A record of Lateglacial/Holocene environmental change from a high-elevation site in the Intermountain West, USA
Records of past vegetation and fire history can be complicated by changes in the depositional environment of a sampling location. However, these changes can alternatively be used as a measure of climate variability. Our study site, ca. 18.0 cal. ka BP record from Little Brooklyn Lake, Wyoming, locat...
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Veröffentlicht in: | Journal of quaternary science 2013-01, Vol.28 (1), p.103-112 |
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Sprache: | eng |
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