The role of hydrological transience in peatland pattern formation


Autoria(s): Morris, P. J.; Baird, A. J.; Belyea, L. R.
Data(s)

2013

Resumo

The 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.

Formato

text

Identificador

http://centaur.reading.ac.uk/32951/1/Morris%20%202013_Role%20of%20hydrological%20transience.pdf

Morris, P. J. <http://centaur.reading.ac.uk/view/creators/90004079.html>, 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 doi: 10.5194/esurfd-1-31-2013 <http://dx.doi.org/10.5194/esurfd-1-31-2013>

Idioma(s)

en

Publicador

Copernicus Publications

Relação

http://centaur.reading.ac.uk/32951/

creatorInternal Morris, P. J.

10.5194/esurfd-1-31-2013

Tipo

Article

PeerReviewed