Northward extent of East Asian monsoon covaries with intensity on orbital and millennial timescales
The magnitude, rate, and extent of past and future East Asian monsoon (EAM) rainfall fluctuations remain unresolved. Here, late Pleistocene–Holocene EAM rainfall intensity is reconstructed using a well-dated northeastern China closed-basin lake area record located at the modern northwestern fringe o...
Gespeichert in:
| Veröffentlicht in: | Proceedings of the National Academy of Sciences - PNAS 2017-02, Vol.114 (8), p.1817-1821 |
|---|---|
| Hauptverfasser: | , , , , , , , , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 1821 |
|---|---|
| container_issue | 8 |
| container_start_page | 1817 |
| container_title | Proceedings of the National Academy of Sciences - PNAS |
| container_volume | 114 |
| creator | Goldsmith, Yonaton Broecker, Wallace S. Xu, Hai Polissar, Pratigya J. deMenocal, Peter B. Porat, Naomi Lan, Jianghu Cheng, Peng Zhou, Weijian An, Zhisheng |
| description | The magnitude, rate, and extent of past and future East Asian monsoon (EAM) rainfall fluctuations remain unresolved. Here, late Pleistocene–Holocene EAM rainfall intensity is reconstructed using a well-dated northeastern China closed-basin lake area record located at the modern northwestern fringe of the EAM. The EAM intensity and northern extent alternated rapidly between wet and dry periods on time scales of centuries. Lake levels were 60 m higher than present during the early andmiddle Holocene, requiring a twofold increase in annual rainfall, which, based on modern rainfall distribution, requires a ∼400 km northward expansion/migration of the EAM. The lake record is highly correlated with both northern and southern Chinese cave deposit isotope records, supporting rainfall “intensity based” interpretations of these deposits as opposed to an alternative “water vapor sourcing” interpretation. These results indicate that EAM intensity and the northward extent covary on orbital and millennial timescales. The termination of wet conditions at 5.5 ka BP (∼35 m lake drop) triggered a large cultural collapse of Early Neolithic cultures in north China, and possibly promoted the emergence of complex societies of the Late Neolithic. |
| doi_str_mv | 10.1073/pnas.1616708114 |
| format | Article |
| fullrecord | <record><control><sourceid>jstor_pubme</sourceid><recordid>TN_cdi_pubmedcentral_primary_oai_pubmedcentral_nih_gov_5338392</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><jstor_id>26479273</jstor_id><sourcerecordid>26479273</sourcerecordid><originalsourceid>FETCH-LOGICAL-a466t-2d45a03cffc7e129560de046b3fec4fc49df674a9c68364a9feee862e89a747e3</originalsourceid><addsrcrecordid>eNpdkUlvFDEQhS0EIkPgzAlkiQuXTry1lwtSFIVFiuACZ8vjLjMedduD7cny73E0IQFOpdL76qmeHkKvKTmhRPHTXXL1hEoqFdGUiidoRYmhgxSGPEUrQpgatGDiCL2odUsIMaMmz9ER0_1CjWKF_Ndc2ubalQnDTYPUcA74wtWGz2p0CS851ZwT9vnKlQgVX8e2wTF1tMZ2i7uUyzo2N2OXJrzEeYaUYl9bXKB6N0N9iZ4FN1d4dT-P0Y-PF9_PPw-X3z59OT-7HJyQsg1sEqMj3IfgFVBmRkkmIEKueQAvghdmClIJZ7zUXPYZAEBLBto4JRTwY_Th4LvbrxeYfE9T3Gx3JS6u3Nrsov1XSXFjf-YrO3KuuWHd4P29Qcm_9lCbXWL1MM8uQd5XS7UcNWOCyI6--w_d5n1JPV6nFBulZiPp1OmB8iXXWiA8PEOJvSvQ3hVoHwvsF2__zvDA_2msA28OwLa2XB51KZRhivPfjoGjZg</addsrcrecordid><sourcetype>Open Access Repository</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1872568250</pqid></control><display><type>article</type><title>Northward extent of East Asian monsoon covaries with intensity on orbital and millennial timescales</title><source>Jstor Complete Legacy</source><source>PubMed Central</source><source>Alma/SFX Local Collection</source><source>Free Full-Text Journals in Chemistry</source><creator>Goldsmith, Yonaton ; Broecker, Wallace S. ; Xu, Hai ; Polissar, Pratigya J. ; deMenocal, Peter B. ; Porat, Naomi ; Lan, Jianghu ; Cheng, Peng ; Zhou, Weijian ; An, Zhisheng</creator><creatorcontrib>Goldsmith, Yonaton ; Broecker, Wallace S. ; Xu, Hai ; Polissar, Pratigya J. ; deMenocal, Peter B. ; Porat, Naomi ; Lan, Jianghu ; Cheng, Peng ; Zhou, Weijian ; An, Zhisheng</creatorcontrib><description>The