Kindle boulder #380, ZP Biofacies, Downes Point Mb, - Young and Ludvigsen 1989: Solvan, Canada
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
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Agnostida
- Eodiscidae
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Pagetia rasettii n. sp.
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51 specimens | |||||||||
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Agnostida
- Peronopsidae
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Peronopsis mariae n. sp.
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70 specimens | |||||||||
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Agnostida
- Ptychagnostidae
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Onymagnostus seminula
(Whitehouse 1939)
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12 specimens | |||||||||
| recombined as Ptychagnostus seminula | ||||||||||
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Ptychagnostus cf. intermedius
(Tullberg 1880)
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1 specimen | |||||||||
| entered as "Ptychagnostus informal cf. intermedius" | ||||||||||
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? Tomagnostus sp.
Howell 1935
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11 specimens | |||||||||
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Trilobita
- Ptychopariida
- Alokistocaridae
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Elrathia kindlei n. sp.
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23 specimens | |||||||||
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Chancia tuberculata n. sp.
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8 specimens | |||||||||
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Trilobita
- Corynexochida
- Oryctocephalidae
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Tonkinella occidentalis n. sp.
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4 specimens | |||||||||
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Trilobita
- Corynexochida
- Zacanthoididae
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Zacanthoides gilberti
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6 specimens | |||||||||
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Parkaspis caboti
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13 specimens | |||||||||
| see common names | ||||||||||
Geography
| Country: | Canada | State/province: | Newfoundland and Labrador |
| Coordinates: | 49.3° North, 65.6° West (view map) | ||
| Paleocoordinates: | 34.7° South, 73.1° West | ||
| Basis of coordinate: | based on political unit | ||
| Geographic resolution: | outcrop |
Time
| Period: | Cambrian | ||
| 10 m.y. bin: | Cambrian 3 | ||
| *Period: | Middle Cambrian - Late/Upper Cambrian | *Epoch: | St. David's |
| *International age/stage: | Late/Upper Solvan | ||
| Key time interval: | Solvan | Zone: | Ptychagnostus gibbus |
| Age range of interval: | 510.00000 - 504.50000 m.y. ago | ||
| * legacy (obsolete) database fields | |||
Stratigraphy
| Geological group: | Cow Head | Formation: | Shallow Bay | Member: | Downes Point | Local bed: | Boulder #380 |
| Stratigraphic resolution: | group of beds | ||||
| Stratigraphy comments: Boulder #380 is from the Zacanthoidid-Pagetia Biofacies. While this monograph deals with the Kindle Zone 1, fauna of the Kindle Zones 2-5 can be found in Westrop et. al 1996. The Downes Point Member is about 100m thick and the general paleoenvironment is a shelf edge/upper slope environment which transported fossils as debris flows forming a deep water sediment apron.. | |||||
Lithology and environment
| Primary lithology: | red or brown lithified grainstone |
| Secondary lithology: | lithified packstone |
| Includes fossils? | Y |
| Includes fossils? | Y |
| Lithology description: The Zacanthoidid-Pagetia biofacies has a lithology of light brown grainstone and packstone with abundant spar and rare lime mud. | |
| Environment: | slope |
Taphonomy
| Modes of preservation: | body,recrystallized |
| Size of fossils: | macrofossils,mesofossils |
| Spatial orientation: | random |
| Disassociated major elements: | all |
| Fragmentation: | frequent |
| Encrustation: | occasional |
Collection methods and comments
| Collection methods: | survey of museum collection |
| Reason for describing collection: | taxonomic analysis |
| Collection method comments: Not all boulders were assignable to a biofacies and only trilobites were described, however other taxa are not known to be omitted since there is no mention of them in the text. The trilobites described here are part of the C. H. Kindle Collection at the Geological Survey of Canada. | |
Metadata
| Database number: | 10826 | ||
| Authorizer: | M. Patzkowsky | Enterer: | P. Borkow |
| Modifier: | J. Alroy | Research group: | marine invertebrate |
| Created: | 2001-06-27 08:58:39 | Last modified: | 2012-10-28 01:16:56 |
| Access level: | the public | Released: | 2001-06-27 08:58:39 |
| Creative Commons license: | CC BY |
Reference information
Primary reference:
| 4030. | G. A. Young and R. Ludvigsen. 1989. Mid-Cambrian trilobites from the lowest part of the Cow Head Group, western Newfoundland. Geological Survey of Canada Bulletin 392:1-28 [M. Patzkowsky/P. Borkow/P. Wagner] |