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Benthic-pelagic coupling in the Barents Sea: an integrated data-model framework
Freitas, F.S.; Hendry, K.R.; Henley, S.F.; Faust, J.C.; Tessin, A.C.; Stevenson, M.A.; Abbott, G.D.; März, C.; Arndt, S. (2020). Benthic-pelagic coupling in the Barents Sea: an integrated data-model framework. Philos. Trans. - Royal Soc., Math. Phys. Eng. Sci. 378(2181): 20190359. https://hdl.handle.net/10.1098/rsta.2019.0359
In: Philosophical Transactions - Royal Society. Mathematical, Physical and Engineering Sciences. Royal Society: London. ISSN 1364-503X; e-ISSN 1471-2962, meer
Peer reviewed article  
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Trefwoord
    Marien/Kust
Author keywords
    organic matter reactivity; degradation rates; nutrient fluxes; reaction-transport model; seafloor; continental shelf
Auteurs  Top 
  • Freitas, F.S., meer
  • Hendry, K.R.
  • Henley, S.F.
  • Faust, J.C.
  • Tessin, A.C.
  • Stevenson, M.A.
  • Abbott, G.D.
  • März, C.
  • Arndt, S., meer
Abstract
    The Barents Sea is experiencing long-term climate-driven changes, e.g. modification in oceanographic conditions and extensive sea ice loss, which can lead to large, yet unquantified disruptions to ecosystem functioning. This key region hosts a large fraction of Arctic primary productivity. However, processes governing benthic and pelagic coupling are not mechanistically understood, limiting our ability to predict the impacts of future perturbations. We combine field observations with a reaction-transport model approach to quantify organic matter (OM) processing and disentangle its drivers. Sedimentary OM reactivity patterns show no gradients relative to sea ice extent, being mostly driven by seafloor spatial heterogeneity. Burial of high reactivity, marine-derived OM is evident at sites influenced by Atlantic Water (AW), whereas low reactivity material is linked to terrestrial inputs on the central shelf. Degradation rates are mainly driven by aerobic respiration (40–75%), being greater at sites where highly reactive material is buried. Similarly, ammonium and phosphate fluxes are greater at those sites. The present-day AW-dominated shelf might represent the future scenario for the entire Barents Sea. Our results represent a baseline systematic understanding of seafloor geochemistry, allowing us to anticipate changes that could be imposed on the pan-Arctic in the future if climate-driven perturbations persist.
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