The role of hydrological transience in peatland pattern formationMorris, P. J., Baird, A. J. and Belyea, L. R. (2013) The role of hydrological transience in peatland pattern formation. Earth Surface Dynamics, 1 (1). pp. 31-66. ISSN 2196-6338
It is advisable to refer to the publisher's version if you intend to cite from this work. See Guidance on citing. To link to this item DOI: 10.5194/esurfd-1-31-2013 Abstract/SummaryThe sloping flanks of peatlands are commonly patterned with non-random, contour-parallel stripes of distinct microhabitats such as hummocks, lawns and hollows. Patterning seems to be governed by feedbacks among peatland hydrological processes, plant micro-succession, plant litter production and peat decomposition. An improved understanding of peatland patterning may provide important insights into broader aspects of the long-term development of peatlands and their likely response to future climate change.
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