Abstract
Coastal sand dunes in Europe (Warming 1891) and lake shore dunes in North America (Cowles 1899a, b, c) were among the first sites of description of relatively long-term vegetation changes. They were also early sites for experimental study of environmental changes correlated with vegetation change. G. D. Fuller, a student of H. C. Cowles, wrote in 1914 of his measurements of evaporation and soil moisture in plant communities believed to form a successional sequence on the Lake Michigan dunes.
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