Bacterial communities and biogeochemical transformations of iron and sulfur in a high saltmarsh soil profile


Autoria(s): LAMBAIS, Marcio R.; OTERO, Xose Luis; CURY, Juliano C.
Contribuinte(s)

UNIVERSIDADE DE SÃO PAULO

Data(s)

18/10/2012

18/10/2012

2008

Resumo

Microbial community structure in saltmarsh soils is stratified by depth and availability of electron acceptors for respiration. However, the majority of the microbial species that are involved in the biogeochemical transformations of iron (Fe) and sulfur (S) in such environments are not known. Here we examined the structure of bacterial communities in a high saltmarsh soil profile and discuss their potential relationship with the geochemistry of Fe and S. Our data showed that the soil horizons Ag (oxic-suboxic), Bg (suboxic), Cri (anoxic with low concentration of pyrite Fe) and Cr-2 (anoxic with high concentrations of pyrite Fe) have distinct geochemical and microbiological characteristics. In general, total S concentration increased with depth and was correlated with the presence of pyrite Fe. Soluble + exchangable-Fe, pyrite Fe and acid volatile sulfide Fe concentrations also increased with depth, whereas ascorbate extractable-Fe concentrations decreased. The occurrence of reduced forms of Fe in the horizon Ag and oxidized Fe in horizon Cr-2 suggests that the typical redox zonation, common to several marine sediments, does not occur in the saltmarsh soil profile studied. Overall, the bacterial community structure in the horizon Ag and Cr-2 shared low levels of similarity, as compared to their adjacent horizons, Bg and Cr-1, respectively. The phylogenetic analyses of bacterial 16S rRNA gene sequences from clone libraries showed that the predominant phylotypes in horizon Ag were related to Alphaproteobacteria and Bacteroidetes. In contrast, the most abundant phylotypes in horizon Cr-2 were related to Deltaproteo-bacteria, Chloroflexi, Deferribacteres and Nitrospira. The high frequency of sequences with low levels of similarity to known bacterial species in horizons Ag and Cr-2 indicates that the bacterial communities in both horizons are dominated by novel bacterial species. (c) 2008 Elsevier Ltd. All rights reserved.

Direccion General de Universidades del Ministerio de Educacion y Ciencia (Spain)

FAPESP

CAPES

CNPq (Brazil)

Identificador

SOIL BIOLOGY & BIOCHEMISTRY, v.40, n.11, p.2854-2864, 2008

0038-0717

http://producao.usp.br/handle/BDPI/19401

10.1016/j.soilbio.2008.08.014

http://dx.doi.org/10.1016/j.soilbio.2008.08.014

Idioma(s)

eng

Publicador

PERGAMON-ELSEVIER SCIENCE LTD

Relação

Soil Biology & Biochemistry

Direitos

restrictedAccess

Copyright PERGAMON-ELSEVIER SCIENCE LTD

Palavras-Chave #Bacteria #Pyritization #Sulfate reduction #Microbial diversity #Saltmarsh #Soil #16S RIBOSOMAL-RNA #PYRITE FORMATION #SULFATE REDUCTION #TRACE-METALS #MICROBIAL DIVERSITY #SEDIMENTARY PYRITE #REDUCING BACTERIA #FE(III) #OXIDATION #ATLANTIC #Soil Science
Tipo

article

original article

publishedVersion