Magnetostratigraphic calibration of the Late Valanginian carbon isotope event in pelagic limestones from Northern Italy and Switzerland

Details Magnetostratigraphic calibration of the Late Valanginian carbon isotope event in pelagic limestones from Northern Italy and Switzerland Magnetostratigraphic calibration of the Late Valanginian carbon isotope event in pelagic limestones from Northern Italy and Switzerland

Jul 1993

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1993e%26psl.118..145c&link_type=abstract

Earth and Planetary Science Letters, Volume 118, Issue 1-4, p. 145-166.

Physics

11

Scientific paper

Magnetostratigraphic, biostratigraphic and carbon isotope data are presented from five Lower Cretaceous pelagic limestone sections in the Southern Alps. A positive carbon isotope event is recorded in bulk carbonate from the Upper Valanginian of all five sections, and the magnetostratigraphy and biostratigraphy provide the age model. The record of the isotope event in absolute time is closely replicated in all five sections. As the sections are located in two paleogeographic basins and are separated by up to 300 km, the synchronous isotope event cannot be interpreted as an artifact of diagenesis. A reduction in magnetization intensity coincident with the δ13C peak may be due to diagenetic magnetite dissolution enhanced by increased organic carbon burial.
According to the age model, which uses GTS89 timescale [1], background δ13C values of 1.5‰ are recorded from 145 to 137 Ma. Between 137 and 136 Ma, δ13C increases to a maximum value of about 3‰ Values begin to decrease from 136 Ma and reach background values at about 132 Ma. The rate of change of δ13C for the onset of the event (about 1.5‰/m.y.) is greater than for the decay (about 0.5‰/m.y.), suggesting an abrupt perturbation of the carbon system from equilibrium, followed by a more gradual return to background values.

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