Al. Lottes et Am. Ziegler, WORLD PEAT OCCURRENCE AND THE SEASONALITY OF CLIMATE AND VEGETATION, Palaeogeography, palaeoclimatology, palaeoecology, 106(1-4), 1994, pp. 23-37
The climatic controls on present-day peat formation are examined in or
der to develop a uniformitarian tool for refining paleoclimate studies
, and to create a retrodictive model for the coals of the geologic rec
ord. A peat database has been compiled for the world and the resulting
patterns are compared with aspects of precipitation and temperature d
rawn from a gridded data set. Precipitation continuity through the ann
ual cycle is important for biologic productivity in the terrestrial re
alm. It is expressed in terms of the number of months with average pre
cipitation above 40 mm. Temperature is limiting at higher latitudes wh
ere the potential growing season may be defined by the number of month
s with mean temperature exceeding 10-degrees-C. A map predicting the g
rowing season has been constructed from these rainfall and temperature
statistics which compares very well with actual vegetation persistenc
e through the year as measured directly from satellite instruments. Ho
wever, biologic production will not result in peat accumulation unless
groundwater levels are maintained through the growing season. Our pea
t prediction map therefore shows the percentage of time that precipita
tion occurs during the potential growing season. Present-day peat accu
mulations are well predicted by this map.