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American Zoologist 2001 41(1):99-112; doi:10.1093/icb/41.1.99
© 2001 by The Society for Integrative and Comparative Biology
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{delta}15N and {delta}13C Measurements of Antarctic Peninsula Fauna: Trophic Relationships and Assimilation of Benthic Seaweeds1

Kenneth H. Dunton2,1
1 The University of Texas at Austin, Marine Science Institute, 750 Channel View Dr., Port Aransas, Texas 78373

Measurements of {delta}13C, {delta}15N, and C/N for a variety of Antarctic peninsula fauna and flora were used to quantify the importance of benthic brown algae to resident organisms and determine food web relationships among this diverse littoral fauna. {delta}13C values ranged from–16.8{per thousand} for benthic algal herbivores (limpets) to –29.8{per thousand} for the krill, Euphausia superba; the average pooled value for brown macroalgae, including their attached filamentous diatoms, was–20.6{per thousand}. There was no correlation between biomass {delta}13C or {delta}15N with C/N content, and consequently both {delta}13C and {delta}15N values were useful in evaluating trophic relationships. {delta}15N values of the fauna ranged from 3.1 to 12.5{per thousand}, with lowest values recorded in suspension feeders (e.g., bryozoans) and highest values in Adelie penguins (12.5{per thousand}) collected in 1989. The comparatively lower {delta}15N value for a Chinstrap penguin (6.9{per thousand}) collected in 1997 is attributed to the different dietary food sources consumed by these species as reflected in their respective {delta}13C values. Significant amounts of benthic macroalgal carbon is incorporated into the tissues of invertebrates and fishes that occupy up to four trophic levels. For many benthic and epibenthic species, including various crustaceans and molluscs, assimilation of benthic algal carbon through detrital pathways ranges from 30 to 100%. Consequently, the trophic importance of benthic brown algae may well extend to many pelagic organisms that are key prey species for birds, fishes, and marine mammals. These data support the hypothesis that benthic seaweeeds, together with their associated epiphytic diatoms, provide an important carbon source that is readily incorporated into Antarctic peninsula food webs.


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