1965
DOI: 10.2307/2423126
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Ecological Consideration of Cypress Heads in Northcentral Florida

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1966
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Cited by 29 publications
(16 citation statements)
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“…(1977), Schlesinger (1978), and Mitsch and Ewe! Earlier studies of cypress-tupelo swamps were primarily phytosociological (Beaven and Oosting 1939, Hall and Penfound 1939, 1943, Monk and Brown 1965 and physiological (Matoon 1916, Demaree 1932, Kurz and Demaree 1934, DenUyl 1961, Dickson and Broyer 1972. Wharton (1970) summarized the value of alluvial swamps in Georgia.…”
Section: Introductionmentioning
confidence: 99%
“…(1977), Schlesinger (1978), and Mitsch and Ewe! Earlier studies of cypress-tupelo swamps were primarily phytosociological (Beaven and Oosting 1939, Hall and Penfound 1939, 1943, Monk and Brown 1965 and physiological (Matoon 1916, Demaree 1932, Kurz and Demaree 1934, DenUyl 1961, Dickson and Broyer 1972. Wharton (1970) summarized the value of alluvial swamps in Georgia.…”
Section: Introductionmentioning
confidence: 99%
“…The cypress swamps, with Taxodium distichum and T. nutmts, are found fringing sloughs, inland l<igoons, ponds, lakes, and small depressions in pine flatwoods. T. nutans is characteristic of depressions in flatwoods where nutrient levels are extremely low and the soils acid (Monk and Brown 1965) while T. distichum is more important in alkaline areas (Laessle 1942). Both cypress communities are subjected to flooding.…”
Section: Introductionmentioning
confidence: 99%
“…Many cypress domes already had been logged or converted to agricultural or urban areas by the middle and end of the 20th century (Monk and Brown, 1965;. Our analysis shows that almost one-third of the extent of this system has been protected for conservation ( fig.…”
Section: Southern Coastal Plain Nonriverine Cypress Domementioning
confidence: 82%
“…Cypress domes have a characteristic dome-shaped appearance, and trees in the center of domes are taller and older than those on the sides (Monk and Brown, 1965;. The system is underlain by a clay pan that keeps water depths at 1-4 ft (0.3-1.2 m) toward the center, with shallower water toward the edges (Monk and Brown, 1965). Some pans are caused by water dissolving the underlying limestone bedrock (Florida Natural Areas Inventory, 2010).…”
Section: Southern Coastal Plain Nonriverine Cypress Domementioning
confidence: 99%