The carbon-isotope signatures of Carnian (Late Triassic) amber drops from Rifugio Dibona (Southern Alps, Italy) were studied and compared with that of other Middle-early Late Triassic fossil plant remains, namely wood and leaves. Amber, wood and leaf carbon-isotope data are highly variable within the same beds. δ13Camber values vary by up to 5.4‰and are enriched by ~2.5‰with respect to associated wood. δ13Cwood and δ13Cleaf ranges are narrower than that of amber (~2–3‰) and the isotopic offset within each bed is similar over time. The high Triassic amber carbon-isotope variability is similar to that of recent resin. Despite the high variability, δ13Cwood and δ13Cleaf illustrate a Middle-early Late Triassic secular positive trend that is similar to that of marine δ13Cinorg data and must record the carbon-isotope evolution of the ocean–atmosphere system.

Carbon-isotope variability of Triassic amber, as compared with wood and leaves (Southern Alps, Italy)

DAL CORSO, JACOPO;PRETO, NEREO;MIETTO, PAOLO;
2011

Abstract

The carbon-isotope signatures of Carnian (Late Triassic) amber drops from Rifugio Dibona (Southern Alps, Italy) were studied and compared with that of other Middle-early Late Triassic fossil plant remains, namely wood and leaves. Amber, wood and leaf carbon-isotope data are highly variable within the same beds. δ13Camber values vary by up to 5.4‰and are enriched by ~2.5‰with respect to associated wood. δ13Cwood and δ13Cleaf ranges are narrower than that of amber (~2–3‰) and the isotopic offset within each bed is similar over time. The high Triassic amber carbon-isotope variability is similar to that of recent resin. Despite the high variability, δ13Cwood and δ13Cleaf illustrate a Middle-early Late Triassic secular positive trend that is similar to that of marine δ13Cinorg data and must record the carbon-isotope evolution of the ocean–atmosphere system.
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11577/2490777
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