Silicate weathering and carbon cycle controls on the Oligocene-Miocene transition glaciation
Changes in both silicate weathering rates and organic carbon burial have been proposed as drivers of the transient “Mi-1” glaciation event at the Oligocene-Miocene transition (OMT; ~23 Ma). However detailed geochemical proxy data are required to test these hypotheses. Here we present records of Li/C...
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Online Access: | https://oro.open.ac.uk/51664/ https://oro.open.ac.uk/51664/2/Stewart_et_al-2017-Paleoceanography.pdf https://doi.org/10.1002/2017PA003115 |
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ftopenunivgb:oai:oro.open.ac.uk:51664 2023-06-11T04:06:38+02:00 Silicate weathering and carbon cycle controls on the Oligocene-Miocene transition glaciation Stewart, Joseph A. James, Rachael H. Anand, Pallavi Wilson, Paul A. 2017 application/pdf https://oro.open.ac.uk/51664/ https://oro.open.ac.uk/51664/2/Stewart_et_al-2017-Paleoceanography.pdf https://doi.org/10.1002/2017PA003115 unknown https://oro.open.ac.uk/51664/2/Stewart_et_al-2017-Paleoceanography.pdf Stewart, Joseph A.; James, Rachael H.; Anand, Pallavi <http://oro.open.ac.uk/view/person/pa2398.html> and Wilson, Paul A. (2017). Silicate weathering and carbon cycle controls on the Oligocene-Miocene transition glaciation. Paleoceanography, 32(10) pp. 1070–1085. Journal Item Public PeerReviewed 2017 ftopenunivgb https://doi.org/10.1002/2017PA003115 2023-05-28T05:56:14Z Changes in both silicate weathering rates and organic carbon burial have been proposed as drivers of the transient “Mi-1” glaciation event at the Oligocene-Miocene transition (OMT; ~23 Ma). However detailed geochemical proxy data are required to test these hypotheses. Here we present records of Li/Ca, Mg/Ca, Cd/Ca, U/Ca, δ 18 O, δ 13 C, and shell weight in planktonic foraminifera from marine sediments spanning the OMT in the equatorial Atlantic Ocean. Li/Ca values increase by 1 μmol/mol across this interval. We interpret this to indicate a ~20% increase in silicate weathering rates, which would have lowered atmospheric CO 2 , potentially forcing the Antarctic glaciation circa 23 Ma. δ 13 C of thermocline dwelling planktonic foraminifera track the global increase in seawater δ 13 C across the OMT and during the Mi-1 event, hence supporting a hypothesized global increase in organic carbon burial rates. High δ 13 C previously measured in epipelagic planktonic foraminifera and high Cd/Ca ratios during Mi-1 are interpreted to represent locally enhanced primary productivity, stimulated by increased nutrients supply to surface waters. The fingerprint of high export production and associated organic carbon burial at this site is found in reduced bottom water oxygenation (inferred from high foraminiferal U/Ca), and enhanced respiratory dissolution of carbonates, characterised by reduced foraminiferal shell weight. Replication of our results elsewhere would strengthen the case that weathering-induced CO 2 sequestration preconditioned climate for Antarctic ice sheet growth across the OMT and increased burial of organic carbon acted as a feedback that intensified cooling at this time. Article in Journal/Newspaper Antarc* Antarctic Ice Sheet Planktonic foraminifera The Open University: Open Research Online (ORO) Antarctic The Antarctic Paleoceanography 32 10 1070 1085 |
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Open Polar |
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The Open University: Open Research Online (ORO) |
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ftopenunivgb |
language |
unknown |
description |
Changes in both silicate weathering rates and organic carbon burial have been proposed as drivers of the transient “Mi-1” glaciation event at the Oligocene-Miocene transition (OMT; ~23 Ma). However detailed geochemical proxy data are required to test these hypotheses. Here we present records of Li/Ca, Mg/Ca, Cd/Ca, U/Ca, δ 18 O, δ 13 C, and shell weight in planktonic foraminifera from marine sediments spanning the OMT in the equatorial Atlantic Ocean. Li/Ca values increase by 1 μmol/mol across this interval. We interpret this to indicate a ~20% increase in silicate weathering rates, which would have lowered atmospheric CO 2 , potentially forcing the Antarctic glaciation circa 23 Ma. δ 13 C of thermocline dwelling planktonic foraminifera track the global increase in seawater δ 13 C across the OMT and during the Mi-1 event, hence supporting a hypothesized global increase in organic carbon burial rates. High δ 13 C previously measured in epipelagic planktonic foraminifera and high Cd/Ca ratios during Mi-1 are interpreted to represent locally enhanced primary productivity, stimulated by increased nutrients supply to surface waters. The fingerprint of high export production and associated organic carbon burial at this site is found in reduced bottom water oxygenation (inferred from high foraminiferal U/Ca), and enhanced respiratory dissolution of carbonates, characterised by reduced foraminiferal shell weight. Replication of our results elsewhere would strengthen the case that weathering-induced CO 2 sequestration preconditioned climate for Antarctic ice sheet growth across the OMT and increased burial of organic carbon acted as a feedback that intensified cooling at this time. |
format |
Article in Journal/Newspaper |
author |
Stewart, Joseph A. James, Rachael H. Anand, Pallavi Wilson, Paul A. |
spellingShingle |
Stewart, Joseph A. James, Rachael H. Anand, Pallavi Wilson, Paul A. Silicate weathering and carbon cycle controls on the Oligocene-Miocene transition glaciation |
author_facet |
Stewart, Joseph A. James, Rachael H. Anand, Pallavi Wilson, Paul A. |
author_sort |
Stewart, Joseph A. |
title |
Silicate weathering and carbon cycle controls on the Oligocene-Miocene transition glaciation |
title_short |
Silicate weathering and carbon cycle controls on the Oligocene-Miocene transition glaciation |
title_full |
Silicate weathering and carbon cycle controls on the Oligocene-Miocene transition glaciation |
title_fullStr |
Silicate weathering and carbon cycle controls on the Oligocene-Miocene transition glaciation |
title_full_unstemmed |
Silicate weathering and carbon cycle controls on the Oligocene-Miocene transition glaciation |
title_sort |
silicate weathering and carbon cycle controls on the oligocene-miocene transition glaciation |
publishDate |
2017 |
url |
https://oro.open.ac.uk/51664/ https://oro.open.ac.uk/51664/2/Stewart_et_al-2017-Paleoceanography.pdf https://doi.org/10.1002/2017PA003115 |
geographic |
Antarctic The Antarctic |
geographic_facet |
Antarctic The Antarctic |
genre |
Antarc* Antarctic Ice Sheet Planktonic foraminifera |
genre_facet |
Antarc* Antarctic Ice Sheet Planktonic foraminifera |
op_relation |
https://oro.open.ac.uk/51664/2/Stewart_et_al-2017-Paleoceanography.pdf Stewart, Joseph A.; James, Rachael H.; Anand, Pallavi <http://oro.open.ac.uk/view/person/pa2398.html> and Wilson, Paul A. (2017). Silicate weathering and carbon cycle controls on the Oligocene-Miocene transition glaciation. Paleoceanography, 32(10) pp. 1070–1085. |
op_doi |
https://doi.org/10.1002/2017PA003115 |
container_title |
Paleoceanography |
container_volume |
32 |
container_issue |
10 |
container_start_page |
1070 |
op_container_end_page |
1085 |
_version_ |
1768378668871057408 |