Abstract
The structure, functioning and dynamics of polar marine ecosystems are strongly influenced by the extent of sea ice. Ice algae and pelagic phytoplankton represent the primary sources of nutrition for higher trophic-level organisms in seasonally ice-covered areas, but their relative contributions to polar marine consumers remain largely unexplored. Here, we investigated the potential of diatom-specific lipid markers and highly branched isoprenoids (HBIs) for estimating the importance of these two carbon pools in an Antarctic pelagic ecosystem. Using GC-MS analysis, we studied HBI biomarkers in key marine species over three years in Adélie Land, Antarctica: euphausiids (ice krill Euphausia crystallorophias and Antarctic krill E. superba), fish (bald notothens Pagothenia borchgrevinki and Antarctic silverfish Pleuragramma antarcticum) and seabirds (Adélie penguins Pygoscelis adeliae, snow petrels Pagodroma nivea and cape petrels Daption capense). This study provides the first evidence of the incorporation of HBI lipids in Antarctic pelagic consumers. Specifically, a di-unsaturated HBI (diene) of sea ice origin was more abundant in ice-associated species than in pelagic species, whereas a tri-unsaturated HBI (triene) of phytoplanktonic origin was more abundant in pelagic species than in ice-associated species. Moreover, the relative abundances of diene and triene in seabird tissues and eggs were higher during a year of good sea ice conditions than in a year of poor ice conditions. In turn, the higher contribution of ice algal derived organic matter to the diet of seabirds was related to earlier breeding and higher breeding success. HBI biomarkers are a promising tool for estimating the contribution of organic matter derived from ice algae in pelagic consumers from Antarctica.
Highlights
Shrinking sea ice threatens the structure, functioning and dynamics of polar marine ecosystems [1,2,3]
The aim of the present study was to evaluate the potential of some novel lipid markers, highly branched isoprenoids (HBIs), for estimating the contribution of organic matter derived from ice algae in pelagic consumers from Antarctica
The present study provides the first evidence that diatom HBI biomarkers are transferred across an Antarctic pelagic ecosystem up to higher trophic levels
Summary
Shrinking sea ice threatens the structure, functioning and dynamics of polar marine ecosystems [1,2,3]. At the base of the polar marine trophic web, some micro-algae, primarily pennate diatoms, bloom under and within sea ice in the spring [4,5,6]. A second source of primary production is pelagic phytoplankton, which bloom during the summer ice melts. Several attempts have been made to estimate the relative contribution of ice algae and phytoplankton to primary production in Arctic and Antarctic waters [5,9]. Ice algae are a significant (direct or indirect) source of nutrition for zooplankton, krill, fish, seabirds and marine mammals [6], their relative contribution to polar marine ecosystems remains poorly understood. A method to trace carbon flow through Arctic marine trophic webs by analysing the stable isotopes of fatty acids was proposed [10]
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