Organic carbon fluxes from glaciers are a key control on biogeochemical cycles in polar regions. Two analyses of carbon cycling in glaciers show the importance of glacier–surface microbial communities in setting these inputs.
References
Boetius, A. et al. Nat. Rev. Microbiol. 13, 677–690 (2015).
Smith, H. J. et al. Nat. Geosci. 10, 356–359 (2017).
Musilova, M. et al. Nat. Geosci. 10, 360–365 (2017).
Bhatia, M. P. et al. Geochim. Cosmochim. Acta 74, 3768–3784 (2010).
Pautler, B. G. et al. Env. Sci. Technol. 46, 3753–3761 (2012).
Hood, E. et al. Nature 462, 1044–1047 (2009).
Stubbins, A. et al. Nat. Geosci. 5, 198–201 (2012).
Singer, G. A. et al. Nat. Geosci. 5, 710–714 (2012).
Franzetti, A. et al. ISME J. 10, 2984–2988 (2016).
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Kujawinski, E. The power of glacial microbes. Nature Geosci 10, 329–330 (2017). https://doi.org/10.1038/ngeo2933
Published:
Issue Date:
DOI: https://doi.org/10.1038/ngeo2933
- Springer Nature Limited