J
Jeffrey A. Dorale
Researcher at University of Iowa
Publications - 32
Citations - 5162
Jeffrey A. Dorale is an academic researcher from University of Iowa. The author has contributed to research in topics: Stalagmite & Speleothem. The author has an hindex of 19, co-authored 32 publications receiving 4663 citations. Previous affiliations of Jeffrey A. Dorale include University of Minnesota & University of Missouri.
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A High-Resolution Absolute-Dated Late Pleistocene Monsoon Record from Hulu Cave, China
Yongjin Wang,Yongjin Wang,Hai Cheng,Richard Lawrence Edwards,Zhisheng An,Jiangying Wu,Chuan-Chou Shen,Jeffrey A. Dorale +7 more
TL;DR: The record links North Atlantic climate with the meridional transport of heat and moisture from the warmest part of the ocean where the summer East Asian Monsoon originates and generally agrees with the timing of temperature changes from the Greenland Ice Sheet Project Two (GISP2).
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Uranium and thorium isotopic and concentration measurements by magnetic sector inductively coupled plasma mass spectrometry
Chuan-Chou Shen,R. Lawrence Edwards,Hai Cheng,Jeffrey A. Dorale,R. B. Thomas,S. Bradley Moran,S. E. Weinstein,H. N. Edmonds +7 more
TL;DR: In this article, sector-field inductively coupled plasma mass spectrometry (ICP-MS) was used to measure the isotopic composition and concentration of uranium and thorium, focusing on the rare isotopes, 230Th and 234U.
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Uranium-series Chronology and Environmental Applications of Speleothems
David Richards,Jeffrey A. Dorale +1 more
TL;DR: Speleothems are bodies of mineral material formed in caves as the result of chemical precipitation from groundwater flowing or dripping in a cave as discussed by the authors, and they can be found in many locations of the globe, sampled at high-resolution and reliably dated using high-precision uranium series techniques.
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Climate and vegetation history of the midcontinent from 75 to 25 ka: A speleothem record from crevice cave, missouri, USA
TL;DR: The thorium-230-dated records reveal that between 75 and 55 ka, the midcontinental climate oscillated on millennial time scales between cold and warm, and vegetation alternated among forest, savanna, and prairie.
Journal ArticleDOI
A high-resolution record of holocene climate change in speleothem calcite from cold water cave, northeast iowa.
Jeffrey A. Dorale,Luis A. González,Mark K. Reagan,David A. Pickett,Michael T. Murrell,Richard G. Baker +5 more
TL;DR: In this paper, high-precision uranium-thorium mass spectrometric chronology and (18)O-(13)C isotopic analysis of speleothem calcite from Cold Water Cave in northeast Iowa have been used to chart mid-Holocene climate change.