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北太平洋大洋钻探研究进展
引用本文:张亚南, 仲义, 陈艇, 赵德博, 王敦繁, 盖聪聪, 姜兆霞, 蒋晓东, 刘青松. 北太平洋大洋钻探研究进展——古海洋与古气候[J]. 海洋地质与第四纪地质, 2022, 42(5): 16-32. doi: 10.16562/j.cnki.0256-1492.2022062501
作者姓名:张亚南  仲义  陈艇  赵德博  王敦繁  盖聪聪  姜兆霞  蒋晓东  刘青松
作者单位:1.南方科技大学海洋科学与工程系海洋磁学中心,深圳 518055;; 2.重庆师范大学长江上游湿地科学研究重庆市重点实验室,重庆 400047;; 3.中国科学院海洋研究所海洋地质与环境重点实验室,青岛 266071;; 4.中国海洋大学海底科学与探测技术教育部重点实验室,青岛 266100
基金项目:国家自然科学基金重点项目“南海与东菲律宾海协同演化研究”(92158208);国家自然科学基金“上新世亚北极太平洋硅藻种群特征及其环境控制因素”(41904069);同济大学海洋地质国家重点实验室开放课题“晚第四纪以来亚北极太平洋地区高-低纬度气候系统响应机制研究”(MGK202209);重庆师范大学博士启动/人才引进项目“三峡库区消落带沉积物环境磁学特征及其对重金属污染的指示”(20XLB021)
摘    要:北太平洋作为全球大洋环流的重要组成部分,在高低纬间热量和物质的传输与再分配方面起到重要的调控作用,进而影响到地球气候系统。基于过去50多年来的大洋钻探工作,前人在北太平洋地球科学的研究上取得了一系列的成果。本文回顾了北太平洋古海洋和古气候方面的研究进展,包括:(1)东亚夏季风和西部边界流演化,以及其对高低纬热量、水汽的传输;(2) 北太平洋中层水和深层水的性质变化、分布范围和驱动机制,以及冰期旋回中水体垂直交换作用的气候响应;(3) 风尘输入对亚洲内陆古环境的反映,及其对北太平洋生产力的铁肥效应。尽管前人针对上述科学问题都开展了相应的研究工作,但目前在对北太平洋上述几方面的认识上仍然存在着分歧。基于对前人研究的总结概括,本文最后提出了未来北太平洋研究的关键科学问题,强调了多圈层、多系统角度对深入认识过去地球气候系统变化的重要性,并对未来大洋航次开展的理想靶区进行了展望。

关 键 词:大洋钻探   东亚夏季风   西部边界流   风尘   生产力   北太平洋
收稿时间:2022-06-25
修稿时间:2022-08-02

Research progress of ocean drilling in the North Pacific Ocean: Paleoceanography and paleoclimate
ZHANG Yanan, ZHONG Yi, CHEN Ting, ZHAO Debo, WANG Dunfan, GAI Congcong, JIANG Zhaoxia, JIANG Xiaodong, LIU Qingsong. Research progress of ocean drilling in the North Pacific Ocean: Paleoceanography and paleoclimate[J]. Marine Geology & Quaternary Geology, 2022, 42(5): 16-32. doi: 10.16562/j.cnki.0256-1492.2022062501
Authors:ZHANG Yanan  ZHONG Yi  CHEN Ting  ZHAO Debo  WANG Dunfan  GAI Congcong  JIANG Zhaoxia  JIANG Xiaodong  LIU Qingsong
Affiliation:1.Southern University of Science and Technology, Department of Ocean Science and Engineering, Shenzhen 518055, China;; 2.Chongqing Normal University, Chongqing key laboratory of wetland science research in the upper Yangtze River, Chongqing 400047, China;; 3.Institute of Oceanology, Chinese Academy of Sciences, Key Laboratory of Marine Geology and Environment, Qingdao 266071, China;; 4.Ocean University of China, Key Laboratory of Submarine Geosciences and Prospecting Techniques, Qingdao 266100, China
Abstract:As an important part of global ocean circulation, the North Pacific Ocean plays a key role in regulating the transfer and redistribution of heat and matter between high and low latitudes, thus affecting the Earth’s climate system. Based on the ocean drilling programs over 50 years in the past, many achievements in geoscience have been made. We reviewed the progresses of paleoclimate research in the North Pacific in the following aspects: (1) the evolution of the East Asian summer monsoon and the western boundary current, as well as their contributions to the transportation of heat and water vapor between high and low latitudes in North Pacific; (2) changes in water property, distribution, and the driving mechanisms of the Pacific Deep Water and North Pacific Intermediate Water, as well as the climatic response of their interaction during glacial-interglacial cycles; (3) the response of aeolian flux to the Asian inland and its iron fertilization effect on the North Pacific productivity. Previous studies have addressed those scientific problems, uncertain issued remain controversial. We therefore proposed the key scientific issues for future research in the North Pacific Ocean, and emphasized the importance of multi-layer and multi-system perspectives for deciphering the past changes of the Earth's climate system. Finally, we suggested the ideal target areas for ocean drilling program in North Pacific in the future.
Keywords:ocean drilling  East Asian summer monsoon  western boundary current  eolian dust  productivity  North Pacific
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