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Methane seep carbonates yield clumped isotope signatures out of equilibrium with formation temperaturesPronounced zonal heterogeneity in Eocene southern high-latitude sea surface temperaturesTerrestrial cooling in Northern Europe during the eocene-oligocene transitionBody temperatures of modern and extinct vertebrates from ¹³C-¹⁸O bond abundances in bioapatiteA new measurement technique reveals temporal variation in delta18O of leaf-respired CO2.Large and unexpected enrichment in stratospheric 16O13C18O and its meridional variation.Long-term continuous sampling of ¹²CO₂, ¹³CO₂ and ¹²C¹⁸O¹⁶O in ambient air with a quantum cascade laser spectrometer.Isotopic ordering in eggshells reflects body temperatures and suggests differing thermophysiology in two Cretaceous dinosaurs.Carbonates in the Martian meteorite Allan Hills 84001 formed at 18 +/- 4 degrees C in a near-surface aqueous environmentCommunity software for challenging isotope analysis: First applications of 'Easotope' to clumped isotopes.Reconstruction of limnology and microbialite formation conditions from carbonate clumped isotope thermometry.Statistical clumped isotope signatures.Tracing formation and durability of calcite in a Punic-Roman cistern mortar (Pantelleria Island, Italy).Dinosaur body temperatures determined from isotopic (¹³C-¹⁸O) ordering in fossil biominerals.Precision and long-term stability of clumped-isotope analysis of CO2 using a small-sector isotope ratio mass spectrometer.Clumped isotope analysis of carbonates: comparison of two different acid digestion techniques.Non-linear mixing effects on mass-47 CO2 clumped isotope thermometry: Patterns and implications.High-precision determination of ¹³C-¹⁸O bonds in CO₂ using multicollector peak hopping.Gas formation. Formation temperatures of thermogenic and biogenic methane.Measurement of rare isotopologues of nitrous oxide by high-resolution multi-collector mass spectrometry.The effects of Porapak™ trap temperature on δ(18)O, δ(13)C, and Δ47 values in preparing samples for clumped isotope analysis.Reducing contamination parameters for clumped isotope analysis: The effect of lowering Porapak™ Q trap temperature to below -50°C.Assessing kinetic fractionation in brachiopod calcite using clumped isotopes.An improved method of high-precision determination of Δ(17)O of CO2 by catalyzed exchange with O2 using hot platinum.Pressure baseline correction and high-precision CO2 clumped-isotope (∆47) measurements in bellows and micro-volume modes.Sample matrix effects on measured carbon and oxygen isotope ratios during continuous-flow isotope-ratio mass spectrometry.Measurements of18O18O and17O18O in the atmosphere and the role of isotope-exchange reactionsExploring the potential of clumped isotope thermometry on coccolith-rich sediments as a sea surface temperature proxyA modified procedure for gas-source isotope ratio mass spectrometry: the long-integration dual-inlet (LIDI) methodology and implications for clumped isotope measurementsBackground effects on Faraday collectors in gas-source mass spectrometry and implications for clumped isotope measurementsInfluence of climate change and uplift on Colorado Plateau paleotemperatures from carbonate clumped isotope thermometry
P2860
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P2860
description
article
@en
im Dezember 2004 veröffentlichter wissenschaftlicher Artikel
@de
wetenschappelijk artikel
@nl
наукова стаття, опублікована в грудні 2004
@uk
ലേഖനം
@ml
name
18O13C16O in Earth’s atmosphere
@en
18O13C16O in Earth’s atmosphere
@nl
type
label
18O13C16O in Earth’s atmosphere
@en
18O13C16O in Earth’s atmosphere
@nl
prefLabel
18O13C16O in Earth’s atmosphere
@en
18O13C16O in Earth’s atmosphere
@nl
P1476
18O13C16O in Earth’s atmosphere
@en
P304
P356
10.1016/J.GCA.2004.05.035
P577
2004-12-01T00:00:00Z