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Effect of global atmospheric carbon dioxide on glacial-interglacial vegetation change
Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences.
2000 (English)In: GLOBAL ECOLOGY AND BIOGEOGRAPHY, ISSN 0960-7447, Vol. 9, no 5, 355-361 p.Article in journal (Refereed) Published
Abstract [en]

Global vegetation changes at the time-scale of the Earth's orbital variations (10(4)-10(5) years) have been interpreted as a direct effect of consequential climatic changes, especially temperature. At mid- and high latitudes, the evidence from fossil data

Place, publisher, year, edition, pages
BLACKWELL SCIENCE LTD , 2000. Vol. 9, no 5, 355-361 p.
Keyword [en]
carbon dioxide; CO2 limitation; GCM; Late Glacial Maximum; palaeoclimate; palaeoecology; Quaternary; tropical mountains; vegetation change; PAPUA-NEW-GUINEA; ELEVATED CO2; CLIMATE INTERACTIONS; C-4 ANNUALS; QUATERNARY; MAXIMUM; ECOSYSTEMS; HISTORY; RECORD
National Category
URN: urn:nbn:se:uu:diva-37685OAI: oai:DiVA.org:uu-37685DiVA: diva2:65584
Addresses: Bennett KD, Uppsala Univ, Dept Earth Sci, Villavagen 16, S-75236 Uppsala, Sweden. Uppsala Univ, Dept Earth Sci, S-75236 Uppsala, Sweden. Univ Oxford, Sch Geog, Oxford OX1 3TB, England.Available from: 2008-10-17 Created: 2008-10-17 Last updated: 2011-01-14

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