Dissolved carbohydrates and its influence on bacterioplankton diversity in the euphotic zone of Equatorial Indian Ocean during southwest monsoon

IF 4.6 Q2 MATERIALS SCIENCE, BIOMATERIALS
Bhaskar V. Parli , Alok K. Sinha , Jane T. Bhaskar
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Abstract

The Equatorial Indian Ocean (EIO) is oligotrophic in nature, low in productivity and characterised by relatively high bacterial biomass and heterotrophic productivity. The microbial biomass is fuelled by dissolved organic carbon (DOC) whose lability depends upon its chemistry. During an expedition in the EIO, samples for dissolved carbohydrates (DCHO), dissolved monosaccharide (MCHO), dissolved polysaccharide (PCHO), total bacterial abundance, total organic carbon (TOC), nutrients, chlorophyll a (chl a), bacterial diversity, and phytoplankton composition were estimated along two transects (TS-1 & TS-2) in the euphotic depth (200 m). DCHO and MCHO samples were analysed using 3-methyl-2-benzothiozolinone hydrazone hydrochloride (MBTH) method. The DCHO, MCHO, and PCHO concentrations in TS-1 ranged from 2.4 to 5.8 μM; 0.7 to 2.7 μM; 0.7 to 3.4 μM, while in TS-2 it ranged from 2.2 to 4.8 μM; 0.3 to 2.8 μM; 0.2 to 3.8 μM, respectively. Vertically, DCHO concentrations decreased within the photic depths in most stations. PCHO concentrations were relatively greater in TS-2 than TS-1, which may be due to preferential removal of MCHO in TS-2. In the top 200 m of the water column, Proteobacteria was the most abundant bacterial phylum followed by Cyanobacteria, Actinobacteriota, Bacteroidota, and SAR-324 while dinoflagellates dominated the phytoplankton population. The distribution of DCHO and PCHO were inversely correlated to salinity, temperature, and chl a. The bacterial heterotrophs like alpha-Proteobacteria, Chloroflexii, and Verrumicrobiota along with SAR324 and Actinobacteriota were clustered with nutrients, while Bdellovibriota and Dadabacteria clustered with MCHO, PCHO, and DCHO. These results highlight the impact of DCHO & PCHO lability on the distribution of bacterial community and delineate oceanographic factors that regulate the distribution of DCHO and its constituents in EIO waters.

西南季风期间赤道印度洋极光带的溶解碳水化合物及其对浮游细菌多样性的影响
赤道印度洋(EIO)属于低营养型海洋,生产力低下,细菌生物量和异养生产力相对较高。微生物生物量由溶解有机碳(DOC)提供动力,而溶解有机碳的稳定性取决于其化学性质。在东印度洋考察期间,沿欣快水深(200 米)的两个横断面(TS-1 和 TS-2)采集了溶解碳水化合物(DCHO)、溶解单糖(MCHO)、溶解多糖(PCHO)、细菌总数、有机碳总量(TOC)、营养物质、叶绿素(chl)、细菌多样性和浮游植物组成的样本。采用 3-甲基-2-苯并硫唑酮腙盐酸盐(MBTH)法分析 DCHO 和 MCHO 样品。TS-1 中的 DCHO、MCHO 和 PCHO 浓度分别为 2.4 至 5.8 μM、0.7 至 2.7 μM、0.7 至 3.4 μM,而 TS-2 中的 DCHO、MCHO 和 PCHO 浓度分别为 2.2 至 4.8 μM、0.3 至 2.8 μM、0.2 至 3.8 μM。从垂直方向看,大多数站点的 DCHO 浓度在光照深度内都有所下降。TS-2 的 PCHO 浓度相对高于 TS-1,这可能是由于 TS-2 优先去除 MCHO 的缘故。在水体顶部 200 米处,细菌门的数量最多,其次是、、、和 SAR-324,而浮游植物种群则以甲藻为主。DCHO 和 PCHO 的分布与盐度、温度和叶绿素成反比。细菌异养生物如-和与 SAR324 和与营养物质聚集在一起,而和与 MCHO、PCHO 和 DCHO 聚集在一起。这些结果突显了 DCHO 和 PCHO 的易变性对细菌群落分布的影响,并阐明了调节 EIO 水域中 DCHO 及其成分分布的海洋学因素。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
ACS Applied Bio Materials
ACS Applied Bio Materials Chemistry-Chemistry (all)
CiteScore
9.40
自引率
2.10%
发文量
464
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