2016
DOI: 10.1111/cag.12241
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Classification of vegetative lagg types and hydrogeomorphic lagg forms in bogs of coastal British Columbia, Canada

Abstract: Key Messages A classification scheme was developed for laggs (marginal transition zones) of bogs. Regional differences in vegetative lagg types were observed. Half of the studied laggs differed from the classic notion of a lagg as being topographically confined.

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Cited by 3 publications
(1 citation statement)
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“…Despite both fens and bogs being peat accumulating environments, there are many differences between fens and bogs. Fens are minerotrophic peatlands as they are supported by surface and groundwater inputs which provide nutrients leached from underlying bedrock and soils from their watershed (Rocchio et al, 2021) Bedford, 1999;Andersen et al, 2017;Dube et al, 2011;Howie & Meerveld, 2016), making it a very acidic environment (pH 4.0 to 4.8). The dome height of a raised bog increases gradually over decades due to peat accumulation.…”
Section: Research Questions and Objectivesmentioning
confidence: 99%
“…Despite both fens and bogs being peat accumulating environments, there are many differences between fens and bogs. Fens are minerotrophic peatlands as they are supported by surface and groundwater inputs which provide nutrients leached from underlying bedrock and soils from their watershed (Rocchio et al, 2021) Bedford, 1999;Andersen et al, 2017;Dube et al, 2011;Howie & Meerveld, 2016), making it a very acidic environment (pH 4.0 to 4.8). The dome height of a raised bog increases gradually over decades due to peat accumulation.…”
Section: Research Questions and Objectivesmentioning
confidence: 99%