H.A. van Adrichem Boogaert
Abstract
Conodonts have been extracted from calcareous units of the Devonian and Lower Carboniferous sequence from 3 areas in the S. part of the Cantabrian Mountains. There can be distinguished Emsian, Givetian, Frasnian, Famennian and Visean faunas.
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Conodonts have been extracted from calcareous units of the Devonian and Lower Carboniferous sequence from 3 areas in the S. part of the Cantabrian Mountains. There can be distinguished Emsian, Givetian, Frasnian, Famennian and Visean faunas.
Key concepts: Conodont, Carboniferous, Viséan, Devonian, Paleontology, Geology, Paleozoic, Tournaisian