深層縁海における底層付近の浮遊粒子状物質濃度の人為的持続的増加
Zhuangcai Tian1, Xiujun Guo2, Jiaming Xiang2
1Shandong Provincial Key Laboratory of Marine Engineering Geology and the Environment, Ocean University of China, Qingdao 266100, China; State Key Laboratory of Intelligent Construction and Healthy Operation and Maintenance of Deep Underground Engineering, China University of Mining and Technology, Xuzhou 221116, P. R. China.
Abstract:
Anthropocene sediment flux from land to sea has quadrupled from 1950 to 2010, mainly due to mineral extraction. The distribution of suspended particulate matter (SPM) in the deep sea influences the marine environment, sedimentation processes, and material cycling. Using long-term survey data and published findings, we observed an upward trend in near-bottom SPM across three representative marginal seas by profile data from the same month or season with time spans ranging from 3 to 10 years. In the South China Sea, four stations indicate a consistent increasing trend in near-bottom SPM, with an average increase of more than twofold, although the rate of increase varied across different regions and depths. Similarly, profiles from the Gulf of Mexico and the Mediterranean Sea also demonstrated an upward trend in near-bottom SPM. These three marginal seas are known hotspots for bottom trawling, with frequent engineering activities and mining. Human activities, especially bottom trawling, are identified as the primary drivers behind the ongoing increase in near-bottom turbidity in these marginal seas. As human activities continue to escalate, it is anticipated that near-bottom SPM in these marginal seas may rise in the future.
関連する概念動画
Primary Production
Global Climate Change
The Sulfur Cycle


