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The micromammal fauna of the reddish continental sediments of the Zorreras Member in the Sorbas Basin of SE Spain contains elements that are characteristic for the latest Miocene, close to the Mio-Pliocene limit. The paleomagnetic analysis shows that the entire sequence has reversed polarity. The combination of these data suggests that the Zorreras section must be correlated to chron C3r.
The micromammal sequence of the Calatayud-Montalbán Basin in Northeast Central Spain is exceptional in terms of its faunal richness and dating accuracy. However, until now, several classical localities with ages close to the Middle to Late Miocene transition have never been directly tied to the Geomagnetic Polarity Time Scale. Here, we present an updated stratigraphic framework for the Daroca area,...
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