Late Pleistocene paleoclimate in the Black Hills of South Dakota from isotope records in speleothems
Two coeval speleothems from the Black Hills are used to investigate δ18O and δ13C variations within Reed’s Cave and reconstruct climate during the Wisconsin glacial period from 82 000 to 24 000 years ago. Variation in growth rates between the two speleothems reveals a strong control of hydrology and...
Published in: | Palaeogeography, Palaeoclimatology, Palaeoecology |
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2004
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Online Access: | https://digitalcommons.usf.edu/kip_articles/3093 https://doi.org/10.1016/S0031-0182(03)00639-4 |
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ftunisfloridatam:oai:digitalcommons.usf.edu:kip_articles-4092 2023-05-15T16:29:28+02:00 Late Pleistocene paleoclimate in the Black Hills of South Dakota from isotope records in speleothems Serefiddin, Feride Schwarcz, Henry P. Ford, Derek C. Baldwin, Steve 2004-01-01T08:00:00Z https://digitalcommons.usf.edu/kip_articles/3093 https://doi.org/10.1016/S0031-0182(03)00639-4 unknown Digital Commons @ University of South Florida https://digitalcommons.usf.edu/kip_articles/3093 https://doi.org/10.1016/S0031-0182(03)00639-4 KIP Articles Speleothems 18O/16O Black Hills Quaternary Stable Isotopes text 2004 ftunisfloridatam https://doi.org/10.1016/S0031-0182(03)00639-4 2022-10-27T17:52:40Z Two coeval speleothems from the Black Hills are used to investigate δ18O and δ13C variations within Reed’s Cave and reconstruct climate during the Wisconsin glacial period from 82 000 to 24 000 years ago. Variation in growth rates between the two speleothems reveals a strong control of hydrology and surface vegetation on isotopic variability and response of δ18O to climate. High-resolution δ18O and δ13C data show that local environmental conditions can produce an offset of δ18O values of up to 4‰ in coeval speleothems but still reveal important climate events. The transition from warmer to cooler periods results in an increase in δ18O of calcite (δ18Oct) in sample RC2 while in sample RC20, another equilibrium deposit coeval to part of the RC2 record, δ18Oct is offset from RC2 by between 0 and −3.5‰, and shows much higher frequency isotopic variation. Speleothem RC2 records interglacial/glacial transitions and interstadial events that are also present in speleothems from North America and Europe. Spectral analysis of the δ18Oct records for both speleothems reveals periodicity at 1000 to 2000 years, similar to millennial scale variability seen in the North Atlantic sediments and the Greenland ice cores. Text Greenland Greenland ice cores North Atlantic Digital Commons University of South Florida (USF) Greenland Black Hills ENVELOPE(-138.838,-138.838,63.466,63.466) Palaeogeography, Palaeoclimatology, Palaeoecology 203 1-2 1 17 |
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Open Polar |
collection |
Digital Commons University of South Florida (USF) |
op_collection_id |
ftunisfloridatam |
language |
unknown |
topic |
Speleothems 18O/16O Black Hills Quaternary Stable Isotopes |
spellingShingle |
Speleothems 18O/16O Black Hills Quaternary Stable Isotopes Serefiddin, Feride Schwarcz, Henry P. Ford, Derek C. Baldwin, Steve Late Pleistocene paleoclimate in the Black Hills of South Dakota from isotope records in speleothems |
topic_facet |
Speleothems 18O/16O Black Hills Quaternary Stable Isotopes |
description |
Two coeval speleothems from the Black Hills are used to investigate δ18O and δ13C variations within Reed’s Cave and reconstruct climate during the Wisconsin glacial period from 82 000 to 24 000 years ago. Variation in growth rates between the two speleothems reveals a strong control of hydrology and surface vegetation on isotopic variability and response of δ18O to climate. High-resolution δ18O and δ13C data show that local environmental conditions can produce an offset of δ18O values of up to 4‰ in coeval speleothems but still reveal important climate events. The transition from warmer to cooler periods results in an increase in δ18O of calcite (δ18Oct) in sample RC2 while in sample RC20, another equilibrium deposit coeval to part of the RC2 record, δ18Oct is offset from RC2 by between 0 and −3.5‰, and shows much higher frequency isotopic variation. Speleothem RC2 records interglacial/glacial transitions and interstadial events that are also present in speleothems from North America and Europe. Spectral analysis of the δ18Oct records for both speleothems reveals periodicity at 1000 to 2000 years, similar to millennial scale variability seen in the North Atlantic sediments and the Greenland ice cores. |
format |
Text |
author |
Serefiddin, Feride Schwarcz, Henry P. Ford, Derek C. Baldwin, Steve |
author_facet |
Serefiddin, Feride Schwarcz, Henry P. Ford, Derek C. Baldwin, Steve |
author_sort |
Serefiddin, Feride |
title |
Late Pleistocene paleoclimate in the Black Hills of South Dakota from isotope records in speleothems |
title_short |
Late Pleistocene paleoclimate in the Black Hills of South Dakota from isotope records in speleothems |
title_full |
Late Pleistocene paleoclimate in the Black Hills of South Dakota from isotope records in speleothems |
title_fullStr |
Late Pleistocene paleoclimate in the Black Hills of South Dakota from isotope records in speleothems |
title_full_unstemmed |
Late Pleistocene paleoclimate in the Black Hills of South Dakota from isotope records in speleothems |
title_sort |
late pleistocene paleoclimate in the black hills of south dakota from isotope records in speleothems |
publisher |
Digital Commons @ University of South Florida |
publishDate |
2004 |
url |
https://digitalcommons.usf.edu/kip_articles/3093 https://doi.org/10.1016/S0031-0182(03)00639-4 |
long_lat |
ENVELOPE(-138.838,-138.838,63.466,63.466) |
geographic |
Greenland Black Hills |
geographic_facet |
Greenland Black Hills |
genre |
Greenland Greenland ice cores North Atlantic |
genre_facet |
Greenland Greenland ice cores North Atlantic |
op_source |
KIP Articles |
op_relation |
https://digitalcommons.usf.edu/kip_articles/3093 https://doi.org/10.1016/S0031-0182(03)00639-4 |
op_doi |
https://doi.org/10.1016/S0031-0182(03)00639-4 |
container_title |
Palaeogeography, Palaeoclimatology, Palaeoecology |
container_volume |
203 |
container_issue |
1-2 |
container_start_page |
1 |
op_container_end_page |
17 |
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1766019162162855936 |