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1.
1999年夏季首次在南海北部海域进行了微微型光合浮游生物(photosynthetic picoplankton)的观测研究,发现了聚球藻(Synechococcus,Syn)、原绿球藻(Prochlorococcus,Pro)和真核球藻(Eukaryotes,Euk)3类微微型光合浮游生物存在,并对其丰度与分布及其环境调控机制进行了研究.结果表明,研究海区Syn,Pro和Euk丰度的总平均值分别为(5.0±7.6)×104,(4.6±4.2)×104和(1.8±1.1)×103个/cm3,Syn种群丰度的高值大多出现在营养盐丰富的雷州半岛及海南岛东部海域的河口、沿岸带与陆架,北部湾次之,是陆坡和开阔海的数十分之一;其水层分布主要在跃层以上,跃层以下其值迅速降低,发现Pro存在两个不同种群:表层种群和深层种群,前者分布型式与Syn相似,后者的分布型式迥然不同,其丰度向营养盐贫瘠的外海、陆坡和开阔海显著增高;同时发现Pro水层分布的高值主要出现在真光层的底部,并往往出现在硝酸盐跃层之上,Euk在不同海域的分布差异不如Syn和Pro来得大,但仍以沿岸带与陆架为高,陆坡与开阔海较低,水层分布的高值大多出现在真光层的底部,而且它是对次表层叶绿素a极大值的主要贡献者,这些分布型式的差异,取决于环境的调控和3类生物生态生理适应的差异.研究海区Syn,Pro和Euk 3类微微型光合浮游生物对微微型光合浮游生物生态生理适应的差异.研究海区Syn,Pro和Euk3类微微型光合浮游生物对微微型光合浮游生物群落总丰度的贡献分别为50.996,47.3%和1.8%. 相似文献
2.
2014年夏季南海北部超微型浮游植物分布及环境因子影响 总被引：3，自引：1，他引：2
利用流式细胞仪BD Accuri C6对2014年夏季南海北部超微型浮游植物进行了现场的观测研究,发现了3类超微型光合自养浮游植物,聚球藻(Synechococcus,Syn)、原绿球藻(Prochlorococcus,Pro)和超微型真核藻类(pico-eukaryotes,Euk),并对其丰度与分布以及环境因子影响进行了研究。结果表明,Syn、Pro和Euk丰度总平均值分别为5.13×103个/mL,3.27×104个/mL和1.85×103个/mL,碳生物量均值分别为1.19μg/L,1.86μg/L和4.51μg/L。Syn、Pro和Euk的丰度表现出不同的分布特征。Syn、Pro和Euk丰度分布趋势呈现近海低而外海高,Syn和Euk丰度高值区分别出现在沿岸带与陆架和上升流影响海域,Pro丰度高值区出现在沿岸带与陆架,低值区出现在上升流影响海域。Syn、Euk丰度高值区主要分布在次表层,Pro丰度高值区主要分布在真光层底部,Euk丰度垂直变化差异相对Syn和Pro较小。超微型浮游植物与环境因子的相关性分析结果表明,Syn、Pro和Euk的碳生物量均与硝酸盐、硅酸盐浓度和深度呈现负相关关系,Pro的碳生物量与磷酸盐浓度呈现正相关关系。 相似文献
3.
微微型浮游植物是水环境生态碳汇的重要基石之一,也是初级生产的重要执行者。选取了一个典型的陆海交界关键带环境——海南东寨港入海口水域,采集了东寨港红树林保护区开阔水域、入港河流和新埠海海端的微微型浮游植物的样品,通过流式细胞仪分析技术对样品进行分析,以探究它们在东寨港水域中的丰度、分布及环境指示意义。结果表明,冬季水域微微型浮游植物以真核浮游植物(Eukaryote,Euk)和聚球藻(Synechococcus,Syn)两大类群为主,其中聚球藻有两个亚群,分别为富含藻蓝蛋白聚球藻(Phycocyanin-rich,PC)和富含藻红蛋白聚球藻(Phycoerythrin-rich,PE)。Syn-PC、Syn-PE和Euk在东寨港水域表层水体的平均丰度分别为(2.61×104±1.09×104)、(3.06×104±7.05×103)、(1.56×105±8.03×104) cells/m L,底层水体的平均丰度分别为(2.64×104±... 相似文献
4.
