Analysis of an ancient global warming event, the Paleocene-Eocene thermal maximum, under examination from ODP Holes 113-689B and 113-690B ...
Spatiotemporal patterns of carbonate dissolution provide a critical constraint on carbon input during an ancient (~55.5 Ma) global warming event known as the Paleocene-Eocene thermal maximum (PETM), yet the magnitude of lysocline shoaling in the Southern Ocean is poorly constrained due to limited sp...
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ftdatacite:10.1594/pangaea.787773 2024-09-15T17:45:49+00:00 Analysis of an ancient global warming event, the Paleocene-Eocene thermal maximum, under examination from ODP Holes 113-689B and 113-690B ... Kelly, Daniel Clay Nielsen, Tina M J Schellenberg, Stephen A 2012 application/zip https://dx.doi.org/10.1594/pangaea.787773 https://doi.pangaea.de/10.1594/PANGAEA.787773 en eng PANGAEA https://dx.doi.org/10.1016/j.margeo.2012.02.003 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Ocean Drilling Program ODP article Collection Supplementary Publication Series of Datasets 2012 ftdatacite https://doi.org/10.1594/pangaea.78777310.1016/j.margeo.2012.02.003 2024-08-01T10:54:23Z Spatiotemporal patterns of carbonate dissolution provide a critical constraint on carbon input during an ancient (~55.5 Ma) global warming event known as the Paleocene-Eocene thermal maximum (PETM), yet the magnitude of lysocline shoaling in the Southern Ocean is poorly constrained due to limited spatial coverage in the circum-Antarctic region. This shortcoming is partially addressed by comparing patterns of carbonate sedimentation at the Site 690 PETM reference section to those herein reconstructed for nearby Site 689. Biochemostratigraphic correlation of the two records reveals that the first ~36 ka of the carbon isotope excursion (CIE) signaling PETM conditions is captured by the Site 689 section, while the remainder of the CIE interval and nearly all of the CIE recovery are missing due to a coring gap. A relatively expanded stratigraphy and higher carbonate content at mid-bathyal Site 689 indicate that dissolution was less severe than at Site 690. Thus, the bathymetric transect delimited by these two ... : Supplement to: Kelly, Daniel Clay; Nielsen, Tina M J; Schellenberg, Stephen A (2012): Carbonate saturation dynamics during the Paleocene-Eocene thermal maximum: Bathyal constraints from ODP sites 689 and 690 in the Weddell Sea (South Atlantic). Marine Geology, 303-306, 75-86 ... Article in Journal/Newspaper Antarc* Antarctic Southern Ocean Weddell Sea DataCite |
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English |
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Ocean Drilling Program ODP |
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Ocean Drilling Program ODP Kelly, Daniel Clay Nielsen, Tina M J Schellenberg, Stephen A Analysis of an ancient global warming event, the Paleocene-Eocene thermal maximum, under examination from ODP Holes 113-689B and 113-690B ... |
topic_facet |
Ocean Drilling Program ODP |
description |
Spatiotemporal patterns of carbonate dissolution provide a critical constraint on carbon input during an ancient (~55.5 Ma) global warming event known as the Paleocene-Eocene thermal maximum (PETM), yet the magnitude of lysocline shoaling in the Southern Ocean is poorly constrained due to limited spatial coverage in the circum-Antarctic region. This shortcoming is partially addressed by comparing patterns of carbonate sedimentation at the Site 690 PETM reference section to those herein reconstructed for nearby Site 689. Biochemostratigraphic correlation of the two records reveals that the first ~36 ka of the carbon isotope excursion (CIE) signaling PETM conditions is captured by the Site 689 section, while the remainder of the CIE interval and nearly all of the CIE recovery are missing due to a coring gap. A relatively expanded stratigraphy and higher carbonate content at mid-bathyal Site 689 indicate that dissolution was less severe than at Site 690. Thus, the bathymetric transect delimited by these two ... : Supplement to: Kelly, Daniel Clay; Nielsen, Tina M J; Schellenberg, Stephen A (2012): Carbonate saturation dynamics during the Paleocene-Eocene thermal maximum: Bathyal constraints from ODP sites 689 and 690 in the Weddell Sea (South Atlantic). Marine Geology, 303-306, 75-86 ... |
format |
Article in Journal/Newspaper |
author |
Kelly, Daniel Clay Nielsen, Tina M J Schellenberg, Stephen A |
author_facet |
Kelly, Daniel Clay Nielsen, Tina M J Schellenberg, Stephen A |
author_sort |
Kelly, Daniel Clay |
title |
Analysis of an ancient global warming event, the Paleocene-Eocene thermal maximum, under examination from ODP Holes 113-689B and 113-690B ... |
title_short |
Analysis of an ancient global warming event, the Paleocene-Eocene thermal maximum, under examination from ODP Holes 113-689B and 113-690B ... |
title_full |
Analysis of an ancient global warming event, the Paleocene-Eocene thermal maximum, under examination from ODP Holes 113-689B and 113-690B ... |
title_fullStr |
Analysis of an ancient global warming event, the Paleocene-Eocene thermal maximum, under examination from ODP Holes 113-689B and 113-690B ... |
title_full_unstemmed |
Analysis of an ancient global warming event, the Paleocene-Eocene thermal maximum, under examination from ODP Holes 113-689B and 113-690B ... |
title_sort |
analysis of an ancient global warming event, the paleocene-eocene thermal maximum, under examination from odp holes 113-689b and 113-690b ... |
publisher |
PANGAEA |
publishDate |
2012 |
url |
https://dx.doi.org/10.1594/pangaea.787773 https://doi.pangaea.de/10.1594/PANGAEA.787773 |
genre |
Antarc* Antarctic Southern Ocean Weddell Sea |
genre_facet |
Antarc* Antarctic Southern Ocean Weddell Sea |
op_relation |
https://dx.doi.org/10.1016/j.margeo.2012.02.003 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.78777310.1016/j.margeo.2012.02.003 |
_version_ |
1810493726854742016 |