A high-resolution speleothem record of climatic variability at the AllerÖd^Younger Dryas transition in Missouri, central United States
Stable isotopic analysis and 234U/230Th mass spectrometry dating of a single calcite stalagmite from Onondaga Cave, east-central Missouri, reveal climatic variability between 13 200 and 12 400 yr BP coincident with the AllerÖd^ Younger Dryas transition in the GISP2 Greenland ice cores. N18O values o...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.556.3998 2023-05-15T16:29:14+02:00 A high-resolution speleothem record of climatic variability at the AllerÖd^Younger Dryas transition in Missouri, central United States R. F. Denniston A L. A. Gonzalez B Y. Asmerom C V. Polyak C M. K. Reagan B M. R. Saltzman D The Pennsylvania State University CiteSeerX Archives 2001 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.556.3998 http://people.ku.edu/~lgonzlez/NewFiles/Publications/Dennistonetal01.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.556.3998 http://people.ku.edu/~lgonzlez/NewFiles/Publications/Dennistonetal01.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://people.ku.edu/~lgonzlez/NewFiles/Publications/Dennistonetal01.pdf Younger Dryas AllerÖd speleothem Missouri isotope text 2001 ftciteseerx 2016-01-08T11:47:47Z Stable isotopic analysis and 234U/230Th mass spectrometry dating of a single calcite stalagmite from Onondaga Cave, east-central Missouri, reveal climatic variability between 13 200 and 12 400 yr BP coincident with the AllerÖd^ Younger Dryas transition in the GISP2 Greenland ice cores. N18O values of speleothem calcite mark decreasing temperatures between 13 200 and 13 000 yr BP while more rapidly decreasing N13C values record a sharp shift toward C3 vegetation at approximately 13 100 yr BP. Because of uncertainties in the chronological control of both this speleothem and the GISP2 record and the brevity of this speleothem record (V800 years), direct comparison of the two sequences is difficult. The interval preserved by this speleothem may span the inter-AllerÖd cold period (IACP) alone, both the IACP and the start of the Younger Dryas, or only the first half of the Younger Dryas. In any case, these data demonstrate that the climate of the North American interior deteriorated significantly and rapidly during the interval Text Greenland Greenland ice cores Unknown Greenland |
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Open Polar |
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Unknown |
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ftciteseerx |
language |
English |
topic |
Younger Dryas AllerÖd speleothem Missouri isotope |
spellingShingle |
Younger Dryas AllerÖd speleothem Missouri isotope R. F. Denniston A L. A. Gonzalez B Y. Asmerom C V. Polyak C M. K. Reagan B M. R. Saltzman D A high-resolution speleothem record of climatic variability at the AllerÖd^Younger Dryas transition in Missouri, central United States |
topic_facet |
Younger Dryas AllerÖd speleothem Missouri isotope |
description |
Stable isotopic analysis and 234U/230Th mass spectrometry dating of a single calcite stalagmite from Onondaga Cave, east-central Missouri, reveal climatic variability between 13 200 and 12 400 yr BP coincident with the AllerÖd^ Younger Dryas transition in the GISP2 Greenland ice cores. N18O values of speleothem calcite mark decreasing temperatures between 13 200 and 13 000 yr BP while more rapidly decreasing N13C values record a sharp shift toward C3 vegetation at approximately 13 100 yr BP. Because of uncertainties in the chronological control of both this speleothem and the GISP2 record and the brevity of this speleothem record (V800 years), direct comparison of the two sequences is difficult. The interval preserved by this speleothem may span the inter-AllerÖd cold period (IACP) alone, both the IACP and the start of the Younger Dryas, or only the first half of the Younger Dryas. In any case, these data demonstrate that the climate of the North American interior deteriorated significantly and rapidly during the interval |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
R. F. Denniston A L. A. Gonzalez B Y. Asmerom C V. Polyak C M. K. Reagan B M. R. Saltzman D |
author_facet |
R. F. Denniston A L. A. Gonzalez B Y. Asmerom C V. Polyak C M. K. Reagan B M. R. Saltzman D |
author_sort |
R. F. Denniston A |
title |
A high-resolution speleothem record of climatic variability at the AllerÖd^Younger Dryas transition in Missouri, central United States |
title_short |
A high-resolution speleothem record of climatic variability at the AllerÖd^Younger Dryas transition in Missouri, central United States |
title_full |
A high-resolution speleothem record of climatic variability at the AllerÖd^Younger Dryas transition in Missouri, central United States |
title_fullStr |
A high-resolution speleothem record of climatic variability at the AllerÖd^Younger Dryas transition in Missouri, central United States |
title_full_unstemmed |
A high-resolution speleothem record of climatic variability at the AllerÖd^Younger Dryas transition in Missouri, central United States |
title_sort |
high-resolution speleothem record of climatic variability at the alleröd^younger dryas transition in missouri, central united states |
publishDate |
2001 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.556.3998 http://people.ku.edu/~lgonzlez/NewFiles/Publications/Dennistonetal01.pdf |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland Greenland ice cores |
genre_facet |
Greenland Greenland ice cores |
op_source |
http://people.ku.edu/~lgonzlez/NewFiles/Publications/Dennistonetal01.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.556.3998 http://people.ku.edu/~lgonzlez/NewFiles/Publications/Dennistonetal01.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766018922474110976 |