Organic matter accumulation, peat chemistry, and permafrost melting in peatlands of boreal Alberta.

In the discontinuous permafrost zone of boreal western continental Canada, permafrost is limited almost exclusively to ombrotrophic peatlands. Permafrost in peatlands recently has been degrading and continues to degrade at its southern limit across western Canada, with no evidence of regeneration. T...

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Bibliographic Details
Main Authors: Turetsky, Merritt., Wieder, R Kelman., Williams, Christopher., Vitt, Dale.
Format: Villanova Faculty Authorship
Published: 2000
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