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Sammanfattning

Boreal peatlands are key high-latitude ecosystem types and act as a carbon (C) sink storing an estimated 25% of the world's soil C. These environments are currently seeing the most substantial changing climate, especially during the winter. CO2 emissions during the winter can correspond to 80% of the growing season's net CO2 assimilation. Yet, our conceptual understanding of the controls on microbial metabolic activity in peat soils at temperatures

Nyckelord

Frozen peat soils; Microbial activity; Metabolism; C-13-NMR; DNA; Carbon cycling

Publicerad i

Soil Biology and Biochemistry
2019, volym: 135, sidor: 438-448
Utgivare: PERGAMON-ELSEVIER SCIENCE LTD

SLU författare

UKÄ forskningsämne

Markvetenskap

Publikationens identifierare

  • DOI: https://doi.org/10.1016/j.soilbio.2019.06.006

Permanent länk till denna sida (URI)

https://res.slu.se/id/publ/101161