Step-wise change of Asian interior climate preceding the Eocene-Oligocene Transition (EOT)
Understanding the global climate change from greenhouse to icehouse conditions at the Eocene-Oligocene Transition (DOT) 34 million years ago requires climatic records from oceanic as well as continental realms of the key Late Eocene "doubthouse" period preceding this switch. Here, we repor...
Published in: | Palaeogeography, Palaeoclimatology, Palaeoecology |
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Language: | English |
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palaeogeography palaeoclimatology palaeoecology
2011
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Online Access: | https://hdl.handle.net/20.500.11897/243191 https://doi.org/10.1016/j.palaeo.2010.11.028 |
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ftpekinguniv:oai:localhost:20.500.11897/243191 2023-05-15T16:41:37+02:00 Step-wise change of Asian interior climate preceding the Eocene-Oligocene Transition (EOT) Abels, Hemmo A. Dupont-Nivet, Guillaume Xiao, Guoqiao Bosboom, Roderic Krijgsman, Wout Abels, HA (reprint author), Univ Utrecht, Dept Earth Sci, Paleomagnet Lab Ft Hoofddijk, Budapestlaan 17, NL-3584 CD Utrecht, Netherlands. Univ Utrecht, Dept Earth Sci, Paleomagnet Lab Ft Hoofddijk, NL-3584 CD Utrecht, Netherlands. Peking Univ, Minist Educ, Key Lab Orogen Belts & Crustal Evolut, Beijing 100871, Peoples R China. Univ Rennes 1, UMR 6118, F-35042 Rennes, France. China Univ Geosci, Minist Educ, Key Lab Biogeol & Environm Geol, Wuhan 430074, Peoples R China. Univ Utrecht, Dept Earth Sci, Paleomagnet Lab Ft Hoofddijk, Budapestlaan 17, NL-3584 CD Utrecht, Netherlands. 2011 https://hdl.handle.net/20.500.11897/243191 https://doi.org/10.1016/j.palaeo.2010.11.028 en eng palaeogeography palaeoclimatology palaeoecology PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY.2011,299,(3-4),399-412. 924371 0031-0182 http://hdl.handle.net/20.500.11897/243191 doi:10.1016/j.palaeo.2010.11.028 WOS:000287058700002 SCI Late Eocene Doubthouse climate Eocene-Oligocene Transition (EOT) Terrestrial record Gypsum Red beds Cyclostratigraphy TIBETAN PLATEAU LACUSTRINE EVAPORITES MIDDLE EOCENE PACIFIC-OCEAN TERUEL BASIN XINING BASIN TARIM BASIN NE SPAIN CHINA PALEOGENE Journal 2011 ftpekinguniv https://doi.org/20.500.11897/243191 https://doi.org/10.1016/j.palaeo.2010.11.028 2021-08-01T08:50:53Z Understanding the global climate change from greenhouse to icehouse conditions at the Eocene-Oligocene Transition (DOT) 34 million years ago requires climatic records from oceanic as well as continental realms of the key Late Eocene "doubthouse" period preceding this switch. Here, we report integrated stratigraphic results from well-dated Late Eocene continental mudflat to saline lake paleoenvironments of the Xining Basin (northeastern Tibetan Plateau, western China) recording regional and global change. Cyclostratigraphic analysis strongly suggests continuous dominance of the 41-kyr obliquity cycle in the whole late Eocene interval down to the base of polarity chron C18n.2n at 39 Ma with additional input of the similar to 100-kyr eccentricity cycle up to the base of chron C13r at similar to 34.7 Ma. This might imply that high-latitude climates dominated the area long before the EOT, probably related to incipient ice-volume fluctuations. Furthermore, our results reveal two paleoenvironmental deterioration steps preceding the Eocene-Oligocene Transition. The first step occurs in the top of chron C17n.ln at similar to 36.6 Ma. This age closely corresponds to (1) the high-altitude pollen appearance in chron Cl 6.2r at similar to 36.4 Ma in the same section, (2) the recently dated final retreat of the Tarim Sea in western China, and (3) a shift from precession to obliquity dominance in the Atlantic Ocean. This near co-occurrence suggests global change at this time. We hypothesize this change is related to an increase in incipient ice sheet volume leading to passing threshold conditions for the high-altitude pollen appearance and Tarim Sea retreat, finally leading to decreased moisture availability in the Xining Basin. At the second step, in the base of chron C13r at similar to 34.7 Ma. a substantial increase in clastic sedimentation rates is observed. This might relate to increased climate variability preceding the greenhouse to icehouse transition at the EOT that prevented landscapes to attain equilibrium configurations. (c) 2010 Elsevier By. All rights reserved. Geography, Physical Geosciences, Multidisciplinary Paleontology SCI(E) 21 ARTICLE 3-4 399-412 299 Journal/Newspaper Ice Sheet Peking University Institutional Repository (PKU IR) Pacific Saline Lake ENVELOPE(-111.528,-111.528,57.081,57.081) Palaeogeography, Palaeoclimatology, Palaeoecology 299 3-4 399 412 |
institution |
Open Polar |
collection |
Peking University Institutional Repository (PKU IR) |
op_collection_id |
ftpekinguniv |
language |
English |
topic |
Late Eocene Doubthouse climate Eocene-Oligocene Transition (EOT) Terrestrial record Gypsum Red beds Cyclostratigraphy TIBETAN PLATEAU LACUSTRINE EVAPORITES MIDDLE EOCENE PACIFIC-OCEAN TERUEL BASIN XINING BASIN TARIM BASIN NE SPAIN CHINA PALEOGENE |
spellingShingle |