Community structure of picoplankton abundance and biomass in the southern Huanghai Sea during the spring and autumn of 2006 总被引：2，自引：0，他引：2
During spring and autumn of 2006,the investigations on abundance,carbon biomass and distribution of picoplankton were carried out in the southern Huanghai Sea(Yellow Sea,sHS) . Three groups of picoplankton-Synechococcus(Syn) ,Picoeukaryotes(PEuk) and heterotrophic bacteria(BAC) were identified,but Prochlorococcus(Pro) was undetected. The average abundance of Syn and PEuk was lower in spring(5.0 and 1.3 × 10 3 cells/cm 3,respectively) than in autumn(92.4 and 2.7 × 10 3 cells/cm 3,respectively) ,but it was opposite for BAC(1.3 and 0.7 × 10 6 cells/cm 3 in spring and autumn,respectively) . And the total carbon biomass of picoplankton was higher in spring(37.23 ± 11.67) mg/m 3 than in autumn(21.29 ± 13.75) mg/m 3 . The ratios of the three cell abundance were 5:1:1 341 and 30:1:124 in spring and autumn,respectively. And the ratios of carbon biomass of them were 5:7:362 and 9:4:4 in spring and autumn,respectively. Seasonal distribution characteristics of Syn,PEuk,BAC were quite different from each other. In spring,Syn abundance decreased in turn in the central waters(where phytoplankton bloom in spring occurred) ,the southern waters and inshore waters of the Shandong Peninsula(where even Syn was undetected) ;the high values of PEuk abundance appeared in the central and southern waters and the inshore of the Shandong Peninsula;the abundance of BAC was nearly three order of magnitude higher than that of photosynthetic picoplankton,and high values appeared in the central waters. In autumn,Syn abundance in central waters was higher than that in surrounding waters,while for PEuk abundance,it decreased in turn in the inshore waters of the Shandong Peninsula,the southern waters and the central waters;BAC presented a complicated blocky type distribution. Sub-surface maximum of each group of picopalnkton appeared in both spring and autumn. Compared with the available literatures concerning the studied area,the range of Syn abundance was larger,and the abundance of BAC was higher. In addition,the conversion factors for calculating picoplanktonic carbon biomass were discussed,with the conversion factors which are different from previous studies in the same surveyed waters. The result of regression analysis showed that there was distinct positive correlation between BAC and photosynthetic picoplankton in spring(r=0.61,P 0.001) ,but no correlation was found in autumn. 相似文献
5.
Standing stock and community structure of photosynthetic picoplankton in the northern South China Sea 总被引：1，自引：0，他引：1
1 Introduction Forthe lastm ore than 20 a,ow ing to the develop-m ent of observation and experim ent technologies form arine m icroorganism s,m arine biologistshave discov-ered m any m icroorganism s w hich are difficult to beobserved by com m on m icroscope before. T hus, thecognition to the m arine phytoplankton com m unitiesand the structure of food chains has achieved im por-tantprogress.E specially,w ith the developm entand ap-plication of epifluorescence m icroscopy and flow cy-tom etry… 相似文献
6.
During Nov. 2006 and Feb. 2007, two investigations were carried out to investigate the abundance, carbon biomass, and distribution
of picoplankton (Pico) and its relationship to the hydrological regime in the East China Sea (ECS). Pico consisted of three
groups of photosynthetic picoplankton (phPico)—Synechococcus (Syn), Prochlorococcus (Pro) and Picoeukaryotes (PEuk)—and heterotrophic bacteria (HBAC). The average abundance of Pro, PEuk and HBAC was lower
in autumn than in winter, but for Syn the opposite trend was observed. Water temperature, salinity, and stability of water
column influenced Pico distribution in both seasons. Regression analysis showed distinct positive correlations between HBAC
and phPico in both seasons. Syn contributed more to phPico in coastal waters, whereas Pro dominanted in the shelf and slope
areas. PEuk was the major contributor to carbon biomass. In the Pico community, HBAC was predominant, both in abundance and
in terms of carbon biomass. The phenomenon of subsurface chlorophyll maximum (SCM) was observed ubiquitously in the shelf
and slope area, and Pico organisms were the major contributors. 相似文献
7.
