Organization of the Niagara Escarpment cliff community. II. Characterization of the physical environment

Abstract

In cliff-edge forests along the Niagara Escarpment, an array of species, including Thuja occidentals, is restricted to the cliff edge while different species, including Acer saccharum, are increasingly dominant away from the cliff on the plateau. This paper presents detailed analyses of 13 components of the physical environment, measured over an 18-month period, as they change across the plateau and towards the cliff edge. Statistically significant differences between the cliff-edge habitat and the adjacent deciduous forest were found in most of the 13 variables, and the results indicate a strong environmental gradient between the cliff edge and deciduous forest habitats. Lower and more rapidly fluctuating soil moisture levels combined with low photosynthetically active radiation at the cliff edge suggest that conditions there are frequently more severe for plants than in the deciduous forest in summer. Additionally, the cliff edge was snow free during the winter and the soils were frozen for a more protracted period than the deciduous forest soils. Soil and litter depths decreased significantly from the deciduous forest toward the cliff edge. The effects of these differences are discussed with reference to the characteristics of species that dominate the deciduous and coniferous cliff-edge zones. Key words: cliff, gradient, Thuja occidentalis, Acer saccharum, microclimate, Niagara Escarpment.