LI Gang, KE Zhixin, LIN Qiang, NI Guangyan, SHEN Pingping, LIU Huaxue, YIN Jianqiang, LI Kaizhi, HUANG Liangmin, TAN Yehui. Longitudinal patterns of spring-intermonsoon phytoplankton biomass, species compositions and size structure in the Bay of Bengal[J]. Acta Oceanologica Sinica, 2012, (2): 121-128. doi: 10.1007/s13131-012-0198-8
Citation:
LI Gang, KE Zhixin, LIN Qiang, NI Guangyan, SHEN Pingping, LIU Huaxue, YIN Jianqiang, LI Kaizhi, HUANG Liangmin, TAN Yehui. Longitudinal patterns of spring-intermonsoon phytoplankton biomass, species compositions and size structure in the Bay of Bengal[J]. Acta Oceanologica Sinica, 2012, (2): 121-128. doi: 10.1007/s13131-012-0198-8
LI Gang, KE Zhixin, LIN Qiang, NI Guangyan, SHEN Pingping, LIU Huaxue, YIN Jianqiang, LI Kaizhi, HUANG Liangmin, TAN Yehui. Longitudinal patterns of spring-intermonsoon phytoplankton biomass, species compositions and size structure in the Bay of Bengal[J]. Acta Oceanologica Sinica, 2012, (2): 121-128. doi: 10.1007/s13131-012-0198-8
Citation:
LI Gang, KE Zhixin, LIN Qiang, NI Guangyan, SHEN Pingping, LIU Huaxue, YIN Jianqiang, LI Kaizhi, HUANG Liangmin, TAN Yehui. Longitudinal patterns of spring-intermonsoon phytoplankton biomass, species compositions and size structure in the Bay of Bengal[J]. Acta Oceanologica Sinica, 2012, (2): 121-128. doi: 10.1007/s13131-012-0198-8
Key Laboratory of Marine Bio-resources Sustainable Utilization, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangdong 510301, China
2.
Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangdong 510650, China
Vertical distributions of phytoplankton biomass, compositions and size structure were investigated during the spring-intermonsoon (April 22 to 30) of 2010 along transact 10°N of the Bay of Bengal, northern Indian Ocean. Surface phytoplankton biomass (Chl a) was (0.065±0.009) μg/L, being greater than 80% of which was contributed by pico-phytoplankton (<3 μm). The Chl a concentration vertically increased to the maximal values at deep chlorophyll maximum (DCM) layer that shoaled eastwards from 75 to 40 m. The Chl a biomass at DCM layer generally varied between 0.2 and 0.4 μg/L, reaching the maximum of 0.56 μg/L with micro-phytoplankton cells (>20 μm) accounting for 58% and nano-(3-20 μm) or pico-cells for 15% and 27%, respectively. In particular, the cells concentration coupling well with phosphate level was observed at middle layer (75-100 m) of 87° to 89°E, dominated by micro-cells diatoms (e.g., Chaetoceros atlanticus v. neapolitana, Chaetoceros femur and Pseudonitzschia sp.) and cyanobacteria (i.e., Trichodesmium hildebrandtii), with the cells concentration reached as high as 4.0×104 and 4.3×104 cells/L. At the rest of the transact however, dinoflagellates (e.g., Amphisdinium carterae and Prorocentrum sp.) were the dominant species, with the cells concentration varying from 0.3×103 to 6.8×103 cells/L. Our results also indicate that the regulation of large cells (micro-, nano-) on phytoplankton biomass merely occurred at DCM layer of the Bay.