2 edition of Devonian events and biostratigraphy of south China found in the catalog.
Devonian events and biostratigraphy of south China
Includes bibliographical references (p. 206-215).
|Statement||S.L. Bai, Z.Q. Bai, X.P. Ma, D.R. Wang & Y.L. Sun.|
|LC Classifications||QE728 .D486 1994|
|The Physical Object|
|Pagination||303 p., 45 p. of plates :|
|Number of Pages||303|
Middle Devonian rugose coral Biostratigraphy of the Fanning River Group, north Queensland, Australia (placoderm fishes) from the Devonian of South China and eastern Australia. AM Journal Article. Read more. Devonian syringostromatid stromatoporoids from the Broken River region, North Queensland Receive the latest news on events. The new occurrence of this group well south of the Song Ma suture suggests close links between the Indochina and South China blocks in Middle Devonian time. The massive sandstone exposures of the Dong Tho Formation may be a southern extension of the Do Son Sandstone Formation of the Hai Phong area, which is located on the South China block.
• The Late Devonian Pho Han Formation represents a sediment-starved carbonate basin on the South China platform. • The Cat Co 3 section experienced long-term anoxia/dysoxia in the Famennian, with euxinia during the Hangenberg Crisis. • Hg chemostratigraphy indicates a possible volcanic trigger for the end-Devonian mass extinction event. Zhao W.-J. & Zhu M. Siluro-Devonian vertebrate biostratigraphy and biogeography of China. Palaeowo 4–26 (). Fang R.-S. et al. The Middle Silurian and Early Devonian Stratigraphy and Palaeontology in Qujing District, Yunnan (Yunnan People's Publishing House, Kunming, ). Zhu M. & Zhao W.-J.
Conodont biostratigraphy of the Little Cedar and lower Coralville formations of the Cedar Valley Group (Middle Devonian) of Iowa and significance of a new species of Polygnathus Frederick S. Rogers University of Iowa, Department of Geology, Iowa City, IA, United States. Gaillot, J., and Vachard, D., , The Khuff Formation (Middle East) and time-equivalents in Turkey and South China: biostratigraphy from Capitanian to Changhsingian times (Permian), new foraminiferal taxa, and palaeogeographical implications: Coloquios de Paleontología, v. 57, p. 37 –
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In South China, The Upper Devonian Lali section is well-exposed for the whole Frasnian and Famennian stages and have been extensively studied in terms of biostratigraphy, chemostratigraphy, and sedimentology (Ji and Ziegler, ; Chen et al., ; Zhang et al., a, Zhang et al., b).
Studies on the Devonian of China have lasted for about years, and important progress has been made recently. Based on well-studied bio- and chronostratigraphy of the Devonian in South China. The Lower Devonian Yujiang Formation (synonym: Yukiang Formation) is widely distributed and well outcropped in the area between Nanning and Liujing along the Yujiang River (synonym: Yukiang River), central Guangxi, South China ().It consists mainly of sandstone, siltstone, mudstone, and by: 1.
Devonian of the World: Proceedings of the 2nd International Symposium on the Devonian System — Mem Volume III: Paleontology, Paleoecology and Biostratigraphy, Pages Global Events and Boundaries Faunal Change and Events Across the Devonian-Carboniferous Boundary of Huangmao Section, Guangxi, South China.
Bai Shunliang, Bai Zhiqiang, Ma Xueping et al., Devonian Events and Biostratigraphy of South China, Beijing: Peking University Press,1– Google Scholar by: Event in South China. Terminology and abbreviations Geologic setting and biostratigraphy across the F–F boundary in the Devonian Period in the South China plate.
Subsequently, a number. Guangxi and southern Guizhou provinces are the most important areas in China for the study of Devonian biostratigraphy and paleontology.
The Devonian transgression initiated from the Qin-Fang (Qinzhou-Fangcheng) remnant trough in southern Guangxi and expanded progressively northwards on the South China plate (e.g., Wu in Zhong et al., 1. Introduction. The Devonian was a crucial period in Earth and biotic history, during which significant events happened (dramatic variation in CO 2 content, radiation of vascular plants and fish, and first amphibians).
