2011
DOI: 10.4202/app.2010.0098
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Earliest Jurassic Patellogastropod, Vetigastropod, and Neritimorph Gastropods from Luxembourg with Considerations on the Triassic—Jurassic Faunal Turnover

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Cited by 14 publications
(18 citation statements)
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“…In the western European epicontinental seas, the pleurotomarioideans were mainly represented by long-ranging genera with high species diversity, such as Pleurotomaria Defrance, 1826, Bathrotomaria Cox, 1956, Pyrgotrochus Fischer, 1885, and Trochotoma Eudes-Deslongchamps, 1843(e.g., Sieberer 1907Cox 1960b;Fischer and Weber 1997;Gründel 2003;Kollmann 2005;Monari et al 2011;Monari and Gatto 2013). In contrast, these genera were either absent or rare and short-lived in the central region of western Tethys.…”
Section: Palaeobiogeographical Historymentioning
confidence: 86%
See 1 more Smart Citation
“…In the western European epicontinental seas, the pleurotomarioideans were mainly represented by long-ranging genera with high species diversity, such as Pleurotomaria Defrance, 1826, Bathrotomaria Cox, 1956, Pyrgotrochus Fischer, 1885, and Trochotoma Eudes-Deslongchamps, 1843(e.g., Sieberer 1907Cox 1960b;Fischer and Weber 1997;Gründel 2003;Kollmann 2005;Monari et al 2011;Monari and Gatto 2013). In contrast, these genera were either absent or rare and short-lived in the central region of western Tethys.…”
Section: Palaeobiogeographical Historymentioning
confidence: 86%
“…In contrast, these genera were either absent or rare and short-lived in the central region of western Tethys. For example, in the Early Jurassic, Trochotoma radiated in the western European shelf and in the carbonate platforms areas (Monari et al 2011), whereas it was absent in the areas of the central western Tethys characterized by pelagic sedimentation. Again, Pleurotomaria occurred from the Early Jurassic to the Early Cretaceous in the European shelf, where it was represented by at least fifty species.…”
Section: Palaeobiogeographical Historymentioning
confidence: 99%
“…Belgium, the Luxembourg Sandstone Formation, up to 100 m thick and the Strassen marl and limestone unit, about 40 m thick (Monari et al, 2011;Schintgen & Förster, 2013). The latter is an informal lateral equivalent of the lower Arlon Formation, which in Belgium has received separate status and has officially been named Strassen Member.…”
Section: Stratigraphy Of the Lower Jurassic In Belgium And The Grand mentioning
confidence: 99%
“…This bay-like extension of the Paris Basin, was located between the London−Brabant−Ardennes Landmass and the Rhenish Massif, connecting the Paris Basin with the epicontinental seas of the Netherlands and northern Germany ( Fig. 1A; see also Monari et al, 2011). The deposits show a convex outcrop pattern, covering the extreme southeast of Belgium (Belgian Lorraine, including the Gaume in the west and the "Pays d'Arlon" (Country of Arlon) in the east) and the southern half of the GD of Luxembourg (essentially Guttland) (Fig.…”
Section: Stratigraphy Of the Lower Jurassic In Belgium And The Grand mentioning
confidence: 99%
“…In recent years, several studies greatly improved the knowledge on the systematics and phylogeny of the extant and fossils gastropods, suggesting that generic and higer level assignments of the older literature need systematic revision (Monari et al, 2011). Thus, an updated systematic knowledge of marine benthic faunas would certaintly facilitate palaeobiogeographical and diversity comparisons across the Late Triassic/Early Jurassic boundary.…”
Section: Introductionmentioning
confidence: 99%