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Quaternary History of Deciduous Forests of Eastern North America and Europe

Davis, Margaret B.·1983·Annals of the Missouri Botanical Garden
DOI 10.2307/2992086
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all as today (isotope curves above dashed lines) for only short periods during the Quaternary. The three cores record nine glacialinterglacial cycles during the last 800,000 years (modified from Johnson, 1982). FiGURe 1. Oxygen-isotope ratios in three deep-sea cores, plotted against time. The low points on the curves represent periods when glaciers were expanded, the high points, periods when glaciers were contracted. Interglacial stages are indicated by Arabic numerals 5, 7,
all as today (isotope curves above dashed lines) for only short periods during the Quaternary. The three cores record nine glacialinterglacial cycles during the last 800,000 years (modified from Johnson, 1982). FiGURe 1. Oxygen-isotope ratios in three deep-sea cores, plotted against time. The low points on the curves represent periods when glaciers were expanded, the high points, periods when glaciers were contracted. Interglacial stages are indicated by Arabic numerals 5, 7,CC-BY-NC-SA · From the PDF
Image 2
CC-BY-NC-SA · From the PDF
3 £11 the retreat of the ice. Small numbers indicate 5 individual sites, as indicated by fossil pollen (see text).
3 £11 the retreat of the ice. Small numbers indicate 5 individual sites, as indicated by fossil pollen (see text).CC-BY-NC-SA · From the PDF
Image 4
CC-BY-NC-SA · From the PDF
was ex Fig ; bes 2 Range extension of four deciduous tree species or ge ds Slowest species to extend its range northward. Beech moved nort ding westward across the lower Great Lakes region (from Davis, 1983) nera following the retreat of the ice. Chestnut hward east of the Appalachians,
was ex Fig ; bes 2 Range extension of four deciduous tree species or ge ds Slowest species to extend its range northward. Beech moved nort ding westward across the lower Great Lakes region (from Davis, 1983) nera following the retreat of the ice. Chestnut hward east of the Appalachians,CC-BY-NC-SA · From the PDF
FIGURE 6 i jm map of Europe, showing the distribution of ice sh and major vegetation types during the full-glacial, L 18, 000 to 20,000 years ago.
FIGURE 6 i jm map of Europe, showing the distribution of ice sh and major vegetation types during the full-glacial, L 18, 000 to 20,000 years ago.CC-BY-NC-SA · From the PDF
Image 7
CC-BY-NC-SA · From the PDF

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Research works printed but not linked: 11

  1. editors), The Late Quaternary of the United States, Vol. II. University of Minnesota Press, Minne- li AKER & T. WEBB, III. 1973. Cal- & Plant Ecology. Blackwell, London & E. S. Deevey. 1964. Pollen accumulatio rates: estimates from late-glacial sediment of Rot ers Lake. Science 145: 1293-1295.
  2. Honey, B. & H. J. B. Birks. 1983. pe Past and Present Pollen for Europe 0-1 An Atlas of 000 Years re Cambridge University Press, i ut
  3. Kine, J. E. & E. H. Linpsay. 1980. Tar tas biotic records from spring -? coil souri. Pp. 63-78 in W. R. Wood & R. B.M Poio; Prehistoric Man and His En c Press, New hie T ju & M. B. Dvd 1972. Pollen ^ dence of Pleistocene and Holocene vegeta | | 1983] the Allegheny Plateau, Maryland. Quaternary Re- search 2: 506-530.
  4. Ohare. T T 2 WEBB, III. 1983. Calibration of nu merical diss milarity measures for matchi modern and fo ssil spectra. Bull. Ecol. Soc. (e 64(2):155.
  5. PETERSON, G. M., T. WEBB, III, zs thai pip, T. VAN DER HAMMEN, T . A. WUM & F. A. STRUT 1979. The continental record of environmental nitial investi- 782, 1935. British floras diitecedenit to the at I e. In Discussions on the origin and oerni pé the British flora. Proc. Roy. Soc London, Ser. B Biol. Sci. 118: 197-241.
  6. SOLOMON, A. M. 1982. Plant community respons to decreased seasonality during full glacial tae AMQUA deis 1982: 82. , D. J. A. SoLoMON. 1981. The role ofi climate Point and species immigration in for- est succession. Pp. 154-177 i
  7. West & D. B. Botkin (editors) ay Succes- sion. Er CA New TAM AE, J. & T. W. ANDERSON. 1970. Hypsi- - al range uo of white pine (Pinus stro- of bus L.) in Quebec, Canada. Canadian Journal 13, 3. Some ary plants. In A. tlam (editor), Atlas of reaktante El- k sevier, Amsterdam.
  8. RAVERSE, A. 1982. Res esponse of world vegetation to Neogene tectonic and climatic events. Alcheringa ; 6: 197-209.
  9. DER HAMMEN, T., T. A. W RA & W. H. ZAG- ( . The floral iic of a? late Ceno- zoic of Europe. Pp. 391-424 in K. K. Turekian Da , The Late Cenozoic Glacial Ages. Yale niversity je New Haven.
  10. VAN Di Whi Late Qua te ernary vegetation history at Perd Pond on the inner coastal plain of South lina. Quaternary Research 13: 187-199. : 1983. Vegetation history of eastern United States 25,000 to 10,000 years ago. Jn H. E. Wright & S. Porter (editors), The Late Quaternary of the United States, ies s I, the late Pleistocene. Uni- versity of Minnesota Press, Minneapolis.
  11. ----. 1970. Pleistocene history of the British flora. Pp. 1-11 in D. Walker & R. G. West (editors), Studies in the Vegetational History of the British Isles. Cambridge University Press, Cambridge. . 1980. Pleistocene forest history of East An- glia. New P 85: 571

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Authors
Davis, M. B.
Venue
Annals of the Missouri Botanical Garden
Publisher
JSTOR
Published
1983
Volume
70
Issue
3
Pages
550
ISSN
0026-6493
DOI
10.2307/2992086
Cited by
273
References
0

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