Abstract

Late Miocene "Lake Pannon" (~11.3 Ma) was a remnant of the Central Paratethyan Sea. Successive freshening and constantly changing environmental conditions, like oxygenation, nutrition and substrate led to a well-documented radiation in molluscs and ostracods. Among ostracods (small crustaceans), Cyprideis is one of the most common genera in "Lake Pannon", as well as in several other ancient lakes, showing numerous adaptations and speciations. Here, we present high-resolution data from an early transgression of "Lake Pannon" in the Eastern Styrian Basin (SE Austria). Mataschen clay pit is in the focus of geologic and paleontologic research since 20 years and its geologic and paleoecologic evolution is well-documented. We drilled five cores covering a ~2.3 m long section and completely sampled it in 5-mm thick intervals to reconstruct minute changes in the ostracod fauna over a transgression of a brackish water body. The dominant genus, Cyprideis, is represented by three species C. mataschensis, C. kapfensteinensis and C. ex gr. pannonica. Through morphometric analyses we highlight the variance of each taxon and suggest that there is no direct ecologic control on size or shape. Furthermore, we found a second, co-occurring morphotype of C. kapfensteinensis which is directly related to an elevation of salinities above 13 psu. The presence of two intermediate specimens between the two morphotypes in the sample directly below the first appearance of C. kapfensteinensis B leads us to the conclusion that we are facing a speciation event leading to four sympatric species of Cyprideis.

Highlights

  • Ostracods of the genus Cyprideis Jones, 1857 [1] are euryhaline, benthic crustaceans typically occurring in coastal brackish waters

  • Cyprideis mataschensis and C. kapfensteinensis are very similar in shape, but C. ex gr

  • We compared the variability in size and shape of 444 female right valves and 349 female left valves of three species of Cyprideis from the Early Pannonian (~11.3 Ma) in the Mataschen clay pit

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Summary

Introduction

Ostracods of the genus Cyprideis Jones, 1857 [1] are euryhaline, benthic crustaceans typically occurring in coastal brackish waters. Their first appearance in the fossil record possibly dates back to the Upper Oligocene [2,3,4]. Recent Cyprideis torosa (Jones, 1850) [5] is known to cope with a wide range of salinities, occurring from slightly brackish to hypersaline environments Populations reach densities of up to 330,000 ind./m2 [7, 8] and are . Speciation of Late Miocene Cyprideis (Crustacea, Ostracoda) design, data collection and analysis, decision to publish, or preparation of the manuscript

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