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Variation in zoobenthic blue carbon in the Arctic's Barents Sea shelf sediments

The flow of carbon from atmosphere to sediment fauna and sediments reduces atmospheric CO(2), which in turn reduces warming. Here, during the Changing Arctic Ocean Seafloor programme, we use comparable methods to those used in the Antarctic (vertical, calibrated camera drops and trawl-collected spec...

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Detalles Bibliográficos
Autores principales: Souster, T. A., Barnes, D. K. A., Hopkins, J.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: The Royal Society Publishing 2020
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7481665/
https://www.ncbi.nlm.nih.gov/pubmed/32862809
http://dx.doi.org/10.1098/rsta.2019.0362