There are a number of geo- and bio-events during the Devonian (e.g., summary in House,Becker et al., ; and Ma et al., — South China), of which the most. The Lali section is located near Lali village, about 50 km west of Yizhou City, Guangxi Province in South China (Fig.
1B), and was paleogeographically situated on the slope of the carbonate platform of the South China plate (Fig. 1B).During the Late Devonian, the South China plate was in a near-equatorial position in the eastern Palaeotethys Ocean (Blakey, ; Fig.
1A). The Hangenberg Crisis at the end of the Devonian is marked by a sudden global mass extinction (main Hangenberg Event), which was especially severe for ammonoids. Among the order Clymeniida, only the cymaclymeniids survived for a short time.
We report the first discovery of Postclymenia cf. evoluta in South China in equivalents of the Hangenberg Black Shale (the regional. The Devonian System of China occurs in the Tianshan–Hingan* Geosyncline of North China, the Yangtze Paraplatform of South China and in the geosynclinal areas of West China.
Devonian formations are entirely absent from the Sino-Korean Paraplatform and the Tarim Platform, but along the border of the Tarim Basin and the slopes of Qilianshan.
The Carboniferous period lasted about 60 Myr, from ~ Ma to ~ Ma. According to the International Commission on Stratigraphy, the Carboniferous System is subdivided into two subsystems, i.e., Mississippian and Pennsylvanian, including 6 series and 7 stages. The Global Stratotype Sections and Points (GSSPs) of three stages have been ratified, the Tournaisian, Visean, and Bashkirian stages.
Sun Y L. Systematic Paleontology, Part 2. New brachiopods across the Eifelian-Givetian boundary. In: Bai S L, Bai Z Q, Ma X P, et al., eds.
Devonian Events and Biostratigraphy of South China. Beijing: Peking University Press, – Google Scholar. Conodont and brachiopod biostratigraphic studies have been conducted at the Mode and Poyuan sections, Guangxi Province, South China.
Combining these with seven previously studied sections, it is suggested that the appearance of the “Spirifer” tonkinensis Fauna in different areas of South China and adjacent areas is diachronous, showing an evident chronological trend from south to north.
A Late-Devonian (Famennian) Renalcis-Epiphyton reef at Zhaijiang, Guilin, South China Article (PDF Available) in Facies 37(1) December. The establishment of the system, series and stage boundaries and correlation of biostratigraphic and chronostratigraphic boundaries in the Devonian strata in South China.
Lithofacies Palaeogeography, Beijing, 29 – (In Chinese, with English abstract). Figure 3. Generalized Devonian carbon and strontium isotope stratigraphy, event stratigraphy in China.
Radiometric age is after Liu et al. ().Relative sea-level change curve is after Ma et al. 87 Sr/ 86 Sr values shown as cross are from GTSand 87 Sr/ 86 Sr values from South China as black and orange solid rectangle are after Huang () and Chen et al.
(), respectively. Silurian/Devonian (S/D) Boundary in W est Qinling of South China (XIGMR and NIGP AS, ; Rong et al., ). Because the comparisons to the S/D index fossils like the. The Late Devonian Frasnian–Famennian Event in South China — Patterns and causes of extinctions, sea level changes, and isotope variations.
Palaeogeography, Palaeoclimatology, Palaeoecology, Vol. Issue., p. Devonian events and biostratigraphy of South China. Studies on the Devonian of China have lasted for about years, and important progress has been made recently. Based on well-studied bio- and chronostratigraphy of Devonian in South China and.
Devonian radiolarians from four new sections at Shaijingpo, Lila, Bazhai, and Shiti Reservoir in southern China are described. Faunas from these localities are assigned to eight f.China Scientific Books Biostratigraphy of the Yangtze Gorge Area (4): Triassic and Jurassic - Author: Zhang Zhenlai, Meng FansongLanguage: Chinese with English summaryPublished on: Soft CoverPreface Introduction The Triassic Series The Jurassic Series Discription of the fossils Foraminifera Triassic Bivalves Jurassic Bivalves Cephalopods Ostracods Conodonts Vertebrate Fossil Plants.The Baoshan region of Yunnan Province, SW China, is one of the best locations to study Wenlock to Pridoli conodonts in China.
Detailed analysis of conodont collections from the Silurian strata.