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Publikováno v:
BMC Genomics, Vol 11, Iss 1, p 85 (2010)
Abstract Background MicroRNAs (miRNAs) repress target genes at the post-transcriptional level, and function in the development and cell-lineage pathways of host species. Tissue-specific expression of miRNAs is highly relevant to their physiological r
Externí odkaz:
https://doaj.org/article/7d65179cf78146e3866c56719cb82b6b
Autor:
Li, Shihu, Deng, Chenglong, Dong, Wei, Sun, Lu, Liu, Suzhen, Qin, Huafeng, Yin, Jiyun, Ji, Xueping, Zhu, Rixiang
Publikováno v:
In Tectonophysics 1 August 2015 655:213-226
Autor:
JABLONSKI, NINA G., SU, DENISE F., FLYNN, LAWRENCE J., JI, XUEPING, DENG, CHENGLONG, KELLEY, JAY, ZHANG, YUGUANG, YIN, JIYUN, YOU, YOUSHAN, YANG, XIN
Publikováno v:
Journal of Vertebrate Paleontology, 2014 Sep 01. 34(5), 1251-1257.
Externí odkaz:
https://www.jstor.org/stable/24523459
Publikováno v:
In Tectonophysics 30 May 2001 334(2):101-113
Publikováno v:
Geological Society of America Bulletin. 118:672-688
Detailed mapping of field relationships along the Red River fault reveals information about the distribution and magnitude of slip along the fault, about its interactions with other regional fault systems, and the relationship between river incision
Autor:
Haruo Saegusa, Masayuki Hyodo, Xue Shunrong, Yin Jiyun, Hideo Nakaya, Ji Xuepin, Atsushi Urabe
Publikováno v:
Journal of Human Evolution. 43:27-41
Two hominid upper central incisors found in the Yuanmou Basin in southwest China in 1965 have affinities with Homo erectus fossils from Zhoukoudian, but exhibit primitive features. The Yuanmou hominid remains are alleged to be coeval with or older th
Publikováno v:
Tectonics. 24
[1] The role of strike-slip faults, such as the Ailao Shan shear zone in southwestern China, in accommodating the India-Eurasia collision remains controversial. Cenozoic sedimentary rocks preserved along the northeast side of the Ailao Shan shear zon
Publikováno v:
In Gondwana Research 2001 4(4):843-843
Publikováno v:
Geosphere. 4:292
The geology east of the Eastern Himalayan Syntaxis is poorly known, although it figures prominently in many models for the Cenozoic tectonics of the India-Eurasia collision and subsequent intracontinental deformation. The little known Chong Shan shea