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Denitrifier communities differ in mangrove wetlands across China.
- Source :
-
Marine pollution bulletin [Mar Pollut Bull] 2020 Jun; Vol. 155, pp. 111160. Date of Electronic Publication: 2020 Apr 27. - Publication Year :
- 2020
-
Abstract
- To explore the geographical variations in the nosZ-denitrifier community and the underlying influential factors, surface sediments were collected from six mangroves across China, including Yunxiao (YX), Futian (FT), Fangchenggang (FCG), Zhanjiang (ZJ), Dongzhaigang (DZG), and Dongfang (DF). The nosZ gene abundance in mangrove sediments were 1.60 × 10 <superscript>5</superscript> -1.17 × 10 <superscript>6</superscript> copies g <superscript>-1</superscript> dry sediment, with a higher density in Avicennia marina forest than the mudflat. Denitrifier community richness and diversity increased with decreasing latitude based on the Chao1 richness and Shannon diversity index, with the highest diversity being observed in the DF mangrove. The denitrifier communities could be classified into three groups including south DF mangrove, middle FCG, ZJ and DZG mangroves, and north YX and FT mangroves based on HCA and PCoA analysis. The nosZ OTUs could be divided into seven distinct clusters with different proportionality characteristics among mangroves. Environmental factors (TN, TOC, and salinity) collectively shape denitrifier communities in mangrove sediments.<br />Competing Interests: Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.<br /> (Copyright © 2020 Elsevier Ltd. All rights reserved.)
- Subjects :
- China
Environmental Monitoring
Geologic Sediments
Avicennia
Wetlands
Subjects
Details
- Language :
- English
- ISSN :
- 1879-3363
- Volume :
- 155
- Database :
- MEDLINE
- Journal :
- Marine pollution bulletin
- Publication Type :
- Academic Journal
- Accession number :
- 32469777
- Full Text :
- https://doi.org/10.1016/j.marpolbul.2020.111160