2009年冬、夏季南海北部超微型浮游生物的分布特征及其环境相关分析 总被引：2，自引：1，他引：1
2009年2月(冬季)和8月(夏季)在南海北部海域(nSCS)采用流式细胞术对聚球藻、原绿球藻、超微型光合真核生物3类超微型光合浮游生物和异养浮游细菌的丰度和碳生物量的时空分布特征进行了研究,并分析了其与环境因子之间的关系。结果表明,夏季聚球藻和原绿球藻的平均丰度高于冬季,超微型光合真核生物和异养浮游细菌的丰度反之,为冬季高于夏季。聚球藻、超微型光合真核生物和异养浮游细菌在富营养的近岸陆架海域丰度较高,而原绿球藻高丰度则出现在陆坡开阔海域。在垂直分布上,聚球藻主要分布在跃层以上,跃层以下丰度迅速降低;原绿球藻高丰度主要出现在真光层底部;超微型光合真核生物在水层中的高值同样出现在真光层底部,且与Pico级份叶绿素a浓度分布一致;异养浮游细菌在水体中的分布与聚球藻类似。这些分布格局的差异,取决于环境条件的变化和4类超微型浮游生物生态生理适应性的差异。在超微型光合浮游生物群落中,各类群碳生物量的贡献因季节和海域类型的不同而发生变化:聚球藻在夏季近岸陆架区占超微型光合浮游生物总碳生物量的41%,原绿球藻在陆坡开阔海成为主要贡献者(50%),超微型光合真核生物碳生物量以冬季为高(在近岸陆架区占比68%)。冬、夏季异养浮游细菌碳生物量均高于超微型光合浮游生物碳生物量。 相似文献
8.
夏季南黄海主要环境因子对微微型浮游生物分布影响 总被引：2，自引：1，他引：1
利用流式细胞技术, 获取南黄海夏季微微型浮游生物丰度数据, 分析了其组成和分布规律, 并探讨了主要的影响因子。2011年夏季, 聚球藻、微微型真核藻、异养细菌在整个调查海区的平均丰度分别在1×104、1×103、1×106 cells/mL数量级上。在全调查海区, 聚球藻和微微型真核藻受温度和光照的限制明显, 主要集中分布在温跃层及其以上水层;而营养盐的限制较小, 它们的影响只有在沿岸流影响明显的西部海区才能较为明显的体现出来。结果表明在该海域浓度较高的营养盐能够促进微微型浮游生物的生长, 但不是其限制因素;异养细菌受环境因子限制较小, 即使在深海也保持着较高的丰度。 相似文献
9.
黄海苏北浅滩海域春夏季浮游植物时空分布及其控制生态因子 总被引：1，自引：0，他引：1
The Subei Shoal is a special coastal area with complex physical oceanographic properties in the Yellow Sea. In the present study, the distribution of phytoplankton and its correlation with environmental factors were studied during spring and summer of 2012 in the Subei Shoal of the Yellow Sea. Phytoplankton species composition and abundance data were accomplished by Uterm?hl method. Diatoms represented the greatest cellular abundance during the study period. In spring, the phytoplankton cell abundance ranged from 1.59×10~3 to 269.78×10~3 cell/L with an average of 41.80×10~3 cell/L, and Skeletonema sp. and Paralia sulcata was the most dominant species. In summer, the average phytoplankton cell abundance was 72.59×10~3 cell/L with the range of 1.78×10~3 to 574.96×10~3 cell/L, and the main dominant species was Pseudo-nitzschia pungens, Skeletonema sp., Dactyliosolen fragilissima and Chaetoceros curvisetus. The results of a redundancy analysis(RDA) showed that turbidity,temperature, salinity, pH, dissolved oxygen(DO), the ratio of dissolved inorganic nitrogen to silicate and SiO_4-Si(DIN/SiO_4-Si) were the most important environmental factors controlling phytoplankton assemblages in spring or summer in the Subei Shoal of the Yellow Sea. 相似文献
10.
