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RESEARCH PRODUCT
Tree-ring δ2H values from lignin methoxyl groups indicate sensitivity to European-scale temperature changes
Frank KepplerBirgit SehlsTobias AnhäuserTobias AnhäuserWerner ThomasClaudia HartlDenis ScholzMarkus GreuleJan Espersubject
010506 paleontologybiologyIsotopePaleontologyScale (descriptive set theory)010502 geochemistry & geophysicsOceanographybiology.organism_classificationAtmospheric sciences01 natural scienceschemistry.chemical_compoundchemistryFagus sylvaticaMeteorological observatoryDendrochronologyLigninPrecipitationEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesChronologydescription
Abstract Stable hydrogen isotope ratios of lignin methoxyl groups (δ2HLM) of wood have been shown to reflect climate-sensitive δ2H values of precipitation (δ2Hprecip). However, a detailed calibration study between high-resolution δ2HLM and δ2Hprecip data has not been performed yet. Here, we present annually resolved δ2HLM values from nine tree-ring series (derived from four Fagus sylvatica L. trees) collected near a station of the Global Isotope Network of Isotopes in Precipitation (GNIP) and the meteorological observatory at Hohenpeisenberg (Germany; ~48°N, 11°E). The nine δ2HLM tree-ring series show highly significant inter-series correlations (Rbar = 0.52) over the common period of overlap 1916–2015 and no sign of a major juvenile trend affecting the first decades of growth. When compared with local instrumental data, the combined δ2HLM chronology is most indicative for annually averaged δ2Hprecip values. In line with this finding, the δ2HLM chronology shows similar climatic imprints as commonly observed for European stable water isotopes. We find the highest correlation (r = 0.72, p
| year | journal | country | edition | language |
|---|---|---|---|---|
| 2020-05-01 | Palaeogeography, Palaeoclimatology, Palaeoecology |