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Liufengshan Hill, Wuxuan Co., Laibin, Guangxi, China
| Mindat.org Locality Page | Wuxuan Co., Laibin, Guangxi, China |
|---|---|
| Lat/Long (Decimal) | 23.6,109.65 |
| Co-ordinates Derivation | based on political unit |
| Given Location | Guangxi, China |
| Mindat.org Region (for given coordinates) | Wuxuan Co., Laibin, Guangxi, China |
Collections
| Collection | Reference | Stratigraphic Name | Comments | Lithology | Age |
|---|---|---|---|---|---|
| Liufengshan Hill, Section 4, Loc. 10 | Zhang R., Pojeta, Jr. J. (1986) | Ertang - Lower | 11 m thick. [JA: originally entered as Emsian; Polygnathus inversus and P. serotinus are present in the lowest unit of the "Sipaian Stage" (probably this formation), so it is late Emsian] | "limestone" | 402.5 - 391.9 Ma Devonian |
| Liufengshan Hill, Section 4, Loc. 11 | Zhang R., Pojeta, Jr. J. (1986) | Ertang - Lower | 21 m thick. [JA: originally entered as Emsian; Polygnathus inversus and P. serotinus are present in the lowest unit of the "Sipaian Stage" (probably this formation), so it is late Emsian] | mudstone | 402.5 - 391.9 Ma Devonian |
| Liufengshan Hill, Section 4, Loc. 16 | Zhang R., Pojeta, Jr. J. (1986) | Ertang - Lower | 23 m thick. [JA: originally entered as Emsian; Polygnathus inversus and P. serotinus are present in the lowest unit of the "Sipaian Stage" (probably this formation), so it is late Emsian] | "limestone" | 402.5 - 391.9 Ma Devonian |
| Liufengshan Hill, Section 4, Loc. 17 | Zhang R., Pojeta, Jr. J. (1986) | Ertang - Lower | 14 m thick. [JA: originally entered as Emsian; Polygnathus inversus and P. serotinus are present in the lowest unit of the "Sipaian Stage" (probably this formation), so it is late Emsian] | "limestone" | 402.5 - 391.9 Ma Devonian |
| Liufengshan Hill, Section 4, Loc. 19 | Zhang R., Pojeta, Jr. J. (1986) | Ertang - Lower | 19 m thick. [JA: originally entered as Emsian; Polygnathus inversus and P. serotinus are present in the lowest unit of the "Sipaian Stage" (probably this formation), so it is late Emsian] | "shale" | 402.5 - 391.9 Ma Devonian |
| Liufengshan Hill, Section 4, Loc. 20 | Zhang R., Pojeta, Jr. J. (1986) | Ertang - Upper | 26 m thick. [JA: originally entered as Emsian; Polygnathus inversus and P. serotinus are present in the lowest unit of the "Sipaian Stage" (probably this formation), so it is late Emsian] | "limestone" | 402.5 - 391.9 Ma Devonian |
| Liufengshan Hill, Section 4, Loc. 22 | Zhang R., Pojeta, Jr. J. (1986) | Ertang - Upper | 13 m thick. [JA: originally entered as Emsian; Polygnathus inversus and P. serotinus are present in the lowest unit of the "Sipaian Stage" (probably this formation), so it is late Emsian] | marl | 402.5 - 391.9 Ma Devonian |
| Liufengshan Hill, Section 4, Loc. 23 | Zhang R., Pojeta, Jr. J. (1986) | Ertang - Upper | 19 m thick. [JA: originally entered as Emsian; Polygnathus inversus and P. serotinus are present in the lowest unit of the "Sipaian Stage" (probably this formation), so it is late Emsian] | "limestone" | 402.5 - 391.9 Ma Devonian |
| Liufengshan Hill, Section 4, Loc. 24 | Zhang R., Pojeta, Jr. J. (1986) | Ertang - Upper | 15 m thick. [JA: originally entered as Emsian; Polygnathus inversus and P. serotinus are present in the lowest unit of the "Sipaian Stage" (probably this formation), so it is late Emsian] | "limestone" | 402.5 - 391.9 Ma Devonian |
| Liufengshan Hill, Section 4, Loc. 25 | Zhang R., Pojeta, Jr. J. (1986) | Ertang - Upper | 6 m thick. [JA: originally entered as Emsian; Polygnathus inversus and P. serotinus are present in the lowest unit of the "Sipaian Stage" (probably this formation), so it is late Emsian] | "shale" | 402.5 - 391.9 Ma Devonian |
| Liufengshan Hill, Section 4, Loc. 26 | Zhang R., Pojeta, Jr. J. (1986) | Ertang - Upper | 7 m thick. [JA: originally entered as Emsian; Polygnathus inversus and P. serotinus are present in the lowest unit of the "Sipaian Stage" (probably this formation), so it is late Emsian] | "limestone" | 402.5 - 391.9 Ma Devonian |
| Liufengshan Hill, Section 4, Loc. 29 | Zhang R., Pojeta, Jr. J. (1986) | Ertang - Upper | 8 m thick. [JA: originally entered as Emsian; Polygnathus inversus and P. serotinus are present in the lowest unit of the "Sipaian Stage" (probably this formation), so it is late Emsian] | "limestone" | 402.5 - 391.9 Ma Devonian |