2006年冬季北黄海网采浮游植物群落结构 总被引：6，自引：1，他引：5
根据2006年12月30日—至2007年1月17日北黄海的调查资料,对该海域浮游植物的种类组成、优势种、丰度及其分布和多样性等基本状况进行了分析。本次调查共鉴定浮游植物4门68属131种,主要以温带近岸和广布性种为主,其中硅藻有53属113种,占总种数的86.3%,甲藻有11属16种,占总种数的12.2%。浮游植物丰度平均值为88.89×104个/m3,硅藻丰度平均值为86.58×104个/m3,甲藻丰度平均值为2.28×104个/m3,硅藻丰度分布趋势决定了浮游植物丰度的分布趋势。辽宁南岸是浮游植物密集区,山东半岛北岸其次,而北黄海中部是浮游植物的稀疏区。优势种为:短角弯角藻(Eucampia zodiacus)、具槽帕拉藻(Paralia sulcata)、尖刺拟菱形藻(Pseu-do-nitzschia pungens)、密连角毛藻(Chaetoceros densus)、柔弱角毛藻(Chaetoceros debilis)、刚毛根管藻(Rhizosolenia setigera)。浮游植物群落Shannon-Weiner物种多样性指数平均值为1.80,Peilou均匀度指数平均值为0.42。与1959年1月相比,2007年1月北黄海浮游植物丰度由150.00×104个/m3降为88.89×104个/m3,下降了近41%,硅藻丰度由148.00×104个/m3降为86.58×104个/m3,而甲藻丰度由1.25×104个/m3上升为2.28×104个/m3,占浮游植物丰度的比例由0.8%上升为2.5%。主要优势种及优势属也发生了一定程度的变化,但浮游植物群落结构仍以硅藻为主、甲藻其次,浮游植物丰度总的分布格局变化不明显。 相似文献
11.
12.
冬夏季南海西部固氮蓝藻 总被引：3，自引：0，他引：3
本研究分析了冬季东北季风期(2006年11月27日-12月16日)及夏季西南季风期(2007年8月11日-9月16日)南海西部越南沿岸区域(10°~17°N,108°~115°E)的网采浮游植物样品,探讨了冬夏两季南海西部固氮蓝藻的物种、丰度及分布特征,以及影响固氮蓝藻丰度与分布的环境因素。冬夏两季南海西部固氮蓝藻主要有束毛藻(Trichodesmium)和胞内植生藻(Richelia intracellularis),束毛藻物种包括铁氏束毛藻(Trichodesmium thiebaultii)、红海束毛藻(Trichodesmium erythraeum)以及汉氏束毛藻(Trichodesmium hildebrandtii),其中铁氏束毛藻为优势种,胞内植生藻主要与根管藻(Rhizosolenia sp.)共生。冬季时束毛藻藻丝体平均丰度为0.194×104 filaments/L,束毛藻细胞平均丰度为0.172×106 cells/L,胞内植生藻细胞平均丰度为0.255×104 cells/L,与笔尖形根管藻(Rhizosolenia styliformis)共生的胞内植生藻居多;蓝藻主要分布在调查海域的北部。夏季时束毛藻藻丝体平均丰度为2.995×104 filaments/L,束毛藻细胞平均丰度为6.007×106 cells/L,胞内植生藻细胞平均丰度为2.198×104 cells/L,与笔尖根管藻共生的胞内植生藻占优势。夏季时固氮蓝藻丰度高于冬季,胞内植生藻宿主更为多样化。本研究中温度及冷窝对蓝藻的分布有重要影响,而盐度单独对蓝藻分布的影响不大,与温度结合时表现出一定的限制作用。 相似文献
13.
