Dh. Vitt, AN OVERVIEW OF FACTORS THAT INFLUENCE THE DEVELOPMENT OF CANADIAN PEATLANDS, Memoirs of the Entomological Society of Canada, (169), 1994, pp. 7-20
Canadian peatlands can be classified into ombrotrophic bogs and minero
trophic fens, the latter subdivided into poor, moderate-rich, and extr
eme-rich fens, each with distinctive indicator species, acidity, alkal
inity, and base cation content. If hydrology is considered the most im
portant factor in peatland classification then the primary division mu
st be between ombrotrophic bogs and minerotrophic fens; however both c
hemical and vegetational differences strongly indicate that the primar
y division of peatlands should be between acidic, Sphagnum-dominated b
ogs and poor fens on the one hand, and alkaline, brown-moss-dominated
rich fens on the other. Although some metals such as sulphur and alumi
num also vary along this gradient, nutrient contents of the surface wa
ters do not. Bogs and fens are oligotrophic to mesotrophic wetlands th
at should be distinguished from eutrophic, non-peat-forming wetlands s
uch as marshes and swamps by the presence in the former of a well-deve
loped ground layer of bryophytes associated with relatively little sea
sonal water level fluctuation. Oligotrophy is probably maintained in b
ogs and poor fens by reduced water flow, whereas rich fens maintain me
sotrophy by having larger water through-puts; however this is not well
documented. Sphagnum appears to have real ecological significance, bo
th in the initial stages of acidification and in controlling surface w
ater temperature. Seasonal variation in surface water chemistry in all
peatland types is relatively small, however precipitation events lead
ing to changes in water levels do affect some chemical components. Alt
hough both autogenic and allogenic factors affect peatland development
, initiation of peat formation and early development of peatlands duri
ng the Early and Mid Holocene were considerably influenced by regional
climatic change. Later developmental patterns during the late Holocen
e and those seen at the present time appear to be more influenced by a
utogenic factors.