In this study we report a new fossillocality found in the continental sediments of the Tudela Formation. This formation is composed of palustrine, lacustrine and distal aluvial facies that represent the sedimentary filling of the west-central sector of the Ebro basin during the Ramblian and Aragonian (/ower Miocene). Based on the study of micromammals remnants, the new fossillocality can be placed within the Ramblian biozone Z.
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