末次冰盛期以来冲绳海槽古海洋环境研究进展

何炽鹏; 李冬玲; 李正; 沙龙滨; 翟滨; 汤佳冰; 李显富

doi:10.11928/j.issn.1001-7410.2020.06.17

末次冰盛期以来冲绳海槽古海洋环境研究进展

- 1.
  宁波大学, 地理与空间信息技术系, 浙江宁波 315211
- 2.
  青岛海洋科学与技术试点国家实验室, 海洋地质过程与环境功能实验室, 山东青岛 266237
- 3.
  自然资源部天然气水合物重点实验室, 青岛海洋地质研究所, 山东青岛 266071
- 4.
  青岛海洋科学与技术国家实验室, 海洋矿产资源评价与探测技术功能实验室, 山东青岛 266237
基金项目:
国家自然科学基金项目（批准号：41776193、41876215和41876070）、青岛海洋科学与技术国家实验室海洋地质过程与环境功能实验室开放基金项目（批准号：MGQNLM201707）和山东省重大科技创新工程专项项目（批准号：2018SDKJ0104）共同资助

详细信息

作者简介:
何炽鹏, 男, 24岁, 硕士研究生, 海洋地理学专业, E-mail:1911073004@nbu.edu.cn

通讯作者: 沙龙滨, E-mail:shalongbin@nbu.edu.cn

中图分类号: P722;P5322

收稿日期: 2020-06-18

修回日期: 2020-09-27

刊出日期: 2020-11-30

Research progress in the paleoenvironment around the Okinawa Trough since the Last Glacial Maximum

- 1.
  Department of Geography and Spatial Information Technology, Ningbo University, Ningbo 315211, Zhejiang
- 2.
  Laboratory for Marine Geology, Pilot National Laboratory for Marine Science and Technology(Qingdao), Qingdao 266237, Shandong
- 3.
  Key Laboratory of Gas Hydrate, Ministry of Natural Resources, Qingdao Institute of Marine Geology, Qingdao 266071, Shandong
- 4.
  Laboratory for Marine Mineral Resources, Pilot National Laboratory for Marine Science and Technology(Qingdao), Qingdao 266237, Shandong

More Information

Corresponding author: Sha Longbin, E-mail: shalongbin@nbu.edu.cn

Received Date: 18 June 2020

Revised Date: 27 September 2020

Publish Date: 30 November 2020

摘要

摘要:
冲绳海槽处于东海与西太平洋边缘的交界处，不仅对全球气候变化响应敏感，其环境变化也影响着东亚边缘海，乃至东亚大陆的环境，是研究古海洋环境的理想区域。该区域的古海洋环境研究多集中于末次冰盛期以来，因此本文以冲绳海槽为主体，总结了该区域末次冰盛期以来古海洋环境变化的相关研究，主要包括3个方面：古海平面、温度和盐度等；沉积物来源及其演化；黑潮及其对海洋环境的影响。该区域末次冰盛期以来的环境变化可大致分为，主要由海平面控制为主的末次冰盛期-早全新世和由黑潮、季风等因素控制的早全新世-现代两个主要的阶段。沉积物主要来自古黄河、长江、日本、台湾岛以及火山喷发物质等，但不同区域、不同时间的物质来源存在差异。另外，黑潮是该区域最主要的海流，其路径和强度末次冰盛期以来经历多次变化，并对其他海洋环境要素产生重大的影响。综合上述研究，提出未来应该系统建立冲绳海槽海洋环境演化历史、加强黑潮对周边流系的影响和陆源物质源-汇过程的系统研究。
- 冲绳海槽 /
- 末次冰盛期 /
- 古海洋
Abstract:
The Okinawa Trough, located at the boundary of the East China Sea and the West Pacific Ocean, is not only sensitive to changes in global climate as well as the local environment, but also affects the environment of the East Asian Marginal Sea and the Asian continent. It is an ideal area to investigate paleoceanography and continent-ocean interactions because of its continuous sedimentation and the rapid paleoenvironmental changes. Most studies of the paleoceanography in the region have focused on the period since the Last Glacial Maximum. This study attempts to summarize those studies, examining three main aspects:(1) The sea level, paleotemperature and paleosalinity changes, (2) the change and trace of the sediment provenance, and (3) the Kuroshio Current and its impact on the oceanic environment. Firstly, the environmental changes since the Last Glacial Maximum in this region can be roughly divided into two main stages:(1) The Last Glacial Maximum to the Early Holocene, in which environment changes are largely determined by sea level, and (2) the Early Holocene to present, in which environmental changes are heavily influenced by factors such as the Kuroshio Current and monsoons. Secondly, the sediments in this area are mainly from the Yellow River, Yangtze River, Japan, Taiwan Island and volcanic eruption, varying in proportion over time. Thirdly, the Kuroshio Current, as the most important current in the region, has undergone many changes since the Last Glacial Maximum, and has exerted significant influences on other elements of the marine environment. As a matter of conclusion, it is urged that scientists in the future do more systematic research of the evolution of the oceanic environment of the Okinawa Trough, the source-sink process of terrestrial materials, and the impact of the Kuroshio Current on the surrounding current system and overall oceanic environment.
- Okinawa Trough /
- Last Glacial Maximum /
- paleooceanography

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图 1
冲绳海槽区域概况及各钻孔位置分布(钻孔位置参考表 1)

Figure 1.
Regional overview of the Okinawa Trough and the distribution of sediment cores(for core locations, refer to Table 1)

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