Knowledge Management System Of Guangzhou Institute of Geochemistry，CAS
Wu, Qiong1,2,3; Zhang, Hua4,5; Ramezani, Jahandar6; Zhang, Fei-fei2,3; Erwin, Douglas H.7,8; Feng, Zhuo9,10; Shao, Long-yi11; Cai, Yao-feng4,5; Zhang, Shu-han2,3; Xu, Yi-gang1,12,13 ; Shen, Shu-zhong2,3
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| The terrestrial end-Permian mass extinction in the paleotropics postdates the marine extinction | |
| Source Publication | SCIENCE ADVANCES
 |
| ISSN | 2375-2548 |
| 2024-01-31 | |
| Volume | 10Issue:5Pages:12 |
| DOI | 10.1126/sciadv.adi7284 |
| Language | 英语 |
| WOS Research Area | Science & Technology - Other Topics |
| Abstract | The end-Permian mass extinction was the most severe ecological event during the Phanerozoic and has long been presumed contemporaneous across terrestrial and marine realms with global environmental deterioration triggered by the Siberian Traps Large Igneous Province. We present high-precision zircon U-Pb geochronology by the chemical abrasion-isotope dilution-thermal ionization mass spectrometry technique on tuffs from terrestrial to transitional coastal settings in Southwest China, which reveals a protracted collapse of the Cathaysian rainforest beginning after the onset of the end-Permian marine extinction. Integrated with high-resolution geochronology from coeval successions, our results suggest that the terrestrial extinction occurred diachronously with latitude, beginning at high latitudes during the late Changhsingian and progressing to the tropics by the early Induan, spanning a duration of nearly 1 million years. This latitudinal age gradient may have been related to variations in surface warming with more degraded environmental conditions at higher latitudes contributing to higher extinction rates. |
| WOS ID | WOS:001185617600014 |
| Indexed By | SCI |
| Citation statistics | |
| Document Type | 期刊论文 |
| Identifier | http://ir.gig.ac.cn/handle/344008/77212 |
| Collection | 同位素地球化学国家重点实验室 |
| Corresponding Author | Shen, Shu-zhong |
| Affiliation | 1.Southern Marine Sci & Engn Guangdong Lab Guangzhou, Guangzhou 511458, Peoples R China 2.Nanjing Univ, State Key Lab Mineral Deposits Res, Nanjing 210023, Peoples R China 3.Nanjing Univ, Sch Earth Sci & Engn, Nanjing 210023, Peoples R China 4.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, LPS, Nanjing 210008, Peoples R China 5.Chinese Acad Sci, Ctr Excellence Life & Paleoenvironm, Nanjing 210008, Peoples R China 6.MIT, Dept Earth Atmospher & Planetary Sci, Cambridge, MA 02139 USA 7.Natl Museum Nat Hist, Dept Paleobiol, MRC 121, Washington, DC 20013 USA 8.Santa Fe Inst, 1399 Hyde Pk Rd, Santa Fe, NM 87501 USA 9.Yunnan Univ, Inst Palaeontol, Yunnan Key Lab Earth Syst Sci, Yunnan Key Lab Palaeobiol,MEC Int Joint Lab Palaeo, Kunming 650500, Peoples R China 10.Southwest United Grad Sch, Kunming 650092, Peoples R China 11.China Univ Min & Technol Beijing, Coll Geosci & Surveying Engn, State Key Lab Coal Resources & Safe Min, Beijing 100083, Peoples R China 12.Chinese Acad Sci, State Key Lab Isotope Geochem, Guangzhou 510640, Peoples R China 13.Chinese Acad Sci, Guangzhou Inst Geochem, Ctr Excellence Deep Earth Sci, Guangzhou 510640, Peoples R China |
| Recommended Citation GB/T 7714 | Wu, Qiong,Zhang, Hua,Ramezani, Jahandar,et al. The terrestrial end-Permian mass extinction in the paleotropics postdates the marine extinction[J]. SCIENCE ADVANCES,2024,10(5):12. |
| APA | Wu, Qiong.,Zhang, Hua.,Ramezani, Jahandar.,Zhang, Fei-fei.,Erwin, Douglas H..,...&Shen, Shu-zhong.(2024).The terrestrial end-Permian mass extinction in the paleotropics postdates the marine extinction.SCIENCE ADVANCES,10(5),12. |
| MLA | Wu, Qiong,et al."The terrestrial end-Permian mass extinction in the paleotropics postdates the marine extinction".SCIENCE ADVANCES 10.5(2024):12. |
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