Expression of soil characteristics related to
weathering and pedogenesis across a geomorphic surface of uniform age in
Michigan
Randall J. Schaetzl,Leslie R. Mikesell and Michael N. Velbel
Our
study explores the range of pedogenic development and near-surface weathering
on a large (>250,000 ha) geomorphic surface in northern lower
Michigan, via the examination of four typical soils. The surface is associated with proglacial
outwash from the Port Huron
advance of the Laurentide ice sheet, dated at about 13 ka. In a GIS we determined the four most
extensive types of upland soils on this surface, and later sampled them. The range of expression on
this outwash plain, when examined pedogenically or from a weathering
perspective, is large, but is captured by these four soils. Numerical rankings along a number of
pedogenic and weathering axes illustrated the considerable range of development,
but they generally were consistent, i.e., rankings for pedogenesis roughly
paralleled those for weathering. The
most weakly developed soil ranked 3rd or 4th on almost all of the pedogenic and
weathering-related parameters, whereas the other three soils exchanged ranks
more freely, depending on the parameter being considered. The best developed soils on this surface are
located in areas that receive more snowfall and, presumably, had less frequent
fires since deglaciation, both of which drive pedogenesis and weathering in
this region.
Soils on surfaces of uniform age are often used in
relative dating applications, by assuming that soil development and weathering
are related primarily to surface age.
Our study shows that this assumption is violated on large geomorphic
surfaces due to the variability of biotic and climatic factors across that
surface. Thus, we suggest that the range
and variability of soil expression must be considered in all soil
chronofunction studies.