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The Solnhofen Limestone or Solnhofen Plattenkalk is a collective term for multiple Late Jurassic lithographic limestones in southeastern Germany, which is famous for its well preserved fossil flora and fauna dating to the late Jurassic (Kimmeridgian-Tithonian). The paleoenvironment is also often referred to as the Solnhofen Archipelago.
The following tables give an overview of notable finds of hominin fossils and remains relating to human evolution, beginning with the formation of the tribe Hominini (the divergence of the human and chimpanzee lineages) in the late Miocene, roughly 7 to 8 million years ago.
Plant macrofossils include leaf, needle, cone, and stem debris; and can be used to identify types of plants formerly growing in the area. Such botanical macrofossil data provide a valuable complement to pollen and faunal data that can be used to reconstruct the prehistoric terrestrial environment.
Image Location of discovery Date of discovery Age of remains in radiocarbon years BP Comments Adams mammoth: Mouth of the Lena River, Siberia [1] 1799 [1] [2] 35,800 [1] [3] It is the first complete mammoth skeleton ever to be reconstructed. Originally, it was an entire mummified mammoth carcass. [2] Beresovka Mammoth Berezovka River, Siberia ...
Qafzeh 25 was discovered in 1979. Due to his overall robustness and tooth wear, the remains are believed to be of a young male. [35] The fossil has undergone heavy taphonomical damages including a complete crushing of the skull and mandible. [36] Its inner ear morphology confirm that it is an anatomically modern human [37]
The images of the living OTUs (29 species) were made available in the early 1960s; those of the fossil ones (48 species) later in the decade. These images were copied using xerography . Copies of all OTUs were in the possession of Dr. Paul A. Ehrlich ( Stanford University ), Dr. W. Wayne Moss (Philadelphia Academy of Sciences) and Robert R ...
Domning had been looking at sirenian fossils from five different bone beds within a 5 meters thick stratigraphic section of the formation and concluded that remains in the three lower bone beds "appear to represent a single taxon". [3] From these, an almost complete skeleton was composed, only missing most of the feet and the tail. [3]
Prior to 2008, fossils of D. spurensis were listed as the species D. haplocerus, until it was determined that D. haplocerus was a species name originally based on undiagnostic fossils. [13] D. smalli [18] Arizona [18] Sonsela? [13] A single lateral osteoderm. A desmatosuchin aetosaur which is very rare in the Chinle Formation.