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 core f...

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Main Authors: 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, Theodore R., Harris, M. Scott, Pyne-O'Donnell, Sean
Other Authors: Asian School of the Environment
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Language:English
Published: 2020
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Online Access:https://hdl.handle.net/10356/136997
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spelling sg-ntu-dr.10356-1369972020-09-26T21:24:24Z 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, Theodore R. Harris, M. Scott Pyne-O'Donnell, Sean Asian School of the Environment Earth Observatory of Singapore Science::Geology Limnology Paleosol 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. Published version 2020-02-11T05:49:07Z 2020-02-11T05:49:07Z 2019 Journal Article Moore, C. R., Brooks, M. J., Goodyear, A. C., Ferguson, T. A., Perrotti, A. G., Mitra, S., ... Pyne-O’Donnell, S. (2019). Sediment cores from White Pond, South Carolina, contain a Platinum Anomaly, Pyrogenic Carbon Peak, and Coprophilous Spore Decline at 12.8 ka. Scientific Reports, 9(1). doi:10.1038/s41598-019-51552-8 2045-2322 https://hdl.handle.net/10356/136997 10.1038/s41598-019-51552-8 31641142 2-s2.0-85073755265 1 9 en Scientific reports © 2019 The Author(s). This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/. application/pdf
institution Nanyang Technological University
building NTU Library
country Singapore
collection DR-NTU
language English
topic Science::Geology
Limnology
Paleosol
spellingShingle Science::Geology
Limnology
Paleosol
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, 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
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.
author2 Asian School of the Environment
author_facet Asian School of the Environment
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, Theodore R.
Harris, M. Scott
Pyne-O'Donnell, Sean
format Article
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, 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 2020
url https://hdl.handle.net/10356/136997
_version_ 1681056037986107392