作者: Elvira Martı́n-Suárez , Matthijs Freudenthal , Jorge Civis
DOI: 10.1016/S0031-0182(00)00170-X
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摘要: Abstract The Upper Miocene succession of Crevillente presents an alternation continental and marine beds. fossils have been studied in order to obtain a reliable correlation with other sections. On the basis these data, entire section can be dated as Tortonian/Messinian. beds fits known eustatic sea-level climatic curves. These correlations are used assign ecological preferences components micromammal faunas at species level; it becomes clear that working genus level does not provide valid results. With assignments, is possible demonstrate consistent differences between coastal plain area Teruel on Meseta Central Spain.