| Marine Ecology Progress Series | |
| Picoplankton abundance and biomass across the eastern South Pacific Ocean along latitude 32.5°S | |
| Gadiel Alarcoacuten1  Osvaldo Ulloa1  Shuichi Watanabe1  Masao Fukasawa1  William K. W. Li1  Carolina Grob1  | |
| 关键词: Picophytoeukaryotes; Bacterioplankton; Carbon biomass; Cyanobacteria; Flow cytometry; | |
| DOI : 10.3354/meps332053 | |
| 学科分类:海洋学与技术 | |
| 来源: Inter-Research | |
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【 摘 要 】
ABSTRACT: The distribution of picoplankton (<2 to 3 µm in diameter) was determined on a transect across the eastern South Pacific Ocean from south of Tahiti to the coast of Chile along 32.5°S latitude during the early austral spring. The abundance of Synechococcus, picophytoeukaryotes and bacterioplankton increased from oligo- to eutrophic conditions, while that of Prochlorococcus decreased according to nutrient availability and hydrographic characteristics. Bacterioplankton dominated across the transect (>75% total picoplanktonic abundance). As expected, Prochlorococcus was the most numerically abundant phytoplankter under very oligotrophic (chlorophyll a concentration ≤0.1 mg m3) and mesotrophic (>0.1 and ≤1 mg m3) conditions. However, in contrast to other subtropical regions, picophytoeukaryotes appear to dominate the <2 µm autotrophic carbon biomass in this region of the South Pacific Ocean at this time of the year. In the upper 200 m of the water column, the integrated carbon biomass of Prochlorococcus, Synechococcus, picophytoeukaryotes and bacterioplankton were in the ratios of 9:1:14:11 and 3:1:8:6 under oligo- and mesotrophic conditions, respectively. Thus, picophytoeukaryotes were 1.4- to 2-fold higher in biomass than both cyanobacteria combined, and slightly more important (1.2- to 1.3-fold) than bacterioplankton. Picophytoeukaryotes could therefore play a dominant ecological and biogeochemical role in subtropical gyres, which extend over a vast area of the worlds oceans.
【 授权许可】
Unknown
【 预 览 】
| Files | Size | Format | View |
|---|---|---|---|
| RO201912010132382ZK.pdf | 816KB |
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