Climate change and microbial populations

DOIResolve DOI:
AuthorSearch for:
TypeBook Chapter
Book titleAntarctic Terrestrial Microbiology
SubjectMicrobial ecology; Bacteriology; Microbial genetic; Microbial genomics; Geology
AbstractBy 2100, the mean air temperature at the Earth’s surface is predicted to increase by 1.4 °C to 5.8 °C, with a disproportionate effect at high altitudes and latitudes. This chapter reviews the currently available information regarding the responses of key microbial parameters, including diversity, community composition, abundance and functions, to climate change in Antarctic soils. For microorganisms inhabiting Antarctic soils, some insight has been gained by comparing microbial communities across latitudinal gradients, or through short-term laboratory incubations and field studies. Rapid responses of mosses, nematodes, soil algae, cyanobacteria, fungi, and bacteria have been observed in some Antarctic soils. Despite these interesting findings, it is difficult to specifically predict the effects of warming on Antarctic soil microorganisms. One reason is the extreme heterogeneity of soil habitats in this region, as they vary from moist eutrophic ornithogenic soils to nutrient- and water-limited Dry Valley soils. Climate change might have rapid and direct effects on soil microbes that are not otherwise limited, but the release of other limitations (e.g., water, nutrients) could be more important in several environments.
Publication date
PublisherSpringer International Publishing
AffiliationNational Research Council Canada
Peer reviewedYes
NPARC number23000087
Export citationExport as RIS
Report a correctionReport a correction
Record identifierf3260c2e-e309-4ada-916c-c66658abdf0f
Record created2016-06-02
Record modified2016-06-02
Bookmark and share
  • Share this page with Facebook (Opens in a new window)
  • Share this page with Twitter (Opens in a new window)
  • Share this page with Google+ (Opens in a new window)
  • Share this page with Delicious (Opens in a new window)