carbon isotope
The successional status of tropical rainforest tree species is associated with differences in leaf carbon isotope discrimination and functional traits
9
Carbon isotope discrimination during litter decomposition can be explained by selective use of substrate with differing δ13C
33
Carbon isotope discrimination and water stress in trembling aspen following variable retention harvesting
7
Calibration of the carbon isotope composition (δ<sup>13</sup>C) of benthic foraminifera
20
Leaf senescence and carbon isotope discrimination in durum wheat(triticum durum desf.) under severe drought conditions
8
Carbon isotope signature of CH4 and CO2 as a tool to unravel diagenetic pathways in lake sediments.
1
Geology, biostratigraphy and carbon isotope chemostratigraphy of the Palaeogene fossil-bearing Dakhla sections, southwestern Moroccan Sahara
47
Multiple Early Eocene carbon isotope excursions associated with environmental changes in the Dieppe-Hampshire Basin (NW Europe)
16
Paleoproductivity during the middle Miocene carbon isotope events: A data-model approach
14
Genotypic Variability in Carbon Isotope Discrimination and Water Use Efficiency among Recombinant Inbred Lines of Sunflower (Helianthus annuus L.)
12
Carbon isotope offsets between benthic foraminifer species of the genus Cibicides ( Cibicidoides ) in the glacial sub-Antarctic Atlantic
21
Carbon Isotope Discrimination as a tool of durum wheat selection and its stability value in eastern High Plateau of Algeria
3
Genetic Control of Water Use Efficiency and Leaf Carbon Isotope Discrimination in Sunflower (Helianthus annuus L.) Subjected to Two Drought Scenarios
16
Carbon isotope labeling of carbamates by late-stage [$^{11}C$], [$^{13}C$] and [$^{14}C$] carbon dioxide incorporation
6
Dynamic Carbon Isotope Exchange of Pharmaceuticals with Labeled CO$_2$
7
The Emergence of Carbon Isotope Exchange
4
A Photochemical Strategy for Carbon Isotope Exchange with CO 2
25
Transition‐Metal‐Free Carbon Isotope Exchange of Phenyl Acetic Acids
8
Carbon isotope ratios suggest no additional methane from boreal wetlands during the rapid Greenland Interstadial 21.2
16
Primary production in coastal lagoons supported by groundwater discharge and porewater fluxes inferred from nitrogen and carbon isotope signatures
46