Sediment Cores from White Pond, South Carolina, contain a Platinum Anomaly, Pyrogenic Carbon Peak, and Coprophilous Spore Decline at 12.8 ka
A widespread platinum (Pt) anomaly was recently documented in Greenland ice and 11 North American sedimentary sequences at the onset of the Younger Dryas (YD) event (~12,800 cal yr BP), consistent with the YD Impact Hypothesis. We report high-resolution analyses of a 1-meter section of a lake co...
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fteastcaroluni:oai:TheScholarship.intra.ecu.edu:10342/8324 2023-05-15T16:29:40+02:00 Sediment Cores from White Pond, South Carolina, contain a Platinum Anomaly, Pyrogenic Carbon Peak, and Coprophilous Spore Decline at 12.8 ka Moore, Christopher R. Brooks, Mark J. Goodyear, Albert C. Ferguson, Terry A. Perrotti, Angelina G. Mitra, Siddhartha Listecki, Ashlyn M. King, Bailey C. Mallinson, David J. Lane, Chad S. Kapp, Joshua D. West, Allen Carlson, David L. Wolbach, Wendy S. Them II, Theodore R. Harris, M. Scott Pyne-O’Donnell, Sean 2019-09-27 application/pdf http://hdl.handle.net/10342/8324 https://doi.org/10.1038/s41598-019-51552-8 unknown http://hdl.handle.net/10342/8324 doi:10.1038/s41598-019-51552-8 Article 2019 fteastcaroluni https://doi.org/10.1038/s41598-019-51552-8 2022-07-11T11:41:23Z A widespread platinum (Pt) anomaly was recently documented in Greenland ice and 11 North American sedimentary sequences at the onset of the Younger Dryas (YD) event (~12,800 cal yr BP), consistent with the YD Impact Hypothesis. We report high-resolution analyses of a 1-meter section of a lake core from White Pond, South Carolina, USA. After developing a Bayesian age-depth model that brackets the late Pleistocene through early Holocene, we analyzed and quantified the following: (1) Pt and palladium (Pd) abundance, (2) geochemistry of 58 elements, (3) coprophilous spores, (4) sedimentary organic matter (OC and sedaDNA), (5) stable isotopes of C (δ13C) and N (δ15N), (6) soot, (7) aciniform carbon, (8) cryptotephra, (9) mercury (Hg), and (10) magnetic susceptibility. We identified large Pt and Pt/Pd anomalies within a 2-cm section dated to the YD onset (12,785 ± 58 cal yr BP). These anomalies precede a decline in coprophilous spores and correlate with an abrupt peak in soot and C/OC ratios, indicative of large-scale regional biomass burning. We also observed a relatively large excursion in δ15N values, indicating rapid climatic and environmental/hydrological changes at the YD onset. Our results are consistent with the YD Impact Hypothesis and impact-related environmental and ecological changes. Article in Journal/Newspaper Greenland East Carolina University: The ScholarShip at ECU Greenland White Pond ENVELOPE(-62.857,-62.857,82.452,82.452) Carbon Peak ENVELOPE(-122.636,-122.636,56.050,56.050) Scientific Reports 9 1 |
institution |
Open Polar |
collection |
East Carolina University: The ScholarShip at ECU |
op_collection_id |
fteastcaroluni |
language |
unknown |
description |
