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• W2017580564 abstract "In ail attempt to unravel the complicated ontogeny of some natural lakes in the North Carolina Coastal Plain on the basis of their accumulated sediments, the writer was led into the analysis of the plant and animal remains contained ill them. Pollens and spores, primarily those of aerial plants. are by far the most abundant of all microfossils in these sediments, and because of their diversity and very long period of accumulation they afford an excellent means of determining the relative total age of the sediments and of correlating the sediments from various parts of the basin as to contemporaneity. Pollen studies in eastern North America have been confined largely to the glaciated portion because of the abundance there of glacial basins filled with peat deposits. Similar studies south of the glacial boundary are few and scattered. The first of these by Lewis and Cocke (1929) and later by Cocke, Lewis, and Patrick (1934) describes the pollen and spores at various levels in the recent deposits of the Dismal Swamp near Lake Drummond in Virginia. Buell (1945) made some investigations on the sediments of Jerome Bay near Singletary Lake, but never published any comprehensive quantitative account of his findings. Cain (1944) reported on the pollen content of some buried soils in South Carolina, but these at present cannot be fitted into an overall chronology of the region for the determination of their relative age. Sears (1935) presented a few diagrams for Arkansas and eastern Tennessee. Darlington (1943) recorded the pollen sequence in a bog in West Virginia. Potzger (1945) shows a few diagrams from southern New Jersey. And finally, Potzger and Tharp (1947) present a significant pollen diagram from a bog in Texas. These analyses are still too scattered and often too fragmentary for one to draw generalizations or to try to find south of the glacial boundary the several postglacial climatic periods that have been established for the glaciated region. (See Deevey 1949, for a review of this problem.) The one generalization that can be made is that all of these southern diagrams which extend back far enough show spruce, and sometimes fir, in the lowermost horizons. It has been surmised that such horizons are from the Pleistocene." @default.
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• W2017580564 date "1951-07-01" @default.
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• W2017580564 title "Pollen Succession in the Sediments of Singletary Lake, North Carolina" @default.
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• W2017580564 doi "https://doi.org/10.2307/1931728" @default.
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