recent studies, however, suggest that carbon exported downward by the respiration, defecation and mortality of micronektonic fishes and squids that undertake diel vertical migration between the epipelagic and mesopelagic zones can contribute much to the total downward carbon flux, e.g., 26-54% in the western equatorial Pacific Ocean (Hidaka et al, 2001), 15-17% in the northeastern Pacific Ocean (Davison et al, 2013), and 12-32% in the subtropical Atlantic Ocean (Ariza et al, 2015).…”
Section: Introductionmentioning
confidence: 99%