Meter-Scale Early Diagenesis of Organic Matter Buried Within Deep-Sea Sediments Beneath the Amazon River Plume
Gravity cores and multi-cores were collected from the Demerara Abyssal plain to examine meter-scale downcore features of early diagenesis in the sediments and relate them to the location of the Amazon River plume in the North Atlantic Ocean. At all sites, the oxygen penetration depth, inferred from...
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ftdoajarticles:oai:doaj.org/article:593e5f64eecd4e1ea116ce328ec491e1 2023-05-15T17:33:51+02:00 Meter-Scale Early Diagenesis of Organic Matter Buried Within Deep-Sea Sediments Beneath the Amazon River Plume Lauren S. Chong William M. Berelson James McManus Nick E. Rollins 2018-07-01T00:00:00Z https://doi.org/10.3389/fmars.2018.00250 https://doaj.org/article/593e5f64eecd4e1ea116ce328ec491e1 EN eng Frontiers Media S.A. https://www.frontiersin.org/article/10.3389/fmars.2018.00250/full https://doaj.org/toc/2296-7745 2296-7745 doi:10.3389/fmars.2018.00250 https://doaj.org/article/593e5f64eecd4e1ea116ce328ec491e1 Frontiers in Marine Science, Vol 5 (2018) carbon diagenesis nitrogen manganese iron biogenic silica sedimentation Science Q General. Including nature conservation geographical distribution QH1-199.5 article 2018 ftdoajarticles https://doi.org/10.3389/fmars.2018.00250 2022-12-31T00:39:16Z Gravity cores and multi-cores were collected from the Demerara Abyssal plain to examine meter-scale downcore features of early diagenesis in the sediments and relate them to the location of the Amazon River plume in the North Atlantic Ocean. At all sites, the oxygen penetration depth, inferred from nitrate and dissolved manganese profiles, was ~10–20 cm and nitrate was depleted within ~50 cm. However, most of the cores also had a secondary nitrate maximum (4–13 μM) at ~50 cm, at a location where we observed changes in gradients of dissolved manganese, iron, and ammonium. Although there is spatial heterogeneity in the profile behavior across the study, we do find subtle diagenetic profile patterns that occur in sediments in relation to their position below the Amazon plume. Dissolved silica profiles show an initial increase downcore, but then all show a decrease to depths of 30–100 cm, thereafter concentrations increase. We suggest this zone of silica uptake is due to reverse weathering processes, possibly involving iron oxidation. A semi-lithified iron crust appeared at nearly all sites, and its position is relict, likely an indicator of the transition from glacial to interglacial sediments. Article in Journal/Newspaper North Atlantic Directory of Open Access Journals: DOAJ Articles Frontiers in Marine Science 5 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
carbon diagenesis nitrogen manganese iron biogenic silica sedimentation Science Q General. Including nature conservation geographical distribution QH1-199.5 |
spellingShingle |
carbon diagenesis nitrogen manganese iron biogenic silica sedimentation Science Q General. Including nature conservation geographical distribution QH1-199.5 Lauren S. Chong William M. Berelson James McManus Nick E. Rollins Meter-Scale Early Diagenesis of Organic Matter Buried Within Deep-Sea Sediments Beneath the Amazon River Plume |
topic_facet |
carbon diagenesis nitrogen manganese iron biogenic silica sedimentation Science Q General. Including nature conservation geographical distribution QH1-199.5 |
description |
Gravity cores and multi-cores were collected from the Demerara Abyssal plain to examine meter-scale downcore features of early diagenesis in the sediments and relate them to the location of the Amazon River plume in the North Atlantic Ocean. At all sites, the oxygen penetration depth, inferred from nitrate and dissolved manganese profiles, was ~10–20 cm and nitrate was depleted within ~50 cm. However, most of the cores also had a secondary nitrate maximum (4–13 μM) at ~50 cm, at a location where we observed changes in gradients of dissolved manganese, iron, and ammonium. Although there is spatial heterogeneity in the profile behavior across the study, we do find subtle diagenetic profile patterns that occur in sediments in relation to their position below the Amazon plume. Dissolved silica profiles show an initial increase downcore, but then all show a decrease to depths of 30–100 cm, thereafter concentrations increase. We suggest this zone of silica uptake is due to reverse weathering processes, possibly involving iron oxidation. A semi-lithified iron crust appeared at nearly all sites, and its position is relict, likely an indicator of the transition from glacial to interglacial sediments. |
format |
Article in Journal/Newspaper |
author |
Lauren S. Chong William M. Berelson James McManus Nick E. Rollins |
author_facet |
Lauren S. Chong William M. Berelson James McManus Nick E. Rollins |
author_sort |
Lauren S. Chong |
title |
Meter-Scale Early Diagenesis of Organic Matter Buried Within Deep-Sea Sediments Beneath the Amazon River Plume |
title_short |
Meter-Scale Early Diagenesis of Organic Matter Buried Within Deep-Sea Sediments Beneath the Amazon River Plume |
title_full |
Meter-Scale Early Diagenesis of Organic Matter Buried Within Deep-Sea Sediments Beneath the Amazon River Plume |
title_fullStr |
Meter-Scale Early Diagenesis of Organic Matter Buried Within Deep-Sea Sediments Beneath the Amazon River Plume |
title_full_unstemmed |
Meter-Scale Early Diagenesis of Organic Matter Buried Within Deep-Sea Sediments Beneath the Amazon River Plume |
title_sort |
meter-scale early diagenesis of organic matter buried within deep-sea sediments beneath the amazon river plume |
publisher |
Frontiers Media S.A. |
publishDate |
2018 |
url |
https://doi.org/10.3389/fmars.2018.00250 https://doaj.org/article/593e5f64eecd4e1ea116ce328ec491e1 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Frontiers in Marine Science, Vol 5 (2018) |
op_relation |
https://www.frontiersin.org/article/10.3389/fmars.2018.00250/full https://doaj.org/toc/2296-7745 2296-7745 doi:10.3389/fmars.2018.00250 https://doaj.org/article/593e5f64eecd4e1ea116ce328ec491e1 |
op_doi |
https://doi.org/10.3389/fmars.2018.00250 |
container_title |
Frontiers in Marine Science |
container_volume |
5 |
_version_ |
1766132492871401472 |