globalchange  > 过去全球变化的重建
DOI: 10.1029/2019PA003568
WOS记录号: WOS:000481820300003
论文题名:
Dynamic Intermediate Waters Across the Late Glacial Revealed by Paired Radiocarbon and Clumped Isotope Temperature Records
作者: Hines, Sophia K., V1,2; Eiler, John M.1; Southon, John R.3; Adkins, Jess F.1
通讯作者: Hines, Sophia K., V
刊名: PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY
ISSN: 2572-4517
EISSN: 2572-4525
出版年: 2019
卷: 34, 期:7, 页码:1074-1091
语种: 英语
英文关键词: radiocarbon ; clumped isotope temperature ; ocean circulation ; intermediate water
WOS关键词: AGE CALIBRATION CURVES ; HIGH-RESOLUTION RECORD ; DEEP-SEA CORALS ; VOSTOK ICE CORE ; NORTH-ATLANTIC ; HEINRICH EVENTS ; SOUTHERN-OCEAN ; LAST DEGLACIATION ; CLIMATE-CHANGE ; CIRCULATION
WOS学科分类: Geosciences, Multidisciplinary ; Oceanography ; Paleontology
WOS研究方向: Geology ; Oceanography ; Paleontology
英文摘要:

Paired radiocarbon and clumped isotope temperature records from U/Th-dated Desmophyllum dianthus corals in the North Atlantic and Southern Ocean provide unique information about the history of intermediate waters (similar to 1,500-1,700 m) across the late glacial and deglaciation (similar to 35-10 ka). These measurements allow for the construction of radiocarbon-temperature crossplots, which help to identify water mass endmembers at different times across the deglaciation. Radiocarbon and temperature values from the late glacial fall outside the range of modern ocean data from near the sample collection sites. In the North Atlantic, radiocarbon values tend to be much older than the modern, while in the Southern Ocean, they are more often younger than the modern. Reconstructed temperatures vary around respective modern ocean values; however, warm waters are observed at the Last Glacial Maximum and across the deglaciation in the north and south. We interpret our data in the context of the modern hydrography of the Western North Atlantic and Southern Ocean, and we draw upon direct comparisons between sediment core-derived reconstructions of ocean circulation from the South Indo-Pacific and our deep-sea coral data from the Southern Ocean. Our North Atlantic data support accepted patterns of reduced North Atlantic Deep Water formation during Heinrich Stadials 1 and 2. In the Southern Ocean, deep-sea coral populations respond to changes in ocean structure that are also reflected in a depth profile of delta C-13 data from New Zealand, and data indicate that there was less influence of Pacific Deep Water between 1,500 and 1,700 m south of Tasmania across much of the deglaciation.


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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/140994
Appears in Collections:过去全球变化的重建

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作者单位: 1.CALTECH, Dept Geol & Planetary Sci, Pasadena, CA 91125 USA
2.Columbia Univ, Lamont Doherty Earth Observ, Palisades, NY 10964 USA
3.Univ Calif Irvine, Earth Syst Sci Dept, Irvine, CA USA

Recommended Citation:
Hines, Sophia K., V,Eiler, John M.,Southon, John R.,et al. Dynamic Intermediate Waters Across the Late Glacial Revealed by Paired Radiocarbon and Clumped Isotope Temperature Records[J]. PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY,2019-01-01,34(7):1074-1091
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