z-logo
open-access-imgOpen Access
Diversity of Archaea in Icelandic hot springs based on 16S rRNA and chaperonin genes
Author(s) -
Mirete Salvador,
de Figueras Carolina G.,
GonzálezPastor Jose E.
Publication year - 2011
Publication title -
fems microbiology ecology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.377
H-Index - 155
eISSN - 1574-6941
pISSN - 0168-6496
DOI - 10.1111/j.1574-6941.2011.01095.x
Subject(s) - chaperonin , biology , phylogenetic tree , archaea , genetics , 16s ribosomal rna , gene , thermophile , ribosomal rna , clade , phylogenetics , groel , hsp60 , ribosomal protein , evolutionary biology , heat shock protein , bacteria , ribosome , escherichia coli , hsp70 , rna
The diversity of archaeal communities growing in four hot springs (65–90 °C, pH 6.5) was assessed with 16S rRNA gene primers specific for the domain Archaea . Overall, mainly uncultured members of the Desulfurococcales , the Thermoproteales and the Korarchaeota , were identified. Based on this diversity, a set of chaperonin heat‐shock protein (Hsp60) gene sequences from different archaeal species were aligned to design two degenerate primer sets for the amplification of the chaperonin gene: Ths and Kor (which can also detect the korarchaeotal chaperonin gene from one of the samples). A phylogenetic tree was constructed using the chaperonin sequences retrieved and other sequences from cultured representatives. The Alpha and Beta paralogs of the chaperonin gene were observed within the main clades and orthologs among them. Cultivated representatives from these clades were assigned to either paralog in the chaperonin tree. Uncultured representatives observed in the 16S rRNA gene analysis were found to be related to the Desulfurococcales . The topologies of the 16S rRNA gene and chaperonin phylogenetic trees were compared, and similar phylogenetic relationships were observed. Our results suggest that the chaperonin Hsp60 gene may be used as a phylogenetic marker for the clades found in this extreme environment.

The content you want is available to Zendy users.

Already have an account? Click here to sign in.
Having issues? You can contact us here