Mesophilic Mineral-Weathering Bacteria Inhabit the Critical-Zone of a Perennially Cold Basaltic Environment

S. Summers, B.C. Thomson, Andy Whiteley, C.S. Cockell

    Research output: Contribution to journalArticlepeer-review

    2 Citations (Scopus)

    Abstract

    © 2016, Copyright © Taylor & Francis Group, LLC. The weathering of silicate in the world's critical-zone (rock-soil interface) is a natural mechanism providing a feedback on atmospheric CO2 concentrations through the carbonate-silicate cycle. We examined culturable bacterial communities from a critical-zone in western Iceland to determine the optimum growth temperature and their ability to solubilize phosphate-containing minerals, which are abundant within the critical-zone area examined here. The majority of isolated bacteria were able to solubilize mineral-state phosphate. Almost all bacterial isolates were mesophilic (growth optima of 20–45°C), despite critical-zone temperatures that were continuously below 15°C, although all isolates could grow at temperatures associated with the critical-zone (−2.8–13.1°C). Only three isolates were shown to have thermal optima for growth that were within temperatures experienced at the critical-zone. These findings show that the bacteria that inhabit the western Icelandic critical-zone have temperature growth optima suboptimally adapted to their environment, implying that other adaptations may be more important for their long-term persistance in this environment. Moreover, our study showed that the cold basaltic critical-zone is a region of active phosphate mineral-weathering.
    Original languageEnglish
    Pages (from-to)52-62
    Number of pages11
    JournalGeomicrobiology Journal
    Volume33
    Issue number1
    DOIs
    Publication statusPublished - 2 Jan 2016

    Fingerprint

    Dive into the research topics of 'Mesophilic Mineral-Weathering Bacteria Inhabit the Critical-Zone of a Perennially Cold Basaltic Environment'. Together they form a unique fingerprint.

    Cite this