Tectonics Modulated Long‐Term Weathering Inputs From the East Asian Continent and Tropical Island Arc to the South China Sea Since the Late Oligocene

Abstract The chemical weathering of Earth's silicate rocks regulates the global climate. However, the exact role of continental weathering with orogenic building and island arc weathering with arc‐continent collisions remains unclear. Here, we established a seawater neodymium isotopic composition ( ε Nd ) record for the northern South China Sea (SCS) since 28 Ma, retrieving from planktonic foraminifera at International Ocean Discovery Program Site U1501. The progressively restricted SCS connection from the Pacific Ocean and intensified weathering inputs from the East Asian Continent correspond to an unradiogenic trend of ε Nd records between 17 and 9 Ma. The radiogenic trend of ε Nd records since 9 Ma could be induced by enhanced tropical island arc weathering inputs in the context of the Luzon Arc‐Eurasian Continent collision, which resulted in significant atmospheric CO 2 consumption. This study highlights that enhanced weathering of tropical island arc potentially significantly contributed to global cooling since the late Miocene.

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Publication Details

Journal
Geophysical Research Letters
Published
2025-05-14
DOI
https://doi.org/10.1029/2024gl114500
Citations
1
Primary Topic
Geological and Geophysical Studies
Type
article
Field-Weighted Citation Impact
2.35

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article

Tectonics Modulated Long‐Term Weathering Inputs From the East Asian Continent and Tropical Island Arc to the South China Sea Since the Late Oligocene

Hualong Jin, Christophe Colin, Anchun Li, Zehua Song et al.
1 citations
Geophysical Research Letters
Geological and Geophysical Studies
2.35
article

Tectonics Modulated Long‐Term Weathering Inputs From the East Asian Continent and Tropical Island Arc to the South China Sea Since the Late Oligocene

Hualong Jin, Christophe Colin, Anchun Li, Zehua Song, Debo Zhao, Zhaojie Yu, Zhimin Jian, Arnaud Dapoigny, Mengjun Li, Jin Zhang, Shiming Wan
article en
1 citations

Abstract

Abstract The chemical weathering of Earth's silicate rocks regulates the global climate. However, the exact role of continental weathering with orogenic building and island arc weathering with arc‐continent collisions remains unclear. Here, we established a seawater neodymium isotopic composition ( ε Nd ) record for the northern South China Sea (SCS) since 28 Ma, retrieving from planktonic foraminifera at International Ocean Discovery Program Site U1501. The progressively restricted SCS connection from the Pacific Ocean and intensified weathering inputs from the East Asian Continent correspond to an unradiogenic trend of ε Nd records between 17 and 9 Ma. The radiogenic trend of ε Nd records since 9 Ma could be induced by enhanced tropical island arc weathering inputs in the context of the Luzon Arc‐Eurasian Continent collision, which resulted in significant atmospheric CO 2 consumption. This study highlights that enhanced weathering of tropical island arc potentially significantly contributed to global cooling since the late Miocene.

Geophysical Research LettersVol. 52(10)
Tongji University (CN), Centre National de la Recherche Scientifique (FR), Université de Versailles Saint-Quentin-en-Yvelines (FR), Chinese Academy of Sciences (CN), Commissariat à l'Énergie Atomique et aux Énergies Alternatives (FR), Université Paris-Saclay (FR), Institute of Oceanology (CN), Qingdao National Laboratory for Marine Science and Technology (CN), Laboratoire des Sciences du Climat et de l'Environnement (FR), CEA Paris-Saclay (FR), Geosciences Paris-Saclay (FR)
National Natural Science Foundation of China, Chinese Academy of Sciences, National Key Research and Development Program of China
Life below water
Openalex Percentile: Top 13%
Geological and Geophysical Studies
2.35
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