TY - JOUR
T1 - Geomorphic influences on ground-flora and overstory composition in upland forests of northwestern lower Michigan
AU - Host, G. E.
AU - Pregitzer, K. S.
PY - 1992/1/1
Y1 - 1992/1/1
N2 - Spatial distribution patterns of the ground flora were significantly associated with glacial landform. Specific overstory-ground flora assemblages recur in characteristic landscape positions. The Interlobate Moraine, a predominant landform in the NE portion of the study area, was characterized by a northern hardwood canopy, primarily sugar maple Acer saccharum, basswood Tilia americana, and red oak Quercus rubra, with herbaceous annuals, perennials, and ephemerals forming the ground flora. Other morainal and glaciofluvial landforms supported oak Quercus spp. overstories with a woody ericaceous or graminoid ground flora. Ground-flora and overstory composition were highly correlated, indicating that they respond similarly to variation in environmental and historical factors. Moisture availability as evidenced by soil texture and the presence of subsurface textural discontinuities, appeared to be a predominant factor influencing species distribution patterns. Since moisture availability and related nutrient dynamics are functions of depositional and postglacial history, regional-scale geomorphic patterns constrain forest composition in a probabilistic manner. -from Authors
AB - Spatial distribution patterns of the ground flora were significantly associated with glacial landform. Specific overstory-ground flora assemblages recur in characteristic landscape positions. The Interlobate Moraine, a predominant landform in the NE portion of the study area, was characterized by a northern hardwood canopy, primarily sugar maple Acer saccharum, basswood Tilia americana, and red oak Quercus rubra, with herbaceous annuals, perennials, and ephemerals forming the ground flora. Other morainal and glaciofluvial landforms supported oak Quercus spp. overstories with a woody ericaceous or graminoid ground flora. Ground-flora and overstory composition were highly correlated, indicating that they respond similarly to variation in environmental and historical factors. Moisture availability as evidenced by soil texture and the presence of subsurface textural discontinuities, appeared to be a predominant factor influencing species distribution patterns. Since moisture availability and related nutrient dynamics are functions of depositional and postglacial history, regional-scale geomorphic patterns constrain forest composition in a probabilistic manner. -from Authors
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U2 - 10.1139/x92-205
DO - 10.1139/x92-205
M3 - Article
AN - SCOPUS:0027079431
SN - 0045-5067
VL - 22
SP - 1547
EP - 1555
JO - Canadian Journal of Forest Research
JF - Canadian Journal of Forest Research
IS - 10
ER -