Institute of Marine Science and Technology, Shandong University, No. 27 Shanda Nan Road, Jinan, 250110, P.R. China.
Tianjin Key Laboratory of Marine Resources and Chemistry, Tianjin University of Science and Technology, No. 29 13th Avenue, Tianjin Economic-Technological Development Area, Tianjin, 300457, P.R. China.
Sci Rep. 2018 Aug 21;8(1):12488. doi: 10.1038/s41598-018-29688-w.
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 × 10 to 160 × 10 coccoliths l and 0.2 × 10 to 68 × 10 cells l, averaged 23 × 10 coccoliths l and 9.4 × 10 cells l, respectively. Biogenic PIC, POC, and rain ratio mean values were 0.50 μgC l, 1.047 μgC l, 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.
我们在东赤道印度洋(EEIO)(80°-94°E,6°N-5°S)的 30 个地点研究了自养钙质颗石藻组合的生物多样性,并评估了区域水文学的重要性。我们分别根据球石和颗石的鉴定,记录了 26 个物种。颗石藻群落主要由 Gephyrocapsa oceanica、Emiliania huxleyi、Florisphaera profunda、Umbilicosphaera sibogae 和 Helicosphaera carteri 组成。颗石和球石的丰度范围为 0.2×10 至 160×10 颗石 l 和 0.2×10 至 68×10 细胞 l,平均值分别为 23×10 颗石 l 和 9.4×10 细胞 l。生物成因磷、颗粒有机碳和雨比的平均值分别为 0.50μgC l、1.047μgC l 和 0.10。赤道以北的表层海洋中存在大量的颗石和球石。在垂直方向上,绝大多数的颗石和球石集中在水深小于 75 米的水中。球石和自由颗石数量之间的比例表明,颗石在运输到深海时经历了不同程度的溶解。丰富的颗石藻主要出现在 90°E 以西的地区,这与 Wyrtki 喷流的存在是一致的。颗石藻的模式和颗石的模式反映了水文学过程。