Grant: Discovery Grants Program - Individual
University of Northern British Columbia
$16,800.00
Soils and quaternary environments of northwestern Canada
EF 2006-07
Résumé
Soils and paleosols - soils of the past - are a rich archive of long-term environmental change in northwestern Canada. Soil evidence will be used to answer two important questions about the environmental history of eastern Beringia - the unglaciated region of Yukon and Alaska joined by lowered sea level to Siberia. Given the magnitude of recent and projected warming in northern Canada, this research program is timely as it will provide direct evidence of how terrestrial ecosystems responded to equally significant environmental changes in the past. First, do soils and their weathering products indicate that early Pleistocene interglacial climates were more temperate than at present? The mineralogy and geochemistry of soils, paleosols, and their parent materials in the west-central Yukon will be examined to identify: (1) inherited influences of preglacial weathering, (2) regional patterns in the properties of soils formed on early Pleistocene and Pliocene glacial deposits, (3) signatures of past climates preserved in the stable isotope composition of soil weathering products, and (4) landscape and historical patterns of soil formation on deeply weathered bedrock in unglaciated uplands. Second, did shifts between forest and steppe-tundra vegetation influence the deposition of silty wind-blown sediments (loess), and its subsequent modification by soil formation? At Kluane Lake, southwestern Yukon, Holocene loess deposition has occurred in a forest-grassland mosaic that provides analogues for many glacial and interglacial vegetation types in eastern Beringia. Examination of soils developed on loess and associated slope deposits will address: (1) differences in loess thickness and morphology in relation to slope position and vegetation type, (2) the historical record of loess redistribution after fires, as reconstructed by radiocarbon dating of buried charcoal, and (3) micromorphological evidence for the mechanisms of loess redistribution on slopes in relation to vegetation types.
Programme
Discovery Grants Program - Individual
Bénéficiaire
Emplacement
British Columbia, Canada
Type de bénéficiaire
Academia
Type
Grant
Source
NSERC's Awards Data
Tel que publié
Application id
283210-2006
Name nom
Sanborn, Paul
Department département
Forestry
Organization id
3
Institution établissement
University of Northern British Columbia
Province en
British Columbia
Province fr
Colombie-Britannique
Country en
CANADA
Country fr
CANADA
Fiscal year exercice financier
2006
Competition year année de concours
2006
Award amount
16800
Program id
RGPIN
Program name en
Discovery Grants Program - Individual
Program name fr
Programme de subventions à la découverte - individuelles
Group en
Discovery grants programs
Group fr
Programmes de subventions à la découverte
Committee code
9
Committee name en
Environmental Earth Sciences
Committee name fr
Sc. de la Terre : environ.
Area of application code
1203
Area of application group en
Advancement of knowledge
Area of application group fr
Avancement des connaissances
Area of application en
Earth sciences
Area of application fr
Sciences de la terre
Research subject code
4800
Research subject group en
Soil science
Research subject group fr
Science du sol
Research subject en
Soil science
Research subject fr
Science du sol
Partie
1
Nb partie
5
Application title
Soils and quaternary environments of northwestern Canada
Keyword
NA
Application summary
Soils and paleosols - soils of the past - are a rich archive of long-term environmental change in northwestern Canada. Soil evidence will be used to answer two important questions about the environmental history of eastern Beringia - the unglaciated region of Yukon and Alaska joined by lowered sea level to Siberia. Given the magnitude of recent and projected warming in northern Canada, this research program is timely as it will provide direct evidence of how terrestrial ecosystems responded to equally significant environmental changes in the past. First, do soils and their weathering products indicate that early Pleistocene interglacial climates were more temperate than at present? The mineralogy and geochemistry of soils, paleosols, and their parent materials in the west-central Yukon will be examined to identify: (1) inherited influences of preglacial weathering, (2) regional patterns in the properties of soils formed on early Pleistocene and Pliocene glacial deposits, (3) signatures of past climates preserved in the stable isotope composition of soil weathering products, and (4) landscape and historical patterns of soil formation on deeply weathered bedrock in unglaciated uplands. Second, did shifts between forest and steppe-tundra vegetation influence the deposition of silty wind-blown sediments (loess), and its subsequent modification by soil formation? At Kluane Lake, southwestern Yukon, Holocene loess deposition has occurred in a forest-grassland mosaic that provides analogues for many glacial and interglacial vegetation types in eastern Beringia. Examination of soils developed on loess and associated slope deposits will address: (1) differences in loess thickness and morphology in relation to slope position and vegetation type, (2) the historical record of loess redistribution after fires, as reconstructed by radiocarbon dating of buried charcoal, and (3) micromorphological evidence for the mechanisms of loess redistribution on slopes in relation to vegetation types.