A widespread platinum (Pt) anomaly was recently documented in Greenland ice and 11 North American sedimentary sequences at the onset of the Younger Dryas (YD) event (~12,800 cal yr BP), consistent with the YD Impact Hypothesis. We report high-resolution analyses of a 1-meter section of a lake core from White Pond, South Carolina, USA. After developing a Bayesian age-depth model that brackets the late Pleistocene through early Holocene, we analyzed and quantified the following: (1) Pt and palladium (Pd) abundance, (2) geochemistry of 58 elements, (3) coprophilous spores, (4) sedimentary organic matter (OC and sedaDNA), (5) stable isotopes of C (δ13C) and N (δ15N), (6) soot, (7) aciniform carbon, (8) cryptotephra, (9) mercury (Hg), and (10) magnetic susceptibility. We identified large Pt and Pt/Pd anomalies within a 2-cm section dated to the YD onset (12,785 ± 58 cal yr BP). These anomalies precede a decline in coprophilous spores and correlate with an abrupt peak in soot and C/OC ratios, indicative of large-scale regional biomass burning. We also observed a relatively large excursion in δ15N values, indicating rapid climatic and environmental/hydrological changes at the YD onset. Our results are consistent with the YD Impact Hypothesis and impact-related environmental and ecological changes. |
format |
Article in Journal/Newspaper |
author |
Moore, Christopher R. Brooks, Mark J. Goodyear, Albert C. Ferguson, Terry A. Perrotti, Angelina G. Mitra, Siddhartha Listecki, Ashlyn M. King, Bailey C. Mallinson, David J. Lane, Chad S. Kapp, Joshua D. West, Allen Carlson, David L. Wolbach, Wendy S. Them II, Theodore R. Harris, M. Scott Pyne-O’Donnell, Sean |
spellingShingle |
Moore, Christopher R. Brooks, Mark J. Goodyear, Albert C. Ferguson, Terry A. Perrotti, Angelina G. Mitra, Siddhartha Listecki, Ashlyn M. King, Bailey C. Mallinson, David J. Lane, Chad S. Kapp, Joshua D. West, Allen Carlson, David L. Wolbach, Wendy S. Them II, Theodore R. Harris, M. Scott Pyne-O’Donnell, Sean Sediment Cores from White Pond, South Carolina, contain a Platinum Anomaly, Pyrogenic Carbon Peak, and Coprophilous Spore Decline at 12.8 ka |
author_facet |
Moore, Christopher R. Brooks, Mark J. Goodyear, Albert C. Ferguson, Terry A. Perrotti, Angelina G. Mitra, Siddhartha Listecki, Ashlyn M. King, Bailey C. Mallinson, David J. Lane, Chad S. Kapp, Joshua D. West, Allen Carlson, David L. Wolbach, Wendy S. Them II, Theodore R. Harris, M. Scott Pyne-O’Donnell, Sean |
author_sort |
Moore, Christopher R. |
title |
Sediment Cores from White Pond, South Carolina, contain a Platinum Anomaly, Pyrogenic Carbon Peak, and Coprophilous Spore Decline at 12.8 ka |
title_short |
Sediment Cores from White Pond, South Carolina, contain a Platinum Anomaly, Pyrogenic Carbon Peak, and Coprophilous Spore Decline at 12.8 ka |
title_full |
Sediment Cores from White Pond, South Carolina, contain a Platinum Anomaly, Pyrogenic Carbon Peak, and Coprophilous Spore Decline at 12.8 ka |
title_fullStr |
Sediment Cores from White Pond, South Carolina, contain a Platinum Anomaly, Pyrogenic Carbon Peak, and Coprophilous Spore Decline at 12.8 ka |
title_full_unstemmed |
Sediment Cores from White Pond, South Carolina, contain a Platinum Anomaly, Pyrogenic Carbon Peak, and Coprophilous Spore Decline at 12.8 ka |
title_sort |
sediment cores from white pond, south carolina, contain a platinum anomaly, pyrogenic carbon peak, and coprophilous spore decline at 12.8 ka |
publishDate |
2019 |
url |
http://hdl.handle.net/10342/8324 https://doi.org/10.1038/s41598-019-51552-8 |
long_lat |
ENVELOPE(-62.857,-62.857,82.452,82.452) ENVELOPE(-122.636,-122.636,56.050,56.050) |
geographic |
Greenland White Pond Carbon Peak |
geographic_facet |
Greenland White Pond Carbon Peak |
genre |
Greenland |
genre_facet |
Greenland |
op_relation |
http://hdl.handle.net/10342/8324 doi:10.1038/s41598-019-51552-8 |
op_doi |
https://doi.org/10.1038/s41598-019-51552-8 |
container_title |
Scientific Reports |
container_volume |
9 |
container_issue |
1 |
_version_ |
1766019366666633216 |