The Pleistocene "Tundra-Steppe" and the productivity paradox: the landscape approach

被引:114
作者
Yurtsev, BA [1 ]
机构
[1] Russian Acad Sci, VL Komarov Bot Inst, St Petersburg 196140, Russia
关键词
D O I
10.1016/S0277-3791(00)00125-6
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Tundra-steppe means either a certain type of plant community with codominance of both steppe and tundra species (including prostrate shrubs), or a type of landscape, codominated by both steppe and tundra (Yurtsev, Relic Steppe Complexes of Northeastern Asia. Nauka Press, Novosibirsk (in Russian) 1981; In: Hopkins, Matthews Jr., Schweger, Young, (Eds.), Paleoecology of Beringia. Academic Press, New York, 1982, pp. 157-177). A discrepancy between Pleistocene glacial climates that were much colder and drier than present in Beringia and the highly diverse herbivorous fossil fauna (the "productivity paradox") is explained in terms of much greater diversity of herbaceous vegetation (grasses, sedges and forbs) in the mosaic of Beringian 'tundra-steppe' landscapes. Analysis of the relic distribution of some predominantly herbaceous plant communities throughout Beringia (Yurtsev, 1981, 1982, Komarovskiye chteniya (Vladivostok) 33 (1986) 3-53 tin Russian); Protection of Gene- and Coenotic Pool of the Herbaceous Biogeocoenoses, Sverdlovsk, 1988, pp. 128-129 (in Russian); Bridges of Science Between North America and the Russian Far East, 45th Arctic Science Conference, Abstracts, Vol. 1. Dalnauka Press, Vladivostok, 1994, p. 268; Paleontological Journal, 6 (1996)) provides the phytogeographic and landscape - ecological grounds for the reconstruction of plant cover of these landscapes. Dry watersheds and slopes had cryophytic (cold-adapted) steppes, cryoxerophytic (cold and dry-adapted) herbaceous and prostrate shrub-herbaceous communities, dry herb-prostrate shrub tundras, and tundra-steppe communities proper. All sorts of depressions on interfluves and in valleys along with concave pediments were occupied by dry steppe-meadows and brackish-water moist meadows. In some specific habitats sparse groupings of continental halophytes (plants growing in saline soils) of "arctic takkyrs", zoochoric (plants with seeds dispersed by animals) groupings of annual-biennial "ruderals" and, finally, sparse xeric-psammophytic (plants adapted to dry, sandy soils) vegetation of "sand seas" occurred. Meadows in valleys and on slope pediments were the most productive as pastures for ungulates due to the redistribution of moisture and nutrients within landscapes. The lowest parts of the exposed shelf in the Bering Strait vicinities were the "bottle-neck" for the dispersal of steppe plants and animals. (C) 2000 Elsevier Science Ltd. All rights reserved.
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页码:165 / 174
页数:10
相关论文
共 39 条
[1]  
4Yurtsev B.A., 1986, KOMAROVSKIYE CHTENIY, V33, P3
[2]  
BERMAN DI, 1997, BER PAL WORKSH, P32
[3]  
BERMUDEZ J, 1990, J GASTROINTEST MOTIL, V2, P281
[4]  
BOCHER TYGE W., 1954, MEDDEL GRONLAND, V148, P1
[5]   Life and times of the Bering land bridge [J].
Elias, SA ;
Short, SK ;
Nelson, CH ;
Birks, HH .
NATURE, 1996, 382 (6586) :60-63
[6]  
ELIAS SA, 1997, BER PAL WORKSH, P57
[7]  
Hibbert D, 1982, PALEOECOLOGY BERINGI, P153, DOI [10.1016/B978-0-12-355860-2.50017-X, DOI 10.1016/B978-0-12-355860-2.50017-X]
[8]  
Hopkins D. M., 1982, PALEOECOLOGY BERINGI, P1, DOI DOI 10.1016/B978-0-12-355860-2.50007-7
[9]  
Hopkins DM, 1982, PALEOECOLOGY BERINGI
[10]  
Katenin A. E., 1991, Botanicheskii Zhurnal (St. Petersburg), V76, P1616