Role of environment and hydrography in determining the picoplankton community structure of Sagami Bay,Japan 总被引：1，自引：0，他引：1
Smita Mitbavkar Toshiro Saino Naho Horimoto Jota Kanda Takashi Ishimaru 《Journal of Oceanography》2009,65(2):195-208
Seasonal variations in the picoplankton community were investigated from June 2002 to March 2004 within the photic zone of
Sagami Bay, Japan. The study area was mostly dominated by coastal waters during the warm period (mixed layer water temperature
≥ 18°C). During the cold period (mixed layer water temperature ≤ 18°C), the water mass was characterized by low temperature
and high saline waters indicative of the North Pacific Subtropical Mode Water (NPSTMW). Occasionally, a third type of water
mass characterized by high temperature and low saline properties was observed, which could be evidence of the intrusion of
warm Kuroshio waters. Synechococcus was the dominant picophytoplankton (5−28 × 1011 cells m−2) followed by Prochlorococcus (1−5 × 1011 cells m−2) and picoeukaryotes during the warm period. Heterotrophic bacteria dominated the picoplankton community throughout the year,
especially in the warm period. During the Kuroshio Current advection, cyanobacterial abundance was high whereas that of picoeukaryotes
and heterotrophic bacteria was low. During the cold period, homogeneously distributed, lower picophytoplankton cell densities
were observed. The dominance of Synechococcus in the warm period reflects the importance of high temperature, low salinity and high Photosynthetically Active Radiation
(PAR) on its distribution. Cyanobacterial and heterotrophic bacterial abundance showed a positive correlation with temperature.
Prochlorococcus and picoeukaryotes showed a positive correlation with nutrients. Picoeukaryotes were the major contributors to the picophytoplankton
carbon biomass. The annual picophytoplankton contribution to the photosynthetic biomass was 32 ± 4%. These observations suggest
that the environmental conditions, combined with the seasonal variability in the source of the water mass, determines the
community structure of picoplankton, which contributes substantially to the phytoplankton biomass and can play a very important
role in the food web dynamics of Sagami Bay. 相似文献
14.
南海北部夏、冬季今生颗石藻分布 总被引：1，自引：1，他引：0
本研究对2009年南海北部(17°~24°N,108°~122°E)夏季和2010年冬季的颗石藻群落结构进行了描述。颗石藻镜检工作以偏光显微镜为主,并辅助于扫描电镜进行物种的鉴定与计数,共鉴定物种11属13种。总体来说,冬季的颗石藻细胞丰度明显高于夏季,夏季细胞丰度介于0.3×103~71.8×103 cells/L之间,平均丰度6.0×103 cells/L;冬季介于0.3×103~64.4×103 cells/L之间,平均丰度6.7×103 cells/L。夏季多样性指数和均匀度指数分别介于0.30~1.98和0.30~0.99之间,冬季分别介于0.51~2.25和0.33~0.99之间。夏季颗石藻细胞表层丰度分布规律不显著,冬季颗石藻分布高值区位于珠江口的外海站位;垂直分布上,颗石藻细胞丰度高值通常出现于次表层水体。调查期间颗石藻类群出现的优势种为纤细伞球藻(Umbellosphaera tenuis(Kamptner)Paasche)、赫氏艾密里藻(Emiliania huxleyi(Lohmann)Hay et Mohler)以及大洋桥石藻(Gephyrocapsa oceanica Kamptner)。典范对应分析(Canonical Correspondence Analysis,CCA)结果表明,夏季优势种赫氏艾密里藻和大洋桥石藻与大部分环境因子呈正相关关系,冬季响应特征不同。 相似文献
15.
南极考察航线跨越全球多个大洋,对认识超微型浮游生物在全球尺度分布及变化具有重要意义。依托中国第33次南极考察,利用流式细胞仪对航线海表水样中的超微型浮游生物进行了现场测定。结果表明,在热带与温带海域,超微型浮游生物量可占总叶绿素a浓度的60%以上,在南大洋则集中在15%～40%;原绿球藻主要分布在40°S以北海域,聚球藻主要分布在50°S以北海域,而超微型真核藻类和异养细菌则在沿线各海域均有明显分布。在纬向上,原绿球藻、聚球藻、超微型真核藻类和异养细菌的平均丰度分别为(5.50±9.09)×103 cells/mL、(13.56±20.33)×103 cells/mL、(3.87±3.08)×103 cells/mL和(6.39±4.78)×105 cells/mL;南大洋海域,超微型真核藻类和异养细菌的平均丰度分别为(3.31±1.46)×103 cells/mL和(4.68±4.39)×105 cells/mL,在少数站位检测到较低丰度的聚球藻,平均值... 相似文献
16.
