Zobrazeno 1 - 10
of 64
pro vyhledávání: '"Zhaoqun Zhang"'
Publikováno v:
Frontiers in Earth Science, Vol 11 (2023)
The Nihewan Basin is infilled by a relatively complete Pliocene to Pleistocene sequence, rich mammalian fossils and containing many Palaeolithic artefacts, implying that it is a unique location for Quaternary multidisciplinary study. Fossil excavatio
Externí odkaz:
https://doaj.org/article/2157d65b238342598bcd684b63b28519
Publikováno v:
Scientific Reports, Vol 12, Iss 1, Pp 1-14 (2022)
Abstract The aridification of Central Asia since the Eocene has widespread evidence, but climate-controlled environmental reorganizations during the Oligocene remain ambiguous. We employed environmental magnetic, mineralogical and geochemical methods
Externí odkaz:
https://doaj.org/article/5c554d765ebb4d13ab47a2c1e292084f
Publikováno v:
Diversity, Vol 15, Iss 6, p 744 (2023)
The Eocene-Oligocene Transition (EOT) was one of the most profound climate changes in the Cenozoic era, characterized by global cooling around 34 million years ago. This time period also witnessed major faunal turnovers, such as the “Mongolian Remo
Externí odkaz:
https://doaj.org/article/975e4a5df998439d866b04532b9213cd
Publikováno v:
PLoS ONE, Vol 12, Iss 3, p e0172733 (2017)
We describe a new species of Rodentia (Mammalia), Argyromys cicigei sp. nov. from Toglorhoi (fossil bed TGW-A/2a) in Mongolia and Ulantatal (fossil beds UTL 1 and UTL 7) in China. Its tooth morphology differs from the type species Argyromys aralensis
Externí odkaz:
https://doaj.org/article/876695a11caa47df96073360dbcdf63b
Autor:
Deyan Ge, Zhixin Wen, Lin Xia, Zhaoqun Zhang, Margarita Erbajeva, Chengming Huang, Qisen Yang
Publikováno v:
PLoS ONE, Vol 8, Iss 4, p e59668 (2013)
Although species within Lagomorpha are derived from a common ancestor, the distribution range and body size of its two extant groups, ochotonids and leporids, are quite differentiated. It is unclear what has driven their disparate evolutionary histor
Externí odkaz:
https://doaj.org/article/07505a1a65fc428b944a624291d3e891
Publikováno v:
Diversity; Volume 15; Issue 6; Pages: 744
The Eocene-Oligocene Transition (EOT) was one of the most profound climate changes in the Cenozoic era, characterized by global cooling around 34 million years ago. This time period also witnessed major faunal turnovers, such as the “Mongolian Remo
The classic Nihewan Fauna, as the representative of early Pleistocene Asian Land Mammal Age Nihewanian, has long been cited for bio- and chronostratigraphic correlation. However, its precise provenance and stratigraphic horizon have remained unsolved
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c84d4b779f56c719d65e8854b48cd804
https://www.repository.cam.ac.uk/handle/1810/353896
https://www.repository.cam.ac.uk/handle/1810/353896
Publikováno v:
Palaeoworld. 30:373-381
The occurrence of Nyctereutes during the Plio-Pleistocene has long been reported in northern China, with the highest abundance in the Nihewan Basin. However, due to site dispersal, the coexistence of different taxa, and lack of a precise stratigraphi
Publikováno v:
Ecology and Evolution, Vol 10, Iss 13, Pp 6333-6355 (2020)
Bai, B, Meng, J, Janis, C M, Zhang, Z-Q & Wang, Y-Q 2020, ' Perissodactyl diversities and responses to climate changes as reflected by dental homogeneity during the Cenozoic in Asia ', Ecology and Evolution, vol. 10, no. 13, 6363, pp. 1-23 . https://doi.org/10.1002/ece3.6363
Ecology and Evolution
Bai, B, Meng, J, Janis, C M, Zhang, Z-Q & Wang, Y-Q 2020, ' Perissodactyl diversities and responses to climate changes as reflected by dental homogeneity during the Cenozoic in Asia ', Ecology and Evolution, vol. 10, no. 13, 6363, pp. 1-23 . https://doi.org/10.1002/ece3.6363
Ecology and Evolution
Cenozoic mammal evolution and faunal turnover are considered to have been influenced and triggered by global climate change. Teeth of large terrestrial ungulates are reliable proxies to trace long‐term climatic changes due to their morphological an
Constraining the provenance of aeolian mineral dust is critical in understanding past climate changes, atmospheric dust activity, circulation, and sediment generation. On the Chinese Loess Plateau (CLP), use of detrital zircon U-Pb age data as source
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1239722ba46624cb61c44cc7db87474d
http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-462674
http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-462674