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Armor At War Series - Wwii - The Battle Of The Bulge

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1973. Modern pollen rain in some Arctic and alpine areas. In: H. J. B. Birks and R. G. ), Quaternary Plant Ecology, pp. 143-168, Blackwell, Oxford. Birks, H. J. B. and H. H. Birks, 1980. Quaternary Palaeoecology. Arnold, London. Birks, H. J. B. and A. D. Gordon, 1985. Numerical Methods in Quaternary Pollen Analysis. Academic Press, New York, 305 pp. Bonny, A. , 1976. Recruitment of pollen to the seston and sediment of some Lake District lakes. Journal of Ecology 64: 859-887. Bonny, A. , 1978.

E. that pollen source areas should increase with basin size. Bradshaw and Webb (1985) have provided the strongest empirical support for both propositions. They showed consistent differences among taxa in pollen source area, and consistent increases in the source area as the basin size increased from zero (samples from the forest floor) through < 9 ha (small basins) to 30-150 ha (moderate-sized basins). Prentice et al. (1987) also showed that the best correspondence between pollen percentages in moderate-sized basins and the surrounding vegetation occurred at different vegetation sampling scales for different taxa, depending on the size of the pollen grains.

Limiting factors in paleoecological reconstruction. In Geobotany, pp. 29-42. Plenum, New York. Olsson, I. , 1986. Radiometric dating. In Berglund, B. E. ) Handbook of Holocene Palaeoecology and Palaeohydrology, pp. 273-312. John Wiley & Sons, New York. Overpeck, J. T. and E. C. Fieri, 1982. The development of age models for Holocene sediment cores: Northeast North American examples, p. 152. In Abstracts, American Quaternary Association, Seattle. Patterson, W. A. III, K. J. Edwards, and D. J. Maguire, 1987.

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