Late Eocene Doubthouse climate Eocene-Oligocene Transition (EOT) Terrestrial record Gypsum Red beds Cyclostratigraphy TIBETAN PLATEAU LACUSTRINE EVAPORITES MIDDLE EOCENE PACIFIC-OCEAN TERUEL BASIN XINING BASIN TARIM BASIN NE SPAIN CHINA PALEOGENE Abels, Hemmo A. Dupont-Nivet, Guillaume Xiao, Guoqiao Bosboom, Roderic Krijgsman, Wout Step-wise change of Asian interior climate preceding the Eocene-Oligocene Transition (EOT) |
topic_facet |
Late Eocene Doubthouse climate Eocene-Oligocene Transition (EOT) Terrestrial record Gypsum Red beds Cyclostratigraphy TIBETAN PLATEAU LACUSTRINE EVAPORITES MIDDLE EOCENE PACIFIC-OCEAN TERUEL BASIN XINING BASIN TARIM BASIN NE SPAIN CHINA PALEOGENE |
description |
Understanding the global climate change from greenhouse to icehouse conditions at the Eocene-Oligocene Transition (DOT) 34 million years ago requires climatic records from oceanic as well as continental realms of the key Late Eocene "doubthouse" period preceding this switch. Here, we report integrated stratigraphic results from well-dated Late Eocene continental mudflat to saline lake paleoenvironments of the Xining Basin (northeastern Tibetan Plateau, western China) recording regional and global change. Cyclostratigraphic analysis strongly suggests continuous dominance of the 41-kyr obliquity cycle in the whole late Eocene interval down to the base of polarity chron C18n.2n at 39 Ma with additional input of the similar to 100-kyr eccentricity cycle up to the base of chron C13r at similar to 34.7 Ma. This might imply that high-latitude climates dominated the area long before the EOT, probably related to incipient ice-volume fluctuations. Furthermore, our results reveal two paleoenvironmental deterioration steps preceding the Eocene-Oligocene Transition. The first step occurs in the top of chron C17n.ln at similar to 36.6 Ma. This age closely corresponds to (1) the high-altitude pollen appearance in chron Cl 6.2r at similar to 36.4 Ma in the same section, (2) the recently dated final retreat of the Tarim Sea in western China, and (3) a shift from precession to obliquity dominance in the Atlantic Ocean. This near co-occurrence suggests global change at this time. We hypothesize this change is related to an increase in incipient ice sheet volume leading to passing threshold conditions for the high-altitude pollen appearance and Tarim Sea retreat, finally leading to decreased moisture availability in the Xining Basin. At the second step, in the base of chron C13r at similar to 34.7 Ma. a substantial increase in clastic sedimentation rates is observed. This might relate to increased climate variability preceding the greenhouse to icehouse transition at the EOT that prevented landscapes to attain equilibrium configurations. (c) 2010 Elsevier By. All rights reserved. Geography, Physical Geosciences, Multidisciplinary Paleontology SCI(E) 21 ARTICLE 3-4 399-412 299 |
author2 |
Abels, HA (reprint author), Univ Utrecht, Dept Earth Sci, Paleomagnet Lab Ft Hoofddijk, Budapestlaan 17, NL-3584 CD Utrecht, Netherlands. Univ Utrecht, Dept Earth Sci, Paleomagnet Lab Ft Hoofddijk, NL-3584 CD Utrecht, Netherlands. Peking Univ, Minist Educ, Key Lab Orogen Belts & Crustal Evolut, Beijing 100871, Peoples R China. Univ Rennes 1, UMR 6118, F-35042 Rennes, France. China Univ Geosci, Minist Educ, Key Lab Biogeol & Environm Geol, Wuhan 430074, Peoples R China. Univ Utrecht, Dept Earth Sci, Paleomagnet Lab Ft Hoofddijk, Budapestlaan 17, NL-3584 CD Utrecht, Netherlands. |
format |
Journal/Newspaper |
author |
Abels, Hemmo A. Dupont-Nivet, Guillaume Xiao, Guoqiao Bosboom, Roderic Krijgsman, Wout |
author_facet |
Abels, Hemmo A. Dupont-Nivet, Guillaume Xiao, Guoqiao Bosboom, Roderic Krijgsman, Wout |
author_sort |
Abels, Hemmo A. |
title |
Step-wise change of Asian interior climate preceding the Eocene-Oligocene Transition (EOT) |
title_short |
Step-wise change of Asian interior climate preceding the Eocene-Oligocene Transition (EOT) |
title_full |
Step-wise change of Asian interior climate preceding the Eocene-Oligocene Transition (EOT) |
title_fullStr |
Step-wise change of Asian interior climate preceding the Eocene-Oligocene Transition (EOT) |
title_full_unstemmed |
Step-wise change of Asian interior climate preceding the Eocene-Oligocene Transition (EOT) |
title_sort |
step-wise change of asian interior climate preceding the eocene-oligocene transition (eot) |
publisher |
palaeogeography palaeoclimatology palaeoecology |
publishDate |
2011 |
url |
https://hdl.handle.net/20.500.11897/243191 https://doi.org/10.1016/j.palaeo.2010.11.028 |
long_lat |
ENVELOPE(-111.528,-111.528,57.081,57.081) |
geographic |
Pacific Saline Lake |
geographic_facet |
Pacific Saline Lake |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
SCI |
op_relation |
PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY.2011,299,(3-4),399-412. 924371 0031-0182 http://hdl.handle.net/20.500.11897/243191 doi:10.1016/j.palaeo.2010.11.028 WOS:000287058700002 |
op_doi |
https://doi.org/20.500.11897/243191 https://doi.org/10.1016/j.palaeo.2010.11.028 |
container_title |
Palaeogeography, Palaeoclimatology, Palaeoecology |
container_volume |
299 |
container_issue |
3-4 |
container_start_page |
399 |
op_container_end_page |
412 |
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1766032079246589952 |