Please use this identifier to cite or link to this item: https://cir.cenieh.es/handle/20.500.12136/3049
Title: The dawn of the Late Villafranchian: Paleoenvironment and age of the Pantalla paleontological site (Italy; Early Pleistocene)
Authors: Cherin, Marco
Basilici, Giorgio
Duval, Mathieu
Shao, Qingfeng
Sier, Mark Jan
Parés, Josep María
Gliozzi, Elsa
Mazzini, Ilaria
Magri, Donatella
Di Rita, Federico
Iurino, Dawid A.
Azzarà, Beatrice
Margaritelli, Giulia
Pazzaglia, Fausto
Keywords: Biochronology;Gelasian;Mammals;Middle-Late Villafranchian;Paleomagnetism;Pollen;Ostracods;U-series/ESR dating
Issue Date: Sep-2023
Publisher: Elsevier
Citation: Quaternary Science Reviews, 2023, 316, 108279
Abstract: Biochronology is the most widely used method for organizing the successions of continental vertebrate faunas in geological time and for allowing the correlation of continental deposits. However, due to the fragmentary nature of the paleontological record and the diachronicity of first and last occurrences of vertebrate taxa in different areas (i.e., bioevents), it is difficult to precisely define the temporal boundaries between biochronological units. That is why it is crucial to calibrate biochronological data with independent proxies wherever possible. Here, thanks to an interdisciplinary approach that combines sedimentology and stratigraphy, vertebrate paleontology, micropaleontology (ostracods), palynology, and geochronology, we provide a chronological framework and a paleoenvironmental reconstruction of the paleontological site of Pantalla (Central Italy). The combination between biochronological/biostratigraphic and geochronological (U-series/ESR dating and paleomagnetism) data allows us to refer the site to c. 2.2 Ma, i.e., in the transition phase between the Middle and Late Villafranchian in the European biochronological scheme. We reconstruct the environment as a fluvial area with a frequently flooded wet floodplain and marked (probably seasonal) variations of the water level of the channel river. The depositional system was surrounded by a conifer-dominated forest, which is suggestive of a glacial phase.
URI: https://cir.cenieh.es/handle/20.500.12136/3049
ISSN: 0277-3791
1873-457X
DOI: 10.1016/j.quascirev.2023.108279
Editor version: https://doi.org/10.1016/j.quascirev.2023.108279
Type: Article
Appears in Collections:Datación por Resonancia Paramagnética Electrónica
Geocronología y Geología



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