Zobrazeno 1 - 10
of 124
pro vyhledávání: '"Ganqing Jiang"'
Publikováno v:
Geoscience Frontiers, Vol 8, Iss 5, Pp 1161-1173 (2017)
The Nanhua basin in South China hosts well-preserved middle–late Neoproterozoic sedimentary and volcanic rocks that are critical for studying the basin evolution, the breakup of the supercontinent Rodinia, the nature and dynamics of the “snowball
Externí odkaz:
https://doaj.org/article/16afcffe14af4cc0931a0b14ca5cb937
Autor:
Haijun Song, Ganqing Jiang, Simon W. Poulton, Paul B. Wignall, Jinnan Tong, Huyue Song, Zhihui An, Daoliang Chu, Li Tian, Zhenbing She, Chengshan Wang
Publikováno v:
Nature Communications, Vol 8, Iss 1, Pp 1-7 (2017)
The evolution of oceanic redox state in the past is poorly known. Here, the authors present a temporal record of banded iron formations and marine red beds, which indicate deep-ocean oxygenation occurred in the middle Ediacaran, coinciding with the o
Externí odkaz:
https://doaj.org/article/c138e0aff57547d3bf50fc2586fc540b
Autor:
Huaichun Wu, Linda A. Hinnov, Shihong Zhang, Ganqing Jiang, Tianshui Yang, Haiyan Li, Dangpeng Xi, Xiaojuan Ma, Chengshan Wang
Publikováno v:
GSA Bulletin. 135:712-724
The Earth’s geologic record of Milankovitch cycles closely tracks Solar System solutions for the past 50 million years. Prior to 50 million years ago (Ma), however, the solutions lose accuracy rapidly due to chaotic behavior of the Solar System. He
Autor:
Dongtao Xu, Xinqiang Wang, Jian-Ming Zhu, Ganqing Jiang, Xiaoying Shi, Xiangli Wang, Swapan K. Sahoo
Publikováno v:
Geochimica et Cosmochimica Acta. 323:258-275
Autor:
Yongbo Peng, Huiming Bao, Ganqing Jiang, Peter Crockford, Dong Feng, Shuhai Xiao, Alan Jay Kaufman, Jiasheng Wang
Publikováno v:
Proceedings of the National Academy of Sciences. 119
Significance Earth system’s response to major perturbations is of paramount interest. On the basis of multiple isotope compositions for pyrite, carbonate-associated sulfate, carbonates, and organics within, we inferred that the much-debated, enigma
Autor:
Dongjie Tang, Xuewu Fu, Xiaoying Shi, Limin Zhou, Wang Zheng, Chao Li, Dongtao Xu, Xiqiang Zhou, Baozeng Xie, Xiyan Zhu, Ganqing Jiang
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b04bd38f7942fb52feccf8ba7262e50f
https://doi.org/10.1002/essoar.10511224.1
https://doi.org/10.1002/essoar.10511224.1
Autor:
Ganqing Jiang
Prepared in conjunction with the 2022 GSA Cordilleran/Rocky Mountain Sections Joint Meeting, this Field Guide showcases trips to geologically interesting areas in Arizona, Nevada, and California. Enjoy a three-day trip to the Buckskin-Rawhide and nor
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::da9a4d63fbf98d91641ed73ddf8ff51c
https://doi.org/10.1130/fld063
https://doi.org/10.1130/fld063
Autor:
Shuhai Xiao, Ganqing Jiang, Qin Ye, Qing Ouyang, Dhiraj M. Banerjee, Birendra P. Singh, A. D. Muscente, Chuanming Zhou, Nigel C. Hughes
Acritarch biostratigraphic and delta C-13 chemostratigraphic data from the Krol A Formation in the Solan area (Lesser Himalaya, northern India) are integrated to aid inter-basinal correlation of early-middle Ediacaran strata. We identified a prominen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::12ab94533dc2b335938976b2e6eb3e46
https://hdl.handle.net/10919/111182
https://hdl.handle.net/10919/111182
Autor:
Malcolm W. Wallace, Stephanie L McColl, Ashleigh v.S. Hood, Ganqing Jiang, Maxwell A. Lechte, Noah J. Planavsky, Galen P. Halverson, Weiqiang Li, Dan Asael
Publikováno v:
Proc Natl Acad Sci U S A
The Earth's most severe ice ages interrupted a crucial interval in eukaryotic evolution with widespread ice coverage during the Cryogenian Period (720 to 635 Ma). Aerobic eukaryotes must have survived the "Snowball Earth" glaciations, requiring the p
Autor:
Timothy W. Lyons, Jeremy D. Owens, Ganqing Jiang, Brian Kendall, Swapan K. Sahoo, Sune G. Nielsen, Ariel D. Anbar, Chadlin M. Ostrander, Gwyneth W. Gordon, Noah J. Planavsky, Stephen J. Romaniello
Publikováno v:
Geochimica et Cosmochimica Acta. 261:191-209
The Ediacaran Doushantuo Formation offers one of the most complete and extensively studied records of end-Neoproterozoic biotic and environmental change. Here, we report multiple coeval negative molybdenum (Mo) isotope excursions (to as low as δ98Mo