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Summers, Stephen; Thomson, Bruce C.; Whiteley, Andrew and Cockell, Charles S.
(2016).
DOI: https://doi.org/10.1080/01490451.2015.1039672
Abstract
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, ability to solubilise 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 persistence in this environment. Moreover, our study showed that the cold basaltic critical-zone is a region of active phosphate mineral-weathering.
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About
- Item ORO ID
- 43257
- Item Type
- Journal Item
- ISSN
- 1521-0529
- Project Funding Details
-
Funded Project Name Project ID Funding Body Not Set Not Set The Centre for Ecology and Hydrology, UK Not Set Not Set The Open University, UK - Keywords
- critical-zone; weathering; bacteria; MPS; soil microbiology
- Academic Unit or School
- Faculty of Science, Technology, Engineering and Mathematics (STEM)
- Copyright Holders
- © 2016 Taylor and Francis
- Depositing User
- Stephen Summers