夏秋季南黄海浮游植物群落及其调控因子 总被引：1，自引：1，他引：0
The phytoplankton water samples were collected in two multidisciplinary investigations which were carried out during summer(June) and autumn(November to December) of 2011. Phytoplankton species composition and abundance data were accomplished by Uterm?hl method. The phytoplankton community was dominated by diatoms and dinoflagellates in the southern Yellow Sea(YS) in summer and autumn. In summer, Paralia sulcata and Prorocentrum dentatum were the predominated species, the cell abundance ranged from 0.074 to 107.733×103 cells/L with an average of 9.057×103 cells/L. Two phytoplankton high abundance appeared in northwest part of the survey area and the Changjiang River Estuary, respectively. In autumn, Par. sulcata became the predominant species, and the phytoplankton cell abundance ranged from 1.035×103 to 8.985×103 cells/L, the average was 3.263×103 cells/L. The phytoplankton abundance in surface layer presented the homogeneous distributions. Canonical Correspondence Analysis(CCA) method was applied for discovering the relationship between environmental factors and the common found phytoplankton species. The responses of phytoplankton to nutrients were varied between summer and autumn. The abundance of most predominant species, Par. sulcata was strongly correlated to temperature and salinity in autumn, but not the case in summer. 相似文献
17.
The Kuroshio East of Taiwan and in the East China Sea and the currents East of Ryukyu Islands during early summer of 1996 总被引：6，自引：0，他引：6
Yaochu Yuan Arata Kaneko Jilan Su Xiaohua Zhu Yonggang Liu Noriaki Gohda Hong Chen 《Journal of Oceanography》1998,54(3):217-226
Using hydrographic data and moored current meter records and the ADCP observed current data during May–June 1996, a modified
inverse method is applied to calculate the Kuroshio east of Taiwan and in the East China Sea and the currents east of Ryukyu
Islands. There are three branches of the Kuroshio east of Taiwan. The Kuroshio in the East China Sea comes from the main (first)
and second branches of the Kuroshio east of Taiwan. The easternmost (third) branch of the Kuroshio flows northeastward to
the region east of Ryukyu Islands. The net northward volume transports of the Kuroshio through Section K2 southeast of Taiwan and Section PN in the East China Sea are 44.4×106 and 27.2×106 m3s−1, respectively. The western boundary current east of Ryukyu Islands comes from the easternmost branch of the Kuroshio east
of Taiwan and an anticyclonic recirculating gyre more east, making volume transports of 10 to 15×106 m3s−1. At about 21°N, 127°E southeast of Taiwan, there is a cold eddy which causes branching of the Kuroshio there. 相似文献
18.
2014年夏季南海北部浮游植物群落结构 总被引：7，自引：0，他引：7
2014年8月20日-9月6日对南海北部(18°~22°N,114°~116°E)的11个站位进行了浮游植物群落结构的调查,其中2个站位为时间连续站。共鉴定出浮游植物4门68属229种(包括变种、变型及未定种),其中硅藻门43属147种,甲藻门20属75种。浮游植物平均细胞丰度为16.318×103 cells/L,硅藻的平均细胞丰度为14.653×103 cells/L,占总丰度的89.80%,硅藻的分布决定了浮游植物的分布。近岸冲淡水含有丰富的营养盐,因此近岸海域的细胞丰度高于大洋海域,垂直分布表现出先增加后降低的趋势。本次调查的优势种为铁氏束毛藻(Trichodesmium thiebautii)、中肋骨条藻(Skeletonema costatum)、拟脆杆藻(Fragilariopsis sp.)、短孢角毛藻(Chaetoceros brevis)、菱形海线藻(Thalassionema nitzschioides)、柔弱伪菱形藻(Pseudo-nitzschia delicatissima)、尖刺伪菱形藻(Pseudo-nitzschia pungens)、扁面角毛藻(Chaetoceros compressus)、洛氏角毛藻(Chaetoceros lorenzianus)以及海洋角毛藻(Chaetoceros pelagicus),各优势种的分布趋势相似,呈现出近岸高于外海的趋势。Shannon-Weiner多样性指数与Pielou均匀度指数的平均值分别为2.37和0.56。浮游植物昼夜垂直变化明显。典范对应分析结果显示浮游植物空间分布主要受总氮盐、硅酸盐、微型浮游动物与盐度的影响。根据细胞丰度进行的站位的聚类分析显示浮游植物群落明显可划分为近岸群聚与大洋群聚。 相似文献
19.
