The analysis of the stable isotope of the tree-ring cellulose is an important tool for paleo climatic investigations. Long tree-ring chronologies consist predominantly of oaks and conifers in Europe, including larch trees (Larix decidua) and cembran pines (Pinus cembra) that form very long tree ring chronologies in the Alps and grow at the treeline, where tree growth is mainly determined by temperature variations. We analyzed δ13C, δ18O and δ2H isotopes in the cellulose extracted from tree-rings of wood samples collected at high altitude in the Swiss and Tyrol Alps, covering the whole Holocene period. We found that larch cellulose was remarkably more depleted in deuterium than that of cembran pine, with mean δ2H values of −113.4 ± 9.7‰ for ...
Carbon and oxygen isotopes (δ13C and δ18O) in tree rings are widely used to reconstruct palaeoclimat...
RATIONALE Carbon, hydrogen and oxygen (C, H and O) stable isotope ratios of whole wood and component...
We have measured annual oxygen and hydrogen isotope ratios in the α-cellulose of the latewood of oak...
Tree rings are one of the most commonly used proxies for palaeoclimatic studies of the Holocene, in...
This is the first Europe-wide comprehensive assessment of the climatological and physiological infor...
Stable isotope ratios from tree rings are important proxies of past climate variations. We have acce...
Cellulose content (CC (%)) in tree rings is usually utilised as a tool to control the quality of the...
Stable isotopes in tree-ring cellulose are important tools for climatic reconstructions even though ...
Oxygen and hydrogen isotopes of cellulose in plant biology are commonly used to infer environmental ...
- The oxygen isotope composition (δ18O) of tree-ring cellulose is used to evaluate tree physiologica...
We analyzed the chronologies of cellulose stable isotopes (\u3b413C and \u3b418O) and tree-ring widt...
The isotopic compositions of cellulose in tree rings provide a record of seasonal and annual climati...
International audienceWe analyzed the chronologies of cellulose stable isotopes (δ13C and δ18O) and ...
open3noSupported by the Italian National Project COFIN-2003 ‘Interventi selvicolturali e basiecofisi...
Carbon and oxygen isotopes (δ13C and δ18O) in tree rings are widely used to reconstruct palaeoclimat...
RATIONALE Carbon, hydrogen and oxygen (C, H and O) stable isotope ratios of whole wood and component...
We have measured annual oxygen and hydrogen isotope ratios in the α-cellulose of the latewood of oak...
Tree rings are one of the most commonly used proxies for palaeoclimatic studies of the Holocene, in...
This is the first Europe-wide comprehensive assessment of the climatological and physiological infor...
Stable isotope ratios from tree rings are important proxies of past climate variations. We have acce...
Cellulose content (CC (%)) in tree rings is usually utilised as a tool to control the quality of the...
Stable isotopes in tree-ring cellulose are important tools for climatic reconstructions even though ...
Oxygen and hydrogen isotopes of cellulose in plant biology are commonly used to infer environmental ...
- The oxygen isotope composition (δ18O) of tree-ring cellulose is used to evaluate tree physiologica...
We analyzed the chronologies of cellulose stable isotopes (\u3b413C and \u3b418O) and tree-ring widt...
The isotopic compositions of cellulose in tree rings provide a record of seasonal and annual climati...
International audienceWe analyzed the chronologies of cellulose stable isotopes (δ13C and δ18O) and ...
open3noSupported by the Italian National Project COFIN-2003 ‘Interventi selvicolturali e basiecofisi...
Carbon and oxygen isotopes (δ13C and δ18O) in tree rings are widely used to reconstruct palaeoclimat...
RATIONALE Carbon, hydrogen and oxygen (C, H and O) stable isotope ratios of whole wood and component...
We have measured annual oxygen and hydrogen isotope ratios in the α-cellulose of the latewood of oak...