Cukur, Deniz, Buchs, David M. ![]() Item availability restricted. |
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Abstract
Grain size analysis of the terrigenous fraction of sediments from IODP Site U1501 was used to characterize depositional patterns in the northern South China Sea since the middle Eocene (∼35 Ma). Fine sand dominates the lower sequence (∼457 to 440 m CSF-A), reflecting turbidite influence on the Chinese continental shelf (∼35-34 Ma). This is followed by a fining-upward trend (4 to 8 phi) marking transition to hemipelagic deposition mostly devoid of turbidites. A new silt-dominated sedimentation regime established at ∼30 Ma, which correlates to the initial expansion of the Pearl River. The regime is accompanied by stable source geochemical proxies (e.g., Zr/TiO 2 values) and remains unaffected by an unconformity (T60) and hiatus at ∼26.8–24.36 Ma. Grain size changes with stable geochemical proxies require variable intensities of terrigenous influx, that we propose reflect the dynamics of surface buoyant plumes and their controlling factors. At ∼16 Ma, sediment fines abruptly (4.7 to 7.5 phi) and grain size remains constant to present, reflecting drier conditions in the source area that began shortly afterward. Observed patterns suggest that grain size data from hemipelagic sediments devoid of turbidites can be combined with source tracers to help reconstruct the intensity of buoyant plumes over time.
Item Type: | Article |
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Date Type: | Published Online |
Status: | In Press |
Schools: | Schools > Earth and Environmental Sciences |
Publisher: | The Geological Society |
ISSN: | 0016-7649 |
Date of First Compliant Deposit: | 16 July 2025 |
Date of Acceptance: | 10 June 2025 |
Last Modified: | 16 Jul 2025 08:30 |
URI: | https://orca.cardiff.ac.uk/id/eprint/179658 |
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