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Rhipidopsis in the upper Permian of the Dead Sea region, Jordan – Another clade of Mesozoic gymnosperms in the Permian?

Subject Area Palaeontology
Term from 2020 to 2023
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 444573967
 
Final Report Year 2023

Final Report Abstract

The fossil flora from the Dead Sea region is with nearly 60 taxa one of the most diverse late Permian floras worldwide. Moreover, it is a mixture of Euramerican, Cathaysian and Gondwa-nan plant taxa, including the last occurrences of typical Paleozoic taxa and precocious appearances of representatives of groups that are traditionally regarded as typical Mesozoic. Our goal was to collect more material of a peculiar Caytonia-like fructification that was found in the spring of 2019 in close association with Rhipidopsis foliage, a segmented hand-shaped leaf whose natural affinity was still unclear. Due to the Corona pandemic the fieldtrip had to be postponed until December 2022. Unfortunately, the original locality did not reveal new material, but a new locality yielded abundant plant fossils, including three specimens of the fertile organs we were looking for, and many Rhipidopsis leaves – the first with good cuticle preservation found in Jordan. In addition, other old and new localities were sampled. A number of spectacular finds were made. One of the highlights was the discovery of minute charophyte fossils. Several show thickened cells, which are in modern representatives typical for brackish influence. Another highlight are the finds of the peltaspermalean seed fern Permophyllocladus polymorphus, both as compressions and as cuticles in bulk-macerated samples. Permophyllocladus also shows adaptations to brackish conditions. Permophyllocladus is a typical Angaran genus like Ustyugia of which two species were found. The Dead Sea region is unique as it is the only place so far known worldwide from which typical elements of all four major floral provinces are known. In addition, 115 palynological samples were taken in plant-bearing localities in order to document changes of the vegetation in time and space.

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