TY - GEN
T1 - Multiproxy cretaceous-paleogene boundary event stratigraphy
T2 - An Umbria-marche basinwide perspective
AU - Sinnesael, Matthias
AU - Montanari, Alessandro
AU - Frontalini, Fabrizio
AU - Coccioni, Rodolfo
AU - Gattacceca, T
AU - Snoeck, C.
AU - Wegner, Wencke
AU - Koeberl, Christian
AU - Morgan, L.
AU - De WInter, N.
AU - DePaolo, D. J.
AU - Claeys, Ph
N1 - Publisher Copyright:
© 2019 The Geological Society of America. All rights reserved.
PY - 2019
Y1 - 2019
N2 - The complete and well-studied pelagic carbonate successions from the Umbria- Marche basin (Italy) permit the study of the event-rich stratigraphic interval around the Cretaceous-Paleogene boundary (e.g., Deccan volcanism, boundary impact, Paleocene recovery, and climate). To test the robustness of various proxy records (bulk carbonate δ
13C, δ
18O,
87Sr/
86Sr, and Ca, Fe, Sr, and Mn concentrations) inside the Umbria-Marche basin, several stratigraphically equivalent sections were investigated (Bottaccione Gorge, Contessa Highway, Fornaci East quarry, Frontale, Morello, and Petriccio core). Besides the classical Gubbio sections of Bottaccione and Contessa, the new Morello section is put forward as an alternative location for this stratigraphic interval because it is less altered by burial diagenesis. Elemental profiles (Ca, Fe, Sr, Mn) acquired by handheld X-ray fluorescence (pXRF) efficiently provide regional chemostratigraphic and paleoenvironmental information. The Deccan volcanism, the Cretaceous-Paleogene boundary, the characteristic pattern of the Sr/Ca profile across the boundary driven by the extinction and recovery of coccolithophores, and the Dan- C2 hyperthermal event are examples of such recorded paleoenvironmental events. Moreover, cyclostratigraphic analyses of proxies of detrital input (magnetic susceptibility and Fe concentrations) show the imprint in the sedimentary record of a 2.4 m.y. eccentricity minimum around 66.45-66.25 Ma, and suggest that the occurrence of the Dan-C2 hyperthermal event was astronomically paced.
AB - The complete and well-studied pelagic carbonate successions from the Umbria- Marche basin (Italy) permit the study of the event-rich stratigraphic interval around the Cretaceous-Paleogene boundary (e.g., Deccan volcanism, boundary impact, Paleocene recovery, and climate). To test the robustness of various proxy records (bulk carbonate δ
13C, δ
18O,
87Sr/
86Sr, and Ca, Fe, Sr, and Mn concentrations) inside the Umbria-Marche basin, several stratigraphically equivalent sections were investigated (Bottaccione Gorge, Contessa Highway, Fornaci East quarry, Frontale, Morello, and Petriccio core). Besides the classical Gubbio sections of Bottaccione and Contessa, the new Morello section is put forward as an alternative location for this stratigraphic interval because it is less altered by burial diagenesis. Elemental profiles (Ca, Fe, Sr, Mn) acquired by handheld X-ray fluorescence (pXRF) efficiently provide regional chemostratigraphic and paleoenvironmental information. The Deccan volcanism, the Cretaceous-Paleogene boundary, the characteristic pattern of the Sr/Ca profile across the boundary driven by the extinction and recovery of coccolithophores, and the Dan- C2 hyperthermal event are examples of such recorded paleoenvironmental events. Moreover, cyclostratigraphic analyses of proxies of detrital input (magnetic susceptibility and Fe concentrations) show the imprint in the sedimentary record of a 2.4 m.y. eccentricity minimum around 66.45-66.25 Ma, and suggest that the occurrence of the Dan-C2 hyperthermal event was astronomically paced.
UR - http://www.scopus.com/inward/record.url?scp=85078242221&partnerID=8YFLogxK
U2 - 10.1130/2019.2542(07)
DO - 10.1130/2019.2542(07)
M3 - Contribution to proceedings
AN - SCOPUS:85078242221
SN - 978-0-8137-2542-0
T3 - Geological Society of America. Special Papers
SP - 133
EP - 158
BT - 250 million years of Earth history in central Italy
A2 - Köberl, Christian
A2 - Bice, David M.
PB - Geological Society of America
CY - Boulder
ER -