Stratigraphic record of the asteroidal Veritas breakup in the Tortonian Monte dei Corvi section (Ancona, Italy)

Alessandro Montanari, Ken Farley, Philippe Claeys, David De Vleeschouwer, Niels De Winter, Stef Vansteenberge, Matthias Sinnesael, Christian Koeberl

Onderzoeksoutput: Articlepeer review

15 Citaten (Scopus)

Samenvatting

The discovery of elevated concentrations of the cosmogenic radionuclide 3He in deep- sea sediments from Ocean Drilling Program (ODP) Site 926 (Atlantic Ocean) and ODP Site 757 (Indian Ocean) points toward ac- cretion of extraterrestrial matter, probably as a result of the catastrophic disruption of a large asteroid that produced the Veritas fam- ily of asteroids at ca. 8.3 ± 0.5 Ma, and which may have had important effects on the global climatic and ecologic systems. Here, we in- vestigated the signatures possibly related to the Veritas event by performing a high- resolution multiproxy stratigraphic analysis through the late Tortonian–early Messinian Monte dei Corvi section near Ancona, Italy. Closely spaced bulk-rock samples through a 36-m-thick section, approximately spanning from ca. 9.9 Ma to ca. 6.4 Ma, show an ~5- fold 3He anomaly starting at ca. 8.5 Ma and returning to background values at ca. 6.9 Ma, con rming the global nature of the event. We then analyzed, at 5 cm intervals, bulk-rock samples for sedimentary and environmen- tal proxies such as magnetic susceptibility, calcium carbonate content, total organic carbon, and bulk carbonate d18O and d13C, through a 21-m-thick section encompassing the 3He anomaly. Available high-resolution sea-surface temperature data (via alkenone analyses) for this site show a temperature decrease starting exactly at the inception of the 3He anomaly. Cyclostratigraphic fast- Fourier-transform spectral analyses of the proxies indicate an age of 8.47 ± 0.05 Ma for the inception of the 3He anomaly. A search for impact ejecta (analogous to what is pres- ent in the late Eocene, where both a 3He anomaly and large-scale impact events are recorded) was not successful. Detailed cy- clostratigraphic analyses of our data suggest that the changes in the stable isotope series and environmental proxy series through this late Tortonian time interval had a common forcing agent, and that perturbations of or- bitally forced climate cycles are present ex- actly through the interval with the enhanced in ux of extraterrestrial 3He. Thus, the che- mostratigraphic evidence for a collisional event that created the Veritas family of aster- oids, coinciding with climate perturbations on Earth, suggests yet another form of inter- action between Earth and the solar system.
Originele taal-2English
Pagina's (van-tot)1357-1376
Aantal pagina's20
TijdschriftGeological Society of America Bulletin
Volume129
Nummer van het tijdschrift(9-10)
DOI's
StatusPublished - 1 sep 2017

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