华南主要大河新生代演化：南海北缘沉积学记录的制约

张增杰; 田云涛; 孙习林; 闫义

doi:10.3799/dqkx.2025.027

Volume 50 Issue 7

Jul. 2025

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Article Navigation > Earth Science > 2025 > 50(7): 2775-2790

Zhang Zengjie, Tian Yuntao, Sun Xilin, Yan Yi, 2025. Cenozoic Evolution of Large Rivers in South China: Constraints from Sedimentary Archive in Northern South China Sea. Earth Science, 50(7): 2775-2790. doi: 10.3799/dqkx.2025.027

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Zhang Zengjie, Tian Yuntao, Sun Xilin, Yan Yi, 2025. Cenozoic Evolution of Large Rivers in South China: Constraints from Sedimentary Archive in Northern South China Sea. Earth Science, 50(7): 2775-2790. doi: 10.3799/dqkx.2025.027

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Cenozoic Evolution of Large Rivers in South China: Constraints from Sedimentary Archive in Northern South China Sea

doi: 10.3799/dqkx.2025.027

1.
Guangdong Provincial Key Laboratory of Geodynamics and Geohazards, School of Earth Sciences and Engineering, Sun Yat-sen University, Zhuhai 519082, China
2.
Faculty of Resources and Environment Science, Hubei University, Wuhan 430062, China
3.
Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China

Received Date: 2024-05-24
Publish Date: 2025-07-25

Abstract

Abstract

The India-Eurasia collision and the uplift of the Tibetan Plateau have profoundly changed the topography and climate patterns of Asia, triggering reorganization of large river systems. Recently, the evolution of large rivers on the northern South China Sea has become a frontier and hot issue in geoscience research. Offshore oil and gas exploration and the implementation of the International Ocean Drilling Program (IODP) have provided continuous and accurately dated sedimentary records for reconstructing the evolution of major rivers in South China. This paper reviews the sedimentary provenance investigations of the Cenozoic basins in the northern South China Sea in the past two decades, and discusses the progress in the evolution of major rivers in South China, such as the Red and Pearl Rivers. Provenance research in the Yinggehai Basin shows that the Red River has been the main supplier since the Late Eocene; and there are differences in provenance signals between the Yinggehai and large rivers of the Tibet Plateau (including the Nujiang, the Lancang and the Yangtze Rivers, indicating that they have not flowed into the Yinggehai Basin since the Late Eocene. During the Eocene to Early Oligocene, the Pearl River Mouth Basin was mainly supplied by the South China, indicating that the Pearl River was relatively small. Driven by the opening of the South China Sea in the Late Oligocene, the Pearl River expanded westward to the southeastern Tibetan Plateau. Cenozoic stratigraphy in Taiwan records that the ancient Minjiang River expanded westward to the Wuyi Mountain in the Late Oligocene. This evidence shows that the opening of the South China Sea controlled the evolution of the large rivers in South China.
- South China Sea,
- Pearl River,
- Red River,
- sedimentary provenance,
- large river evolution,
- sedimentology,
- marine geology

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References(98)

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Cenozoic Evolution of Large Rivers in South China: Constraints from Sedimentary Archive in Northern South China Sea

doi: 10.3799/dqkx.2025.027

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