Hipparion material from Gaojiashan locality in the Late Miocene of Linxia Basin, Gansu, China and associated mammalian fossil assemblage

2017 ◽  
Vol 30 (5) ◽  
pp. 677-693
Author(s):  
Yikun Li ◽  
Wen He ◽  
Shanqin Chen ◽  
Shiqi Wang ◽  
Boyang Sun ◽  
...  
2010 ◽  
Vol 55 (4) ◽  
pp. 587-597 ◽  
Author(s):  
Shaokun Chen ◽  
Tao Deng ◽  
Sukuan Hou ◽  
Qinqin Shi ◽  
Libo Pang

Palaios ◽  
2011 ◽  
Vol 26 (1) ◽  
pp. 55-65 ◽  
Author(s):  
M. S. DOMINGO ◽  
L. DOMINGO ◽  
I. M. SANCHEZ ◽  
M. T. ALBERDI ◽  
B. AZANZA ◽  
...  

2021 ◽  
Author(s):  
Boyang Sun ◽  
Yan Liu ◽  
Wen He ◽  
Shanqin Chen ◽  
Tao Deng

Abstract Here, we report well–preserved skulls and postcranial specimens of the subgenus Hippotherium from the Linxia Basin, Gansu, China. Based on morphological comparison, the species of subgenus Hippotherium in China, Hipparion weihoense and Hipparion chiai, should be ascribed to the same species, H. weihoense. The species Hipparion prostylum (later Hipparion aff. brachypus) from Maragheh, Iran should also be ascribed to H. weihoense. Phylogenetic analysis shows the subgenus Hippotherium derived from the North American genus Cormohipparion, and as a basal group of Hipparion in Eurasia, representing the Hipparion Datum. Analysis on locomotive ability indicates that H. weihoense likely lived in an open habitat, whereas other species of subgenus Hippotherium likely lived in closed habitats. This result indicates a palaeoecological pattern in the early Late Miocene in Eurasia: influenced by a series of geological events, aridification of mid–latitude Asia progressed, whereas Europe and North Africa remained relatively humid; as the genus originated from East Asia, Hipparion divided rapidly into different groups with differing functional morphology to occupy diverse niches.


2014 ◽  
Vol 54 (2) ◽  
pp. 249-277 ◽  
Author(s):  
Grzegorz Worobiec

Abstract Leaf macroremains collected in the Bełchatów Lignite Mine (central Poland) were investigated. The fossil assemblage consists of leaves of Acer, Betula, Carpinus, Dicotylophyllum, Fagus, ?Magnolia, “Parrotia”, Pinus, Quercus, and Zelkova. Mesophytic (zonal) elements dominate, with admixture of riparian (azonal) leaf taxa. The floristic composition points to late Neogene (late Miocene to late Pliocene) age and suggests favourable temperate climate with mild winters.


Geobios ◽  
2020 ◽  
Vol 59 ◽  
pp. 1-28 ◽  
Author(s):  
René Hoffmann ◽  
M. Aleksandra Bitner ◽  
Andrzej Pisera ◽  
Manfred Jäger ◽  
Gerald Auer ◽  
...  

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