Early Ordovician sponge-Calathium-microbial reefs on the Yangtze Platform margin of the South China Block

Beitrag in einer Fachzeitschrift
(Originalarbeit)


Details zur Publikation

Autorinnen und Autoren: Li Q, Lin Y, Kießling W
Zeitschrift: Gff
Verlag: Taylor & Francis: STM, Behavioural Science and Public Health Titles
Jahr der Veröffentlichung: 2014
Band: 136
Heftnummer: 1
Seitenbereich: 157-161
ISSN: 1103-5897


Abstract


Early Ordovician (late Tremadocian to early Floian) reefs on the Yangtze Platform margin of the Hunghuayuan Formation at Zhangzhai section in southeastern Guizhou, South China show three types of reefs in two broad categories: microbial-dominated (stromatolite and lithistid sponge-Calathium-calcimicrobial) reefs and metazoan-dominated (lithistid sponge-Calathium) reefs. These reef types represent different communities controlled by varying environmental settings. Stromatolites tended to develop in the shallow subtidal zone, whereas unlaminated calcimicrobial mounds and metazoan-dominated reefs thrived at greater depths. This is the first report on metazoan-dominated reefs at the platform margin of the Hunghuayuan Formation. © 2014 © 2014 Taylor & Francis.



FAU-Autorinnen und Autoren / FAU-Herausgeberinnen und Herausgeber

Kießling, Wolfgang Prof. Dr.
Lehrstuhl für Paläoumwelt
Li, Qijian
Lehrstuhl für Paläoumwelt


Einrichtungen weiterer Autorinnen und Autoren

Nanjing Institute of Geology and Paleontology


Zitierweisen

APA:
Li, Q., Lin, Y., & Kießling, W. (2014). Early Ordovician sponge-Calathium-microbial reefs on the Yangtze Platform margin of the South China Block. Gff, 136(1), 157-161. https://dx.doi.org/10.1080/11035897.2013.862852

MLA:
Li, Qijian, Yue Lin, and Wolfgang Kießling. "Early Ordovician sponge-Calathium-microbial reefs on the Yangtze Platform margin of the South China Block." Gff 136.1 (2014): 157-161.

BibTeX: 

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