Abstract

For the first time gastropods from the Besano Formation (Anisian/Ladinian boundary) are documented. The material was collected from three different outcrops at Monte San Giorgio (Southern Alps, Ticino, Switzerland). The taxa here described are Worthenia (Humiliworthenia)? aff. microstriata, Frederikella cf. cancellata, ?Trachynerita sp., ?Omphaloptycha sp. 1 and ?Omphaloptycha sp. 2. They represent the best preserved specimens of a larger collection and document the presence in this formation of the clades Vetigastropoda, Neritimorpha and Caenogastropoda that were widespread on the Alpine Triassic carbonate platforms. True benthic molluscs are very rarely documented in the Besano Formation, which is interpreted as intra-platform basin sediments deposited in usually anoxic condition. Small and juvenile gastropods could have been lived as pseudoplankton attached to floating algae or as free-swimming veliger planktotrophic larval stages. Accumulations of larval specimens suggest unfavorable living conditions with prevailing disturbance in the planktic realm or mass mortality events. However, larger gastropods more probably were washed in with sediments disturbed by slumping and turbidite currents along the basin edge or storm activity across the platform of the time equivalent Middle San Salvatore Dolomite.

Highlights

  • The Middle Triassic Besano Formation is exposed in the Monte San Giorgio area, across the boundary of Southern Switzerland (Canton Ticino) and Northern Italy (Province Varese), was registered in 2003 as a UNESCO World Heritage Site because of its important vertebrate fauna from the Middle Triassic (Furrer 2003)

  • HF used unpublished data referring to gastropods from the PIMUZ excavations at Monte San Giorgio

  • The available specimen seems to be closely related to Worthenia (Humiliworthenia) microstriata Nützel et al 2018, differing in having a broad umbilicus

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Summary

Introduction

The Middle Triassic Besano Formation (formerly called “Grenzbitumenzone” in most publications) is exposed in the Monte San Giorgio area, across the boundary of Southern Switzerland (Canton Ticino) and Northern Italy (Province Varese), was registered in 2003 as a UNESCO World Heritage Site because of its important vertebrate fauna from the Middle Triassic (Furrer 2003). Invertebrate fossils are relatively common in this formation and some of the main clades of marine molluscs such as ammonoids, coleoids and bivalves (especially the genus Daonella) have been documented, notably by Airaghi (1911, 1912), Rieber (1965, 1968, 1969, 1970, 1973a, b, 1974a, b) and Schatz (2005a, b) They represent mostly nektonic cephalopods or bivalves adapted to an Editorial handling: D.

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