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印度西南海岸阿勒皮附近泥滩地区的微生物分布。

Microbial distribution in Mudbank regions off Alappuzha, South-West coast of India.

机构信息

Department of Marine Biology, Microbiology and Biochemistry, Cochin University of Science and Technology, Cochin 682016, Cochin, India.

CSIR-National Institute of Oceanography, Regional Centre, Cochin - 682 018, Cochin, Kerala, India.

出版信息

Environ Monit Assess. 2024 Oct 29;196(11):1117. doi: 10.1007/s10661-024-13176-y.

Abstract

The coastal waters of Kerala, in the South Eastern Arabian Sea (SEAS), are unique during the Southwest monsoon season due to the concurrent occurrence of two physical processes, the upwelling and Mudbanks. However, little is known about the viral ecology and activity in a system where upwelling and Mudbanks coexist, though it is generally recognized that microbial assemblages play a vital role in the food web dynamics of marine systems, particularly in upwelling. Water samples were taken from monsoon and pre-monsoon period from three locations, (M1, M2, and M3) off Alappuzha, on the southwest coast of India to examine the viral activity and distribution. The dissolved oxygen levels showed the incursion of hypoxic waters in all the stations during the peak upwelling period. Upwelling signals were prominent in all the stations, but Mudbank and upwelling co-occurred at M2 alone during monsoon. The abundance of viruses ranged from 0.86 to 15.68 × 10 Viral-like Particles (VLPs mL) and prokaryotic abundance ranged from 2.73-16.26 × 10 cells mL. Viral and prokaryotic abundance was significantly higher in the monsoon compared to pre and late-monsoon. Based on Transmission electron microscopy (TEM) results, the non-tailed viruses constituted the major (43%) proportion of the total viruses in this study region. However, the viral production rates and viral-mediated bacterial mortality were high in the pre-monsoon compared to the monsoon and late-monsoon periods. There was no obvious effect of Mudbanks on viral dynamics and the observed variations in virological and hydrological features were governed mainly by coastal upwelling.

摘要

喀拉拉邦的沿海水域位于东南阿拉伯海(SEAS),在西南季风季节由于两种物理过程的同时发生而独具特色,这两种过程分别是上升流和泥滩。然而,尽管人们普遍认识到微生物群落在海洋系统的食物网动态中起着至关重要的作用,特别是在上升流中,但在一个上升流和泥滩共存的系统中,关于病毒生态学和活动的了解甚少。本研究从印度西南海岸的阿勒皮(Alappuzha)附近的三个地点(M1、M2 和 M3)采集了季风和季风前期间的水样,以检查病毒活性和分布。溶解氧水平表明,在上升流高峰期所有站点都有缺氧水入侵。所有站点都有明显的上升流信号,但只有在季风期间,M2 站点同时出现了泥滩和上升流。病毒丰度范围为 0.86 至 15.68×10 个病毒样颗粒(VLPs mL),原核生物丰度范围为 2.73-16.26×10 个细胞 mL。与前季风和晚季风相比,季风期间病毒和原核生物丰度显著更高。根据透射电子显微镜(TEM)结果,无尾病毒构成了本研究区域总病毒的主要(43%)比例。然而,与季风和晚季风相比,前季风期间病毒的生产速率和病毒介导的细菌死亡率较高。泥滩对病毒动态没有明显影响,观察到的病毒学和水文学特征的变化主要受沿海上升流控制。

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