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    Volume 46 Issue 9
    Oct.  2021
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    Chen Senran, Xu Zhongjie, Kong Jintao, Cheng Rihui, Wang Liaoliang, 2021. Paleoclimatic Evolution during Late Triassic-Early-Middle Jurassic in South Guangdong of South China Continental Margin and Its Responses to the Tectonic Regime Transition. Earth Science, 46(9): 3290-3306. doi: 10.3799/dqkx.2020.265
    Citation: Chen Senran, Xu Zhongjie, Kong Jintao, Cheng Rihui, Wang Liaoliang, 2021. Paleoclimatic Evolution during Late Triassic-Early-Middle Jurassic in South Guangdong of South China Continental Margin and Its Responses to the Tectonic Regime Transition. Earth Science, 46(9): 3290-3306. doi: 10.3799/dqkx.2020.265

    Paleoclimatic Evolution during Late Triassic-Early-Middle Jurassic in South Guangdong of South China Continental Margin and Its Responses to the Tectonic Regime Transition

    doi: 10.3799/dqkx.2020.265
    • Received Date: 2020-09-06
      Available Online: 2021-10-14
    • Publish Date: 2021-10-14
    • The Early Mesozoic tectonic regime transition in South China had a profound impact on the paleoclimate evolution in southern Guangdong,but the study of its internal relationship is still insufficient. In order to understand the response relationship,the mudstone samples collected from Xiaoping Formation,Jinji Formation and Qiaoyuan Formation in South Guangdong in Upper Triassic-Lower-Middle Jurassic were used for the main element analyses by X-ray fluorescence spectrometry,ICP-MS trace and rare earth element tests,combined with the comprehensive analysis of sedimentary and paleontological characteristics. According to the tests,the CIA (75.7-81.3),Sr/Cu (0.83-21.30),Rb/Sr (2.32-12.80),Mg/Ca (0.57-2.50) and Sr/Ba (0.04-0.19) of mudstone samples from Xiaoping Formation in Fenggang indicate that it was in a warm and humid climate in the Early Triassic,and the redox index δCe(0.93-0.95) indicates a weak oxidation environment,indirectly reflecting the warm and humid climate; The CIA (77.5-82.2),Sr/Cu (8.41-13.30),Rb/Sr (2.08-5.83),Mg/Ca (0.79-3.10) and Sr/Ba (0.06-0.26) of mudstone samples from Xiaoping Formation in Ma'an indicate that it was in a hot and dry climate in the Late Triassic,and the redox index δCe(1.04-1.05) indicates a reduction environment,indirectly reflecting the dry and hot climate; The CIA (77.1-82.3),Sr/Cu (1.51-4.38),Rb/Sr (2.16-12.10),Mg/Ca (0.84-2.94) and Sr/Ba (0.04-0.24) of mudstone samples from Jinji and Qiaoyuan formations indicate that the paleoclimate of Early Jurassic-Early-Middle Jurassic was mainly warm and humid,with a brief time of hot and dry climate. And the redox index δCe (0.92-1.00) indicates a weak reduction-weak oxidation environment,indirectly reflecting the paleoclimate was mainly warm and humid,with a brief time of hot and dry climate. Compared with other areas in South China continental margin,the paleoclimate underwent the same change of warm and humid (the early of Late-Triassic)-dry and heat (the late of Late-Triassic)-mainly warm and humid,dry and hot for a brief time (Early Jurassic-Early-Middle Jurassic). This evolution of paleoclimate in South Guangdong from Late Triassic to Early-Middle Jurassic is exactly in response to the transition from Tethys tectonic domain to paleo-Pacific tectonic domain.

       

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