环境压力源对孟加拉哈尔达河浮游植物群落的影响评估

M. Hossain, M. Sarker, Md. Milon Sarker, Afsana Kabir Dipty, Nazmun Naher Rima, N. Sultana
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摘要

哈尔达河是孟加拉国的一条98公里长的潮汐淡水河,它有一个独特的特点,因为它是全球唯一的天然繁殖地和印度主要鲤鱼受精卵的唯一来源。本研究首先总结了环境胁迫因素对孟加拉国哈尔达河浮游植物丰度、群落及其多样性的影响。2019年1月和2020年8月,从哈尔达河收集并分析了季节(冬季、季风)、水深、温度、pH值、盐度、溶解氧和营养物质等环境数据。从孟加拉国哈尔达河中鉴定出了34个浮游植物属,包括5个纲。采用双因素方差分析分析季风和冬季对理化和生物参数的影响。结果表明,季风与冬季在观测参数上存在显著的交互作用((F9, 160)= 34.999, p= 0.0)。水温(F 125.31, Fcrit 4.130, p= 0.0)和营养物(F 11.118, Fcrit 2.322, p= 0.0)显示了哈尔达河浮游植物浓度的显著变化。在温度和营养物质方面,水深对哈尔达河浮游植物群落的影响也显著(F = 1.790, F = 1.719, p= 0.0),细胞密度分别在表层和底层水体最高和最低。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Impact of environmental stressors on the phytoplankton communities to assess the River Halda, Bangladesh
Halda is a 98 km-long tidal freshwater river of Bangladesh, which has a unique feature since it is the only natural breeding ground and the sole source of fertilized eggs of Indian Major Carps globally. The present study firstly summarizes the impact of environmental stressors to understand phytoplankton abundance, community, and their diversity in Halda River, Bangladesh. Environmental data as seasons (Winter, Monsoon), water depths, temperature, pH, Salinity, dissolved oxygen, and nutrients were collected and analyzed from the Halda River in January 2019 and August, 2020.  Thirty-four phytoplankton genera, comprising five classes, were identified from the Halda River, Bangladesh. A two-way ANOVA was performed to analyze the effect of Monsoon and Winter on the physicochemical and biological parameters. It revealed that there was a statistically significant ((F9, 160)= 34.999, p= 0.0) interaction between Monsoon and Winter on the observed parameters. The water temperature (F 125.31, Fcrit 4.130, p= 0.0) and nutrients (F 11.118, Fcrit 2.322, p= 0.0) revealed significant change in the phytoplankton concentrations in the Halda River. As of the temperature and nutrients, water depths also significantly (F 1.790, Fcrit 1.719, p= 0.0) affect the phytoplankton communities in the Halda River showing the highest and lowest cell density in the surface and bottom water, respectively.
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