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1.
The summer distributions of planktonic microbial communities (heterotrophic and phtosynthetic bacteria, phtosynthetic and heterotrophic nanoflagellates, ciliate plankton, and microphytoplankton) were compared between inner and outer areas of Lake Sihwa, divided by an artificial breakwater, located on the western coast of Korea, in September 2003. The semienclosed, inner area was characterized by hyposaline surface water (<17 psu), and by low concentrations of dissolved oxygen (avg. 0.4 mg L1) and high concentrations of inorganic nutrients (nitrogenous nutrients >36 μM, phosphate <4 μM) in the bottom layer. Higher densities of heterotrophic bacteria and nanoflagellates also occurred in the inner area than did in the outer area, while microphytoplankton (mainly diatoms) occurred abundantly in the outer area. A tiny tintinnid ciliate, Tintinnopsis nana, bloomed into more than 106 cells L1 at the surface layer of the inner area, while its abundance was much lower (103-104 cells L1) in the outer area of the breakwater. Ciliate abundance was highly correlated with heterotrophic bacteria (r = 0.886, p < 0.001) and heterotrophic flagellates (r = 0.962, p < 0.001), indicating that rich food availability may have led to theT. nana bloom. These results suggest that the breakwater causes the eutrophic environment in artificial lakes with limited flushing of enriched water and develops into abundant bacteria, nanoflagellates, and ciliates.  相似文献   
2.
Month-to-month fluctuations in the abundance of bacteria and heterotrophic nanoflagellates (HNF) and bacterial production, as well as various chemical (nutrients, oxygen) and physical (salinity, temperature) parameters were analysed at a station located in the open middle Adriatic Sea during one decade (1997-2006). Being influenced by both coastal waters and open Adriatic circulation in the surface layer, and by the deep Adriatic water masses in the deep layers (100 m), this station is quite suitable for detecting the environmental changes occurring in the open Adriatic Sea with respect to the circulation of its water masses and their long-term changes and anomalies. Multivariate methods were used to identify seasonal and inter-annual changes of the investigated parameters, associating observed changes to the changes in Adriatic water masses and circulation regimes. The analyses showed that bacterial abundance and production were controlled by different water mass dynamics during 1997-2001 compared to 2002-2006 period, particularly noticeable in different seasonal patterns of biological parameters. The interplay between North Adriatic Dense Water (NAdDW) and Levantine Intermediate Water (LIW) resulted in a change in the available nutrients (NAdDW is poor in orthophosphates), and as a consequence different bacterial abundance and production. A few periods were examined in detail, such as 2004, when LIW inflow was particularly strong and was accompanied by an increase of bacterial and HNF abundances, as well as of bacterial production.  相似文献   
3.
A study was carried out to investigate the grazing pressure of heterotrophic nanoflagellates(HNF) on bacteria assemblages in the Yellow Sea Cold Water Mass(YSCWM) area in October, 2006. The results show that the HNF abundance ranges from 303 to 1 388 mL-1, with a mean of 884 mL-1. The HNF biomass is equivalent to 10.6%–115.6% of that of the bacteria. The maximum abundance of the HNF generally occurred in the upper 30 m water layer, with a vertical distribution pattern of surface layer abundance greater than middle layer abundance, then bottom layer abundance. The hydrological data show that the YSCWM is located in the northeastern part of the study area, typically 40 m beneath the surface. A weak correlation is found between the abundances of HNF and bacteria in both the YSCWM and its above water layer. One-way ANOVA analysis reveals that the abundance of HNF and bacteria differs between inside the YSCWM and in the above water mass. The ingestion rates of the HNF on bacteria was 8.02±3.43 h-1 in average. The grazing rate only represented 22.75%±6.91% of bacterial biomass or 6.55%+4.24% of bacterial production, implying that the HNF grazing was not the major factor contributing to the bacterial loss in the YSCWM areas.  相似文献   
4.
于2009年7月20日至8月16日(夏季),2010年1月6日至30日(冬季),2010年10月26日至11月24日(秋季)和2011年4月30日至2011年5月24日(春季)在南海北部调查了微型异养鞭毛虫的生态分布特点。结果表明:春、夏、秋、冬的微型异养鞭毛虫丰度分别为0.05×103~1.93×103,0.03×103~2.65×103,0.09×103~2.05×103和0.04×103~1.84×103 cells/mL,生物量(以碳计)分别为0.56~19.50,0.04~24.11,0.96~14.80和0.29~22.26 μg/L。4个季节的微型异养鞭毛虫丰度均以2~5 μm粒级的为主,其所占比例超过65%,10~20 μm粒级所占比例通常低于10%。在水平分布上,微型异养鞭毛虫的丰度随离岸距离的增加逐渐降低;在垂直分布上,微型异养鞭毛虫的丰度随深度的增加逐渐降低,但夏季微型异养鞭毛虫丰度的高值多出现在次表层叶绿素a极大值层(DCM层)。微型异养鞭毛虫的丰度分布受到多重因素的交互影响,并且其所受调控模式在不同季节存在差异:春季和秋季微型异养鞭毛虫主要受下行调控;夏季微型异养鞭毛虫主要受上行调控;冬季上行和下行调控对微型异养鞭毛虫的影响相近。  相似文献   
5.
