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"Forest-succession and ecology in the Knysna Region" ...Phillips, John Frederick Vicars, January 1931 (has links)
Thesis (D. SC.)--Edinburgh. / Includes bibliographical references (p. [321]-327; separate lists of references at end of appendices 1, 2 and 4: p. 255, 305 and 319).
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Structure of Texas vegetation east of the 98th meridianTharp, Benjamin Carroll, January 1900 (has links)
Thesis (Ph. D.)--University of Texas, 1925. / Bibliography: p. [89]-97.
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Structure of Texas vegetation east of the 98th meridianTharp, Benjamin Carroll, January 1900 (has links)
Thesis (Ph. D.)--University of Texas, 1925. / Bibliography: p. [89]-97.
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Atlantic coastal plain plants in the sand barrens of northwestern WisconsinMcLaughlin, Willard T. January 1932 (has links)
Presented as Thesis (Ph. D.)--University of Wisconsin--Madison, 1931. / Reprinted from Ecological monographs, vol. 2 (July 1932). Includes bibliographical references (p. 380-383).
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An ecological cross section of the Mississippi River in the region of St. Louis, MoHus, Henri, January 1908 (has links)
Thesis (Ph. D.)--Washington University, 1908. / Cover title. Offprint: Annual report of the Missouri Botanical Garden, 19th.
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An ecological cross section of the Mississippi River in the region of St. Louis, MoHus, Henri, January 1908 (has links)
Thesis (Ph. D.)--Washington University, 1908. / Cover title. Offprint: Annual report of the Missouri Botanical Garden, 19th.
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The interpretations of habitat, growth rate, and associated vegetation in the aspen community of Minnesota and Wisconsin ...Kittredge, Joseph, January 1900 (has links)
Thesis (PH. D.)--University of Minnesota, 1931. / Cover title. Vita. "Reprinted from Ecological monographs, 8 ... April, 1938." "Literature cited": p. 243-246.
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Effects of abiotic factors and cattle grazing on gypsum outcrop plant communities in the Cimarron Gypsum Hills, northwestern Oklahoma /Rice, Kristi Dawn. January 2008 (has links) (PDF)
Thesis (M.S.), Biology--University of Central Oklahoma, 2008. / Includes bibliographical references (leaves 98-104).
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Vegetation changes following fire in the pinyon-juniper type of west central UtahBarney, Milo Arnel 01 May 1972 (has links)
A total of 28 burn areas, that varied in age from 3-100+- years, were analyzed in a study of succession following fire, in the pin yon-juniper woodlands of west central Utah. Data were collected by means of the line-point and quadrat methods. These data were subjected to a multiple regression analysis. Canopy cover, basal area (sq. ft./acre) and density (trees/acre) of juniper were highly correlated with age of burn. Percentage dead sagebrush was found to be positively correlated with density of junipers. The stages of succession following fire began with weedy annuals, that reached a peak within 3-4 years. Juniper woodlands are well developed 85-90 years following fire. Intermediate stages of succession varied, but followed a general pattern of perennial grasses, perennial grasses-shrubs and perennial grasses-shrubs-trees. Tree height and stem diameter are positively correlated with age of Utah juniper. Thirty-three years is the average minimum age at which Utah juniper produce seed.
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Distribution of the major plant communities in UtahFoster, Robert Howard 01 May 1968 (has links)
Utah is a state containing a complexity of landforms in a unique continental setting which results in a variety of climatic and edaphic conditions. The variety, however, is not expressed on a latitudinal plane from north to south but is primarily altitudinal, changing from the playa or valley floors to the mountain tops. The associated arrangement of vegetation, consequently, is usually according to elevation, the elevation generally regulation precipitation and thus edaphic conditions. Slope exposure and position of landforms relative to storm-tracks are modifiers, and prevent fixed posisions for many vegetation types. Vegetation in Utah is as variable as are the physical features. Plant communities range from the salt-tolerant pickleweed types in the Great Basin playas to the alpine grass-carex communities of the upper Uinta Mountains. In the fine textured soils of the playa bottoms deflocculation of colloidal clays due to high salt concentrations is common and prevents water percolation. Up the mountain side the gradient generally increases, salts become less concentrated, soils more coarse or loamy, water percolation increases, temperatures are lower, and precipitation is higher. Plant communities change with these features and can generally be identified with a given environment anywhere in the state. Contemporary vegetation in Utah was divided into two major groups based on location in desert or mountain areas. These major groups were broken into subdivisions according to the general types of vegetation in each, and the subdivision into communities. The breakdown is as follows: I. DESERT VEGETATION TYPES A. Warm Temperate Desert Shrubs Creosotebush - Bursage Community B. Salt Marsh Vegetation Pickleweed Community Saltgrass Community C. Cold Temperate Desert Shrubs 1. Communities on Saline Soils and Regosols Greaseweed Community Shadscale Community Castle Valley Clover Community Mat-Atriplex Community 2. Communities on Non-saline Desert and Sierozem Soils Blackbrush Community Uinta Basin Codominant Community Desert Grass Community Horsebrush Community Winterfat Community Little Rabbitbrush Community Lower Riverbotom Community Sagebrush Community D. Pigmy Conifers Juniper-pinyon COmmunity II. Mountain Vegetation Types E. Mountain Shrubs Mountain brush Community F. Mountain Deciduous Forest Aspen Community G. Mountain Coniferous Forests Ponderosa Pine Community Lodgepole Pine Community Spruce-fir Community
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