为全面了解黄海典型海区微微型浮游植物的季节变化特征,于2009年7月至2010年6月在北黄海獐子岛海域和2010年1~12月在南黄海胶州湾进行逐月调查采样,利用流式细胞仪检测了表层海水中微微型浮游植物(picophytoplankton)的丰度,包括聚球藻(Synechococcus,SYN)和微微型真核浮游植物(picoeukaryotes,PEUK),并分析了其与环境因子的关系。獐子岛海域和胶州湾SYN和PEUK全年广泛分布,獐子岛海域SYN丰度范围在0.05×103~120.00×103cells/mL之间,丰度在秋季最高;胶州湾SYN丰度范围在0.02×103~61.80×103cells/mL之间,丰度在夏季最高。獐子岛海域PEUK丰度范围在0.01×103~18.76×103cells/mL之间,丰度在秋季最高;胶州湾PEUK丰度范围在0.25×103~95.57×103 cells/mL之间,丰度在春季最高。獐子岛海域微微型浮游植物丰度组成以SYN为主;而胶州湾以PEUK为主。PEUK是两海区微微型浮游植物生物量的主要贡献者。相关性分析结果表明,温度是影响两海区SYN丰度季节变化的最主要因素;影响PEUK季节分布的因素不完全一致,獐子岛海域PEUK丰度主要受温度调控;胶州湾PEUK丰度主要受温度和营养盐浓度影响。与已有研究比较,这两个海区的微微型浮游植物生物量对浮游植物生物量的贡献明显高于其他温带沿岸海域,预示微微型浮游植物在獐子岛海域和胶州湾生态系统中的重要作用,值得进一步深入研究。 相似文献
20.
2010年秋季南海北部浮游植物群落结构研究 总被引：5，自引：0，他引：5
2010年10月26日-11月24日在南海北部进行了浮游植物群落结构的调查,共鉴定浮游植物4门70属204种(包括未定种12种),浮游植物以硅藻为主,其物种数为146种,其细胞丰度占总浮游植物细胞丰度的93.17%;甲藻次之,其物种数为51种,占总浮游植物细胞丰度的0.63%;金藻门3属4种及蓝藻门2属3种;蓝藻门中以红海束毛藻(Trichodesmium erythraeum)为主。调查区浮游植物的细胞丰度介于0.06×103~107.50×103 cells/L之间,平均值为5.00×103 cells/L。海南岛东北部和粤东近岸表层浮游植物丰度较高。垂直分布上,表层和25 m层的浮游植物细胞丰度较高。浮游植物主要优势种类有菱形海线藻(Thalassionema nitzschioides)、舟形藻(Navicula spp.)、中肋骨条藻(Skeletonema costatum)、旋链角毛藻(Chaetoceros curvisetus)、斯氏几内亚藻(Guinardia stolterforthii)、具槽帕拉藻(Paralia sulcata)等。调查区表层和5 m层Shannon-Wiener多样性指数平均值分别为3.14和2.83,Pielou均匀度指数平均值分别为0.73和0.77;两种指数在表层和5 m层均表现出较高的一致性。环境分析表明除硅酸盐外,浮游植物细胞丰度与其他环境因子均呈极显著性的相关性,主要受到氮元素及磷酸盐的共同限制作用。 相似文献