Seafloor microplastic hotspots controlled by deep-sea circulation

Author:

Kane Ian A.1ORCID,Clare Michael A.2,Miramontes Elda34ORCID,Wogelius Roy1ORCID,Rothwell James J.5ORCID,Garreau Pierre6ORCID,Pohl Florian7ORCID

Affiliation:

1. School of Earth and Environmental Sciences, University of Manchester, Manchester M13 9PL, UK.

2. National Oceanography Centre, University of Southampton Waterfront Campus, Southampton SO14 3ZH, UK.

3. Faculty of Geosciences, University of Bremen, 28359 Bremen, Germany.

4. MARUM-Center for Marine Environmental Sciences, University of Bremen, 28359 Bremen, Germany.

5. Department of Geography, University of Manchester, Manchester M13 9PL, UK.

6. IFREMER, Univ. Brest, CNRS UMR 6523, IRD, Laboratoire d’Océanographie Physique et Spatiale (LOPS), IUEM, 29280, Plouzané, France.

7. Department of Earth Sciences, Durham University, Durham DH1 3LE, UK.

Abstract

Not just settling What controls the distribution of microplastics on the deep seafloor? Kane et al. show that the answer to that question is more complicated than particles simply settling from where they are found on the sea surface (see the Perspective by Mohrig). Using data that they collected off the coast of Corsica, the authors show that thermohaline-driven currents can control the distribution of microplastics by creating hotspots of accumulation, analogous to their role in causing focused areas of seafloor sediment deposition. Such currents also supply oxygen and nutrients to deep-sea benthos, so deepsea biodiversity hotspots are also likely to be microplastic hotspots. Science , this issue p. 1140 ; see also p. 1055

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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