Results 101 to 110 of about 26,538 (206)
The terrestrial sediment archives of northern Germany provide important insights into Late Pleistocene climate variability, but continuous and well‐dated records remain rare. In particular, the age and stratigraphic position of the Oerel and Glinde interstadials within the Early Weichselian to pleniglacial transition remain poorly constrained.
Alexis Badai Samudra +6 more
wiley +1 more source
Carbon (δ13C) and oxygen (δ18O) isotope compositions are considered indicators of the effect of water conditions on plant photosynthesis (δ13C) and transpiration (δ18O).
Fatima Zahra Rezzouk +3 more
doaj +1 more source
Vertical seed dispersal, which plays a key role in plant escape and/or expansion under climate change, was recently evaluated for the first time using negative correlation between altitudes and oxygen isotope ratio of seeds.
Shoji Naoe +3 more
doaj +1 more source
Quantifying errors in coral-based ENSO estimates: toward improved forward modeling of δ18O
The oxygen isotopic ratio (δ18O) in tropical Pacific coral skeletons reflects past El Niño-Southern Oscillation (ENSO) variability, but the δ18O-ENSO relationship is poorly quantified.
B Fox-Kemper (16153652) +3 more
core
Appendix B. Multivariate analysis of δ13C and δ18O signatures of fish otoliths.
Multivariate analysis of δ13C and δ18O signatures of fish ...
Chantal M. Huijbers (364776) +3 more
core +1 more source
This study investigates the ecology of the extinct European Hippopotamus from the late Early–Middle Pleistocene (c. 900–400 ka) sequence of the Megalopolis Basin, a glacial microrefugium for temperate taxa in southern Greece. Using stable carbon (δ13C) and oxygen (δ18O) isotope analyses and microwear analyses of Hippopotamus dental elements, we ...
Effrosyni Roditi +9 more
wiley +1 more source
Tree-ring δ18O and δ2H stable isotopes reflect the global meteoric water line
IntroductionThe Global Meteoric Water Line (GMWL) describes the linear relationship between stable hydrogen (δ2H) and oxygen (δ18O) isotopes in precipitation over large spatial scales and therefore represents a unique reference for water isotopic values.
Tito Arosio +16 more
doaj +1 more source
Key Points Triple oxygen isotope ratios of two primary (VSMOW, SLAP) and twelve secondary water isotopic reference materials were precisely measured using BrF5 fluorination‐IRMS. The measured Δ'17OVSMOW value for SLAP (34 ± 6 per meg) demonstrates that VSMOW‐SLAP normalisation ensures interlaboratory comparability, but introduces systematic offsets for
Ryoji Tanaka +2 more
wiley +1 more source
Diurnal to interannual rainfall δ18O variations in northern Borneo driven by regional hydrology [PDF]
The relationship between climate variability and rainfall oxygen isotopic (δ18O) variability is poorly constrained, especially in the tropics, where many key paleoclimate records rely on past rainfall isotopes as proxies for hydroclimate. Here we present
Andrew Alex, anak Tuen +5 more
core
Key Points New arsenopyrite reference materials (Niko and Sacra) for in situ multiple sulfur isotope measurement. Niko and Sacra are homogenous, near‐stoichiometric arsenopyrite. Niko serves as a primary matrix‐matched reference material, with lower measurement repeatability; Sacra is recommended as a secondary reference and quality control material ...
Bruna Coldebella +4 more
wiley +1 more source

