Where: Namur, Belgium (50.2° N, 4.9° E: paleocoordinates 13.1° S, 5.0° E)
• coordinate based on nearby landmark
When: Polygnathus communis conodont zone, Lower Member (Waulsort Formation), Ivorian (353.8 - 346.7 Ma)
• Late Tournaisian, Tn 3; was Carboniferous Limestone; Godefroid et al. 2006 note that this is from the lower half of the formation.
Environment/lithology: lithified wackestone
•cavity fillings, including voids formed after decay of soft-bodied organisms (and sometimes modified subsequently by local collapse and dissolution) as well as
•fracture fillings. Other sparry fabrics were formed by neomorphism. The matrix material surrounding the sparry masses is predominantly wackestone.
•
•A rich macrofauna of brachiopods and molluscs is common in the spar-rich facies (Demanet, 1958). Microbial processes probably played an important role in producing and fixing the carbonate muds.
Size class: macrofossils
Collection methods: trilobites only
Primary reference: G. Hahn, R. Hahn, and C. Brauckmann. 1982. Die Trilobiten des belgischen Kohlenkalkes (Unter-Karbon). 4. Phillipsia. Geologica et Palaeontologica 16:163-182 [D. Korn/D. Korn/D. Korn]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 37243: authorized by Dieter Korn, entered by Daniela Liebsch on 09.03.2004, edited by Dieter Korn and Pete Wagner
Creative Commons license: CC BY (attribution)
Taxonomic list
Gastropoda | |
"Agnesia discrepans n. sp." = Pauquysia discrepans1
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"Ptychomphalus pisum n. sp." = Mourlonia pisa1, "Ptychomphalus agassizi n. sp." = Mourlonia agassizi1
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"Murchisonia acuminata n. sp." = Stegocoelia (Hypergonia) acuminata1
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"Bellerophon umbilicatus" = Teutonophon umbilicatus3, "Bucaniopsis exilis" = Retispira exilis3, "Bellerophon pinguis" = Waagenella pinguis3, Bellerophon sulcatulus3, Bellerophon demaneti3
| |
Phanerotinus intermedius n. sp.1
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Trilobita | |
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