The Pleistocene ``Tundra-Steppe'' and the productivity paradox: the landscape approach
By B. A. Yurtsev. 2001
154 citations recorded by the source corpus.
Subfields: Atmospheric Science, Plant Science
View Paper: https://www.semanticscholar.org/paper/bf57550e72140fd17adfab8139c938901ec126f9
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In Atmospheric Science
- P. Groves
- Daniel H. Mann
- R. Reanier
- Jed O. Kaplan
- M. Kunz
- Benjamin V. Gaglioti
- Harry John Betteley Birks
- Pierre Legendre
In Plant Science
Citations in the corpus
- Ice-age megafauna in Arctic Alaska: extinction, invasion, survival (2013, background): “8) were excavated at the Engigstciak archaeological site 600 km east of the study area in the northwestern Yukon Territory (Cinq-Mars et al., 1991; MacNeish, 2000), though it is uncertain whether these bison represent B. priscus or Bison occidentalis.”
- Geophysical Applications of Vegetation Modeling (2001, background): “The existence and nature of a herbaceous vegetation type with floristic affinities to tundra and yet capable of supporting significant populations of large mammals has been a subject of much debate [Brubaker et al., 1983; Guthrie, 1985; Guthrie and Stoker, 1990; Lloyd et al., 1994; Ritchie, 1985; Yu”
- Biodiversity in temperate European grasslands: origin and conservation. (2005, unknown): “In terms of flora, the steppe-tundra was an intermediate between modern temperate grassland and tundra, or a mosaic of analogs of these biomes, generally having much drier and more alkaline soils than modern tundra (Yurtsev, 2001; Zazula et al. , 2003).”
- The Ecological implications of a Yakutian mammoth's last meal (2008, background): “…that the vegetation was not uniform but locally differentiated into communities under the influence of factors such as exposure or shelter influencing snowlie and water availability (Elias et al., 1996; Kienast et al., 2001, 2005; Yurtsev, 2001; Goetcheus and Birks, 2001; Zazula et al., 2006b).”
- Beringia as a glacial refugium for boreal trees and shrubs: new perspectives from mapped pollen data (2005, background): “Even under the extreme climatic regimes of the LGM, the Beringian landscape was likely characterized by a wide range of temperature and moisture conditions (Schweger, 1982; Guthrie, 2001; Yurtsev, 2001).”