Cutting a newly extracted permafrost core into sections. Click on the photo for an enlarged image. |
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Carbon (C) stored within permafrost in northern boreal forest soils may become available
for microbial metabolism if soil temperatures continue to increase over the coming decades,
resulting in a positive feedback to climate warming. Understanding the potential of
permafrost carbon to be degraded requires a detailed understanding of the microbiology and
biochemistry of permafrost soils. Utilizing novel techniques in molecular biology,
fluorometry, and mass spectrometry, we will analyze the biological and chemical
constraints on C cycling at the molecular level.
There are three primary factors that may limit the rate at which decomposition of permafrost C occurs:
- chemical limitation, whereby high lignin and phenolic concentrations or low nitrogen (N) concentrations limit decomposition,
- biological limitation, whereby the microorganisms producing the proper suite of enzymes to decompose soil organic C are not present, and
- physical limitation, whereby low temperatures and low oxygen availability limit decomposition
Our strategy involves taking cores from two different permafrost conditions:
- a site with continuous permafrost and a shallow active layer (~40 cm) near Coldfoot, AK
- soils with a warmer climate, average annual temperatures near 0°C,
discontinuous permafrost, and a deeper active layer (~55 cm) near Fairbanks, AK
The following methods will be employed:
- incubation for potential CO 2 and DOC fluxes
- pyrolysis-gas chromatography/mass spectrometry (PYR-GCMS)
- specific ultraviolet absorbance (SUVA, a measure of aromatic DOC) and fluorescence spectroscopy
- quantitative PCR (QPCR)
- the measurement of enzyme activity associated with functional genes
- an enzyme digest experiment
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