Further insights into how sediment redox status controls the preservation and composition of sedimentary biomarkers
Further insights into how sediment redox status controls the preservation and composition of sedimentary biomarkers
Sedimentary biomarker distributions can record ocean productivity and community structure, but their interpretation must consider alteration during organic matter (OM) export and burial. Large changes in the water column redox state are known to impact on the preservation of biomarkers, but more subtle variation in sediment redox conditions, characteristic of major modern ocean basins, have been less thoroughly investigated. Here we evaluate changes in biomarker distributions during sinking and burial across a nearshore to offshore transect in the southwestern Cape Basin (South East Atlantic), which includes a range of sedimentary environments. Biomarker concentrations and distributions in suspended particulate matter from the upper water column were determined and compared with underlying sedimentary biomarker accumulation rates and distributions. Biomarker distributions were similar in surface and subsurface waters, indicating that the OM signature is exported from the ocean mixed layer with minimal alteration. We show that, while export production (100 m) is similar along this transect, 230Thxs-corrected biomarker accumulation rate varies by over an order of magnitude in sediments and is directly associated with sedimentary redox conditions, ranging from oxic to nitrogenous-ferruginous. Biomarker distributions are dominated by sterols in surface water, and by alkenones in underlying sediments, which we propose to be primarily the result of selective preservation. Notably, the difference in sediment O2 penetration depth is associated with relative biomarker preservation. Subtle variation in sedimentary redox conditions has a dramatic impact on the distribution of preserved biomarkers. We discuss mechanisms for preferential degradation of specific biomarkers within this setting.
Biomarker preservation, Atlantic Ocean, Paleoproductivity proxies
220-234
Hernández-Sánchez, Maria T.
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LaRowe, Douglas E.
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Deng, Feifei
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Homoky, William B.
39da18e9-28b8-42c4-8e17-2cb66af8ee4d
Browning, Thomas J.
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Martin, Patrick
01ce1c59-3926-46c9-a556-fac39e0ee16b
Mills, Rachel A.
a664f299-1a34-4b63-9988-1e599b756706
Pancost, Richard D.
5914e19e-7777-4304-9fd8-86e2e9cfe8a1
November 2014
Hernández-Sánchez, Maria T.
16b5a9d7-d790-473a-b3a2-b6b133ee9ce3
LaRowe, Douglas E.
dc1ece0e-a3ea-428a-8bf7-fc2809b7f179
Deng, Feifei
4cffab76-0fb3-43d1-a3a9-359b6c023cb8
Homoky, William B.
39da18e9-28b8-42c4-8e17-2cb66af8ee4d
Browning, Thomas J.
5ca7f9b5-c1cd-493a-aed1-b371006a59e4
Martin, Patrick
01ce1c59-3926-46c9-a556-fac39e0ee16b
Mills, Rachel A.
a664f299-1a34-4b63-9988-1e599b756706
Pancost, Richard D.
5914e19e-7777-4304-9fd8-86e2e9cfe8a1
Hernández-Sánchez, Maria T., LaRowe, Douglas E., Deng, Feifei, Homoky, William B., Browning, Thomas J., Martin, Patrick, Mills, Rachel A. and Pancost, Richard D.
(2014)
Further insights into how sediment redox status controls the preservation and composition of sedimentary biomarkers.
Organic Geochemistry, 76, .
(doi:10.1016/j.orggeochem.2014.08.006).
Abstract
Sedimentary biomarker distributions can record ocean productivity and community structure, but their interpretation must consider alteration during organic matter (OM) export and burial. Large changes in the water column redox state are known to impact on the preservation of biomarkers, but more subtle variation in sediment redox conditions, characteristic of major modern ocean basins, have been less thoroughly investigated. Here we evaluate changes in biomarker distributions during sinking and burial across a nearshore to offshore transect in the southwestern Cape Basin (South East Atlantic), which includes a range of sedimentary environments. Biomarker concentrations and distributions in suspended particulate matter from the upper water column were determined and compared with underlying sedimentary biomarker accumulation rates and distributions. Biomarker distributions were similar in surface and subsurface waters, indicating that the OM signature is exported from the ocean mixed layer with minimal alteration. We show that, while export production (100 m) is similar along this transect, 230Thxs-corrected biomarker accumulation rate varies by over an order of magnitude in sediments and is directly associated with sedimentary redox conditions, ranging from oxic to nitrogenous-ferruginous. Biomarker distributions are dominated by sterols in surface water, and by alkenones in underlying sediments, which we propose to be primarily the result of selective preservation. Notably, the difference in sediment O2 penetration depth is associated with relative biomarker preservation. Subtle variation in sedimentary redox conditions has a dramatic impact on the distribution of preserved biomarkers. We discuss mechanisms for preferential degradation of specific biomarkers within this setting.
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Accepted/In Press date: 26 August 2014
Published date: November 2014
Keywords:
Biomarker preservation, Atlantic Ocean, Paleoproductivity proxies
Organisations:
Geochemistry
Identifiers
Local EPrints ID: 368389
URI: http://eprints.soton.ac.uk/id/eprint/368389
ISSN: 0146-6380
PURE UUID: 5637379f-e844-4cb7-8884-6fcc192ea323
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Date deposited: 27 Aug 2014 14:17
Last modified: 15 Mar 2024 02:46
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Author:
Maria T. Hernández-Sánchez
Author:
Douglas E. LaRowe
Author:
Feifei Deng
Author:
William B. Homoky
Author:
Thomas J. Browning
Author:
Patrick Martin
Author:
Richard D. Pancost
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