Dominant 100,000-year precipitation cyclicity in a lateMiocene lake from northeast Tibet
East Asian summer monsoon (EASM) precipitation received by northern China over the past 800 thousand years (ky) is characterized by dominant 100-ky periodicity, mainly attributed to CO2 and Northern Hemisphere insolation-driven ice sheet forcing. We established an EASM record in the Late Miocene fro...
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Online Access: | http://ir.ieecas.cn/handle/361006/5591 https://doi.org/10.1126/sciadv.1600762 |
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ftchinacascieeca:oai:ir.ieecas.cn:361006/5591 2023-06-11T04:06:25+02:00 Dominant 100,000-year precipitation cyclicity in a lateMiocene lake from northeast Tibet Nie,JS(Nie,Junsheng) Garzione,C(Garzione,Carmala) Su,QD(Su,Qingda) Liu,QS(Liu,Qingsong) Zhang,R(Zhang,Rui) Heslop, D(Heslop.David) Necula, C(Necula,Cristian) Zhang,SH(Zhang,Shihong) Song,YG(Song,Yougui) Luo,Z(Luo,Zeng) Nie,Junsheng 2017-03-29 http://ir.ieecas.cn/handle/361006/5591 https://doi.org/10.1126/sciadv.1600762 英语 eng Science Advances http://ir.ieecas.cn/handle/361006/5591 doi:10.1126/sciadv.1600762 null Antarctica East Asian Monsoon Tibetan Plateau Eccentricity Ice Sheets Orbital Forcing 期刊论文 2017 ftchinacascieeca https://doi.org/10.1126/sciadv.1600762 2023-05-08T13:22:53Z East Asian summer monsoon (EASM) precipitation received by northern China over the past 800 thousand years (ky) is characterized by dominant 100-ky periodicity, mainly attributed to CO2 and Northern Hemisphere insolation-driven ice sheet forcing. We established an EASM record in the Late Miocene from lacustrine sediments in the Qaidam Basin, northern China, which appears to exhibit a dominant 100-ky periodicity similar to the EASM records during the Late Quaternary. Because evidence suggests that partial or ephemeral ice existed in the Northern Hemisphere during the Late Miocene, we attribute the 100-ky cycles to CO2 and Southern Hemisphere insolation-driven Antarctic ice sheet forcing. This indicates a >6-million year earlier onset of the dominant 100-ky Asian monsoon and, likely, glacial and CO2 cycles and may indicate dominant forcing of Northern Hemisphere climate by CO2 and Southern Hemisphere ice sheets in a warm world. Report Antarc* Antarctic Antarctica Ice Sheet Institute of Earth Environment: IEECAS OpenIR (Chinese Academy of Sciences) Antarctic Science Advances 3 3 |
institution |
Open Polar |
collection |
Institute of Earth Environment: IEECAS OpenIR (Chinese Academy of Sciences) |
op_collection_id |
ftchinacascieeca |
language |
English |
topic |
Antarctica East Asian Monsoon Tibetan Plateau Eccentricity Ice Sheets Orbital Forcing |
spellingShingle |
Antarctica East Asian Monsoon Tibetan Plateau Eccentricity Ice Sheets Orbital Forcing Nie,JS(Nie,Junsheng) Garzione,C(Garzione,Carmala) Su,QD(Su,Qingda) Liu,QS(Liu,Qingsong) Zhang,R(Zhang,Rui) Heslop, D(Heslop.David) Necula, C(Necula,Cristian) Zhang,SH(Zhang,Shihong) Song,YG(Song,Yougui) Luo,Z(Luo,Zeng) Nie,Junsheng Dominant 100,000-year precipitation cyclicity in a lateMiocene lake from northeast Tibet |
topic_facet |
Antarctica East Asian Monsoon Tibetan Plateau Eccentricity Ice Sheets Orbital Forcing |
description |
East Asian summer monsoon (EASM) precipitation received by northern China over the past 800 thousand years (ky) is characterized by dominant 100-ky periodicity, mainly attributed to CO2 and Northern Hemisphere insolation-driven ice sheet forcing. We established an EASM record in the Late Miocene from lacustrine sediments in the Qaidam Basin, northern China, which appears to exhibit a dominant 100-ky periodicity similar to the EASM records during the Late Quaternary. Because evidence suggests that partial or ephemeral ice existed in the Northern Hemisphere during the Late Miocene, we attribute the 100-ky cycles to CO2 and Southern Hemisphere insolation-driven Antarctic ice sheet forcing. This indicates a >6-million year earlier onset of the dominant 100-ky Asian monsoon and, likely, glacial and CO2 cycles and may indicate dominant forcing of Northern Hemisphere climate by CO2 and Southern Hemisphere ice sheets in a warm world. |
format |
Report |
author |
Nie,JS(Nie,Junsheng) Garzione,C(Garzione,Carmala) Su,QD(Su,Qingda) Liu,QS(Liu,Qingsong) Zhang,R(Zhang,Rui) Heslop, D(Heslop.David) Necula, C(Necula,Cristian) Zhang,SH(Zhang,Shihong) Song,YG(Song,Yougui) Luo,Z(Luo,Zeng) Nie,Junsheng |
author_facet |
Nie,JS(Nie,Junsheng) Garzione,C(Garzione,Carmala) Su,QD(Su,Qingda) Liu,QS(Liu,Qingsong) Zhang,R(Zhang,Rui) Heslop, D(Heslop.David) Necula, C(Necula,Cristian) Zhang,SH(Zhang,Shihong) Song,YG(Song,Yougui) Luo,Z(Luo,Zeng) Nie,Junsheng |
author_sort |
Nie,JS(Nie,Junsheng) |
title |
Dominant 100,000-year precipitation cyclicity in a lateMiocene lake from northeast Tibet |
title_short |
Dominant 100,000-year precipitation cyclicity in a lateMiocene lake from northeast Tibet |
title_full |
Dominant 100,000-year precipitation cyclicity in a lateMiocene lake from northeast Tibet |
title_fullStr |
Dominant 100,000-year precipitation cyclicity in a lateMiocene lake from northeast Tibet |
title_full_unstemmed |
Dominant 100,000-year precipitation cyclicity in a lateMiocene lake from northeast Tibet |
title_sort |
dominant 100,000-year precipitation cyclicity in a latemiocene lake from northeast tibet |
publishDate |
2017 |
url |
http://ir.ieecas.cn/handle/361006/5591 https://doi.org/10.1126/sciadv.1600762 |
geographic |
Antarctic |
geographic_facet |
Antarctic |
genre |
Antarc* Antarctic Antarctica Ice Sheet |
genre_facet |
Antarc* Antarctic Antarctica Ice Sheet |
op_relation |
Science Advances http://ir.ieecas.cn/handle/361006/5591 doi:10.1126/sciadv.1600762 |
op_rights |
null |
op_doi |
https://doi.org/10.1126/sciadv.1600762 |
container_title |
Science Advances |
container_volume |
3 |
container_issue |
3 |
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1768378363419820032 |