华南陆缘晚三叠-早、中侏罗世海平面相对升降与古气候演化的地球化学记录

许中杰; 程日辉; 张莉; 王嘹亮; 孔媛

doi:10.3799/dqkx.2012.011

Volume 37 Issue 1

Jan. 2012

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Article Navigation > Earth Science > 2012 > 37(1): 113-124

XU Zhong-jie, CHENG Ri-hui, ZHANG Li, WANG Liao-liang, KONG Yuan, 2012. The Geochemistry Records of Sea-Level Relative Movement and Paleoclimatic Evolution of the South China Continental Margin in Late Triassic-Early-Middle Jurassic. Earth Science, 37(1): 113-124. doi: 10.3799/dqkx.2012.011

Citation:

XU Zhong-jie, CHENG Ri-hui, ZHANG Li, WANG Liao-liang, KONG Yuan, 2012. The Geochemistry Records of Sea-Level Relative Movement and Paleoclimatic Evolution of the South China Continental Margin in Late Triassic-Early-Middle Jurassic. Earth Science, 37(1): 113-124. doi: 10.3799/dqkx.2012.011

Citation:

XU Zhong-jie, CHENG Ri-hui, ZHANG Li, WANG Liao-liang, KONG Yuan, 2012. The Geochemistry Records of Sea-Level Relative Movement and Paleoclimatic Evolution of the South China Continental Margin in Late Triassic-Early-Middle Jurassic. Earth Science, 37(1): 113-124. doi: 10.3799/dqkx.2012.011

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The Geochemistry Records of Sea-Level Relative Movement and Paleoclimatic Evolution of the South China Continental Margin in Late Triassic-Early-Middle Jurassic

doi: 10.3799/dqkx.2012.011

1.
College of Earth Sciences, Jilin University, Changchun 130061, China
2.
Guangzhou Marine Geological Survey, Guangzhou 510075, China

Received Date: 2010-12-28
Publish Date: 2012-01-15

Abstract

Abstract

The margin of South China in Late Triassic-Middle Jurassic had undergone multi transgression-regression cycles. The element geochemistry character indicates the paleosalinity and the water depth records the relative movements of the sea level. There are three levels of sea level change in the margin of South China. The grade III sea-level fluctuated frequently. There were 3 times in Late Triassic, 4 times in Early Jurassic and 2 times in Early or Middle Jurassic. These fluctuations constituted a large-scale transgression-regression cycle. The relative movements curve of the grade I sea-level is synchronous with the change of the long-period global sea-level curve in early Norian-late Sinemurian of the margin of South China. But it is contrary in late Sinemurian-Aalenian. The relative movements curve of the grade III sea-level and the short-period global sea-level curve occurred 4 fluctuations in Rhaetian-late Sinemurian. And they were almost simultaneously in time. The element migration and enrichment which were indicated by Sr/Cu reflected the warm-humid and dry-heat of the climate. The area of Middle Guangdong-East Guangdong in Late Triassic-Early-Middle Jurassic undergone the climate change of warm-humid to dry-heat and to warm-humid.
- the margin of South China,
- Early Mesozoic,
- sea-level change,
- paleoclimate,
- geochemistry,
- marine geology

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References(52)

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The Geochemistry Records of Sea-Level Relative Movement and Paleoclimatic Evolution of the South China Continental Margin in Late Triassic-Early-Middle Jurassic

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