Department of Marine Biology, Microbiology, Biochemistry, School of Marine Sciences, Cochin University of Science and Technology (CUSAT), Kochi 682016, India; National Centre for Polar and Ocean Research, Ministry of Earth Sciences, Headland Sada, Vasco-da-Gama, Goa 403 804, India.
Department of Marine Biology, Microbiology, Biochemistry, School of Marine Sciences, Cochin University of Science and Technology (CUSAT), Kochi 682016, India; National Centre for Polar and Ocean Research, Ministry of Earth Sciences, Headland Sada, Vasco-da-Gama, Goa 403 804, India.
Mar Pollut Bull. 2021 Apr;165:112126. doi: 10.1016/j.marpolbul.2021.112126. Epub 2021 Mar 2.
Benthic nitrogen fixation in the tropical estuaries plays a major role in marine nitrogen cycle, its contribution to nitrogen budget and players behind process is not well understood. The present study was estimated the benthic nitrogen fixation rate in a tropical estuary (Cochin) and also evaluated the contribution of various diazotrophic bacterial communities. Nitrogen fixation was detected throughout year (0.1-1.11 nmol N g h); higher activity was observed in post-monsoon. The nifH gene abundance was varied from 0.8 × 10 to 0.6 × 10 copies gdry sediment; highest was detected in post-monsoon. The Cluster I and Cluster III were the dominant diazotrophs. Sulfur reducing bacterial phylotypes (Deltaproteobacteria) contributed up to 2-72% of total nitrogen fixation. These bacteria may provide new nitrogen to these systems, counteracting nitrogen loss via denitrification and anammox. Overall, the study explained the importance of benthic nitrogen fixation and role of diazotrophs in a monsoon influenced tropical estuarine environments.
热带河口的底栖固氮在海洋氮循环中起着重要作用,但人们对其对氮收支的贡献以及参与固氮过程的生物并不了解。本研究估算了热带河口(科钦)的底栖固氮速率,并评估了各种固氮细菌群落的贡献。氮固定全年都有检测到(0.1-1.11 nmol N g h);后季风期的活性更高。nifH 基因丰度在 0.8×10 到 0.6×10 拷贝 gdry 沉积物之间变化;后季风期最高。聚类 I 和聚类 III 是主要的固氮生物。硫还原细菌(δ变形菌门)在总氮固定中占比 2-72%。这些细菌可能为这些系统提供新的氮,抵消反硝化和厌氧氨氧化导致的氮损失。总的来说,该研究解释了底栖固氮的重要性以及固氮生物在受季风影响的热带河口环境中的作用。