Also known as Schiet Hoogte farm; Suurberg Gorge; Lake Mentz
Where: Eastern Cape, South Africa (33.2° S, 25.1° E: paleocoordinates 81.8° S, 163.7° W)
When: Waaiport Formation (Witteberg Group), Tournaisian (358.9 - 346.7 Ma)
• "miospores including S. balteatus and S. pretiosus were interpreted to be no older than mid-Tournaisian." (Lakin et al 2016)
•Unconformably overlain by Dwyka formation
Environment/lithology: lacustrine - large; lithified, fine-grained, nodular, black, carbonaceous mudstone and lithified, sandy marl
•"The fish are confined to a narrow band of sandy marl of about five inches in thickness" (Gardiner 1969)
Size class: macrofossils
Preservation: concretion
Primary reference: B. G. Gardiner. 1969. New palaeoniscoid fish from the Witteberg series of South Africa. Zoological Journal of the Linnean Society 48(4):423-452 [E. Dunne/S. Fasey]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 226927: authorized by Emma Dunne, entered by Sophie Fasey on 10.08.2022
Creative Commons license: CC BY (attribution)
Taxonomic list
Osteichthyes | |
Aestuarichthys fulcratus Gardiner 1969 | |
Sundayichthys elegantulus n. gen. n. sp.
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Mentzichthys maraisi n. sp., Mentzichthys walshi n. gen. n. sp., Mentzichthys jubbi n. sp., Mentzichthys theroni
Mentzichthys maraisi n. sp. Gardiner 1969 Holotype PRV 631; PRV 638 (specimen without skull), PRV 632
Mentzichthys walshi n. gen. n. sp. Jubb 1965
Mentzichthys theroni Gardiner 1969 ? Holotype: SAM 13570 (Evans 2005 suspects the holotype is from this locality, not Soetendalsvlei)
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Australichthys longidorsalis n. gen. n. sp.
Australichthys longidorsalis n. gen. n. sp. Gardiner 1969 Holotype: Holotype PRV 639a (Marais species B, pl. 4a)
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Willomorichthys striatulus, Darlingtonichthys raumi n. gen. n. sp., Glenconnorichthys jamesi n. gen. n. sp., Catastropheichthys almondi n. gen. n. sp.
Willomorichthys striatulus Gardiner 1969 ray-finned fish
Glenconnorichthys jamesi n. gen. n. sp. Evans 2005 ray-finned fish ? Holotype: SAM 13553 (recorded as being from Soetendalsvlei, but “definitely” from this locality per Evans et al. 2005)
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