Astronomically paced climate evolution during the Late Paleozoic icehouse-to-greenhouse transition

• Published in: Global and Planetary Change
• Main Authors: Fang, Qiang, Wu, Huaichun, Shen, Shu-zhong, Fan, Junxuan, Hinnov, Linda A., Yuan, Dongxun, Zhang, Shihong, Yang, Tianshui, Chen, Jun, Wu, Qiong
• Format: Report
• Language: English
• Published: ELSEVIER 2022
• Subjects: Long-term obliquity; Artinskian and Kungurian; Climate transition; Continental aridification; Oceanic anoxia; CONODONTS; CARBON; CYCLE; Physical Geography; Geology; Geography; Physical; Geosciences; Multidisciplinary; Ice Sheet
• Online Access: http://ir.nigpas.ac.cn/handle/332004/40911; http://ir.nigpas.ac.cn/handle/332004/40912; https://doi.org/10.1016/j.gloplacha.2022.103822

Late Paleozoic deglaciation is Earth's first icehouse-to-greenhouse transition with extensive vegetation, but the response of tropical climate to this transition has not yet been fully addressed. Here, cyclostratigraphic analysis was conducted on the magnetic susceptibility (MS) record of a deep marine carbonate succession in South China to construct the astrochronology of late Cisuralian (Early Permian), and decipher the evolutionary response to the climate transition in the MS and delta C-13(carb) time series. The constructed astronomical time scale indicates an age of 272.83 +/- 0.2 Ma for the Cisuralian-Guadalupian boundary in South China. Synchronizing global records demonstrates a complicated linkage between low and high latitudes, involving secular changes in atmospheric pCO(2), ice volume, tropical climate and carbon cycling. In the final stage of the Early Permian icehouse (~290-288.2 Ma), the delivery of moisture from low to high latitudes was reduced in comparison with that in the icehouse apex. A more humid climate facilitated the development of tropical coal forests and more storage of C-12 on land. In a full greenhouse condition (~281-272 Ma), the tropical responses to a rise in atmospheric pCO(2) involved continental drying and ocean stagnation. On a shorter time scale, the nodes of 1.36 Myr obliquity cycles triggered ice-sheet expansion and enhanced tropical precipitation during an icehouse condition. With the gradual transition to an arid greenhouse, the insolation-climate relationship began to change at ~285.1 Ma, and the obliquity nodes became associated instead with terrestrial aridity and marine anoxia. These results bring into a focus pattern of shifting dynamics involving Earth's astronomical parameters and climate change for icehouse and greenhouse worlds in the Late Paleozoic Era.