| 北冰洋楚科奇海陆架到陆坡表层沉积物有机碳载荷的变化 |
| |
| 引用本文： | 李中乔,王心怡,金海燕,季仲强,陈建芳.北冰洋楚科奇海陆架到陆坡表层沉积物有机碳载荷的变化[J].海洋学报(英文版),2017,36(8):131-136. |
| |
| 作者姓名： | 李中乔 王心怡 金海燕 季仲强 陈建芳 |
| |
| 作者单位： | 国家海洋局海洋生态系统与生物地球化学重点实验室, 杭州 301112,浙江大学海洋学院, 舟山 316021,国家海洋局海洋生态系统与生物地球化学重点实验室, 杭州 301112;卫星海洋环境动力学国家重点实验室, 杭州 310012,国家海洋局海洋生态系统与生物地球化学重点实验室, 杭州 301112,国家海洋局海洋生态系统与生物地球化学重点实验室, 杭州 301112 |
| |
| 基金项目： | The National Natural Science Foundation of China under contract Nos 41606211, 41276198, 41406217 and 41306200; the China Polar Environment Comprehensive Investigation and Assessment Programs under contract Nos Chinare-03-04 and Chinare-04-03; the National Science Foundation for Post-doctoral Scientists of China under contract No. 2016M591968; the Scientific Research Fund of Second Institute of Oceanography, SOA under contract No. JG1502. |
| |
| 摘 要： | 沉积物单位表面积上吸附的有机碳被广泛用于示踪有机碳载荷的变化。本文研究了北冰洋典型边缘海——楚科奇海表层沉积物的有机碳载荷。研究发现陆架区沉积物的有机碳载荷高于陆坡区。相比于已报道的东西伯利亚海和马更些河，楚科奇海陆坡区沉积物的有机碳载荷也较低。这种有机碳载荷的变化可能和陆坡区的初级生产力较低，以及沉积物在传输过程中经历的氧化降解有关。沉积物的有机碳含量和比表面积呈线性相关，在有机碳轴上有正截距，表明一部分有机碳来自于岩石的贡献。此外，陆架区低有机碳载荷的沉积物含有的岩石有机碳更高。本研究的数据有助于深刻理解楚科奇海区域的碳循环问题。
|
| 关 键 词： | 楚科奇海 北极 表层沉积物 有机碳载荷 碳循环 |
| 收稿时间： | 2016/3/30 0:00:00 |
Variations in organic carbon loading of surface sediments from the shelf to the slope of the Chukchi Sea, Arctic Ocean |
| |
| LI Zhongqiao,WANG Xinyi,JIN Haiyan,JI Zhongqiang and BAI Youcheng.Variations in organic carbon loading of surface sediments from the shelf to the slope of the Chukchi Sea, Arctic Ocean[J].Acta Oceanologica Sinica,2017,36(8):131-136. |
| |
| Authors: | LI Zhongqiao WANG Xinyi JIN Haiyan JI Zhongqiang and BAI Youcheng |
| |
| Institution: | Laboratory of Marine Ecosystem and Biogeochemistry, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China,Laboratory of Marine Chemistry and Environment, Ocean College, Zhejiang University, Zhoushan 316021, China,Laboratory of Marine Ecosystem and Biogeochemistry, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China;State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China,Laboratory of Marine Ecosystem and Biogeochemistry, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China and Laboratory of Marine Ecosystem and Biogeochemistry, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China |
| |
| Abstract: | The content of organic carbon (OC) normalized to the specific surface area (SSA) of sediment is widely used to trace variations in OC loading (OC/SSA). This study presents observations of OC/SSA of surface sediments collected in the Chukchi Sea, a typical Arctic marginal sea. Shelf sediments exhibit much higher OC/SSA values than slope sediments in the study area. Compared with OC/SSA values reported from the East Siberian Shelf and Mackenzie River, the slope sediments possess lower OC loading. This abrupt decrease in OC/SSA is mostly related to the lower primary production on slope as well as possible oxidization processes. The results of linear regression analysis between OC and SSA indicate a sedimentary source rock for the OC in the Chukchi Sea sediments. Moreover, shelf sediments with low SSA possess a larger rock OC fraction than slope sediments do. The dataset of the present study enables a more thorough understanding of regional OC cycling in the Chukchi Sea. |
| |
| Keywords: | Chukchi Sea Arctic surface sediments organic carbon loading carbon cycle |
| 本文献已被 CNKI SpringerLink 等数据库收录！ |
| 点击此处可从《海洋学报(英文版)》浏览原始摘要信息 |
| 点击此处可从《海洋学报(英文版)》下载免费的PDF全文 |
|
