Abstract

The Serrulinini, a small relict group of clausiliids occurring in coastal regions of the Black and Caspian Seas and the Caucasus, are currently classified within the Phaedusinae, however paraphyletic origin of the Serrulinini is also widely debated with Pontophaedusa funiculum (Mousson) being most phylogenetically distinct from other taxa. As life history data may have taxonomical value, we conducted long-term observations in laboratory culture to assess reproductive modes, fecundity and growth pattern of three serruline species. Caspiophaedusa perlucens (O. Boettger) and Pravispira semilamellata (Mousson) produced partly calcified eggs with regular, spiral arrangement of crystals; their juveniles hatched after 17–18 days; the generation time was long and significantly exceeded one year. P. funiculum laid heavily calcified, elongated eggs. The incubation time in P. funiculum varied depending on the humidity, with a tendency towards short embryo-retention. The generation time in P. funiculum was one year. In all the studied species, egg calcification differed from the pattern common for other oviparous Phaedusinae which produce partly calcified eggs with homogeneous distribution of crystals. The calcite crystal distribution in the egg membranes reported here for the Serrulinini suggests some potential of these characters in phylogenetic context.

Highlights

  • Georgia, together with adjacent territories situated in the Caucasus biodiversity hotspot, is known as a centre of plant endemism with little studied and probably underestimated invertebrate richness (Mumladze et al 2020)

  • According to Tompa (1976), in terms of degree of calcification, three types of eggs are distinguished in land snails: uncalcified, partly calcified, and heavily calcified

  • Most of the stylommatophoran families produce a single kind of eggs (Tompa 1976)

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Summary

Introduction

Together with adjacent territories situated in the Caucasus biodiversity hotspot, is known as a centre of plant endemism with little studied and probably underestimated invertebrate richness (Mumladze et al 2020). It is an important refuge of Tertiary biota, where many hygro-thermophilous relict species found shelters during the Quaternary climate oscillations (Milne & Abbott 2002). This refers, among others, to the Colchic region, which was continuously forested since the Miocene and preserved possibly one of the oldest forest ecosystems in Western Eurasia (Tarkhnishvili et al 2012). Ecological preferences in the extant Serrulinini seem to be limited to sheltered protective micro-refuges providing perma-

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