NDLI: Pulsed turbidite and methane seep records in the north western South China Sea since the last glacial maximum

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Relationships between the Hadley circulation and tropical sea surface temperature with different meridional structures simulated in CMIP6 models

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Methane release effects on foraminiferal tests in northern South China Sea

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Diversification of cephalic shield shape and antenna in phyllosoma I of slipper and spiny lobsters (Decapoda: Achelata)

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Integrated Multi-Trophic Aquaculture (IMTA): Strategic model for sustainable mariculture in Samanco Bay, Peru

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Chronic cold-stress induced histopathological changes, oxidative stress, and alterations in liver functions and nutrient composition of hybrid red tilapia and the potential protection of unsaturated fatty acids

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Molecular identification of an insulin-like peptide from the swimming crab Portunus trituberculatus and evidence for its glucoregulation function

Response of nutrients and primary production to high wind and upwelling-favorable wind in the Arctic Ocean: A modeling perspective

Interannual modulations in sea level rise over tropical Northwest Pacific in satellite altimeter measurements

Reproductive performance of captive-reared Indian white shrimp, Penaeus indicus, broodstocks over two generations

Genome-wide identification, structural and evolutionary characteristics, and expression analysis of aquaporin gene family members in Mercenaria mercenaria

Eddy-induced sea surface salinity changes in the South China Sea

Spatial distribution of the demersal chondrichthyan community from the western Mediterranean trawl bycatch

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Pulsed turbidite and methane seep records in the north western South China Sea since the last glacial maximum

Content Provider	frontiers
Author	Li, Jingrui Miao, Xiaoming Feng, Xiuli Jiang, Rui Zhao, Mengwei Dan, Xiaopeng Xiao, Qianwen Wei, Jiangong
Abstract	The small-scale event layers in the continental margin contain abundant dynamic environment information, and pose a challenge to the interpretation of continuous sedimentary records, giving geological significance to their accurate identify and possible genesis. Here, pulsed turbidite layers since the last glacial maximum (LGM) in a gravity core in the northwestern South China Sea (SCS) was analyzed to investigate the precisely identification, possible causes and the role of marine environmental change during the late Quaternary in formation of these small-scale event layers in the SCS. Eight potential pulsed turbidite layers, according to the petrographic characteristics, grain size parameters and element geochemistry, were identified. Meanwhile, indicators including total sulfur (TS)/total organic carbon (TOC) ratio, CaCO3 content, and chromium-reducible sulfur (CRS) revealed these horizons were mostly related to methane seep events. Constrained by foraminifera shells AMS14C results, these events were determined to have occurred from the LGM to early Holocene, Similar records in the northern and southern slopes suggests the universal occurrence of these small-scale layers in the SCS. The comprehensive analysis showed that the development of these event layers over the past 25 ka can be divided into three stages, 25-15.5 ka, 15.5-7 ka and 7 ka to present. Late Quaternary ocean environment changes, especially sea level and bottom water temperature, controlled the occurrence of regional small-scale event layers in the SCS. The regional scale mechanism is that the pressure and temperature change affect the stability of hydrate and the methane seepage, and thus the strata stability. Corresponding to the lowest, the rapid increase and the highest levels of the sea level and bottom water temperature, the temporal evolution pattern of small-scale event layers in the SCS showed a highest, decreased and lowest frequency, respectively. The linkage between the late Quaternary marine environmental change and turbidite deposition through gas activities in this study can act as a useful reference for further understanding the continental margin sedimentary process.
ISSN	22967745
DOI	10.3389/fmars.2023.1147751
Volume Number	10
Journal	Frontiers in Marine Science
Language	English
Publisher Date	2023-03-03
Access Restriction	Open
Subject Keyword	Bottom water temperature Turbidite deposition Methane seep South China Sea Sea-level change
Content Type	Text
Resource Type	Article
Subject	Global and Planetary Change Oceanography Ocean Engineering Aquatic Science Water Science and Technology

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