2016
DOI: 10.1007/s00300-016-2041-8
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Latitudinal dependence of body condition, growth rate, and stable isotopes of juvenile capelin (Mallotus villosus) in the Bering and Chukchi Seas

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Cited by 5 publications
(2 citation statements)
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“…Therefore, in the marine environment, stable carbon isotope ratios (δ 13 C), can show differences between benthic and pelagic foragers, between near shore and offshore foragers and between freshwater and saltwater foragers [30][31][32]. Additionally, they can reflect latitudinal gradients across ocean basins [33,34]. Stable nitrogen isotope ratios (ratio of 15 N : 14 N isotopes in a tissue, with respect to an international standard) are considered a proxy for trophic level, as nitrogen isotopes experience metabolic fractionation as they move up the food chain from prey to predator [29,35,36].…”
Section: Stable Isotopesmentioning
confidence: 99%
“…Therefore, in the marine environment, stable carbon isotope ratios (δ 13 C), can show differences between benthic and pelagic foragers, between near shore and offshore foragers and between freshwater and saltwater foragers [30][31][32]. Additionally, they can reflect latitudinal gradients across ocean basins [33,34]. Stable nitrogen isotope ratios (ratio of 15 N : 14 N isotopes in a tissue, with respect to an international standard) are considered a proxy for trophic level, as nitrogen isotopes experience metabolic fractionation as they move up the food chain from prey to predator [29,35,36].…”
Section: Stable Isotopesmentioning
confidence: 99%
“…5). Эти вариации связаны с размером рыб и отражают различия в трофическом статусе отдельных размерных (возрастных) когорт сайки и мойвы [14,22]. Закономерные изменения изотопного состава азота и спектра питания по мере роста показаны на примере сайки (рис.…”
Section: материал и методыunclassified