High-resolution record of climate change in the Owens Lake Basin, California, for the period 52,500 to 12,500 YBP

EXTRACT (SEE PDF FOR FULL ABSTRACT):High-resolution oxygen-18 and total inorganic carbon (TIC) studies of cored sediments from the Owens Lake Basin, California, indicate that Owens Lake was hydrologically open (overflowing) most of the time between 52,500 and 12,500 carbon-14 YBP. . The lack of a st...

Full description

Bibliographic Details
Main Authors: Benson, Larry, Burdett, James, Kashgarian, Michaele, Lund, Steve, Rye, Robert
Format: Other/Unknown Material
Language:English
Published: 1996
Subjects:
Atmospheric Sciences
Chemistry
Earth Sciences
Limnology
PACLIM
hydrology
North Atlantic
Online Access:http://hdl.handle.net/1834/31628
id ftoceandocs:oai:aquadocs.org:1834/31628
record_format openpolar
spelling ftoceandocs:oai:aquadocs.org:1834/31628 2023-05-15T17:26:19+02:00 High-resolution record of climate change in the Owens Lake Basin, California, for the period 52,500 to 12,500 YBP Benson, Larry Burdett, James Kashgarian, Michaele Lund, Steve Rye, Robert 1996 application/pdf 217-230 http://hdl.handle.net/1834/31628 en eng http://hdl.handle.net/1834/31628 http://aquaticcommons.org/id/eprint/15814 8 2014-12-09 00:29:58 15814 Atmospheric Sciences Chemistry Earth Sciences Limnology PACLIM hydrology conference_item 1996 ftoceandocs 2023-04-06T17:04:27Z EXTRACT (SEE PDF FOR FULL ABSTRACT):High-resolution oxygen-18 and total inorganic carbon (TIC) studies of cored sediments from the Owens Lake Basin, California, indicate that Owens Lake was hydrologically open (overflowing) most of the time between 52,500 and 12,500 carbon-14 YBP. . The lack of a strong correspondence between North Atlantic climate records and the Owens Lake delta-oxygen-18 record has two possible explanations: (1) the sequence of large and abrupt climate change indicated in North Atlantic records is not global in scope and is largely confined to the North Atlantic and surrounding areas, or (2) Owens Lake is located in a part of the Great Basin that is relatively insensitive to the effects of climate perturbations recorded in the North Atlantic region. Other/Unknown Material North Atlantic IODE-UNESCO: OceanDocs - E-Repository of Ocean Publications
institution Open Polar
collection IODE-UNESCO: OceanDocs - E-Repository of Ocean Publications
op_collection_id ftoceandocs
language English
topic Atmospheric Sciences
Chemistry
Earth Sciences
Limnology
PACLIM
hydrology
spellingShingle Atmospheric Sciences
Chemistry
Earth Sciences
Limnology
PACLIM
hydrology
Benson, Larry
Burdett, James
Kashgarian, Michaele
Lund, Steve
Rye, Robert
High-resolution record of climate change in the Owens Lake Basin, California, for the period 52,500 to 12,500 YBP
topic_facet Atmospheric Sciences
Chemistry
Earth Sciences
Limnology
PACLIM
hydrology
description EXTRACT (SEE PDF FOR FULL ABSTRACT):High-resolution oxygen-18 and total inorganic carbon (TIC) studies of cored sediments from the Owens Lake Basin, California, indicate that Owens Lake was hydrologically open (overflowing) most of the time between 52,500 and 12,500 carbon-14 YBP. . The lack of a strong correspondence between North Atlantic climate records and the Owens Lake delta-oxygen-18 record has two possible explanations: (1) the sequence of large and abrupt climate change indicated in North Atlantic records is not global in scope and is largely confined to the North Atlantic and surrounding areas, or (2) Owens Lake is located in a part of the Great Basin that is relatively insensitive to the effects of climate perturbations recorded in the North Atlantic region.
format Other/Unknown Material
author Benson, Larry
Burdett, James
Kashgarian, Michaele
Lund, Steve
Rye, Robert
author_facet Benson, Larry
Burdett, James
Kashgarian, Michaele
Lund, Steve
Rye, Robert
author_sort Benson, Larry
title High-resolution record of climate change in the Owens Lake Basin, California, for the period 52,500 to 12,500 YBP
title_short High-resolution record of climate change in the Owens Lake Basin, California, for the period 52,500 to 12,500 YBP
title_full High-resolution record of climate change in the Owens Lake Basin, California, for the period 52,500 to 12,500 YBP
title_fullStr High-resolution record of climate change in the Owens Lake Basin, California, for the period 52,500 to 12,500 YBP
title_full_unstemmed High-resolution record of climate change in the Owens Lake Basin, California, for the period 52,500 to 12,500 YBP
title_sort high-resolution record of climate change in the owens lake basin, california, for the period 52,500 to 12,500 ybp
publishDate 1996
url http://hdl.handle.net/1834/31628
genre North Atlantic
genre_facet North Atlantic
op_source http://aquaticcommons.org/id/eprint/15814
8
2014-12-09 00:29:58
15814
op_relation http://hdl.handle.net/1834/31628
_version_ 1766117943969579008

Similar Items