To investigate the seasonal variation and community structure of nano- and microzooplankton in Gyeonggi Bay of the Yellow Sea, the abundance and carbon biomass of nano- and microzooplankton were evaluated at 10-day intervals from January 1997 to December 1999. Four major groups of nano- and microzooplankton communities were classified: heterotrophic ciliates, heterotrophic dinoflagellates (HDF), heterotrophic nanoflagellates (HNF), and copepod nauplii. The total carbon biomass of nano- and microzooplankton ranged from 10.2 to 168.8 μg C L−1 and was highest during or after phytoplankton blooms. Nano- and microzooplankton communities were composed of heterotrophic ciliates (7.4–81.4%; average 41.7% of total biomass), HDF (0.1–70.3%; average 26.1% of total biomass), copepod nauplii (1.6–70.6%; average 20.7% of total biomass), and HNF (0.8–59.5%; average 11.5% of total biomass). The relative contribution of individual components in the nano- and microzooplankton communities appeared to differ by seasons. Ciliates accounted for the most major component of nano- and microzooplankton communities, except during summer and phytoplankton blooming seasons, whereas HDF were more dominant during the phytoplankton blooming seasons. The abundance and biomass of nano- and microzooplankton generally followed the seasonal dynamics of phytoplankton. The size and community distribution of nano- and microzooplankton was positively correlated with size-fractionated phytoplankton. The carbon requirement of microzooplankton ranged from 60 to 83% of daily primary production, and was relatively high when phytoplankton biomass was high. Therefore, our result suggests that the seasonal variation in the community and size composition of nano- and microzooplankton appears to be primarily governed by phytoplankton size and concentration as a food source, and their abundance may greatly affect trophic dynamics by controlling the seasonal abundance of phytoplankton.  相似文献   
6.
Microbial plankton biomass, primary production (PP) and phytoplankton growth rates (μ) were estimated along the NW Iberian margin during an upwelling relaxation event. Although the interaction between wind forcing and coastline singularities caused high spatial variability in PP (0.4-8.4 g C m−2 d−1), two domains (coastal and oceanic) could be distinguished regarding microbial plankton biomass and μ. At the coastal domain, with higher influence of upwelling, diatoms showed an important contribution (27 ± 17%) to total autotrophic biomass (AB). Nonetheless, AB was dominated by autotrophic nanoflagellates (ANF) at both realms, accounting for 62 ± 16% and 89 ± 6% of the integrated AB at the coastal and oceanic domain respectively. AB and heterotrophic biomass (HB) were significantly higher at the oceanic than at the coastal domain, with both biomasses covarying according to HB:AB = 0.33. Whereas the low phytoplankton carbon to chlorophyll a ratio (Cph:chl a = 38 ± 3) and the high μ = 0.54 ± 0.09 d−1 registered at the coastal stations suggest that phytoplankton was not nutrient limited at this domain, the values (Cph:chl a = 157 ± 8; μ = 0.17 ± 0.02 d−1) recorded at the oceanic domain point to severe nutrient limitation. However, the high Fv/Fm fluorescence ratios (0.56 ± 0.09) measured at the sea surface in the oceanic domain suggest that nutrient limitation did not occur. To reconcile these two apparently opposite views, it is suggested the occurrence of mixotrophic nutrition of ANF, with heterotrophic nutrition supplying about 75% of carbon requirements.  相似文献   
7.
鞭毛虫和纤毛虫在海洋微食物环和经典食物链间的能量流动中起着重要的枢纽作用,但其在水母暴发过程中的作用仍然不明。本研究基于2011年春季以及水母旺发的夏季黄海专项航次,通过荧光染色技术和定量蛋白银法研究了南黄海水母频发海域3个断面(E:33°N,G:34°N,I:35°N)的鞭毛虫和纤毛虫的群落结构和时空分布特点,对其与水母的发生关系进行了初步探讨。结果表明,春夏两季的微型鞭毛虫丰度均以近岸水域为最高,向外海递减,高值区大多出现在水体表层及底层附近。夏季总微型鞭毛虫的丰度和生物量较春季略高,且异养微型鞭毛虫比例升高。纤毛虫丰度的水平分布与鞭毛虫正相反,以近岸较低,向外海递增,主要分布在表层及10m水层。在水母出现的E和G断面,夏季纤毛虫数量显著降低,丰度仅为春季的30%—40%;而未见水母的I断面夏季较春季的数量升高了一个数量级。推测夏季水母发生的E、G断面纤毛虫丰度明显降低系因水母的捕食压力所致,纤毛虫数量的减少导致对鞭毛虫的摄食压力降低,鞭毛虫数量增加;而未见水母的I断面纤毛虫则维持较高的丰度值。本研究表明,水母作为浮游生态系统的顶级捕食者,可通过营养级联效应对微小型浮游动物群落产生影响。  相似文献   
8.
