Standing stock and community structure of photosynthetic picoplankton in the northern South China Sea

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…     

海洋细菌对钢的腐蚀作用

从青岛港钢板桩的锈层中分离到三种腐蚀性细菌。经鉴定这三种细菌是氧化硫杆菌(Thiobacillus thiooxidans),排硫杆菌(Thiobacillus thioparus)和脱硫脱硫弧菌(Desulfovib-iodesulforicans)。用失重法测定了这三种细菌对四种钢样的腐蚀速率。氧化硫杆菌的腐蚀速率为53.5m.d.d.(毫克/平方分米/天)(BJ_2),83.3(902),121.8(CXL-4)和81.0(7~#)。排硫杆菌的腐蚀速率为23.6mdd(BJ_2)。脱硫脱硫弧菌的腐蚀速率为9.9m.d.d.(BJ_2),9.2(902),3.7(CXL-4)和2.9(7~#)。这三种细菌对钢都具有很强的腐蚀能力。     

Basin-Scale Geographic Patterns of Bacterioplankton Biomass and Production in the Subarctic Pacific, July–September 1997

Bacterial biomass and production rate were measured in the surface (0–100 m) and mesopelagic layers (100–1,000 m) in the subarctic Pacific and the Bering Sea between July–September, 1997. Depth profiles were determined at stations occupied in oceanic domains including the subarctic gyres (western, Bering Sea, and Gulf of Alaska) and a boundary region south of the gyres. In the surface layer (0–100 m), both bacterial biomass and production were generally high in the western and Bering Sea gyres, with the tendency of decrease toward east. This geographic pattern was consistent with the dominant regime of phytoplankton biomass at the time of our survey. A significant portion of variation in bacterial production was explained by the concentration of chlorophyll a (r ² = 0.340, n = 60, P < 0.001) and, to the greater extent, by the concentration of semilabile total organic carbon (SL-TOC = TOC at a given depth—TOC at 1,000 m, r ² = 0.488, n = 59, P < 0.0001). Temperature significantly improved the regression model: temperature and chlorophyll jointly explained 60% of variation in bacterial production. These results support the hypothesis that bacteiral growth is largely regulated by the combination of temperature and the supply of dissolved organic carbon in subarctic surface waters. In the mesopelagic layer (100–1,000 m), the geographic pattern of bacterial production was strikingly different from the surface phytoplankton distribution: the production was high in the boundary region where the phytoplankton biomass was lowest. Bacterial growth appeared to be largely controlled by the supply of organic carbon, as indicated by the strong dependency of bacterial production on SL-TOC (r ² = 0.753, n = 75, P < 0.0001). The spatial uncoupling between surface phytoplankton and mesopelagic bacterial production suggests that the supply rate of labile dissolved organic carbon in the mesopelagic zone does not simply reflect the magnitude of the particulate organic carbon flux in the subarctic Pacific.     

Body size–abundance distributions of nano- and micro-phytoplankton guilds in coastal marine ecosystems

This study focuses on body size–abundance distributions of nano- and micro-phytoplankton guilds in coastal marine areas of the Southern Adriatic–Ionian region. The aim of the study was to evaluate the occurrence of common patterns of body size–abundance distributions in relation to physical, chemical and biological environmental forcing factors and to taxonomic composition of phytoplankton guilds. This paper is based on data collected during four oceanographic cruises carried out seasonally along the Southern Apulian coast (Adriatic and Ionian Seas, SE Italy) as a part of the INTERREG II Italy–Greece Program. The study was performed at 21 stations located on 7 transects perpendicular to the coastline, with 3 stations per transect at a distance of 3, 9 and 15 NM from the coastline. At each station, profiles of the major physical features of the water were determined and water samples were collected for phytoplankton and nutrient analysis. Overall, 320 nano- and micro-phytoplankton taxa were identified, 76% of which at species level, with phytoplankton cells ranging in size from 0.008 to 4697.54 ng. Body size–abundance distributions showed some common features: they were relatively invariant (average similarity 65%) with respect to taxonomic composition (average similarity 32%), right skewed (90%), leptokurtic (77%) and log normal (76%). Moreover, abiotic, biotic and spatial ecosystem components accounted for up to 75% of body size–abundance distribution variation. The results of this study suggest that body size–abundance distributions are an intrinsic property of marine phytoplankton communities, emphasising functional dependence on ecological constraints related to trophic factors and intra-guild coexistence relationships.     

胶州湾西北部海域大型底栖动物群落研究

自2003年9月~2004年9月在胶州湾西北部养殖区内外隔月取样,共获得7个航次的大型底栖动物样品。用PRIMER软件对大型底栖动物群落进行分析,结果表明:养殖区内站位的丰度值、生物量及群落结构与外面站位差别较大,经相关检验站位之间差异显著,说明养殖区内因为养殖活动已经引起大型底栖生物的剧烈扰动;还发现胶州湾养西北部海域群落种类组成季节变化明显,与历史资料相比,棘皮动物数量明显减少,软体动物特别是菲律宾蛤仔是胶州湾大型底栖动物生物量的主要贡献种。根据LUSTER聚类和MDS标序的结果,把底栖生物群落划分为四大生物组。比较发现,胶州湾西北部及附近海域大型底栖生物群落已经发生了变化,通过对底栖生物群落与环境因子的分析认为,造成变动的原因可能是渔业活动的加剧和湾内水体污染的压力。     

Distribution of dominant species and abundance of nannofossils in surface sediments of the central and northern parts of the South China Sea——Comparison and discussion

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Abundance and distribution of dinoflagellate cysts in Xiamen Western Harbor

In a grid investigation, dinoflagellate cysts were collected from sediments in Xiamen Western Harbor in May of 2000,from which five species of cysts were identified: Alexandrium tamarensis, A. minutum, Lingulodinium polyedra,Gonyaulax scrippsae and Gymnodinium catenatum, account for about 21% in the species composition. The quantitative analysis of the sediments shows that the number of dinoflagellate cysts varies from 51 to 256 cysts/g of sediment, the highest value (>200 cysts/g) being recorded at the stations of the central part of the bay, while the lowest (＜100 cysts/g) at the bay mouth. A good linear relationship is found between cyst amount and fine-grained sediments. Complex physiognomies on the seabed, topographty in the bay and weak water exchange are the main factors not only in cyst accumulation but also in their distribution pattern, and have resulted in the difference in cyst densities between the inner bay and the outer bay in the harbor.