560 Paläontologie; Paläozoologie
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This work provides the first revision and illustration of the type material of the ammonite species Parahoplites abichi Anthula [Type species of Protacanthoplites Tovbina] and Parahoplites aschiltaensis Anthula [Type species of Acanthohoplites Sinzow] from the upper Aptian (Lower Cretaceous) of Dagestan, Russia. The close affinities and synonymy between these two species are confirmed, and Acanthohoplites aschiltaensis is here retained as the senior valid name by its long quoting history and its historical use as a zonal index of the upper Aptian. The genus Protacanthoplites should be thus synonymised with Acanthohoplites by priority in the date of publication. Comparison with, and distinction from, closely allied Acanthohoplitidae is provided.
The early Tournaisian (Early Carboniferous; Mississippian) ammonoids from the classical abandoned limestone quarry of Gattendorf (Upper Franconia) are revised, using the historical collections as well as so far undescribed material. The ammonoid assemblage is composed of prionoceratid ammonoids of the six genera Mimimitoceras, Paragattendorfia, Stockumites, Acutimitoceras, Gattendorfia and Gattenpleura, which indicate a stratigraphic position near the Devonian–Carboniferous boundary in the earliest Carboniferous. The new species Stockumites hofensis sp. nov. and S. nonaginta sp. nov. are described.
Aus dem Dogger Norddeutschlands und des nordwestlichen Polens sowie aus Dogger-Geschieben werden 1 Art der Neritimorpha und 30 Arten der Caenogastropoda beschrieben. Neu sind 7 Arten. 14 Arten werden bereits beschriebenen Arten zugeordnet und 10 unter offener Nomenklatur beschrieben. Neu sind die Gattung Bicorempterus (Aporrhaidae) und die Familien Naricopsinidae, Tripartellidae und Maturifusidae. Die beschriebenen Caenogastropoden zeigen mehr Gemeinsamkeiten zu bisher aus dem Dogger Mittel- und Westeuropas bekannt gemachten Faunen als es bei den Archaeogastropoda und den Heterostropha der Fall war. Die Gleichsetzung der hier vorgestellten Arten mit aus der Literatur bekannten ist oftmals problematisch. Taxonomisch relevante Details besonders der Frühontogenese wurden bisher kaum beschrieben. Auch Fragen der innerartlichen Variation wurden nur gelegentlich angesprochen. Vatopsis antiquus n. sp. ist der älteste genauer bekannte Vertreter der Cerithiopsoidea. Pictavia und Oonia konnten als Vertreter der Ampullospiridae erkannt werden (Ausbildung des Protoconchs). Naricopsina repräsentiert eine Gruppe, die möglicherweise zu den echten Naticidae führte. Einige Gattungen der Aporrhaidae können genauer gefaßt werden. Maturifusus ist der älteste sichere Vertreter der höheren Caenogastropoda (Neomesogastropoda).
Glyptostrobus Endlicher is well represented in early Early Cretaceous to Pleistocene deposits in the middle to high latitudes of North America and Eurasia. Although the taxonomy and nomenclature of the genus is complicated, the fossil record indicates Glyptostrobus was represented by a small number of species. The genus first appears in Aptian age deposits from western Canada and Greenland, and achieved a wide distribution early in its evolutionary history. Exchange of Glyptostrobus between Asia and North America occurred across the Spitsbergen and Beringian corridors, which were functional about 110 and 100 million years ago, respectively The Late Cretaceous fossil record of Glyptostrobus shows that the genus had spread into Russia, China and the shores of the Turgai Strait. By the early Tertiary, Glyptostrobus was a prominent constituent of the polar broad-leaved deciduous forests. Paleocene age deposits across western Canada and the United States indicate the genus was present in great abundance in the lowland warm temperate and subtropical forests east of the Rocky Mountains. The broad distribution in North America and Russia during the Paleocene and Eocene indicates that Glyptostrobus grew and reproduced under a diverse range of climatic and environmental conditions, including the cold and unique lighting conditions of the polar latitudes. The presence of Glyptostrobus in Europe indicates the North Atlantic land bridges that extended between North America and Eurasia (Fennoscandia) and Europe during the early Tertiary were used. In Europe, extensive Glyptostrobus dominated swan1ps occupied the Central European Depression during the late Tertiary. Increasing global aridity and cooling, as well as landscape stabilization together with increasing competition for resources and habitat by representatives of the Pinaceae, seem to have forced the genus out of North America, Europe and most of Asia during the Miocene and Pliocene. In Japan, Glyptostrobus persisted until the early Pleistocene. After the early Pleistocene extinction in Japan, Glyptostrobus reappeared in southeastern China. Details of the taxonomic and biogeographic history of Glyptostrobus are examined.