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Akademický článek

GALNT2 targeted by miR-139-5p promotes proliferation of clear cell renal cell carcinoma via inhibition of LATS2 activation

Autor: Haisheng Yi, Lingyun Liu, Jingshun Zhang, Kaimin Guo, Yin Cao, Penghao Sun, Hongliang Wang

Publikováno v: Discover Oncology, Vol 15, Iss 1, Pp 1-13 (2024)

Abstract Polypeptide N-Acetylgalactosaminyltransferase (GALNTs) are critical enzymes that initiate mucin type-O glycosylation, and are closely associated with the occurrence and development of multiple cancers. However, the significance of GALNT2 in

Externí odkaz: https://doaj.org/article/703b58851bf54cfbb001da60db96f231

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Akademický článek

Study on the microstructure characteristics of Late Cretaceous aeolian sand in the playa from Chuxiong Basin

Autor: Hailei Tang, Rui Liang, Haisheng Yi, Gaojie Li

Publikováno v: Kuangchan zonghe liyong, Vol 0, Iss 1, Pp 48-59 (2022)

Cretaceous greenhouse, a long-lasting typical warminginterval in the history of the earth, and the regional paleotopography effect triggered a wide spread arid-climate belt in East Asia accompanying with extensive paleo-desert outcrops and evaporite

Externí odkaz: https://doaj.org/article/614e3d874df347d3b15bfbe28cee7438

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Akademický článek

Carbon Isotope Stratigraphy across the Devonian–Carboniferous Boundary in the East Paleo-Tethys Realm, Tibet, China

Autor: Zhanhu Cai, Haisheng Yi, Hong You

Publikováno v: Minerals, Vol 13, Iss 9, p 1144 (2023)

The Devonian–Carboniferous boundary is one of the most important turning points in geological history, marked by the Late Paleozoic Ice Age and Late Devonian extinction. This study investigates the carbon isotope stratigraphy across the Devonian–

Externí odkaz: https://doaj.org/article/6cca083a9c0945d6a3600f81690a281d

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Eocene–Oligocene glaciation on a high central Tibetan Plateau

Autor: Guoqing Xia, Chihua Wu, Ahmed Mansour, Xin Jin, Haisheng Yi, Gaojie Li, Qiushuang Fan, Zhiqiang Shi, Julian B. Murton, Junling Pei, Juan Pedro Rodríguez-López

Publikováno v: Geology. 51:559-564

The nature of glaciation (bipolar vs. unipolar) during the Eocene–Oligocene transition (EOT) remains unresolved. Here, we report the occurrence of frost marks, ice-rafted debris (IRD), and glendonites from the Upper Eocene to Lower Oligocene Niubao

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::5bf62587687d85c71d9b346d573608f4
https://doi.org/10.1130/g51104.1

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