2016
DOI: 10.3389/fmars.2016.00252
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Patterns in Stable Isotope Values of Nitrogen and Carbon in Particulate Matter from the Northwest Atlantic Continental Shelf, from the Gulf of Maine to Cape Hatteras

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Cited by 40 publications
(34 citation statements)
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“…Multiple data points in the same location were averaged using the mean isotopic value. Known latitudinal and longitudinal gradients in δ 13 C and δ 15 N for phytoplankton, particulate organic matter (POM) and dissolved organic matter (POM) were used as a visual guide to inform the spatial interpretation of skate isotope values (Bauer et al 2001, McKinney et al 2010, Oczkowski et al 2016, Magozzi et al 2017.…”
Section: Discussionmentioning
confidence: 99%
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“…Multiple data points in the same location were averaged using the mean isotopic value. Known latitudinal and longitudinal gradients in δ 13 C and δ 15 N for phytoplankton, particulate organic matter (POM) and dissolved organic matter (POM) were used as a visual guide to inform the spatial interpretation of skate isotope values (Bauer et al 2001, McKinney et al 2010, Oczkowski et al 2016, Magozzi et al 2017.…”
Section: Discussionmentioning
confidence: 99%
“…Food webs associated with the continental shelf of the NW Atlantic are predominantly supported by pelagic phytoplankton-based primary production, although fluvial production from land run-off may provide additional allochthonous sources of production to proximate regions from the coastline (Oczkowski et al 2016). A number of studies have revealed a relatively distinct spatial pattern in pelagic phytoplankton, POM, and DOM, with regards to δ 13 C and δ 15 N (Bauer et al 2001, McKinney et al 2010, Oczkowski et al 2016, Magozzi et al 2017. Patterns are assumed to be driven by various biogeochemical mechanisms such as temperature (Goericke and Fry 1994, Lara et al 2010, Magozzi et al 2017, dissolved carbon dioxide concentrations (i.e.…”
Section: Discussionmentioning
confidence: 99%
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“…However, the defining of end‐member isotope values is an unsettled issue (Kandasamy et al, ; Miller et al, ). Earlier studies have indicated that the δ 13 C of planktonic OM in the coastal region widely varied from the inner to the outer shelf, with less negative δ 13 C and high δ 15 N in the inner shelf (Liu et al, ; Miller & Page, ; Oczkowski et al, ). This suggests the difficulty in addressing carbon sources in the marine environment based on δ 13 C values alone.…”
Section: Introductionmentioning
confidence: 99%