引用本文:	孙晓霞,孙松.胶州湾浮游植物粒级结构及其时空变化.海洋与湖沼,2012,43(3):411-418.

【打印本页】【HTML】【下载PDF全文】【查看/发表评论】【下载PDF阅读器】【关闭】

过刊浏览高级检索

本文已被：浏览 2461次下载 2197次	码上扫一扫！
分享到：微信更多字体:加大+\|默认\|缩小-
胶州湾浮游植物粒级结构及其时空变化
孙晓霞¹, 孙松^1,2
1.中国科学院海洋研究所山东胶州湾海洋生态系统国家野外科学观测研究站;2.中国科学院海洋研究所海洋生态与环境科学重点实验室

摘要:

基于 2003—2010 年间对胶州湾分粒级叶绿素a 浓度的连续观测, 系统研究了胶州湾浮游植物粒级结构的季节变化、年际变化及长期变化特征。结果表明, 胶州湾表层浮游植物粒级组成以小型和微型浮游植物为主, 其浓度由东北部和北部向湾中间及湾外逐渐递减。不同区域分粒级叶绿素a浓度的季节与年际变化规律相似。小型和微型浮游植物表现出明显的双峰型季节变化, 小型浮游植物的高峰值通常出现在冬季, 而微型浮游植物则出现在夏季。长期变化结果表明, 冬季小型浮游植物所占比例自90 年代起表现为增加的趋势, 而夏季的变化规律与冬季相反, 自1998 年开始, 小型浮游植物所占比例下降, 微型浮游植物比例有所上升。春季和秋季小型和微型浮游植物的贡献率没有表现出明显的升高或降低趋势, 但微微型浮游植物的贡献率在2000 年之后显著低于2000 年之前。统计分析结果表明, 温度、营养盐浓度与结构是影响胶州湾浮游植物粒级结构变动的重要因素。

关键词: 浮游植物, 粒级结构, 时空变化, 胶州湾

DOI：10.11693/hyhz201203003003

分类号:

基金项目:中国科学院知识创新工程重要方向项目群项目, KZCX2-YW-Q07-01 号; 国家重点基础研究发展计划(973)项目,2011CB403603 号; 中国科学院战略性先导科技专项, XDA05030401 号; 国家自然科学基金项目, 40876083 号

附件

PHYTOPLANKTON SIZE STRUCTURE AND ITS TEMPORAL AND SPATIAL CHANGES IN JIAOZHOU BAY

SUN Xiao-Xia¹, SUN Song^1,2

1.Jiaozhou Bay Marine Ecosystem Research Station, Institute of Oceanology, Chinese Academy of Sciences;2.Key Laboratory of Marine Ecology and Environmental Science, Institute of Oceanology, Chinese Academy of Sciences

Abstract:

On the basis of the monthly observation of concentrations of size-fractionated Chl.a during 2003—2010, the phytoplankton size structure and its seasonal, annual, and long term changes in Jiaozhou Bay were studied. Results indicated that the micro- and nano-phytoplankton were the main components in the phytoplankton community in Jiaozhou Bay. The concentration of Chl.a decreased from the north and northeast to the middle and the south of the bay. The seasonal and annual changes of the size-fractionated Chl.a concentrations were similar in different areas of the bay. The micro- and nano-phytoplankton showed a seasonal change of double-peak, with the micro-phytoplankton peak in winter and nanophytoplankton peak in summer. The percentage of the micro-, nano- and pico-phytoplankton in different areas were similar. The results of the long term changes indicated that the percentage of the micro-phytoplankton was increasing since 1990s in the winter, and the nano-phytoplankton percentage increases in the summer. The percentage of pico-phytoplankton significantly decreased after 2000. The temperature, the concentration and structure of nutrients were important factors affecting the change of the size fractionated Chl.a in Jiaozhou Bay.

Key words: Phytoplankton, Size structure, Temporal and spatial change, Jiaozhou Bay