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What global biogeochemical consequences will marine animal–sediment interactions have during climate change

Bibliographic Data

ID19568765
AuthorsThomas S Bianchi (0000-0002-3068-2933, University of Florida), Robert C Aller (0000-0003-4360-8406, Stony Brook University), Trisha B Atwood (0000-0001-7153-5190, Utah State University), Craig J Brown (0000-0002-5125-978X, Dalhousie University), Luis A Buatois (0000-0001-9523-750X, University of Saskatchewan), Lisa A Levin (0000-0002-2858-8622, Scripps Institution of Oceanography), Jeffrey S Levinton (0000-0001-7149-224X, Stony Brook University), Jack J Middelburg (0000-0003-3601-9072, Utrecht University), Elise S Morrison (0000-0003-2569-4259, University of Florida), Pierre Regnier (0000-0002-4531-0868, Université Libre de Bruxelles), Michael R Shields (0000-0002-6194-2689, Texas A&M University), P V R Snelgrove (0000-0002-6725-0472, Memorial University of Newfoundland), Erik E Sotka (0000-0001-5167-8549, College of Charleston), Ryan R E Stanley (0000-0002-6313-0844, Fisheries and Oceans Canada)
Year2021
Volume9
Issue1
Publication date2021-06-08
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueElementa Science of the Anthropocene (JOURNAL)
Journal identifiersISSN: 2325-1026 • E-ISSN: 2325-1026
PublisherUniversity of California Press (PUBLISHER • US)
DOI10.1525/elementa.2020.00180
OpenAlexW3172218008
LanguageEN
Citations received1
References cited180

Benthic animals profoundly influence the cycling and storage of carbon and other elements in marine systems, particularly in coastal sediments. Recent climate change has altered the distribution and abundance of many seafloor taxa and modified the vertical exchange of materials between ocean and sediment layers. Here, we examine how climate change could alter animal-mediated biogeochemical cycling in ocean sediments. The fossil record shows repeated major responses from the benthos during mass extinctions and global carbon perturbations, including reduced diversity, dominance of simple trace fossils, decreased burrow size and bioturbation intensity, and nonrandom extinction of trophic groups. The broad dispersal capacity of many extant benthic species facilitates poleward shifts corresponding to their environmental niche as overlying water warms. Evidence suggests that locally persistent populations will likely respond to environmental shifts through either failure to respond or genetic adaptation rather than via phenotypic plasticity. Regional and global ocean models insufficiently integrate changes in benthic biological activity and their feedbacks on sedimentary biogeochemical processes. The emergence of bioturbation, ventilation, and seafloor-habitat maps and progress in our mechanistic understanding of organism–sediment interactions enable incorporation of potential effects of climate change on benthic macrofaunal mediation of elemental cycles into regional and global ocean biogeochemical models

Benthic zone · Biogeochemical cycle · Biology · Bioturbation · Climate change · Environmental change · Sediment · Environmental Science · Isotope Analysis in Ecology · Marine and coastal ecosystems · Marine Biology and Ecology Research · Ecology · Geology · Oceanography · Paleontology

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Unique citing works1
Citations per year1
Citation span2025 - 2025 (1)
Citation velocityrecent
Highly citedNo
Citation typesNeutral: 1

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