Organic Matter Sources in North Atlantic Fjord Sediments

To better constrain the global carbon cycle fundamental knowledge of the role of carbon cycling on continental margins is crucial. Fjords are particularly important shelf areas for carbon burial due to relatively high sedimentation rates and high organic matter fluxes. As terrigenous organic matter...

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Main Authors: Faust, JC, Knies, J
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 2019
Subjects:
Online Access:https://eprints.whiterose.ac.uk/153733/
https://eprints.whiterose.ac.uk/153733/1/Faust%20and%20Knies%202019%20G3.pdf
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spelling ftleedsuniv:oai:eprints.whiterose.ac.uk:153733 2023-05-15T16:03:48+02:00 Organic Matter Sources in North Atlantic Fjord Sediments Faust, JC Knies, J 2019-06 text https://eprints.whiterose.ac.uk/153733/ https://eprints.whiterose.ac.uk/153733/1/Faust%20and%20Knies%202019%20G3.pdf en eng American Geophysical Union https://eprints.whiterose.ac.uk/153733/1/Faust%20and%20Knies%202019%20G3.pdf Faust, JC orcid.org/0000-0001-8177-7097 and Knies, J (2019) Organic Matter Sources in North Atlantic Fjord Sediments. Geochemistry, Geophysics, Geosystems, 20 (6). pp. 2872-2885. ISSN 1525-2027 Article NonPeerReviewed 2019 ftleedsuniv 2023-01-30T22:24:30Z To better constrain the global carbon cycle fundamental knowledge of the role of carbon cycling on continental margins is crucial. Fjords are particularly important shelf areas for carbon burial due to relatively high sedimentation rates and high organic matter fluxes. As terrigenous organic matter is more resistant to remineralization than marine organic matter, a comprehensive knowledge of the carbon source is critical to better constrain the efficiency of organic carbon burial in fjord sediments. Here we investigated highly productive fjords in northern Norway and compare our results with both existing and new organic carbon to organic nitrogen ratios and carbon stable isotope compositions from fjords in mid‐Norway, west Svalbard, and east Greenland. The marine organic carbon contribution varies significantly between these fjords, and the contribution of marine organic carbon in Norwegian fjords is much larger than previously suggested for fjords in NW Europe and also globally. Additionally, northern Norwegian fjords show very high marine carbon burial rates (73.6 gC · m‐2 · year‐1) suggesting that these fjords are probably very distinct carbon burial hotspots. We argue that the North Atlantic Current inflow sustains these high burial rates and changes in the current strength due to ongoing climate change are likely to have a pronounced effect on carbon burial in North Atlantic fjords. Article in Journal/Newspaper East Greenland Greenland north atlantic current North Atlantic Northern Norway Svalbard White Rose Research Online (Universities of Leeds, Sheffield & York) Svalbard Greenland Norway
institution Open Polar
collection White Rose Research Online (Universities of Leeds, Sheffield & York)
op_collection_id ftleedsuniv
language English
description To better constrain the global carbon cycle fundamental knowledge of the role of carbon cycling on continental margins is crucial. Fjords are particularly important shelf areas for carbon burial due to relatively high sedimentation rates and high organic matter fluxes. As terrigenous organic matter is more resistant to remineralization than marine organic matter, a comprehensive knowledge of the carbon source is critical to better constrain the efficiency of organic carbon burial in fjord sediments. Here we investigated highly productive fjords in northern Norway and compare our results with both existing and new organic carbon to organic nitrogen ratios and carbon stable isotope compositions from fjords in mid‐Norway, west Svalbard, and east Greenland. The marine organic carbon contribution varies significantly between these fjords, and the contribution of marine organic carbon in Norwegian fjords is much larger than previously suggested for fjords in NW Europe and also globally. Additionally, northern Norwegian fjords show very high marine carbon burial rates (73.6 gC · m‐2 · year‐1) suggesting that these fjords are probably very distinct carbon burial hotspots. We argue that the North Atlantic Current inflow sustains these high burial rates and changes in the current strength due to ongoing climate change are likely to have a pronounced effect on carbon burial in North Atlantic fjords.
format Article in Journal/Newspaper
author Faust, JC
Knies, J
spellingShingle Faust, JC
Knies, J
Organic Matter Sources in North Atlantic Fjord Sediments
author_facet Faust, JC
Knies, J
author_sort Faust, JC
title Organic Matter Sources in North Atlantic Fjord Sediments
title_short Organic Matter Sources in North Atlantic Fjord Sediments
title_full Organic Matter Sources in North Atlantic Fjord Sediments
title_fullStr Organic Matter Sources in North Atlantic Fjord Sediments
title_full_unstemmed Organic Matter Sources in North Atlantic Fjord Sediments
title_sort organic matter sources in north atlantic fjord sediments
publisher American Geophysical Union
publishDate 2019
url https://eprints.whiterose.ac.uk/153733/
https://eprints.whiterose.ac.uk/153733/1/Faust%20and%20Knies%202019%20G3.pdf
geographic Svalbard
Greenland
Norway
geographic_facet Svalbard
Greenland
Norway
genre East Greenland
Greenland
north atlantic current
North Atlantic
Northern Norway
Svalbard
genre_facet East Greenland
Greenland
north atlantic current
North Atlantic
Northern Norway
Svalbard
op_relation https://eprints.whiterose.ac.uk/153733/1/Faust%20and%20Knies%202019%20G3.pdf
Faust, JC orcid.org/0000-0001-8177-7097 and Knies, J (2019) Organic Matter Sources in North Atlantic Fjord Sediments. Geochemistry, Geophysics, Geosystems, 20 (6). pp. 2872-2885. ISSN 1525-2027
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