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Historical botany From Wikipedia, the free encyclopedia
It is suggested a late Pliocene age (Reuverian) for this flora. Palynofloras from drill cores in the surroundings of Frankfurt am Main and Hanau also suggests a late Pliocene age. The Pliocene flora of Frankfurt am Main described by Karl Mädler during the first half of the twentieth century is a key flora for the European Pliocene.
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In total 16 gymnosperm species in 15 genera and 73 angiosperm species (of which 15 could not be assigned to a genus) in 40 genera are recognised in the leaf record. Main characteristics of the flora are the high diversity of conifers, deciduous angiosperm genera such as Eucommia, Magnolia and Sassafras, a diverse assemblage of exclusively deciduous Fagaceae, including six species of oaks, the high diversity of Rosaceae, whereas evergreen taxa are shrubs typical of the understorey as Buxus, Ilex, Pachysandra, Prunus lusitanica and Viscum.
These features indicate cool temperate climatic conditions comparable to present-day Lugano in southern Switzerland. The flora shows a strong biogeographic link with East Asia, surprisingly high levels of Pliocene endemisms and that the European flora was more diverse in woody species shortly before the onset of the major Pleistocene glaciations than today. The early part of the Pliocene (5.3–3.6 Ma) was characterised by warm conditions (ca. 3 °C higher global surface temperatures) and higher sea levels (10–20 m) and slightly higher CO2 concentrations.
During the second part of the Pliocene, gradual cooling culminated in a significant intensification of northern hemispheric glaciation at ca. 2.75 Ma. Despite this, many exotic taxa persisted as relicts from older epochs and modern diversity patterns of trees and shrubs across the Northern Hemisphere were established only during and after the major Pleistocene glaciations.[1][2][3]
Fossil plant remains had been discovered in the excavation pit of the Höchst lock in 1884, a sandy clay layer, many more fossil seeds, fruits and leaves were uncovered in 1885 during the construction of the Frankfurt water clarifier near Niederrad. The works on these plant fossils were edited by GEYLER & KINKELIN and their results were published in the 15th volume of the Treatises of the Senckenbergische Naturforschende Gesellschaft in 1887. The plant fossils are kept at the Naturmuseum Senckenberg in Frankfurt am Main.[4]
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The fossil leaves comprising the flora have been recovered in Niederrad which is a quarter of Frankfurt am Main, Germany. It is part of the Ortsbezirk Süd and is subdivided into the Stadtbezirke Niederrad-Nord, Niederrad-Süd and the new Niederrad-West. Niederrad is bordered in the north by the River Main, in the west by the A5 Autobahn, in the south by the Main Railway and Flughafenstraße, and in the east by the former Niederrad Racecourse, Kennedyallee and the Main-Neckar Railway.
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