Late Holocene elemental and isotopic carbon and nitrogen records from the East China Sea inner shelf: Implications for monsoon and upwelling
文献类型：期刊论文
| 作者 | Hu, BQ ; Li, J ; Zhao, JT ; Wei, HL ; Yin, XJ ; Li, GG ; Liu, Y ; Sun, ZL ; Zou, L ; Bai, FL ; Dou, YG ; Wang, LB ; Sun, RT |
| 刊名 | MARINE CHEMISTRY
 |
| 出版日期 | 2014 |
| 卷号 | 162页码:60-70 |
| 关键词 | East China Sea Stable isotopes East Asian monsoon Upwelling Late Holocene |
| ISSN号 | 0304-4203 |
| 通讯作者 | junli741001@gmail.com |
| 中文摘要 | The East China Sea (ECS) is characterized by a relatively high riverine martial input that is associated with East Asian monsoon systems. In this study, we investigated a 272 cm-long sediment core (THB-2) from the ECS inner shelf for the AMS C-14 dating, grain size, total organic carbon (TOC), total nitrogen (TN), and stable carbon and nitrogen (delta C-13 and delta N-15) isotopes to provide insights into previous changes in the monsoon-climate and the intensity of the coastal upwelling. A three end-member (riverine, deltaic, and marine) mixing model was applied to determine the temporal variations in sedimentary organic matter sources. The transport and burial of the Changjiang riverine organic carbon in the ECS inner shelf is strongly controlled by the combined effects of the monsoon-climate and human activities during the late Holocene. The sedimentary delta N-15 records of the THB-2 core are more complex and may be best explained by changes in the nutrient utilization in the coastal zone surface waters. The downcore variations of the marine organic matter-delta N-15 are closely related to the intensity of East Asian summer monsoon during the last 3.6 ka. The stronger East Asian summer monsoon likely favored the intensive coastal upwelling and additional Changjiang discharge during the 3.6-2.7 ka and 0.4-0 ka periods, which triggered the greater relative nitrate utilization in the coastal surface water. (C) 2014 Elsevier B.V. All rights reserved. |
| 学科主题 | Chemistry ; Oceanography |
| 收录类别 | SCI |
| 资助信息 | National Key Basic Research Program of China [2013CB429701]; National Natural Science Foundation of China [41206049, 41006021, 41376079]; Open Foundation of the State Key Laboratory of Loess and Quaternary Geology [SKLLQG1107]; Open Foundation of the CAS Key Laboratory of Marginal Sea Geology [MSGL12-01]; Open Foundation of the Key Laboratory of Marine Hydrocarbon Resources and Environmental Geology [MRE201231] |
| 原文出处 | ELSEVIER SCIENCE BV |
| WOS记录号 | WOS:000337012700007 |
| 公开日期 | 2014-12-11 |
| 源URL | [http://ir.scsio.ac.cn/handle/344004/10624]  |
| 专题 | 南海海洋研究所_中科院边缘海地质重点实验室 |
| 推荐引用方式 GB/T 7714 | Hu, BQ,Li, J,Zhao, JT,et al. Late Holocene elemental and isotopic carbon and nitrogen records from the East China Sea inner shelf: Implications for monsoon and upwelling[J]. MARINE CHEMISTRY,2014,162:60-70. |
| APA | Hu, BQ.,Li, J.,Zhao, JT.,Wei, HL.,Yin, XJ.,...&Sun, RT.(2014).Late Holocene elemental and isotopic carbon and nitrogen records from the East China Sea inner shelf: Implications for monsoon and upwelling.MARINE CHEMISTRY,162,60-70. |
| MLA | Hu, BQ,et al."Late Holocene elemental and isotopic carbon and nitrogen records from the East China Sea inner shelf: Implications for monsoon and upwelling".MARINE CHEMISTRY 162(2014):60-70. |
入库方式： OAI收割
来源：南海海洋研究所
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