Tracing carbon sources through aquatic and terrestrial food webs using amino acid stable isotope fingerprinting.

Tracing the origin of nutrients is a fundamental goal of food web research but methodological issues associated with current research techniques such as using stable isotope ratios of bulk tissue can lead to confounding results. We investigated whether naturally occurring δ(13)C patterns among amino...

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Main Authors: Thomas Larsen, Marc Ventura, Nils Andersen, Diane M O'Brien, Uwe Piatkowski, Matthew D McCarthy
Format: Article
Language:English
Published: Public Library of Science (PLoS) 2013-01-01
Series:PLoS ONE
Online Access:http://europepmc.org/articles/PMC3775739?pdf=render
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spelling doaj-1dd7506948fb465694474ff2c8a2189b2020-11-24T20:40:21ZengPublic Library of Science (PLoS)PLoS ONE1932-62032013-01-0189e7344110.1371/journal.pone.0073441Tracing carbon sources through aquatic and terrestrial food webs using amino acid stable isotope fingerprinting.Thomas LarsenMarc VenturaNils AndersenDiane M O'BrienUwe PiatkowskiMatthew D McCarthyTracing the origin of nutrients is a fundamental goal of food web research but methodological issues associated with current research techniques such as using stable isotope ratios of bulk tissue can lead to confounding results. We investigated whether naturally occurring δ(13)C patterns among amino acids (δ(13)CAA) could distinguish between multiple aquatic and terrestrial primary production sources. We found that δ(13)CAA patterns in contrast to bulk δ(13)C values distinguished between carbon derived from algae, seagrass, terrestrial plants, bacteria and fungi. Furthermore, we showed for two aquatic producers that their δ(13)CAA patterns were largely unaffected by different environmental conditions despite substantial shifts in bulk δ(13)C values. The potential of assessing the major carbon sources at the base of the food web was demonstrated for freshwater, pelagic, and estuarine consumers; consumer δ(13)C patterns of essential amino acids largely matched those of the dominant primary producers in each system. Since amino acids make up about half of organismal carbon, source diagnostic isotope fingerprints can be used as a new complementary approach to overcome some of the limitations of variable source bulk isotope values commonly encountered in estuarine areas and other complex environments with mixed aquatic and terrestrial inputs.http://europepmc.org/articles/PMC3775739?pdf=render
collection DOAJ
language English
format Article
sources DOAJ
author Thomas Larsen
Marc Ventura
Nils Andersen
Diane M O'Brien
Uwe Piatkowski
Matthew D McCarthy
spellingShingle Thomas Larsen
Marc Ventura
Nils Andersen
Diane M O'Brien
Uwe Piatkowski
Matthew D McCarthy
Tracing carbon sources through aquatic and terrestrial food webs using amino acid stable isotope fingerprinting.
PLoS ONE
author_facet Thomas Larsen
Marc Ventura
Nils Andersen
Diane M O'Brien
Uwe Piatkowski
Matthew D McCarthy
author_sort Thomas Larsen
title Tracing carbon sources through aquatic and terrestrial food webs using amino acid stable isotope fingerprinting.
title_short Tracing carbon sources through aquatic and terrestrial food webs using amino acid stable isotope fingerprinting.
title_full Tracing carbon sources through aquatic and terrestrial food webs using amino acid stable isotope fingerprinting.
title_fullStr Tracing carbon sources through aquatic and terrestrial food webs using amino acid stable isotope fingerprinting.
title_full_unstemmed Tracing carbon sources through aquatic and terrestrial food webs using amino acid stable isotope fingerprinting.
title_sort tracing carbon sources through aquatic and terrestrial food webs using amino acid stable isotope fingerprinting.
publisher Public Library of Science (PLoS)
series PLoS ONE
issn 1932-6203
publishDate 2013-01-01
description Tracing the origin of nutrients is a fundamental goal of food web research but methodological issues associated with current research techniques such as using stable isotope ratios of bulk tissue can lead to confounding results. We investigated whether naturally occurring δ(13)C patterns among amino acids (δ(13)CAA) could distinguish between multiple aquatic and terrestrial primary production sources. We found that δ(13)CAA patterns in contrast to bulk δ(13)C values distinguished between carbon derived from algae, seagrass, terrestrial plants, bacteria and fungi. Furthermore, we showed for two aquatic producers that their δ(13)CAA patterns were largely unaffected by different environmental conditions despite substantial shifts in bulk δ(13)C values. The potential of assessing the major carbon sources at the base of the food web was demonstrated for freshwater, pelagic, and estuarine consumers; consumer δ(13)C patterns of essential amino acids largely matched those of the dominant primary producers in each system. Since amino acids make up about half of organismal carbon, source diagnostic isotope fingerprints can be used as a new complementary approach to overcome some of the limitations of variable source bulk isotope values commonly encountered in estuarine areas and other complex environments with mixed aquatic and terrestrial inputs.
url http://europepmc.org/articles/PMC3775739?pdf=render
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