magnitude, rate, and extent of past and future East Asian monsoon (EAM) rainfall fluctuations remain unresolved. Here, late Pleistocene–Holocene EAM rainfall intensity is reconstructed using a well-dated northeastern China closed-basin lake area record located at the modern northwestern fringe of the EAM. The EAM intensity and northern extent alternated rapidly between wet and dry periods on time scales of centuries. Lake levels were 60 m higher than present during the early andmiddle Holocene, requiring a twofold increase in annual rainfall, which, based on modern rainfall distribution, requires a ∼400 km northward expansion/migration of the EAM. The lake record is highly correlated with both northern and southern Chinese cave deposit isotope records, supporting rainfall “intensity based” interpretations of these deposits as opposed to an alternative “water vapor sourcing” interpretation. These results indicate that EAM intensity and the northward extent covary on orbital and millennial timescales. The termination of wet conditions at 5.5 ka BP (∼35 m lake drop) triggered a large cultural collapse of Early Neolithic cultures in north China, and possibly promoted the emergence of complex societies of the Late Neolithic.</description><identifier>ISSN: 0027-8424</identifier><identifier>EISSN: 1091-6490</identifier><identifier>DOI: 10.1073/pnas.1616708114</identifier><identifier>PMID: 28167754</identifier><language>eng</language><publisher>United States: National Academy of Sciences</publisher><subject>Correlation analysis ; Geological time ; Lakes ; Orbits ; Paleoclimate science ; Physical Sciences ; Rain ; Wind</subject><ispartof>Proceedings of the National Academy of Sciences - PNAS, 2017-02, Vol.114 (8), p.1817-1821</ispartof><rights>Volumes 1–89 and 106–114, copyright as a collective work only; author(s) retains copyright to individual articles</rights><rights>Copyright National Academy of Sciences Feb 21, 2017</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a466t-2d45a03cffc7e129560de046b3fec4fc49df674a9c68364a9feee862e89a747e3</citedby><cites>FETCH-LOGICAL-a466t-2d45a03cffc7e129560de046b3fec4fc49df674a9c68364a9feee862e89a747e3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/26479273$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/26479273$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>230,314,723,776,780,799,881,27901,27902,53766,53768,57992,58225</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/28167754$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Goldsmith, Yonaton</creatorcontrib><creatorcontrib>Broecker, Wallace S.</creatorcontrib><creatorcontrib>Xu, Hai</creatorcontrib><creatorcontrib>Polissar, Pratigya J.</creatorcontrib><creatorcontrib>deMenocal, Peter B.</creatorcontrib><creatorcontrib>Porat, Naomi</creatorcontrib><creatorcontrib>Lan, Jianghu</creatorcontrib><creatorcontrib>Cheng, Peng</creatorcontrib><creatorcontrib>Zhou, Weijian</creatorcontrib><creatorcontrib>An, Zhisheng</creatorcontrib><title>Northward extent of East Asian monsoon covaries with intensity on orbital and millennial timescales</title><title>Proceedings of the National Academy of Sciences - PNAS</title><addtitle>Proc Natl Acad Sci U S A</addtitle><description>The magnitude, rate, and extent of past and future East Asian monsoon (EAM) rainfall fluctuations remain unresolved. Here, late Pleistocene–Holocene EAM rainfall intensity is reconstructed using a well-dated northeastern China closed-basin lake area record located at the modern northwestern fringe of the EAM. The EAM intensity and northern extent alternated rapidly between wet and dry periods on time scales of centuries. Lake levels were 60 m higher than present during the early andmiddle Holocene, requiring a twofold increase in annual rainfall, which, based on modern rainfall distribution, requires a ∼400 km northward expansion/migration of the EAM. The lake record is highly correlated with both northern and southern Chinese cave deposit isotope records, supporting rainfall “intensity based” interpretations of these deposits as opposed to an alternative “water vapor sourcing” interpretation. These results indicate that EAM intensity and the northward extent covary on orbital and millennial timescales. The termination of wet conditions at 5.5 ka BP (∼35 m lake drop) triggered a large cultural collapse of Early Neolithic cultures in north China, and possibly promoted the emergence of complex societies of the Late Neolithic.