Results 21 to 30 of about 9,376 (253)
Late Miocene hominoid from Niger
Abstract African Late Miocene hominoids are rare, having been reported from six localities in Kenya, Ethiopia and Chad ranging in age from 10.5 to 5.5 Ma. We here report the occurrence of a hominoid in Niger associated with a vertebrate fauna which indicates an age of between 11–5 Ma.
Pickford, M. +4 more
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New age findings with microfossils of the Van Formation (Van, Eastern Anatolia)
Van Formation, which is mainly represented by conglomerate, sandstone, marl and limestone, covers a large area around the Van province. The age of the unit was assigned in different localities of the region as late Oligocene - middle Miocene ...
Sefer Örçen +3 more
doaj +1 more source
Tectonic evolution of the southern part of Central Viet Nam and the adjacent area
Interpretations of seismic, gravity and magnetic anomalies and structural data on the coastal zone of southern part of Central Viet Nam (SCVN) and the adjacent Tertiary basins suggest several phases in the tectonic evolution of the study region since the
Phung Van Phach, Le Duc Anh
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Late miocene magnetobiostratigraphy of Crete
Six Upper Miocene marine clay sections on Crete (Greece) have been subjected to a detailed magnetobiostratigraphic analysis. Six correlatable polarity zones are recognized and these demonstrate the regional synchrony of planktonic foraminiferal biohorizons.
Langereis, C.G. +2 more
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Early Miocene micromammal fossils from Gucheng in Linxia, Gansu, China [PDF]
The micromammal fossils collected from the Shangzhuang Formation of the Linxia Basin, Gansu, are described here. The assemblage consists of 16 species of 13 genera belonging to 7 families, including one new species and one taxon previously unknown from ...
WANG Ban-Yue, QIU Zhu-Ding, LI Lu
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Late Cenozoic Cooling History of the Xigaze Fore-Arc Basin along the Yarlung–Zangbo Suture Zone (Southern Tibet): New Insights from Low-Temperature Thermochronology [PDF]
The Tibetan Plateau is currently the widest and highest elevation orogenic plateau on Earth. It formed as a response to the Cenozoic and is still ongoing collision between the Indian and Eurasian plates.
Shida Song +7 more
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Gomphotheres existed in the Siwaliks from the middle Miocene (14.2Ma) to the middle Pleistocene (0.8Ma) and became extinct later on. In this paper, we tried to discuss the reasons of such extinction of gomphotheres in the lower Pleistocene time span by ...
Muhammad Ameen +4 more
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Biostratigraphic and lithofacial studies of sediments in the Tankhoi Tertiary field, which evolution reflects transformations of the terrain in the Baikal region at the Oligocene-Miocene, Early-Middle Miocene, Miocene-Pliocene and Early-Late Pliocene ...
S. V. Rasskazov +5 more
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Insights into the Middle–Late Miocene palaeoceanographic development of Cyprus (eastern Mediterranean) from a new δ18O and δ13C stable isotope composite record [PDF]
The Middle to Late Miocene was a time of significant global climate change. In the eastern Mediterranean region, these climatic changes coincided with important tectonic events, which resulted in changes to the organisation of oceanic gateways, altering ...
T. Cannings +3 more
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Paleobiogeography of Crown Deer
The article describes the paleobiogeographic history of the modern subfamilies so-called “crown deer” of the family Cervidae (Artiodactyla, Mammalia) in the world from the late Miocene to the late Pleistocene.
Roman Croitor
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