KMS Institute of Vertebrate Paleontology and Paleoanthropology
Isotopic evidence for continental ice sheet in mid-latitude region in the supergreenhouse Early Cretaceous | |
Yang, Wu-Bin1; Niu, He-Cai1; Sun, Wei-Dong1,2; Shan, Qiang1; Zheng, Yong-Fei3; Li, Ning-Bo1,4; Li, Cong-Ying2; Arndt, Nicholas T.5; Xu, Xing6; Jiang, Yu-Hang1,4; Yu, Xue-Yuan1; niuhc@gig.ac.cn; weidongsun@gig.ac.cn | |
2013-09-24 | |
发表期刊 | SCIENTIFIC REPORTS |
ISSN | 2045-2322 |
卷号 | 3页码:0—0 |
文章类型 | Article |
摘要 | Cretaceous represents one of the hottest greenhouse periods in the Earth's history, but some recent studies suggest that small ice caps might be present in non-polar regions during certain periods in the Early Cretaceous. Here we report extremely negative delta O-18 values of -18.12 parts per thousand to -13.19 parts per thousand for early Aptian hydrothermal zircon from an A-type granite at Baerzhe in northeastern China. Given that A-type granite is anhydrous and that magmatic zircon of the Baerzhe granite has delta O-18 value close to mantle values, the extremely negative delta O-18 values for hydrothermal zircon are attributed to addition of meteoric water with extremely low delta O-18, mostly likely transported by glaciers. Considering the paleoaltitude of the region, continental glaciation is suggested to occur in the early Aptian, indicating much larger temperature fluctuations than previously thought during the supergreenhouse Cretaceous. This may have impact on the evolution of major organism in the Jehol Group during this period. |
关键词 | U-pb Age Super-large Rare Meteoric Water Zircon Megacrysts Fluid Inclusions Oxygen Isotopes Ne China Granite Record Crystal |
WOS标题词 | Science & Technology |
URL | 查看原文 |
关键词[WOS] | U-PB AGE ; SUPER-LARGE RARE ; METEORIC WATER ; ZIRCON MEGACRYSTS ; FLUID INCLUSIONS ; OXYGEN ISOTOPES ; NE CHINA ; GRANITE ; RECORD ; CRYSTAL |
收录类别 | SCI |
语种 | 英语 |
WOS研究方向 | Science & Technology - Other Topics |
WOS类目 | Multidisciplinary Sciences |
WOS记录号 | WOS:000324747900003 |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.205/handle/311034/4111 |
专题 | 中科院古脊椎所(2000年以后) |
通讯作者 | niuhc@gig.ac.cn; weidongsun@gig.ac.cn |
作者单位 | 1.Chinese Acad Sci, Guangzhou Inst Geochem, CAS Key Lab Mineral & Metallogeny, Guangzhou 510640, Peoples R China 2.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou 510640, Peoples R China 3.Univ Sci & Technol China, Sch Earth & Space Sci, CAS Key Lab Crust Mantle Mat & Environm, Hefei 230026, Peoples R China 4.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 5.Univ Grenoble, ISTerre, F-38401 St Martin Dheres, France 6.Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Key Lab Evolutionary Systemat Vertebrates, Beijing 100044, Peoples R China |
推荐引用方式 GB/T 7714 | Yang, Wu-Bin,Niu, He-Cai,Sun, Wei-Dong,et al. Isotopic evidence for continental ice sheet in mid-latitude region in the supergreenhouse Early Cretaceous[J]. SCIENTIFIC REPORTS,2013,3:0—0. |
APA | Yang, Wu-Bin.,Niu, He-Cai.,Sun, Wei-Dong.,Shan, Qiang.,Zheng, Yong-Fei.,...&weidongsun@gig.ac.cn.(2013).Isotopic evidence for continental ice sheet in mid-latitude region in the supergreenhouse Early Cretaceous.SCIENTIFIC REPORTS,3,0—0. |
MLA | Yang, Wu-Bin,et al."Isotopic evidence for continental ice sheet in mid-latitude region in the supergreenhouse Early Cretaceous".SCIENTIFIC REPORTS 3(2013):0—0. |
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