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Biogeosciences An interactive open-access journal of the European Geosciences Union
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BG | Articles | Volume 16, issue 21
Biogeosciences, 16, 4183–4199, 2019
https://doi.org/10.5194/bg-16-4183-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
Biogeosciences, 16, 4183–4199, 2019
https://doi.org/10.5194/bg-16-4183-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 06 Nov 2019

Research article | 06 Nov 2019

Organic-carbon-rich sediments: benthic foraminifera as bio-indicators of depositional environments

Elena Lo Giudice Cappelli et al.

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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by editor) (17 Sep 2019) by Hiroshi Kitazato
AR by Elena Lo Giudice Cappelli on behalf of the Authors (18 Sep 2019)  Author's response    Manuscript
ED: Publish as is (25 Sep 2019) by Hiroshi Kitazato
Publications Copernicus
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Short summary
Fjords are known sinks of organic carbon (OC); however, little is known about the long-term fate of the OC stored in these sediments. The reason for this knowledge gap is the post-depositional degradation of OC. This study uses benthic foraminifera (microorganisms with calcite shells) to discriminate between post-depositional OC degradation and actual OC burial and accumulation in fjordic sediments, as foraminifera would only preserve the latter information in their assemblage composition.
Fjords are known sinks of organic carbon (OC); however, little is known about the long-term fate...
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