Devonian sea surface temperature and paleoecology changes constrained by in situ oxygen isotopes of fish fossils
文献类型：期刊论文
| 作者 | Lu, Chang2,3,5; Cui, Xin-Dong1,4; Chen, Jun5; Cui, Ze-Xian5; Zhu, Min3,4 ; Xu, Yi-Gang2,3,5
|
| 刊名 | PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
 |
| 出版日期 | 2024-04-01 |
| 卷号 | 639页码:12 |
| 关键词 | Paleotemperature Paleoecology SIMS Oxygen isotope Devonian Fish enamel |
| ISSN号 | 0031-0182 |
| DOI | 10.1016/j.palaeo.2024.112059 |
| 通讯作者 | Xu, Yi-Gang(yigangxu@gig.ac.cn) |
| 英文摘要 | Significant changes occurred in both terrestrial and marine environments in the Devonian, during which complex terrestrial life radiated rapidly from the ocean. However, the reconstruction of the seawater temperatures for this period is still noticeably insufficient, largely due to a lack of appropriate geological archives especially in freshwater and near-shore marine deposits. In this study, we carried out a detailed characterization of microstructure, elements and isotopes of Early and Late Devonian fish fossils from Yunnan and Ningxia, China, respectively. The results show that fish enamels were relatively more resistant to diagenetic alteration than fossil dentine and bones, and can serve as valuable archives for Paleozoic temperature and ecology reconstruction. In situ oxygen isotopes of the enamel apatite (delta 18O(p)) of Early Devonian fossil fishes (sarcopterygians and antiarchs) vary from 16%o to 18%o, in good agreement with those of contemporaneous conodonts. The corresponding seawater temperatures are calculated to be >30degree celsius, therefore lending support to a greenhouse climate of the Early Devonian. In contrast, Late Devonian fish enamels tend to have lower delta 18Op than those of the contemporaneous conodonts. The difference in delta 18O(p) is attributable to the change in the living environment during the transition of the fish-to-tetrapod. |
| WOS关键词 | DIAGENETIC ALTERATION ; BIOGENIC APATITES ; CONODONT APATITE ; DELTA-O-18 ; PHOSPHATE ; EVOLUTION ; CARBONATE ; TEETH ; RECONSTRUCTION ; SEAWATER |
| 资助项目 | National Natural Science Foundation of China[42288201] ; PI Project of Southern Marine Science and Engineering Guangzhou Laboratory (Guangzhou)[GML2022006] |
| WOS研究方向 | Physical Geography ; Geology ; Paleontology |
| 语种 | 英语 |
| WOS记录号 | WOS:001178545500001 |
| 出版者 | ELSEVIER |
| 资助机构 | National Natural Science Foundation of China ; PI Project of Southern Marine Science and Engineering Guangzhou Laboratory (Guangzhou) |
| 源URL | [http://119.78.100.205/handle/311034/23487]  |
| 专题 | 中国科学院古脊椎动物与古人类研究所 |
| 通讯作者 | Xu, Yi-Gang |
| 作者单位 | 1.Peking Univ, Sch Earth & Space Sci, Key Lab Orogen Belts & Crustal Evolut, Minist Educ, Beijing 100871, Peoples R China 2.Southern Marine Sci & Engn Guangdong Lab Guangzhou, Guangzhou 511458, Peoples R China 3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 4.Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, CAS Key Lab Vertebrate Evolut & Human Origins, Beijing 100044, Peoples R China 5.Chinese Acad Sci, State Key Lab Isotope Geochem, Guangzhou Inst Geochem, Guangzhou 510640, Peoples R China |
| 推荐引用方式 GB/T 7714 | Lu, Chang,Cui, Xin-Dong,Chen, Jun,et al. Devonian sea surface temperature and paleoecology changes constrained by in situ oxygen isotopes of fish fossils[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2024,639:12. |
| APA | Lu, Chang,Cui, Xin-Dong,Chen, Jun,Cui, Ze-Xian,Zhu, Min,&Xu, Yi-Gang.(2024).Devonian sea surface temperature and paleoecology changes constrained by in situ oxygen isotopes of fish fossils.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,639,12. |
| MLA | Lu, Chang,et al."Devonian sea surface temperature and paleoecology changes constrained by in situ oxygen isotopes of fish fossils".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 639(2024):12. |
入库方式： OAI收割
来源：古脊椎动物与古人类研究所
浏览0
下载0
收藏0
其他版本
除非特别说明，本系统中所有内容都受版权保护，并保留所有权利。