Zobrazeno 1 - 10
of 32
pro vyhledávání: '"Qiu, Zhanxiang"'
Publikováno v:
In Palaeogeography, Palaeoclimatology, Palaeoecology 15 October 2023 628
Autor:
Zheng, Yan, Qiu, Zhanxiang, Qiu, Zhuding, Li, Lu, Wei, Xiaohao, Zhang, Rui, Yue, Leping, Deng, Tao
Publikováno v:
In Palaeogeography, Palaeoclimatology, Palaeoecology 1 August 2023 623
Publikováno v:
Science, 2011 Mar 01. 331(6021), 1136-1137.
Externí odkaz:
http://dx.doi.org/10.1126/science.331.6021.1136-b
Autor:
Wang, Xiaoming, Qiu, Zhuding, Li, Qiang, Wang, Banyue, Qiu, Zhanxiang, Downs, William R., Xie, Guangpu, Xie, Junyi, Deng, Tao, Takeuchi, Gary T., Tseng, Zhijie J., Chang, Meeman, Liu, Juan, Wang, Yang, Biasatti, Dana, Sun, Zhencheng, Fang, Xiaomin, Meng, Qingquan
Publikováno v:
In Palaeogeography, Palaeoclimatology, Palaeoecology 2007 254(3):363-385
Autor:
Wang, Xiaoming, Wang, Banyue, Qiu, Zhanxiang, Xie, Guangpu, Xie, Junyi, Downs, Will, Qiu, Zhuding, Deng, Tao
Publikováno v:
In Earth and Planetary Science Letters 2003 208(3):253-269
Publikováno v:
Zoological Journal of the Linnean Society. Nov2004, Vol. 142 Issue 3, p405-421. 17p.
Autor:
Qiu Zhanxiang, Wang Banyue
Publikováno v:
Bulletin of the American Museum of Natural History. 279:116-124
The ursid fossils collected from Saint Jacques include Pachycynodon tedfordi, new species, Amphicynodon sp., and Cephalogale sp. The distinctive features of Pachycynodon tedfordi are: short premolar series relative to molars, diastemata between c and
Autor:
Qiu Zhanxiang
Publikováno v:
Bulletin of the American Museum of Natural History. 279:18-31
Three major carnivoran dispersal waves of filter-bridge type between Eurasia and North America are recognized in the late Neogene. The first is around 20 Ma, probably from 21 Ma to 19–18 Ma, during which intermittent dispersals might have occurred.
Publikováno v:
Journal of Vertebrate Paleontology. 11:519-526
Publikováno v:
Paleobiology. 17:246-265
The Late Neogene vertebrate fossil record from Yushe Basin presents multiple, superposed assemblages from a single area, spanning roughly the interval of 6–2 Ma. Both large and small mammals show peak species richness in the middle Pliocene but ind