Where: Guizhou, China (27.0° N, 107.4° E: paleocoordinates 43.2° N, 164.4° E)
• coordinate stated in text
• outcrop-level geographic resolution
When: Lower Sequence Member (Doushantuo Formation), Ediacaran (635.0 - 541.0 Ma)
• from units 4A and 4B, 635-551 Ma; Base of "Lower Sequence" member is dated at 632.5. This overlies Lower Dolomite.
• group of beds-level stratigraphic resolution
Environment/lithology: marine; lithified phosphorite
Size class: microfossils
Primary reference: P. Liu, S. Xiao, C. Yin, C. Zhou, L. Gao and F. Tang. 2008. Systematic description and phylogenetic affinity of tubular microfossils from the Ediacaran Doushantuo Formation at Weng'an, south China. Palaeontology 51(2):339-366 [W. Kiessling/U. Merkel]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 112153: authorized by Wolfgang Kiessling, entered by Uta Merkel on 05.07.2011
Creative Commons license: CC BY (attribution)
Taxonomic list
Sinocyclocyclicus guizhouensis | |
Sinocyclocyclicus guizhouensis Xue 1992 | |
Ramitubus increscens | |
Ramitubus increscens n. gen. n. sp.
Ramitubus increscens n. gen. n. sp. Liu et al. 2008 | |
Ramitubus decrescens | |
Ramitubus decrescens n. sp.
Ramitubus decrescens n. sp. Liu et al. 2008 | |
Quadratitubus orbigoniatus | |
Quadratitubus orbigoniatus Xue 1992 | |
Crassitubus costatus | |
Crassitubus costatus n. gen. n. sp.
Crassitubus costatus n. gen. n. sp. Liu et al. 2008 |