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BG | Articles | Volume 16, issue 21
Biogeosciences, 16, 4183–4199, 2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
Biogeosciences, 16, 4183–4199, 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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Cited articles

Alve, E.: Opportunistic features of the foraminifer Stainforthia fusiformis (Williamson): evidence from Frierfjord, Norway, J. Micropalaeontol., 13, 24–24,, 1994. 
Alve, E.: Benthic foraminiferal responses to estuarine pollution; a review, J. Foramin. Res., 25, 190–203,, 1995. 
Alve, E.: A common opportunistic foraminiferal species as an indicator of rapidly changing conditions in a range of environments, Estuar. Coast. Shelf S., 57, 501–514,, 2003. 
Alve, E. and Murray, J. W.: High benthic fertility and taphonomy of foraminifera: A case study of the Skagerrak, North Sea, Mar. Micropaleontol., 31, 157–175,, 1997. 
Alve, E. and Murray, J. W.: Marginal marine environments of the Skagerrak and Kattegat: A baseline study of living (stained) benthic foraminiferal ecology, Palaeogeogr. Palaeocl., 146, 171–193,, 1999. 
Publications Copernicus
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...
Final-revised paper