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DOI | 10.1134/S0869593819040051 |
Marine Reptiles and Climates of the Jurassic and Cretaceous of Siberia | |
Rogov, M. A.1,2; Zverkov, N. G.1,3,4; Zakharov, V. A.1; Arkhangelsky, M. S.5,6 | |
发表日期 | 2019 |
ISSN | 0869-5938 |
EISSN | 1555-6263 |
卷号 | 27期号:4页码:398-423 |
英文摘要 | All current data on the Jurassic and Cretaceous climates of Siberia based on isotope, paleontological, and lithological proxies are summarized. The late Pliensbachian cooling episode, early Toarcian warming, promptly replaced by long-term Middle Jurassic cooling at the end of the Toarcian, and a long-term warm interval in the Late Jurassic are clearly recorded. From the end of the Ryazanian, a gradual cooling episode began, which apparently continued throughout the Early Cretaceous except for a brief warming episode in the early Aptian. At the beginning of the Late Cretaceous, the climate became warmer; the peak of warming is recorded at the Cenomanian-Turonian boundary. Then, the middle-late Turonian was marked by a relatively cold episode. Later, in the Coniacian-Campanian, the climate warmed again, but at the end of the Campanian another cooling episode occurred. New findings of marine reptiles are described from the Toarcian, Kimmeridgian, Volgian, and Santonian-Campanian deposits of north of Eastern Siberia. All existing records of marine reptiles known from the Jurassic and Cretaceous of Siberia are revised, and all the findings (from 51 localities) are positioned in relation to paleolatitudes. It is established that the majority of occurrences of these fossils were within the polar paleolatitudes (70 degrees-87 degrees). We found no direct correlation between climate fluctuations and the distribution of these organisms. Taking into account the newest data showing that representatives of the majority of Jurassic and Cretaceous large groups of marines reptiles were able to maintain a more or less constant body temperature and were also able to undertake large-scale seasonal migrations, it is reasonable to be cautious in interpreting the presence of remains of these animals as indicators of a warm climate. |
WOS研究方向 | Geology ; Paleontology |
来源期刊 | STRATIGRAPHY AND GEOLOGICAL CORRELATION
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/99546 |
作者单位 | 1.Russian Acad Sci, Inst Geol, Moscow 119017, Russia; 2.St Petersburg State Univ, St Petersburg 199034, Russia; 3.Moscow MV Lomonosov State Univ, Moscow 119991, Russia; 4.Russian Acad Sci, Borissiak Paleontol Inst, Moscow 117647, Russia; 5.Saratov State Tech Univ, Saratov 410054, Russia; 6.Saratov NG Chernyshevskii State Univ, Saratov 410012, Russia |
推荐引用方式 GB/T 7714 | Rogov, M. A.,Zverkov, N. G.,Zakharov, V. A.,et al. Marine Reptiles and Climates of the Jurassic and Cretaceous of Siberia[J],2019,27(4):398-423. |
APA | Rogov, M. A.,Zverkov, N. G.,Zakharov, V. A.,&Arkhangelsky, M. S..(2019).Marine Reptiles and Climates of the Jurassic and Cretaceous of Siberia.STRATIGRAPHY AND GEOLOGICAL CORRELATION,27(4),398-423. |
MLA | Rogov, M. A.,et al."Marine Reptiles and Climates of the Jurassic and Cretaceous of Siberia".STRATIGRAPHY AND GEOLOGICAL CORRELATION 27.4(2019):398-423. |
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