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• W2185204992 abstract "Zusammenfassung Abstract The Jordan Valley south of Lake Tiberias has post Messinian deposits with saline character succeeded by fresh water deposits. These were deformed by further vertical and horizontal movements in the Jordan Valley Rift. Those encompassing the Al Qarn Formation after deformation came to lie next to sands and gravels of an ancient Jordan River and were inundated by Lake Lisan and covered by the bottom deposits of its salty waters. They have a structural contact to deposits of the Tayba Formation that formed in a sea at late Oligocene to early Miocene times. Exposure of Al Qarn Formation was created when the King Abdulla Canal was constructed. Since about twelve thousand years and after Lisan lake had dried up and shrank to become the Dead Sea, the Al Qarn Formation had been present as it is now. Of the fauna which at Al Qarn times lived in a lake and in creeks issuing into it, the shells of the mollusks have been preserved, especially well in one layer that is of a fine sandy and marly composition. Dominant and well visible shells belong to Melanopsis, of which 5 species are recognized, and one of these is described as new, Melanopsis salamei. Very common is Valvata saucyi that is much smaller and found in the screened washings. They are evidence for shallow beach environment in case of Melanopsis, and vegetated pond environment in case of Valvata. Also present is a Theodoxus that closely resembles the species still living in Jordan also next to the outcrop in King Abdulla Canal. Common is Bithynia syriaca that connects to Erq el Ahmar Formation and no longer lives in Jordan. Juvenile shells of a Hydrobia could belong to the same species that is still present in the region. The tiny Islamia is new to the region, here described as Islamia jordanica, but also no longer living here. Melanoides from Al Qarn Formation has a different early ornament of the shell which distinguishes from the species of that genus that lives in Jordan now and is named Melanoides abuhabili. A small planispiral Valvata closely resembles Valvata piscinalis that occurs in the region but not in Jordan and juvenile shells of Galba are close to Galba truncatula that lives in creeks in Jordan. Very common is Gyraulus with quite variable shell, and a small limpet that according to the shape of its embryonic shell is a Ferrissia of which the species is here newly described as Ferrissia urdunica. A tiny bivalve is placed with Pisidium and the large shells of Unio were recognized only in the field, but shells were too brittle to be collected." @default.
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• W2185204992 date "2013-01-01" @default.
• W2185204992 modified "2023-09-27" @default.
• W2185204992 title "Mollusks of the Pleistocene Al-Qarn Formation of the Jordan Rift-Valley in Jordan" @default.
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