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- Δ13C abstract "In geochemistry, paleoclimatology and paleoceanography δ13C is an isotopic signature, a measure of the ratio of stable isotopes 13C : 12C, reported in parts per thousand (per mil, ‰).The definition is, in per mil:where the standard is an established reference material.δ13C varies in time as a function of productivity, organic carbon burial and vegetation type.".
- Δ13C thumbnail Benthic_foraminifera.jpg?width=300.
- Δ13C wikiPageID "17737260".
- Δ13C wikiPageRevisionID "606652430".
- Δ13C subject Category:Bioindicators.
- Δ13C subject Category:Carbon.
- Δ13C subject Category:Environmental_isotopes.
- Δ13C subject Category:Geochemistry.
- Δ13C subject Category:Isotopes_of_carbon.
- Δ13C subject Category:Paleoclimatology.
- Δ13C comment "In geochemistry, paleoclimatology and paleoceanography δ13C is an isotopic signature, a measure of the ratio of stable isotopes 13C : 12C, reported in parts per thousand (per mil, ‰).The definition is, in per mil:where the standard is an established reference material.δ13C varies in time as a function of productivity, organic carbon burial and vegetation type.".
- Δ13C label "D13C".
- Δ13C label "Δ13C".
- Δ13C label "Δ13C".
- Δ13C label "Δ13C".
- Δ13C sameAs %CE%9413C.
- Δ13C sameAs Δ13C.
- Δ13C sameAs Δ13C.
- Δ13C sameAs Q3278929.
- Δ13C sameAs Q3278929.
- Δ13C wasDerivedFrom Δ13C?oldid=606652430.
- Δ13C depiction Benthic_foraminifera.jpg.
