Paleotemperature evolution and its driving mechanism during the formation of limestone-marl alternations in first member of Middle Permian Maokou Formation in Sichuan Basin

FAN Jianping; SONG Jinmin; LIU Shugen; JIANG Qingchun; LI Zhiwu; YANG Di; JIN Xin; SU Wang; YE Yuehao; HUANG Shipeng; WANG Jiarui; JIANG Hua; LUO Ping

doi:10.11781/sysydz202304726

Volume 45 Issue 4

Jul. 2023

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Article Navigation > PETROLEUM GEOLOGY & EXPERIMENT > 2023 > 45(4): 726-738

FAN Jianping, SONG Jinmin, LIU Shugen, JIANG Qingchun, LI Zhiwu, YANG Di, JIN Xin, SU Wang, YE Yuehao, HUANG Shipeng, WANG Jiarui, JIANG Hua, LUO Ping. Paleotemperature evolution and its driving mechanism during the formation of limestone-marl alternations in first member of Middle Permian Maokou Formation in Sichuan Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2023, 45(4): 726-738. doi: 10.11781/sysydz202304726

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FAN Jianping, SONG Jinmin, LIU Shugen, JIANG Qingchun, LI Zhiwu, YANG Di, JIN Xin, SU Wang, YE Yuehao, HUANG Shipeng, WANG Jiarui, JIANG Hua, LUO Ping. Paleotemperature evolution and its driving mechanism during the formation of limestone-marl alternations in first member of Middle Permian Maokou Formation in Sichuan Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2023, 45(4): 726-738. doi: 10.11781/sysydz202304726

Citation:

FAN Jianping, SONG Jinmin, LIU Shugen, JIANG Qingchun, LI Zhiwu, YANG Di, JIN Xin, SU Wang, YE Yuehao, HUANG Shipeng, WANG Jiarui, JIANG Hua, LUO Ping. Paleotemperature evolution and its driving mechanism during the formation of limestone-marl alternations in first member of Middle Permian Maokou Formation in Sichuan Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2023, 45(4): 726-738. doi: 10.11781/sysydz202304726

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Paleotemperature evolution and its driving mechanism during the formation of limestone-marl alternations in first member of Middle Permian Maokou Formation in Sichuan Basin

doi: 10.11781/sysydz202304726

1.
State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation (Chengdu University of Technology), Chengdu, Sichuan 610059, China
2.
Xihua University, Chengdu, Sichuan 610039, China
3.
PetroChina Research Institute of Petroleum Exploration & Development, Beijing 100083, China

Received Date: 2022-12-03
Rev Recd Date: 2023-04-29
Publish Date: 2023-07-28

Abstract

Abstract

From the Late Carboniferous to the end of Middle Permian, the most intense glacial event in history of Phanerozoic occurred and it is also the last transition period from icehouse stage to greenhouse stage in geological history. In this paper, the paleotemperature and paleoclimate in the first member of the Middle Permian Maokou Formation (Mao-1) were restored by means of thin section identification, scanning electron microscope, major elements, trace elements, carbon isotopes, oxygen isotopes and strontium isotopes, and the major climate evolution process and its driving mechanism in the Middle Permian were discussed. The results show that the biological assemblage type (mainly composed of foraminifera, brachiopods and molluscs, without reef-building organisms or calcareous green algae) and rock structure characteristics (supported by bioclastic and plaster, without oolitic or other non-skeletal particles) of the limestone-marl alternations in the Mao-1 member are similar to those of the international typical cool-water carbonate. During the limestone sedimentary period, the paleotemperature of seawater was 3.72 to 12.38 ℃ (8.15 ℃ in average, δ¹⁸O standard) or 13.79 to 14.28 ℃ (13.90 ℃ in average, ω(Mg)/ ω(Ca) standard), while during the marl sedimentary period, the paleotemperature of seawater was 7.00 to 14.24 ℃ (10.97 ℃ in average, δ¹⁸O standard) and 13.82 to 15.41 ℃ (14.27 ℃ in average, ω(Mg)/ω(Ca) standard). The paleotemperature changes in the sedimentary period of Mao-1 Member was mainly driven by the short eccentricity cycle of Milankovitch. The cyclical change of the short eccentricity was the driving mechanism of paleotemperature and paleoclimate cycle changes.
- limestone-marl alternation,
- cool-water carbonate,
- paleotemperature,
- first member of Maokou Formation,
- Middle Permian,
- Sichuan Basin

All authors disclose no relevant conflict of interests.
The study was designed by FAN Jianping, SONG Jinmin, LIU Shugen and LUO Ping. The experimental operation was completed by FAN Jianping, JIN Xin and WANG Jiarui. The manuscript was drafted and revised by FAN Jianping, SONG Jinmin, LIU Shugen, JIANG Qingchun, LI Zhiwu, YANG Di, SU Wang, YE Yuehao, HUANG Shipeng and JIANG Hua. All the authors have read the last version of paper and consented for submission.

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References(48)

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Paleotemperature evolution and its driving mechanism during the formation of limestone-marl alternations in first member of Middle Permian Maokou Formation in Sichuan Basin

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Paleotemperature evolution and its driving mechanism during the formation of limestone-marl alternations in first member of Middle Permian Maokou Formation in Sichuan Basin

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