학술논문
Quelonios del Eoceno Medio de Mallorca
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TEXT
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Source
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Language
Spanish
Abstract
[ES]La Fm. de calizas de Peguera, de edad bartoniense, se extiende ampliamente por la Serra de Tramuntana de Mallorca. Está constituída por una potente serie de calizas lacuestres organógenas muy someras que, en la base, intercalan noveles carbonosos con restos de carofitas y vertebrados. En estas calizas basales, junto con restos dentarios de cocodrrílidos, se han encontrado dos familiar de Quelonios fósiles: EMYDIDAE y TRIONYCHIDAE.
[EN]Fm. Peguera limestone, old Bartonian, is widely spread in the Serra de Tramuntana in Mallorca. It consists of a powerful series of very shallow-organogenic limestones lacuestres that, at base, interspersed with traces of carbonaceous novel charophytes and vertebrates. In these limestones baseline, along with dental remains of cocodrrílidos, have found two families of fossil Chelonia: Emydidae and Trionychidae.
[EN]Fm. Peguera limestone, old Bartonian, is widely spread in the Serra de Tramuntana in Mallorca. It consists of a powerful series of very shallow-organogenic limestones lacuestres that, at base, interspersed with traces of carbonaceous novel charophytes and vertebrates. In these limestones baseline, along with dental remains of cocodrrílidos, have found two families of fossil Chelonia: Emydidae and Trionychidae.