. Contributions from the Osborn Botanical Laboratory. Plants. 386 George E. Nichols, usually covered with broad-leaved trees, such as maple, beech and birch, because it is well ; In other words, Macoun would seem to intimate that in the mountains, as the writer has shown to be locally the case in the lowland, the evergreen coniferous forest is to be regarded as an edaphic rather than. Figure 47.—Primeval coniferous forest of the regional climax type; mountains near Cape North. a climatic climax association-type. With this opinion the writer emphatically disagrees for reasons which
. Contributions from the Osborn Botanical Laboratory. Plants. 386 George E. Nichols, usually covered with broad-leaved trees, such as maple, beech and birch, because it is well ; In other words, Macoun would seem to intimate that in the mountains, as the writer has shown to be locally the case in the lowland, the evergreen coniferous forest is to be regarded as an edaphic rather than. Figure 47.—Primeval coniferous forest of the regional climax type; mountains near Cape North. a climatic climax association-type. With this opinion the writer emphatically disagrees for reasons which are briefly outlined below. In ascending the mountain slopes which flank the plateau, there is a gradual transition from the forests of the lowland climax type to those of the highland, a transition which has been repeatedly traced out and verified. In passing upward, the. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Osborn Botanical Laboratory. [New Haven?] Osborn Botanical Laboratory, Yale University
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