The role of microorganisms in the transfer of carbon of marine systems is very important in open oligotrophic oceans. Here, we analyze the picoplankton structure, the heterotrophic bacterioplankton activity, and the predator-prey relationships between heterotrophic bacteria and nanoflagellates during two large scale cruises in the Central Atlantic Ocean (∼29°N to ∼40°S). Latitud cruises were performed in 1995 between March-April and October-November. During both cruises we crossed the regions of different trophic statuses; where we measured different biological variables both at the surface and at the deep chlorophyll maximum (DCM). The concentration of chlorophyll a varied between 0.1 and 0.8 mg m−3, the abundance of heterotrophic bacteria varied between <1.0 × 105 and >1.0 × 106 cells ml−1, and that of heterotrophic nanoflagellates between <100 and >1.0 × 104 cells ml−1. The production of heterotrophic bacteria varied more than three orders of magnitude between <0.01 and 24 μgC L−1 d−1; and the growth rates were in the range <0.01-2.1 d−1. In the Latitud-II cruise, Prochlorococcus ranged between <103 and >3 × 105 cells ml−1, Synechococcus between <100 and >1.0 × 104 cells ml−1, and picoeukaryotes between <100 and >104 cells ml−1.Two empirical models were used to learn more about the relationship between heterotrophic bacteria and nanoflagellates. Most bacterial production was ingested when this production was low, the heterotrophic nanoflagellates could be controlled by preys during Latitud-I cruise at the DCM, and by predators in the surface and in the Latitud-II cruise. Our results were placed in context with others about the structure and function of auto- and heterotrophic picoplankton and heterotrophic nanoplankton in the Central Atlantic Ocean.  相似文献   
9.
The analysis of 103 samples collected quantitatively from the southern Taiwan Strait (22°4'-24°3'N, 117°5'-119°9'E), China, in August 1997 indicates that the abundance of heterotrophic nanoflagellates (HNF) ranges from 391 to 1 846 ×103 cell/dm3, with an average of 949 × 103 cell/dm3, and 96.2% of cells are in size of 2-22 μm in all HNF met in the samples. The HNF cells are 9.83-45.79 μg/dm3 after conversion from cell number to carbon content, with an average of 22.82 μg/dm3 . The HNF abundance is relatively low in comparison with other areas. The nitrogen and phosphorus nutrients of the water are lower than previous investigations, which may be caused by the El Nino. The biomass of HNF is higher in southern waters, where cell concentration is 3-5 folds higher than that in other waters, and nearly 2-fold as high as the average of the investigated areas. The HNF is mainly habitat in 0-30 m water layer. Both horizontal and vertical HNF distribution must be influenced by hy-drographical dynamic pro  相似文献   
10.
为研究温度对微型鞭毛虫(Nanoflagellates,NF)摄食细菌的影响,于广西近岸海区采集NF自然群落,置于实验室不同温度下(14℃、22℃、28℃)培养9天,观察细菌和NF的丰度变化。并以荧光细菌标记法研究不同温度下异养微型鞭毛虫(Hetertrophic Nanoflagellates,HNF)和含色素微型鞭毛虫(Pigmented Nanoflagellates,PNF)对细菌的摄食率,计算不同类型NF的群落摄食率。此外,研究还比较了不同粒径PNF (<3 μm和3~10 μm)对细菌的摄食。结果表明,不同类型的NF对细菌的摄食率由大到小为:3~10 μm PNF、HNF、小于3 μm PNF。较之PNF,HNF的摄食受温度影响较小。PNF的摄食率在22℃最大。而且,不同大小PNF的摄食对温度的响应有所不同。升温可以提高3~10 μm PNF的摄食率,但会抑制小于3 μm PNF的摄食。而降温抑制3~10 μm PNF的摄食,但降温对小于3 μm PNF摄食的抑制作用比升温小。但无论是3~10 μm PNF还是小于3 μm PNF,升温均会降低其丰度。而由于丰度减小对群落摄食率的影响更大,因此,升温降低PNF的群落摄食率。  相似文献   
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