Diversity and geochemical structuring of bacterial communities along a salinity gradient in a carbonate aquifer subject to seawater intrusion

Abstract In aquifers subject to saline water intrusion, the mixing zone between freshwater and saltwater displays strong physico-chemical gradients. Although the microbial component of these specific environments has been largely disregarded, the contribution of micro-organisms to biogeochemical rea...

Full description

Saved in:
Bibliographic Details
Published inFEMS microbiology ecology Vol. 90; no. 3; pp. 922 - 934
Main Authors Héry, Marina, Volant, Aurélie, Garing, Charlotte, Luquot, Linda, Elbaz Poulichet, Françoise, Gouze, Philippe
Format Journal Article
LanguageEnglish
Published Oxford, UK Blackwell Publishing Ltd 01.12.2014
Oxford University Press
Wiley-Blackwell
Subjects
Online AccessGet full text

Cover

Loading…
More Information
Summary:Abstract In aquifers subject to saline water intrusion, the mixing zone between freshwater and saltwater displays strong physico-chemical gradients. Although the microbial component of these specific environments has been largely disregarded, the contribution of micro-organisms to biogeochemical reactions impacting water geochemistry has previously been conjectured. The objective of this study was to characterize and compare bacterial community diversity and composition along a vertical saline gradient in a carbonate coastal aquifer using high throughput sequencing of 16S rRNA genes. At different depths of the mixing zone, stable geochemical and hydrological conditions were associated with autochthonous bacterial communities harboring clearly distinct structures. Diversity pattern did not follow the salinity gradient, although multivariate analysis indicated that salinity was one of the major drivers of bacterial community composition, with organic carbon, pH and CO2 partial pressure. Correlation analyses between the relative abundance of bacterial taxa and geochemical parameters suggested that rare taxa may contribute to biogeochemical processes taking place at the interface between freshwater and saltwater. Bacterial respiration or alternative metabolisms such as sulfide oxidation or organic acids production may be responsible for the acidification and the resulting induced calcite dissolution observed at a specific depth of the mixing zone. Distinct bacterial communities are shaped by physico-chemical gradients in the freshwater-saltwater mixing zone of an aquifer. The wide range of their potential metabolic capacities can impact the groundwater geochemical properties. Distinct bacterial communities are shaped by physico-chemical gradients in the freshwater-saltwater mixing zone of an aquifer. The wide range of their potential metabolic capacities can impact the groundwater geochemical properties.
Bibliography:ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 14
content type line 23
ISSN:0168-6496
1574-6941
1574-6941
DOI:10.1111/1574-6941.12445