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1.
The study of genus LeptaenopyxisHavlicek, 1963 in the Lower Devonian from Armorican Massif allows to recognize four species: Leptaenopyxis kerfornei n. sp., Leptaenopyxis cf. bouei (Barrande), Leptaenopyxis sp. 1 and Leptaenopyxis sp. 2. These species were described, until now, under specific name boueiBarrande, 1848. From this study it follows some biostratigraphical and palaeobiogeographical results for the Armorican Massif and its relations with surrounding areas during Lower Devonian time.  相似文献   

2.
New research made in the Hettangian sequence in Quercy by one of us (R.C.) has led to the discovery of shell beds constituted solely of Bivalvia in two deposits in the departement of Tarn, one near Vaour, the other near Les Cabannes-de-Cordes. These Eomiodon and Cuneigervillia-Pteromya signify an environment of abnormal salinity and permit long distance correlations.  相似文献   

3.
Three osteostracan genera, Tannuaspis, Tuvaspis and Ilemoraspis, from the Silurian and Devonian of the Autonomous Republic of Tuva and the Autonomous Region of Khakassia (USSR), are revised on the basis of the type material briefly described by Obruchev (1956, 1961, 1964). Tannuaspis bears some resemblances with the Tremataspididae. Tuvaspis may be closely related to Tannuaspis. Finally, there is no evidence of paired fins and cornual processes in Ilemoraspis (neither is there any evidence of their absence). Tannuaspis and Ilemoraspis share some characters which are not found in any other osteostracan: widely separated orbits, very small and oval lateral fields, situated at the same level as the median dorsal field. These resemblances may suggest that these two genera (to which Tuvaspis may be added) form a monophyletic group of osteostracans, which may be endemic to this part of Central Asia.  相似文献   

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