Temporal variation of picoplankton in the spring bloom of Yellow Sea, China

CORC > 海洋研究所 > 中国科学院海洋研究所 > 海洋生态与环境科学重点实验室

	Temporal variation of picoplankton in the spring bloom of Yellow Sea, China
	Zhao, Yuan 1; Zhao, Li 1,2; Xiao, Tian 1; Liu, Chenggang 3; Sun, Jun 7; Zhou, Feng 4; Liu, Sumei 5; Huang, Lingfeng 6
刊名	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY
	2013-12-01
卷号	97 页码:72-84
关键词	Synechococcus Picoeukaryote Heterotrophic bacteria Spring bloom Yellow Sea
ISSN号	0967-0645
通讯作者	Xiao, T
中文摘要	Temporal variation of Synechococcus, picoeukaryote and heterotrophic bacteria abundance and depth integrated biomass during three spring blooms in 2007 and 2009 were investigated in the Yellow Sea, China. Synechococcus and picoeukaryote responded differently to different types and course of spring blooms. During the diatom blooms of 2007 and Bloom B20 in 2009, Synechococcus and picoeukaryote abundances decreased sharply during the bloom period. However, during a mixed dinoflagellate and diatom bloom of Bloom B23 in 2009, Synechococcus and picoeukaryote increased in abundance and biomass along the bloom. During all three spring blooms, heterotrophic bacteria biomass had a similar increasing trend. Ciliate and heterotrophic nanoflagellate grazing could be responsible for Synechococcus and picoeukaiyote abundance and biomass decrease during the spring blooms. (C) 2013 Elsevier Ltd. All rights reserved.
英文摘要	Temporal variation of Synechococcus, picoeukaryote and heterotrophic bacteria abundance and depth integrated biomass during three spring blooms in 2007 and 2009 were investigated in the Yellow Sea, China. Synechococcus and picoeukaryote responded differently to different types and course of spring blooms. During the diatom blooms of 2007 and Bloom B20 in 2009, Synechococcus and picoeukaryote abundances decreased sharply during the bloom period. However, during a mixed dinoflagellate and diatom bloom of Bloom B23 in 2009, Synechococcus and picoeukaryote increased in abundance and biomass along the bloom. During all three spring blooms, heterotrophic bacteria biomass had a similar increasing trend. Ciliate and heterotrophic nanoflagellate grazing could be responsible for Synechococcus and picoeukaiyote abundance and biomass decrease during the spring blooms. (C) 2013 Elsevier Ltd. All rights reserved.
学科主题	Oceanography
WOS标题词	Science & Technology ; Physical Sciences
类目[WOS]	Oceanography
研究领域[WOS]	Oceanography
关键词[WOS]	SUMMER PHYTOPLANKTON MAXIMUM ; NORTH-ATLANTIC OCEAN ; CHROOCOCCOID CYANOBACTERIA ; COASTAL WATERS ; HETEROTROPHIC BACTERIA ; EUTROPHIC RESERVOIR ; COMMUNITY ; MARINE ; DYNAMICS ; BACTERIOPLANKTON
收录类别	SCI
原文出处	10.1016/j.dsr2.2013.05.015
语种	英语
WOS记录号	WOS:000328807800008
公开日期	2014-07-17
内容类型	期刊论文
源URL	[http://ir.qdio.ac.cn/handle/337002/16497]
专题	海洋研究所_海洋生态与环境科学重点实验室
作者单位	1.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China 2.Chinese Acad Sci, Grad Univ, Beijing 10086, Peoples R China 3.State Ocean Adm, Inst Oceanog 2, Key Lab Marine Ecosyst & Biogeochem, Hangzhou 310012, Zhejiang, Peoples R China 4.State Ocean Adm, Inst Oceanog 2, State Key Lab Satellite Ocean Environm Dynam, Hangzhou 310012, Zhejiang, Peoples R China 5.Ocean Univ China, Coll Chem & Chem Engn, Minist Educ, Key Lab Marine Chem Theory & Technol, Qingdao 266100, Peoples R China 6.Xiamen Univ, Dept Oceanog, Xiamen 361005, Peoples R China 7.Tianjin Univ Sci & Technol, Coll Marine Sci & Engn, Tianjin 300457, Peoples R China
推荐引用方式 GB/T 7714	Zhao, Yuan,Zhao, Li,Xiao, Tian,et al. Temporal variation of picoplankton in the spring bloom of Yellow Sea, China[J]. DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY,2013,97:72-84.
APA	Zhao, Yuan.,Zhao, Li.,Xiao, Tian.,Liu, Chenggang.,Sun, Jun.,...&Huang, Lingfeng.(2013).Temporal variation of picoplankton in the spring bloom of Yellow Sea, China.DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY,97,72-84.
MLA	Zhao, Yuan,et al."Temporal variation of picoplankton in the spring bloom of Yellow Sea, China".DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY 97(2013):72-84.