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XXI.—The Climate during the Pleistocene Period

Published online by Cambridge University Press:  15 September 2014

G. C. Simpson
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Summary

It is assumed that the glaciation of Northern Europe during the great Ice Age was due to a shift of the pole associated with appreciable variations of solar radiation.

The shift of the pole brought Europe into sufficiently high latitudes to permit of the formation of an ice-sheet; but the large variations of climate during the Ice Age, as shown by the interglacial epochs, were due to the oscillations of the solar energy.

If two complete cycles of solar radiation occurred during the Pleistocene Period, it is possible to account for four advances of the ice in the Alps as demonstrated by Penck and Brückner, but the interglacial epochs were not all warm. The Günz-Mindel and the Riss-Würm interglacial epochs occurred at the maximum of the solar radiation and were, therefore, warm interglacial epochs; but the Mindel-Riss interglacial epoch occurred at a minimum of solar radiation and was, therefore, a cold interglacial epoch.

At a maximum of solar radiation—that is, during a warm interglacial epoch—the climate of North-West Europe was warm and very wet, with a relatively small annual variation of temperature. As the intensity of solar radiation decreased, the mean temperature fell and the annual variation of temperature increased. At the same time the amount of precipitation decreased. The fall of temperature occurred sufficiently rapidly compared with the decrease in precipitation to cause the glaciers of the Alps to advance and for an ice-sheet to form over Scandinavia. As the solar radiation still further decreased, the lack of precipitation caused the glaciers of the Alps to retreat. At the minimum of solar radiation there was a cold interglacial epoch with low mean temperature, a large annual variation of temperature and very low precipitation; in fact, a truly continental climate.

With these changes of climate went a corresponding change in the flora, the sequence being: park land, forest, tundra, grass with sparse trees, and steppe. In this way it has been found possible to determine a sequence of climates and of fauna and flora for the whole Pleistocene Period, which is supported by the geological and archæological evidence available. In particular it is possible to arrange the sequence of human culture, the geological strata of East Anglia, and the history of the ice in the Alps into the scheme of climate change.

The two maxima of solar radiation were accompanied by increased precipitation in all parts of the world, so accounting for the two pluvial periods which are known to have occurred during the Pleistocene Period.

Type
Proceedings
Information
Proceedings of the Royal Society of Edinburgh , Volume 50 , 1931 , pp. 262 - 296
Copyright
Copyright © Royal Society of Edinburgh 1931

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References

page 262 note * Penck, and Brückner, , Die Alpen im Eiszeitalter (Leipzig, 1909).Google Scholar

page 262 note † Penck and Brückner, loc. cit., p. 1168.

page 263 note * Penck and Brückner, loc. cit., p. 1142.

page 263 note † Köppen-Wegener, , Die Klimate der geologischen Vorzeit (Berlin, 1924), ch. vii.Google Scholar

page 264 note * Simpson, , Quart. Jour. Roy. Met. Soc., vol. liii, pp. 213–24, 1927.Google Scholar

page 268 note * (a) Simpson, Mem. Roy. Met. Soc., vol. iii, No. 21, 1928; (b) Mem. Manchester Lit. and Phil. Soc., vol. lxxiv, p. 1, 1929.

page 269 note * Kerner, , Sitzb. Akad. Wiss. Wien, vol. cxxxi, p. 153, 1922.Google Scholar

page 269 note † Brooks, , Climate Through the Ages (London, 1926).Google Scholar

page 270 note * Harmer, , Geol. Mag., vol. lxiii, p. 27, 1926.CrossRefGoogle Scholar

page 273 note * Soergel, , Lösse, Eiszeiten, und Palaeolithische Kulturen (Jena, 1919).Google Scholar

page 274 note * Loc. cit., p. 171.

page 274 note † In the shading I have covered two areas represented by Köppen and Wegener as being open sea. I cannot see how, under the condition represented, there could be open sea between latitudes 70° and 80°, nor how the sea could be maintained open to the west of Ireland without a warm ocean current, which could not exist with the wind distribution shown. These, however, are small points of detail without any significance to the main argument.

page 286 note * Wright, The Quarternary Ice Age, pp. 137–40.

page 286 note † Penck and Brückner, loc. cit., p. 839.

page 286 note ‡ Moir, Reid, The Antiquity of Man in East Anglia (Cambridge, 1927).Google Scholar

page 289 note * Reid, Clement, “The Geology of the Country Around Cromer,” Mem. Geol. Survey (London, 1882.)Google Scholar

page 289 note † The Upper Chalky Boulder Clay of East Anglia and the Brown Boulder Clay of the Hunstanton district (Reid Moir, Nature, 15th February 1930) are probably an early and a late phase of the Würm glaciation, and may correspond with Würm I and Würm II of the Alpine glaciation.

page 290 note * Moir, Reid, The Antiquity of Man in East Anglia (Cambridge, 1927), p. 101.Google Scholar

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page 292 note * Olbricht, loc. cit., p. 373.

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page 294 note † Meinardus, , Nach. Gesell, d. Wiss. zu Göttingen, Math.-Phys. Kl., Heft 2, 1928.Google Scholar

page 294 note ‡ G. K. Gilbert, “Lake Bonneville,” Washington, D.C., U.S. Geol. Survey, Monograph 1, 1890; I. C. Russell, “Geological History of Lake Lahontan: A Quaternary Lake of North-Western Nevada,” Washington, D.C., U.S. Geol. Survey, Monograph 11, 1885.

page 295 note * Wayland, , Man, vol. xxix, pp. 118–21, 1929.CrossRefGoogle Scholar Summary in Nature, vol. cxxi, p. 279, 1929.