Xinqiang Wang
Xinqiang Wang
在 cugb.edu.cn 的电子邮件经过验证
标题
引用次数
引用次数
年份
Ocean oxygenation in the wake of the Marinoan glaciation
SK Sahoo, NJ Planavsky, B Kendall, X Wang, X Shi, C Scott, AD Anbar, ...
Nature 489 (7417), 546-549, 2012
3082012
The origin of decoupled carbonate and organic carbon isotope signatures in the early Cambrian (ca. 542–520 Ma) Yangtze platform
G Jiang, X Wang, X Shi, S Xiao, S Zhang, J Dong
Earth and Planetary Science Letters 317, 96-110, 2012
1472012
Oceanic oxygenation events in the anoxic Ediacaran ocean
SK Sahoo, NJ Planavsky, G Jiang, B Kendall, JD Owens, X Wang, X Shi, ...
Geobiology 14 (5), 457-468, 2016
1422016
New U–Pb age from the basal Niutitang Formation in South China: Implications for diachronous development and condensation of stratigraphic units across the Yangtze platform at …
X Wang, X Shi, G Jiang, W Zhang
Journal of Asian Earth Sciences 48, 1-8, 2012
822012
Organic carbon isotope constraints on the dissolved organic carbon (DOC) reservoir at the Cryogenian–Ediacaran transition
G Jiang, X Wang, X Shi, S Zhang, S Xiao, J Dong
Earth and Planetary Science Letters 299 (1-2), 159-168, 2010
692010
Extremely low oxygen concentration in mid-Proterozoic shallow seawaters
D Tang, X Shi, X Wang, G Jiang
Precambrian Research 276, 145-157, 2016
602016
Paired carbonate and organic carbon isotope variations of the Ediacaran Doushantuo Formation from an upper slope section at Siduping, South China
X Wang, G Jiang, X Shi, S Xiao
Precambrian Research 273, 53-66, 2016
532016
Chemocline instability and isotope variations of the Ediacaran Doushantuo basin in South China
GQ Jiang, SH Zhang, XY Shi, XQ Wang
Science in China Series D: Earth Sciences 51 (11), 1560-1569, 2008
472008
Organic carbon isotope gradient and ocean stratification across the late Ediacaran-Early Cambrian Yangtze Platform
XQ Wang, XY Shi, GQ Jiang, DJ Tang
Science China Earth Sciences 57 (5), 919-929, 2014
372014
Cyclostratigraphic constraints on the duration of the Datangpo Formation and the onset age of the Nantuo (Marinoan) glaciation in South China
X Bao, S Zhang, G Jiang, H Wu, H Li, X Wang, Z An, T Yang
Earth and Planetary Science Letters 483, 52-63, 2018
352018
贺兰山地区中元古代微生物席成因构造
史晓颖, 王新强, 蒋干清, 刘典波, 高林志
地质论评 54 (5), 2008
352008
Increase of seawater Mo inventory and ocean oxygenation during the early Cambrian
X Wang, X Shi, X Zhao, D Tang
Palaeogeography, Palaeoclimatology, Palaeoecology 440, 621-631, 2015
232015
Mass-occurrence of oncoids at the Cambrian Series 2–Series 3 transition: implications for microbial resurgence following an early Cambrian extinction
W Zhang, X Shi, G Jiang, D Tang, X Wang
Gondwana Research 28 (1), 432-450, 2015
212015
New U-Pb age constraints on the upper Banxi Group and synchrony of the Sturtian glaciation in South China
G Song, X Wang, X Shi, G Jiang
Geoscience Frontiers 8 (5), 1161-1173, 2017
192017
Nitrogen isotope constraints on the early Ediacaran ocean redox structure
X Wang, G Jiang, X Shi, Y Peng, DC Morales
Geochimica et Cosmochimica Acta 240, 220-235, 2018
182018
Iodine content of the carbonates from the Doushantuo Formation and shallow ocean redox change on the Ediacaran Yangtze Platform, South China
H Wei, X Wang, X Shi, G Jiang, D Tang, L Wang, Z An
Precambrian Research 322, 160-169, 2019
142019
New biostratigraphic and chemostratigraphic data from the Ediacaran Doushantuo Formation in intra-shelf and upper slope facies of the Yangtze platform: Implications for …
AD Hawkins, S Xiao, G Jiang, X Wang, X Shi
Precambrian Research 300, 28-39, 2017
142017
Morphological association of microbially induced sedimentary structures (MISS) as a paleoenvironmental indicator: an example from the proterozoic succession of the southern …
DJ Tang, XY Shi, G Jiang, XQ Wang
Microbial mats in siliciclastic depositional systems through time: Tulsa …, 2011
142011
华南埃迪卡拉纪陡山沱盆地氧化界面的迁移与碳同位素异常
蒋干清, 张世红, 史晓颖, 王新强
中国科学: D 辑 38 (12), 1481-1495, 2008
142008
Nitrogen isotope evidence for redox variations at the Ediacaran-Cambrian transition in South China
X Wang, X Shi, D Tang, W Zhang
The Journal of Geology 121 (5), 489-502, 2013
132013
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