Abstract
Early Upper Devonian Tropidocoryphinae (Proetida, Trilobita) show unequivocal evidence of eye-reduction leading to blindness and extinction slightly before or during the Kellwasser Event. The obviously gradualistic evolution can be related to environmental change.
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References
BUGGISCH, W. (1972): Zur Geologie und Geochemie der Kellwasserkalke und ihre begleitenden Sedimente (Unteres Oberdevon). — Abh. hess. L.-Amt Bodenforsch. 62, 1–68.
FEIST, R. (1985): Devonian Stratigraphy of the Southeastern Montagne Noire (France). — Cour. Forsch.-Inst. Senckenberg 75, 331–352.
— & KLAPPER, G. (1985): Stratigraphy and Conodonts in pelagic sequences across the Middle-Upper Devonian boundary, Montagne Noire, France. — Palaeontographica A 188, 1–18.
KLAPPER, G. (1983): The Devonian of the eastern Montagne Noire (France). — in: FEIST, R. (ed.): I.U.G.S. Subcomm. Devonian Stratigraphy, Guidebook, Field Meeting, September 1983, U.S.T.L. Montpellier.
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© 1986 Springer-Verlag
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Feist, R., Clarkson, E.N.K. (1986). Evolution of the last Tropidocoryphinae (Trilobita) during the Frasnian. In: Walliser, O.H. (eds) Global Bio-Events. Lecture Notes in Earth Sciences, vol 8. Springer, Berlin, Heidelberg. https://doi.org/10.1007/BFb0010205
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DOI: https://doi.org/10.1007/BFb0010205
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