Distribution of living coccolithophores in eastern Indian Ocean during spring intermonsoon

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作者
Haijiao Liu
Jun Sun
Dongxiao Wang
Xiaodong Zhang
Cuixia Zhang
Shuqun Song
Satheeswaran Thangaraj
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[1] Shandong University,Institute of Marine Science and Technology
[2] Tianjin University of Science and Technology,Tianjin Key Laboratory of Marine Resources and Chemistry
[3] Tianjin University of Science and Technology,College of Marine and Environmental Sciences
[4] South China Sea Institute of Oceanology,State Key Laboratory of Tropical Oceanography (LTO)
[5] Chinese Academy of Sciences,CAS Key Laboratory of Marine Ecology and Environmental Sciences, Institute of Oceanology
[6] Chinese Academy of Sciences,undefined
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We studied the biodiversity of autotrophic calcareous coccolithophore assemblages at 30 locations in the Eastern Equatorial Indian Ocean (EEIO) (80°–94°E, 6°N–5°S) and evaluated the importance of regional hydrology. We documented 26 species based on the identification of coccospheres and coccoliths, respectively. The coccolithophore community was dominated by Gephyrocapsa oceanica, Emiliania huxleyi, Florisphaera profunda, Umbilicosphaera sibogae, and Helicosphaera carteri. The abundance of coccoliths and coccospheres ranged from 0.2 × 103 to 160 × 103 coccoliths l−1 and 0.2 × 103 to 68 × 103 cells l−1, averaged 23 × 103 coccoliths l−1 and 9.4 × 103 cells l−1, respectively. Biogenic PIC, POC, and rain ratio mean values were 0.50 μgC l−1, 1.047 μgC l−1, and 0.10 respectively. High abundances of both coccoliths and coccospheres in the surface ocean layer occurred on the north of the equator. Vertically, the great majority of coccoliths and coccospheres were concentrated in water taken from depths of <75 m. The ratios between the number of coccospheres and free coccoliths indicated that coccoliths experience different levels of dissolution when transported to deep water. Abundant coccolithophores mainly occurred at the west of 90°E, which is in accordance with the presence of Wyrtki jets. Patterns of coccolithosphores and of coccoliths have been reflected in hydrological processes.
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