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作 者:张武昌[1,2,3] 赵苑 董逸 李海波[1,2,3] 赵丽 肖天[1,2,3] ZHANG Wu-Chang;ZHAO Yuan;DONG Yi;LI Hai-Bo;ZHAO Li;XIAO Tian(CAS Key Laboratory of Marine Ecology and Environmental Sciences,Institute of Oceanology,Chinese Academy of Sciences,Qingdao 266071,China;Laboratory for Marine Ecology and Environmental Science,Pilot National Laboratory for Marine Science and Technology(Qingdao),Qingdao 266237,China;Center for Ocean Mega-Science,Chinese Academy of Sciences,Qingdao 266071,China)
机构地区:[1]中国科学院海洋研究所,中国科学院海洋生态与环境科学重点实验室,山东青岛266071 [2]青岛海洋科学与技术试点国家实验室,海洋生态与环境科学功能实验室,山东青岛266237 [3]中国科学院海洋大科学研究中心,山东青岛266071
出 处:《海洋与湖沼》2022年第2期247-260,共14页Oceanologia Et Limnologia Sinica
基 金:国家自然科学基金项目,42076139号,41576164号;中国科学院战略性先导科技专项,XDB42030402号。
摘 要:与太平洋和大西洋相比,印度洋有独特的季风和洋流系统和由此驱动的浮游生物分布及生产规律。在全球变暖的背景下,印度洋的变暖趋势比太平洋和大西洋更为显著,是研究变暖对海洋浮游生态系统影响的热点海区之一。文章结合国内外文献,评述印度洋浮游生态系统的现状、特点及对全球变暖的响应,包括印度洋的浮游生物地理分布、南北印度洋浮游生态系统的特点、印度洋特殊气候现象的生态学效应等内容。我国的印度洋浮游生态学研究正处于发展阶段,建议将跨越10°S不同生物地理分布区中浮游生物的交汇格局、低盐水覆盖的孟加拉湾独特最小含氧带浮游生态研究和东印度洋暖池区漂浮生物对海洋变暖的响应作为切入点。Compared with the Pacific and Atlantic Oceans,the Indian ocean has a unique system of monsoons and currents that drive the distribution and production of plankton.In the context of global warming,Indian Ocean has a more pronounced warming trend than that in the Pacific and Atlantic Oceans,making it one of the hotspots for studying the effects of warming on marine planktonic ecosystems.The status,characteristics and response to global warming of planktonic ecosystems in the Indian Ocean is reviewed.The main topics include the geographic distribution of plankton,the characteristics of planktonic ecosystems in the North and South Indian Ocean,and the ecological effects of special climatic phenomena.The study of plankton ecology in the Indian Ocean is in the development stage in China.The authors recommend the following research topics as entry points:the plankton convergence pattern across different biogeographic distribution areas spanning 10°S,the study of plankton ecology in the unique Oxygen Minimum Zone in the Bengal Bay covered by low salinity surface water,and the response of neuston to ocean warming in the Eastern Indian Ocean Warm Pool.
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