| Liufengshan Hill, Section 4, Loc. 30 | Zhang R., Pojeta, Jr. J. (1986) | Ertang - Upper | 4 m thick. [JA: originally entered as Emsian; Polygnathus inversus and P. serotinus are present in the lowest unit of the "Sipaian Stage" (probably this formation), so it is late Emsian] | "limestone" | 402.5 - 391.9 Ma Devonian |
| Liufengshan Hill, Section 4, Loc. 31 | Zhang R., Pojeta, Jr. J. (1986) | Ertang - Upper | 3 m thick. [JA: originally entered as Emsian; Polygnathus inversus and P. serotinus are present in the lowest unit of the "Sipaian Stage" (probably this formation), so it is late Emsian] | "shale" | 402.5 - 391.9 Ma Devonian |
| Liufengshan Hill, Section 4, Loc. 32 | Zhang R., Pojeta, Jr. J. (1986) | Ertang - Upper | 2 m thick. [JA: originally entered as Emsian; Polygnathus inversus and P. serotinus are present in the lowest unit of the "Sipaian Stage" (probably this formation), so it is late Emsian] | "shale" | 402.5 - 391.9 Ma Devonian |
| Liufengshan Hill, Section 4, Loc. 33 | Zhang R., Pojeta, Jr. J. (1986) | Ertang - Upper | 14 m thick. [JA: originally entered as Emsian; Polygnathus inversus and P. serotinus are present in the lowest unit of the "Sipaian Stage" (probably this formation), so it is late Emsian] | "shale" | 402.5 - 391.9 Ma Devonian |
| Liufengshan Hill, Section 4, Loc. 34 | Zhang R., Pojeta, Jr. J. (1986) | Ertang - Upper | 19 m thick. [JA: originally entered as Emsian; Polygnathus inversus and P. serotinus are present in the lowest unit of the "Sipaian Stage" (probably this formation), so it is late Emsian] | "shale" | 402.5 - 391.9 Ma Devonian |
| Liufengshan Hill, Section 4, Loc. 35 | Zhang R., Pojeta, Jr. J. (1986) | Ertang - Upper | 20 m thick. [JA: originally entered as Emsian; Polygnathus inversus and P. serotinus are present in the lowest unit of the "Sipaian Stage" (probably this formation), so it is late Emsian] | "shale" | 402.5 - 391.9 Ma Devonian |
| Liufengshan Hill, Section 4, Loc. 36 | Zhang R., Pojeta, Jr. J. (1986) | Ertang - Upper | 7 m thick. [JA: originally entered as Emsian; Polygnathus inversus and P. serotinus are present in the lowest unit of the "Sipaian Stage" (probably this formation), so it is late Emsian] | mudstone | 402.5 - 391.9 Ma Devonian |
| Liufengshan Hill, Section 4, Loc. 37 | Zhang R., Pojeta, Jr. J. (1986) | Ertang - Upper | 20 m thick. [JA: originally entered as Emsian; Polygnathus inversus and P. serotinus are present in the lowest unit of the "Sipaian Stage" (probably this formation), so it is late Emsian] | "limestone" | 402.5 - 391.9 Ma Devonian |
| Liufengshan Hill, Section 4, Loc. 4 | Zhang R., Pojeta, Jr. J. (1986) | Ertang - Lower | 16 m thick. [JA: originally entered as Emsian; Polygnathus inversus and P. serotinus are present in the lowest unit of the "Sipaian Stage" (probably this formation), so it is late Emsian] | "limestone" | 402.5 - 391.9 Ma Devonian |
| Liufengshan Hill, Section 4, Loc. 6 | Zhang R., Pojeta, Jr. J. (1986) | Ertang - Lower | 6 m thick. [JA: originally entered as Emsian; Polygnathus inversus and P. serotinus are present in the lowest unit of the "Sipaian Stage" (probably this formation), so it is late Emsian] | "limestone" | 402.5 - 391.9 Ma Devonian |
| Liufengshan Hill, Section 4, Loc. 8 | Zhang R., Pojeta, Jr. J. (1986) | Ertang - Lower | 18 m thick. [JA: originally entered as Emsian; Polygnathus inversus and P. serotinus are present in the lowest unit of the "Sipaian Stage" (probably this formation), so it is late Emsian] | "limestone" | 402.5 - 391.9 Ma Devonian |
| Liufengshan Hill, Section 4, Loc. 9 | Zhang R., Pojeta, Jr. J. (1986) | Ertang - Lower | 4 m thick. [JA: originally entered as Emsian; Polygnathus inversus and P. serotinus are present in the lowest unit of the "Sipaian Stage" (probably this formation), so it is late Emsian] | mudstone | 402.5 - 391.9 Ma Devonian |
| Liufengshan Hill, Section 4, Loc. 1 | Zhang R., Pojeta, Jr. J. (1986) | Shanglun Dolomite | 32 m thick. The Shanglun Dolomite conformably overlies the Lower Devonian Yujiang Fm. So even though it is not explicitly stated what age it is, since it is between two other fms of Emsian age, I left it as Emsian. | dolomite | 407.6 - 393.3 Ma Early/Lower Devonian |
Recorded Fossils
References
Data courtesy of: PBDB: The Paleobiology Database, Creative Commons CC-BY licenced. , GBIF: the Global Biodiversity Information Facility, various licences, iDigBio, various licences, and EOL: The Encyclopedia of Life (Open Data Public Domain). Because fossils are made of minerals too!
