globalchange  > 气候减缓与适应
DOI: 10.1002/2014GL059884
论文题名:
East central North America climates during marine isotope stages 3-5
作者: Springer G.S.; Rowe H.D.; Hardt B.; Cheng H.; Edwards R.L.
刊名: Geophysical Research Letters
ISSN: 0094-10101
EISSN: 1944-9832
出版年: 2014
卷: 41, 期:9
起始页码: 3233
结束页码: 3237
语种: 英语
英文关键词: climate variability ; glacial ; interglacial ; paleoclimatology
Scopus关键词: Carbon ; Climate change ; Geochronology ; Glacial geology ; Isotopes ; Oxygen ; Sea level ; Carbon and oxygen isotopes ; Climate variability ; Eastern north america ; glacial ; interglacial ; Laurentide ice sheets ; Marine isotope stages ; Paleoclimatology ; Moisture ; climate variation ; glacial-interglacial cycle ; ice sheet ; moisture ; oxygen isotope ; paleoclimate ; Pleistocene ; sea level change ; stalagmite ; Canada ; Laurentian Mountains ; Quebec [Canada] ; United States ; Virginia
英文摘要: Long-term, high-resolution stalagmite carbon and oxygen isotope records from eastern North America (ENA) provide a midlatitude history of relative changes in moisture availability and climate states during the last interglacial and glacial inception (127.7 to 41.6ka before present). The West Virginia carbon record shows low-amplitude variability at orbital time scales, superimposed on a long-term asymmetric pattern similar to global sea level changes. Relative moisture availability peaked at ~114ka, and following a brief dry interval at ~96ka, moisture availability gradually decreased. The almost linear change in moisture availability over ENA may reflect gradual changes in midlatitude zonal circulation as the polar cell and Laurentide Ice Sheet expanded or decreased. In contrast, our oxygen record is precession modulated and in phase with spring insolation, perhaps due to changes in precipitation seasonality. The separate pacings by eccentricity (carbon) and precession (oxygen) expose an underlying complexity that will be a challenge to explain. Key Points A Late Pleistocene climate history is reconstructed for eastern North America Relative moisture abundances correlate with orbital-level sea level changes The last interglacial ended abruptly, but Ice Age climates changed slowly © 2014. American Geophysical Union. All Rights Reserved.
URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84901917787&doi=10.1002%2f2014GL059884&partnerID=40&md5=e32ba993804f0829eea98a774b193166
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/7365
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作者单位: Department of Geological Sciences, Ohio University, Athens, OH, United States

Recommended Citation:
Springer G.S.,Rowe H.D.,Hardt B.,et al. East central North America climates during marine isotope stages 3-5[J]. Geophysical Research Letters,2014-01-01,41(9).
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