AUTHOR=Vander Zanden Hannah B. , Soto David X. , Bowen Gabriel J. , Hobson Keith A. 

TITLE=Expanding the Isotopic Toolbox: Applications of Hydrogen and Oxygen Stable Isotope Ratios to Food Web Studies

JOURNAL=Frontiers in Ecology and Evolution

VOLUME=4

YEAR=2016

URL=https://www.frontiersin.org/journals/ecology-and-evolution/articles/10.3389/fevo.2016.00020

DOI=10.3389/fevo.2016.00020

ISSN=2296-701X

ABSTRACT=<p>The measurement of stable carbon (δ<sup>13</sup>C) and nitrogen (δ<sup>15</sup>N) isotopes in tissues of organisms has formed the foundation of isotopic food web reconstructions, as these values directly reflect assimilated diet. In contrast, stable hydrogen (δ<sup>2</sup>H) and oxygen (δ<sup>18</sup>O) isotope measurements have typically been reserved for studies of migratory origin and paleoclimate reconstruction based on systematic relationships between organismal tissue and local environmental water. Recently, innovative applications using δ<sup>2</sup>H and, to a lesser extent, δ<sup>18</sup>O values have demonstrated potential for these elements to provide novel insights in modern food web studies. We explore the advantages and challenges associated with three applications of δ<sup>2</sup>H and δ<sup>18</sup>O values in food web studies. First, large δ<sup>2</sup>H differences between aquatic and terrestrial ecosystem end members can permit the quantification of energy inputs and nutrient fluxes between these two sources, with potential applications for determining allochthonous vs. autochthonous nutrient sources in freshwater systems and relative aquatic habitat utilization by terrestrial organisms. Next, some studies have identified a relationship between δ<sup>2</sup>H values and trophic position, which suggests that this marker may serve as a trophic indicator, in addition to the more commonly used δ<sup>15</sup>N values. Finally, coupled measurements of δ<sup>2</sup>H and δ<sup>18</sup>O values are increasing as a result of reduced analytical challenges to measure both simultaneously and may provide additional ecological information over single element measurements. In some organisms, the isotopic ratios of these two elements are tightly coupled, whereas the isotopic disequilibrium in other organisms may offer insight into the diet and physiology of individuals. Although a coherent framework for interpreting δ<sup>2</sup>H and δ<sup>18</sup>O data in the context of food web studies is emerging, many fundamental uncertainties remain. We highlight directions for targeted research that will increase our understanding of how these markers move through food webs and reflect ecological processes.</p>