</description><subject>Correlation analysis</subject><subject>Geological time</subject><subject>Lakes</subject><subject>Orbits</subject><subject>Paleoclimate science</subject><subject>Physical Sciences</subject><subject>Rain</subject><subject>Wind</subject><issn>0027-8424</issn><issn>1091-6490</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><recordid>eNpdkUlvFDEQhS0EIkPgzAlkiQuXTry1lwtSFIVFiuACZ8vjLjMedduD7cny73E0IQFOpdL76qmeHkKvKTmhRPHTXXL1hEoqFdGUiidoRYmhgxSGPEUrQpgatGDiCL2odUsIMaMmz9ER0_1CjWKF_Ndc2ubalQnDTYPUcA74wtWGz2p0CS851ZwT9vnKlQgVX8e2wTF1tMZ2i7uUyzo2N2OXJrzEeYaUYl9bXKB6N0N9iZ4FN1d4dT-P0Y-PF9_PPw-X3z59OT-7HJyQsg1sEqMj3IfgFVBmRkkmIEKueQAvghdmClIJZ7zUXPYZAEBLBto4JRTwY_Th4LvbrxeYfE9T3Gx3JS6u3Nrsov1XSXFjf-YrO3KuuWHd4P29Qcm_9lCbXWL1MM8uQd5XS7UcNWOCyI6--w_d5n1JPV6nFBulZiPp1OmB8iXXWiA8PEOJvSvQ3hVoHwvsF2__zvDA_2msA28OwLa2XB51KZRhivPfjoGjZg</recordid><startdate>20170221</startdate><enddate>20170221</enddate><creator>Goldsmith, Yonaton</creator><creator>Broecker, Wallace S.</creator><creator>Xu, Hai</creator><creator>Polissar, Pratigya J.</creator><creator>deMenocal, Peter B.</creator><creator>Porat, Naomi</creator><creator>Lan, Jianghu</creator><creator>Cheng, Peng</creator><creator>Zhou, Weijian</creator><creator>An, Zhisheng</creator><general>National Academy of Sciences</general><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7QG</scope><scope>7QL</scope><scope>7QP</scope><scope>7QR</scope><scope>7SN</scope><scope>7SS</scope><scope>7T5</scope><scope>7TK</scope><scope>7TM</scope><scope>7TO</scope><scope>7U9</scope><scope>8FD</scope><scope>C1K</scope><scope>FR3</scope><scope>H94</scope><scope>M7N</scope><scope>P64</scope><scope>RC3</scope><scope>7X8</scope><scope>5PM</scope></search><sort><creationdate>20170221</creationdate><title>Northward extent of East Asian monsoon covaries with intensity on orbital and millennial timescales</title><author>Goldsmith, Yonaton ; Broecker, Wallace S. ; Xu, Hai ; Polissar, Pratigya J. ; deMenocal, Peter B. ; Porat, Naomi ; Lan, Jianghu ; Cheng, Peng ; Zhou, Weijian ; An, Zhisheng</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a466t-2d45a03cffc7e129560de046b3fec4fc49df674a9c68364a9feee862e89a747e3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Correlation analysis</topic><topic>Geological time</topic><topic>Lakes</topic><topic>Orbits</topic><topic>Paleoclimate science</topic><topic>Physical Sciences</topic><topic>Rain</topic><topic>Wind</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Goldsmith, Yonaton</creatorcontrib><creatorcontrib>Broecker, Wallace S.</creatorcontrib><creatorcontrib>Xu, Hai</creatorcontrib><creatorcontrib>Polissar, Pratigya J.</creatorcontrib><creatorcontrib>deMenocal, Peter B.</creatorcontrib><creatorcontrib>Porat, Naomi</creatorcontrib><creatorcontrib>Lan, Jianghu</creatorcontrib><creatorcontrib>Cheng, Peng</creatorcontrib><creatorcontrib>Zhou, Weijian</creatorcontrib><creatorcontrib>An, Zhisheng</creatorcontrib><collection>PubMed</collection><collection>CrossRef</collection><collection>Animal Behavior Abstracts</collection><collection>Bacteriology Abstracts (Microbiology B)</collection><collection>Calcium & Calcified Tissue Abstracts</collection><collection>Chemoreception Abstracts</collection><collection>Ecology Abstracts</collection><collection>Entomology Abstracts (Full archive)</collection><collection>Immunology Abstracts</collection><collection>Neurosciences Abstracts</collection><collection>Nucleic Acids Abstracts</collection><collection>Oncogenes and Growth Factors Abstracts</collection><collection>Virology and AIDS Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>Engineering Research Database</collection><collection>AIDS and Cancer Research Abstracts</collection><collection>Algology Mycology and Protozoology Abstracts (Microbiology C)</collection><collection>Biotechnology and BioEngineering Abstracts</collection><collection>Genetics Abstracts</collection><collection>MEDLINE - Academic</collection><collection>PubMed Central (Full Participant titles)</collection><jtitle>Proceedings of the National Academy of Sciences - PNAS</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Goldsmith, Yonaton</au><au>Broecker, Wallace S.