2012
Upper Famennian to Visean Foraminifers and some carbonate Microproblematica from South China
HANCE, Luc, Hongfei HOU, Daniel VACHARD, Francois Xavier DEVUYST, Jiří KALVODA et. al.Základní údaje
Originální název
Upper Famennian to Visean Foraminifers and some carbonate Microproblematica from South China
Autoři
HANCE, Luc (56 Belgie, garant), Hongfei HOU (156 Čína), Daniel VACHARD (250 Francie), Francois Xavier DEVUYST (56 Belgie), Jiří KALVODA (203 Česká republika, domácí), Edouard POTY (56 Belgie) a Xianghe WU (208 Dánsko)
Vydání
Beijing, 330 s. Geological Publ ish ing House, 20 11 .10, 2012
Nakladatel
Geological Publishing House
Další údaje
Jazyk
angličtina
Typ výsledku
Odborná kniha
Obor
10500 1.5. Earth and related environmental sciences
Stát vydavatele
Čína
Utajení
není předmětem státního či obchodního tajemství
Forma vydání
tištěná verze "print"
Kód RIV
RIV/00216224:14310/12:00058616
Organizační jednotka
Přírodovědecká fakulta
ISBN
978-7-116-07409-5
Klíčová slova anglicky
Carboniferous foraminifers biostratigraphy
Změněno: 19. 3. 2013 15:09, prof. RNDr. Jiří Kalvoda, CSc.
Anotace
V originále
The present volume gives a synthesis of the foraminiferal researches conducted on the Mississippian of South China between 1985 and 2009, in the context of a scientific cooperation between the Chinese Academy of Geological Sciences, Belgium scientific institutions and individual scientists. The foraminifers and their biostratigraphy constitute the main part of the work, but additional information on conodonts, corals and incertae sedis is also given. The samples were collected in Hunan, Guangxi and Guizhou Provinces. Dialectically, the foraminifer biozonation of Belgium is emended at the light of the Chinese data. The main changes concern the Tournaisian zones MFZ4 to MFZ6, much better documented in South China, and MFZ11 which recorded a longer time interval. The upper boundary of this zone is indeed coinciding with a sequence boundary in Belgium, corresponding to a significant gap. The investigated section are described and the indication of the samples origin is given. The abundant material serves as basis for a deep revision of the foraminifer systematic which forms the main part of this work.
Návaznosti
GA205/08/0182, projekt VaV |
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MSM0021622412, záměr |
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