0000000001313953

AUTHOR

Päivi Kaislahti Tillman

showing 4 related works from this author

Long-term climate variability in continental subarctic Canada: A 6200-year record derived from stable isotopes in peat

2010

The rapid warming of arctic regions during recent decades has been recorded by instrumental monitoring, but the natural climate variability in the past is still sparsely reconstructed across many a ...

PeatbiologyGlobal warmingPaleontologyClimate changeOceanographybiology.organism_classificationSphagnumSubarctic climateNatural (archaeology)OceanographyArcticPaleoclimatologyEcology Evolution Behavior and SystematicsGeologyEarth-Surface Processes
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Comparison of stable carbon and oxygen isotopes in Picea glauca tree rings and Sphagnum fuscum moss remains from subarctic Canada

2012

AbstractStable isotope ratios from tree rings and peatland mosses have become important proxies of past climate variations. We here compare recent stable carbon and oxygen isotope ratios in cellulose of tree rings from white spruce (Picea glauca), growing near the arctic tree line; and cellulose of Sphagnum fuscum stems, growing in a hummock of a subarctic peatland, in west-central Canada. Results show that carbon isotopes in S. fuscum correlate significantly with July temperatures over the past ~20 yr. The oxygen isotopes correlate with both summer temperature and precipitation. Analyses of the tree-ring isotopes revealed summer temperatures to be the main controlling factor for carbon iso…

PeatbiologyStable isotope ratiochemistry.chemical_elementbiology.organism_classificationSphagnum fuscumMossSubarctic climateIsotopes of oxygenArts and Humanities (miscellaneous)chemistryBotanyGeneral Earth and Planetary SciencesCarbonGeologyEarth-Surface ProcessesQuaternary Research
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(Table 1) Stable oxygen and carbon isotopic ratios of tree rings, and tree ring width of white spruce (Picea glauca), Ennadai Lake

2012

Stable isotope ratios from tree rings and peatland mosses have become important proxies of past climate variations. We here compare recent stable carbon and oxygen isotope ratios in cellulose of tree rings from white spruce (Picea glauca), growing near the arctic tree line; and cellulose of Sphagnum fuscum stems, growing in a hummock of a subarctic peatland, in west-central Canada. Results show that carbon isotopes in S. fuscum correlate significantly with July temperatures over the past ~20 yr. The oxygen isotopes correlate with both summer temperature and precipitation. Analyses of the tree-ring isotopes revealed summer temperatures to be the main controlling factor for carbon isotope var…

Picea glauca standard deviationPicea glauca δ18O tree ringsPicea glauca tree ring widthInternational Polar Year (2007-2008) (IPY)tree ring widthtree ringsSample IDTree ring samplingPicea glauca δ13C tree ringsInternational Polar Year 2007 2008 IPYδ13CEarth System Researchstandard deviationPicea glaucaδ18O
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Radiocarbon dates, accumulation rates, δ¹³C and July temperature of profiles obtained from Selwyn and Misaw Lake, subarctic Canada

2010

The rapid warming of arctic regions during recent decades has been recorded by instrumental monitoring, but the natural climate variability in the past is still sparsely reconstructed across many areas. We have reconstructed past climate changes in subarctic west-central Canada. Stable carbon and oxygen isotope ratios (d13C, d18O) were derived from a single Sphagnum fuscum plant component; alpha-cellulose isolated from stems. Periods of warmer and cooler conditions identified in this region, described in terms of a "Mediaeval Climatic Anomaly" and "Little Ice Age" were registered in the temperature reconstruction based on the d13C record. Some conclusions could be drawn about wet/dry shifts…

International Polar Year (2007-2008) (IPY)
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