</au><au>Xu, Hai</au><au>Polissar, Pratigya J.</au><au>deMenocal, Peter B.</au><au>Porat, Naomi</au><au>Lan, Jianghu</au><au>Cheng, Peng</au><au>Zhou, Weijian</au><au>An, Zhisheng</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Northward extent of East Asian monsoon covaries with intensity on orbital and millennial timescales</atitle><jtitle>Proceedings of the National Academy of Sciences - PNAS</jtitle><addtitle>Proc Natl Acad Sci U S A</addtitle><date>2017-02-21</date><risdate>2017</risdate><volume>114</volume><issue>8</issue><spage>1817</spage><epage>1821</epage><pages>1817-1821</pages><issn>0027-8424</issn><eissn>1091-6490</eissn><abstract>The magnitude, rate, and extent of past and future East Asian monsoon (EAM) rainfall fluctuations remain unresolved. Here, late Pleistocene–Holocene EAM rainfall intensity is reconstructed using a well-dated northeastern China closed-basin lake area record located at the modern northwestern fringe of the EAM. The EAM intensity and northern extent alternated rapidly between wet and dry periods on time scales of centuries. Lake levels were 60 m higher than present during the early andmiddle Holocene, requiring a twofold increase in annual rainfall, which, based on modern rainfall distribution, requires a ∼400 km northward expansion/migration of the EAM. The lake record is highly correlated with both northern and southern Chinese cave deposit isotope records, supporting rainfall “intensity based” interpretations of these deposits as opposed to an alternative “water vapor sourcing” interpretation. These results indicate that EAM intensity and the northward extent covary on orbital and millennial timescales. The termination of wet conditions at 5.5 ka BP (∼35 m lake drop) triggered a large cultural collapse of Early Neolithic cultures in north China, and possibly promoted the emergence of complex societies of the Late Neolithic.</abstract><cop>United States</cop><pub>National Academy of Sciences</pub><pmid>28167754</pmid><doi>10.1073/pnas.1616708114</doi><tpages>5</tpages><oa>free_for_read</oa></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0027-8424 |
| ispartof | Proceedings of the National Academy of Sciences - PNAS, 2017-02, Vol.114 (8), p.1817-1821 |
| issn | 0027-8424 1091-6490 |
| language | eng |
| recordid | cdi_pubmedcentral_primary_oai_pubmedcentral_nih_gov_5338392 |
| source | Jstor Complete Legacy; PubMed Central; Alma/SFX Local Collection; Free Full-Text Journals in Chemistry |
| subjects | Correlation analysis Geological time Lakes Orbits Paleoclimate science Physical Sciences Rain Wind |
| title | Northward extent of East Asian monsoon covaries with intensity on orbital and millennial timescales |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-07T18%3A00%3A27IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-jstor_pubme&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Northward%20extent%20of%20East%20Asian%20monsoon%20covaries%20with%20intensity%20on%20orbital%20and%20millennial%20timescales&rft.jtitle=Proceedings%20of%20the%20National%20Academy%20of%20Sciences%20-%20PNAS&rft.au=Goldsmith,%20Yonaton&rft.date=2017-02-21&rft.volume=114&rft.issue=8&rft.spage=1817&rft.epage=1821&rft.pages=1817-1821&rft.issn=0027-8424&rft.eissn=1091-6490&rft_id=info:doi/10.1073/pnas.1616708114&rft_dat=%3Cjstor_pubme%3E26479273%3C/jstor_pubme%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=1872568250&rft_id=info:pmid/28167754&rft_jstor_id=26479273&rfr_iscdi=true |