末次盛冰期以来南海北部神狐海域沉积有机质的组成特征及其古气候/环境意义

雷艳; 胡建芳; 向荣; 付少英; 李永祥; 曹怀仁

doi:10.3969/j.issn.0253-4193.2017.11.007

末次盛冰期以来南海北部神狐海域沉积有机质的组成特征及其古气候/环境意义

doi: 10.3969/j.issn.0253-4193.2017.11.007

1.
中国科学院广州地球化学研究所, 广东广州 510640;中国科学院大学, 北京 100049
2.
中国科学院广州地球化学研究所, 广东广州 510640
3.
中国科学院南海海洋研究所, 广东广州 510301
4.
广州海洋地质调查局, 广东广州 510760
5.
南京大学地球科学与工程学院, 江苏南京 210046

基金项目: 国家重点研发计划（2016YFA0601204）；广州海洋地质调查局"天然气水合物分解的沉积记录"项目（GZH201100311-02）；国家自然科学基金（41576053）；有机地球化学国家重点实验室自主课题项目（SKLOGA201603B）。

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出版历程
- 收稿日期: 2016-12-23
- 修回日期: 2017-03-24

Composition of sedimentary organic matter in Shenhu, northern South China Sea since the Last Glacial Maximum and its implication for paleoclimate

1.
Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China;University of Chinese Academy of Sciences, Beijing 100049, China
2.
Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
3.
South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China
4.
Guangzhou Marine Geological Survey, Guangzhou 510760, China
5.
School of Earth Sciences and Engineering, Nanjing University, Nanjing 210046, China

摘要

摘要: 通过对两根沉积柱GHE27L和GHE24L的总有机碳（TOC）、总氮（TN）、C/N比值及稳定碳同位素（δ¹³C_org）的分析，本文探讨了21.1 ka BP以来南海北部陆坡神狐海域沉积有机质的组成特征及可能的古气候/环境信息。沉积柱GHE27L的TOC含量、TN含量、C/N比值及δ¹³C_org值分别为0.53%~1.81%，0.07%~0.18%，8.2~16.0和-23.6‰~-20.3‰。沉积柱GHE24L各参数则分布为0.45%~1.65%，0.09%~0.24%，5.3~12.2和-22.6‰~-20.4‰。沉积柱总体有机质的剖面变化显示，末次盛冰期以来南海北部沉积有机质具有海洋和陆地混合来源，但以海洋有机质来源为主。冰期陆源有机质对总有机质的相对贡献比全新世高。末次盛冰期南海北部气候相对干旱，C₄植被发育。全新世夏季风增强、降雨增多。自2.0 ka BP以来，人类活动对南海北部海洋初级生产力产生一定的影响。
- 南海北部 /
- 末次盛冰期 /
- 稳定碳同位素 /
- 古气候
Abstract: The total organic carbon (TOC), total nitrogen (TN), C/N ratios and the stable carbon isotope of bulk sediment organic matter (δ¹³C_org) in the GHE27L and GHE24L cores, collected from Shenhu area in the northern South China Sea (NSCS), were analyzed to reveal the composition of sedimentary organic matter (OM) and the paleoclimate changes since the Last Maximum Glacial (LMG). The values of TOC, TN, C/N, and δ¹³C_org ranged from 0.53% to 1.81%, 0.07% to 0.18%, 8.2 to 16.0 and-23.6‰ to 20.3‰ in Core GHE27L, and 0.45% to 1.65%, 0.09% to 0.24%, 5.3 to 12.2 and-22.6‰ to-20.4‰ in Core GHE24L, respectively. The profiles of bulk OM indicated that the OM mixed origins from both terrigenous and marine OM, and that marine OC was the major source of OC in the NSCS since the LGM. The relative contribution of terrigenous OM in the glaciation was higher than that in the Holocene. The climate was dry and C₄ plants were to thrive in the NSCS during the last glaciation. The precipitation enhanced due to the strong summer Asian Monsoon in the NSCS during the Holocene. However, it seems that the primary productivity in the NSCS was impacted by the anthropogenic activities since the last 2.0 ka BP.
- northern South China Sea /
- Last Glacial Maximum /
- stable carbon isotope /
- paleoclimate

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