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印度尼西亚北部苏拉维斯蓝碧海峡2012-2015年东南季风期间浮游植物的变化
引用本文:唐森铭,RACHMAN Arief,FITRIA Nurul,THOHA Hikmah,陈彬.印度尼西亚北部苏拉维斯蓝碧海峡2012-2015年东南季风期间浮游植物的变化[J].海洋学报(英文版),2018,37(12):9-17.
作者姓名:唐森铭  RACHMAN Arief  FITRIA Nurul  THOHA Hikmah  陈彬
作者单位:自然资源部第三海洋研究所, 福建厦门 361005,印度尼西亚科学院海洋科学研究中心, 雅加达 14430,印度尼西亚科学院海洋科学研究中心, 雅加达 14430,印度尼西亚科学院海洋科学研究中心, 雅加达 14430,自然资源部第三海洋研究所, 福建厦门 361005
基金项目:The China-Indonesia Maritime Cooperation Fund Project"China-Indonesia Bitung Ecological Station Establishment".
摘    要:2013年4月,2014年5月,2012年6月和2015年10月在印度尼西亚北部苏拉维斯蓝碧海峡(Lembeh Strait)进行了4个航次的海洋生态调查,研究了蓝碧海峡的浮游植物种类组成,以及浮游植物群落结构的季节变化及其驱动因子。四个航次的调查中记录了5类浮游植物和416个种(类)。调查区浮游植物密度平均为2348cells/L,硅藻和甲藻种类最多。蓝藻种类最少,但丰度很高。季风转换期的4月份和10月份浮游植物丰度总量较低,东南季风期间5月份和6月份的浮游植物丰度较高。除了束毛藻(Trichodesmium)之外,常见种是浮游硅藻。浮游植物的丰度和多样性的季节性变化明显。海链藻(Thalassionema)、拟菱形藻(Pseudo-nitzschia)和蓝藻类的束毛藻对群落的不相似性贡献最大。由于蓝碧海峡南部营养盐浓度较高,南部水域的硅藻和甲藻密度稍高于海峡北部。虽然,南北两个水体中蓝藻的分布趋于均匀,但蓝碧海峡南部也有较高密度。与雅加达湾以及中国的一些海湾相比,蓝碧海峡的浮游植物丰度相当低。分析表明,SE季风期间上升流营养盐是左右浮游植物丰度月变化的重要因素。蓝碧海峡浮游生态系原始,且接近天然本底,人类活动背景噪声低,能够清晰地响应大环境的变化,是研究浮游生态系统的理想区域。

关 键 词:蓝碧海峡(Lembeh  Strait)  浮游植物多样性  群落变化  束毛藻  季风
收稿时间:2017/6/15 0:00:00

Phytoplankton changes during SE monsoonal period in the Lembeh Strait of North Sulawesi, Indonesia, from 2012 to 2015
TANG Senming,RACHMAN Arief,FITRIA Nurul,THOHA Hikmah and CHEN Bin.Phytoplankton changes during SE monsoonal period in the Lembeh Strait of North Sulawesi, Indonesia, from 2012 to 2015[J].Acta Oceanologica Sinica,2018,37(12):9-17.
Authors:TANG Senming  RACHMAN Arief  FITRIA Nurul  THOHA Hikmah and CHEN Bin
Institution:1.Third Institute of Oceanography, Ministry of Natural Resources, Xiamen 361005, China2.Research Center for Oceanography, Indonesian Institute of Sciences, Jakarta 14430, Indonesia
Abstract:Phytoplankton species composition and abundance in the Lembeh Strait waters was studied in four cruises of April 2013, May 2014, June 2012 and October 2015, during the period of monsoon transition time of SE monsoon. With data obtained the seasonal alternations of phytoplankton community structures and its driving factors were discussed. A total of 416 taxa belonging to 5 classes of phytoplankton were recorded in the four month surveys. Phytoplankton density was averaged 2 348 cell/L and diatoms and dinoflagellates had the most diversified species. Cyanobacterium was characterized by its low species numbers but high abundance in the waters of Lembeh Strait. Total phytoplankton abundance occurred low in April and October in the monsoon transition period and it raised high in May and June during the SE monsoon. Frequently occurred species were pelagic diatoms in addition to cyanobacterium Trichodesmium. Abundance and diversity of phytoplankton significantly differed seasonally. The diatoms Thalassionema and Pseudo-nitzschia, and cyanobacterium Trichodesmium contributed most to the community dissimilarities. Due to potentially higher nutrient supply in the south of Lembeh Strait, diatoms and dinoflagellates showed higher densities in the south than in the north of the strait. Though, cyanobacterium preferred distributing much evenly in all waters, it had higher density in the southern Lembeh Strait. Total phytoplankton abundance is quite low compared with the Jakarta Bay and some bays in China. Analysis showed that nutrients from upwelling forced by SE monsoon are the key factor varying the monthly phytoplankton abundances. Due to its primitive nature state, Lembeh water can be an ideal location for the study of pelagic ecosystem under merely the influence of macro environment changes with lower background noise from human activities.
Keywords:Lembeh Strait  phytoplankton diversity  community alternation  Trichodesmium  monsoon
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