0000000000480084

AUTHOR

Rolf T. W. Siegwolf

showing 3 related works from this author

Warm season precipitation signal in δ 2 H values of wood lignin methoxyl groups from high elevation larch trees in Switzerland

2017

RATIONALE In this study, we tested stable hydrogen isotope ratios of wood lignin methoxyl groups (δ 2Hmethoxyl values) as a palaeoclimate proxy in dendrochronology. This is a quite new method in the field of dendrochronology and the sample preparation is much simpler than the methods used before to measure δ2H values from wood. METHODS We measured δ 2Hmethoxyl values in high elevation larch trees (Larix decidua Mill.) from Simplon Valley (southern Switzerland). Thirty-seven larch trees were sampled and five individuals analysed for their δ 2Hmethoxyl values at annual (1971-2009) and pentadal resolution (1746-2009). The δ 2Hmethoxyl values were measured as CH3I released upon treatment of the…

010504 meteorology & atmospheric sciencesbiologyHydrogen isotope010401 analytical chemistryOrganic ChemistryXylemPositive correlationbiology.organism_classificationWarm season01 natural sciences0104 chemical sciencesAnalytical Chemistrychemistry.chemical_compoundAnimal sciencechemistryHigh elevationDendrochronologyLigninLarchSpectroscopy0105 earth and related environmental sciencesRapid Communications in Mass Spectrometry
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A 350 year drought reconstruction from Alpine tree ring stable isotopes

2010

[1] Climate reconstructions based on stable isotopes in tree rings rely on the assumption that fractionation-controlling processes are strongly linked to meteorological variables. In this context, we investigated the climate sensitivity of 350 years of carbon and oxygen isotope ratios of tree ring cellulose from European larch obtained at a high-elevation site in the Swiss Alps (∼2100 m above sea level). Unlike tree ring width and maximum latewood density, which contain only summer temperature information at this site, we found that our stable isotope series reveal additionally to temperature a striking sensitivity to precipitation (mainly for carbon) and sunshine duration (mainly for oxyge…

0106 biological sciencesAtmospheric ScienceGlobal and Planetary Change010504 meteorology & atmospheric sciencesStable isotope ratioContext (language use)Dendroclimatology15. Life on landAtmospheric sciences01 natural sciencesIsotopes of oxygen13. Climate actionIsotopes of carbonClimatologySunshine durationDendrochronologyEnvironmental ChemistryEnvironmental sciencePrecipitation010606 plant biology & botany0105 earth and related environmental sciencesGeneral Environmental ScienceGlobal Biogeochemical Cycles
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Low-frequency noise inδ13C andδ18O tree ring data: A case study ofPinus uncinatain the Spanish Pyrenees

2010

[1] Isotopic discrimination measurements in tree rings are becoming increasingly important estimators of past environmental change. Potential biases inherent to these parameters, including age trend and level offset are, however, not well understood. We here perform measurements on a new millennium-long data set of decadally resolved δ18O and δ13C discrimination from 25 high-elevation pine trees in the Spanish Pyrenees to investigate whether such low-frequency biases exist and how they alter the long-term behavior of derived time series. Alignment of the tree ring data by biological age reveals age trends over the first one to four centuries after germination. On average, isotope values cha…

Atmospheric ScienceGlobal and Planetary ChangeSeries (stratigraphy)Environmental changeδ13Cδ18OStable isotope ratioEcologyEstimatorDendrochronologyEnvironmental ChemistryPhysical geographyTree (set theory)General Environmental ScienceMathematicsGlobal Biogeochemical Cycles
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