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Speleothem Paleoclimatology for the Caribbean, Central America, and North America

Bibliographic Data

ID15801867
AuthorsJessica Oster (0000-0002-1780-2435, Vanderbilt University, corresponding author), Sophie Warken (0000-0003-3293-9074, Heidelberg University), Sophie F Warken (0000-0002-3339-1488, Department of Geosciences, University of Heidelberg, 69120 Heidelberg, Germany), Natasha Sekhon (0000-0002-4513-2301, The University of Texas at Austin), Monica M Arienzo (0000-0003-3444-9810, Desert Research Institute), Matthew S Lachniet (0000-0001-5250-0144, University of Nevada, Las Vegas)
Year2019
Volume2
Issue1
Pages5-5
Publication date2019-01-28
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueQuaternary (JOURNAL)
Journal identifiersISSN: 2571-550X • E-ISSN: 2571-550X
PublisherMultidisciplinary Digital Publishing Institute (PUBLISHER • CH)
DOI10.3390/quat2010005
OpenAlexW2909876377
LanguageEN
Citations received6
References cited159

Speleothem oxygen isotope records from the Caribbean, Central, and North America reveal climatic controls that include orbital variation, deglacial forcing related to ocean circulation and ice sheet retreat, and the influence of local and remote sea surface temperature variations. Here, we review these records and the global climate teleconnections they suggest following the recent publication of the Speleothem Isotopes Synthesis and Analysis (SISAL) database. We find that low-latitude records generally reflect changes in precipitation, whereas higher latitude records are sensitive to temperature and moisture source variability. Tropical records suggest precipitation variability is forced by orbital precession and North Atlantic Ocean circulation driven changes in atmospheric convection on long timescales, and tropical sea surface temperature variations on short timescales. On millennial timescales, precipitation seasonality in southwestern North America is related to North Atlantic climate variability. Great Basin speleothem records are closely linked with changes in Northern Hemisphere summer insolation. Although speleothems have revealed these critical global climate teleconnections, the paucity of continuous records precludes our ability to investigate climate drivers from the whole of Central and North America for the Pleistocene through modern. This underscores the need to improve spatial and temporal coverage of speleothem records across this climatically variable region

Cave · Climate change · Climatology · Geography · Northern Hemisphere · Paleoclimatology · Precipitation · Sea surface temperature · Speleothem · Teleconnection · Cryospheric studies and observations · Geology and Paleoclimatology Research · Pleistocene-Era Hominins and Archaeology · Geology · Oceanography

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Unique citing works6
Citations per year0,86
Citation span2019 - 2024 (6)
Citation velocityrecent
Highly citedNo
Citation typesNeutral: 5

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