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Geographic patterns of soft-bottoms benthic communities in Chilean Patagonian fjords (47°S-54°S)-influence of environmental stress on diversity patterns and stable isotope signatures

Journal

PROGRESS IN OCEANOGRAPHY
Volume 204, Issue -, Pages -

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.pocean.2022.102810

Keywords

Glaciomarine and glaciofluvial environments; Organismal stable isotopes; C; N ratios

Categories

Funding

  1. National Oceanographic Committee (CONA-CHILE) [CONA-C23F-1709, C25F 19-05]
  2. Research Department of the PUCV [DII-PUCV 223.730/2016]
  3. COPAS Sur-Austral ANID [AFB170006]
  4. COPAS COASTAL [FB210021]

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The benthic community in the Chilean Patagonia is affected by environmental stressors such as glacier melt and river discharge, which result in changes in its diversity and trophic structure.
The benthic community in the Chilean Patagonia is as rich and highly diverse as the spatial variation of its habitats and food sources. Environmental stress from glacier melt and river discharge are known drivers of benthic community dynamics. Here, we analyze longitudinal patterns of soft-bottom benthic communities across transects of glacier-marine environments and how these habitats may respond to changes in the environmental conditions. To assess the relationships between environmental heterogeneity (marine and glacial habitats) and benthic biodiversity, this paper reviews biological (mega- and macroinfauna) and sedimentological dataset from multiple oceanographic campaigns in Chilean Patagonian fjords. Furthermore, we analyze isotopic compositions of epibenthic and macroinfaunal organisms (613C/615N and C/N) to determine particulate organic carbon (POC) and particulate organic nitrogen (PON) availability and organismal stoichiometric budgets within each benthic community. Our results showed that glaciomarine and glaciofluvial environmental stress negatively affected nutrient reservoirs and organic matter (OM) availability, and hence produced changes in benthic diversity and trophic structure throughout the fjords. These conditions shaped the benthic community where small-bodied polychaetes and opportunistic species dominated. Additionally, we found a strong relationship between OM and nutrient availability with faunal isotopic composition, but a decoupling in C/N ratios between fauna and sediment OM, suggesting preferential organic carbon use under limited nitrogen in fjord sediments.

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