Sekwi Formation
| Sekwi Formation | |
|---|---|
| Stratigraphic range: ; Fallotaspis, Nevadella, and Bonnia-Olenellus trilobite zones[2] | |
| Type | Formation |
| Underlies | |
| Overlies |
|
| Thickness | 700 m[2] |
| Location | |
| Region | Northwest Territories |
| Country | Canada |
The Sekwi Formation is a geologic formation in Northwest Territories, Canada, which preserves fossils dating back to the Cambrian period.
The formation principally comprises shallow water carbonates, but deepens to include mid-shelf mudstones, both calcareous and siliciclastic.[2]
It dates from c. 525-510 Ma, the Nevadella / Bonnia-Olenellus trilobite zones.[3]
See also
References
- ^ Dewing, K.; Sharp, R J; Ootes, L; Turner, E C; Gleeson, S (2006). Geological Survey of Canada, Current Research (Online) no. 2006-A4. ISBN 9780662431343.
- ^ a b c d RANDELL, ROBERT D.; LIEBERMAN, BRUCE S.; HASIOTIS, STEPHEN T.; POPE, MICHAEL C. (September 2005). "New Chancelloriids From the Early Cambrian Sekwi Formation With a Comment on Chancelloriid Affinities". Journal of Paleontology. 79 (5): 987–996. doi:10.1666/0022-3360(2005)079[0987:NCFTEC]2.0.CO;2. S2CID 130292492.
- ^ Dilliard, K.A.; Pope, M.C.; Coniglio, M.; Hasiotis, S.T.; Lieberman, B.S. (2007). "Stable isotope geochemistry of the lower Cambrian Sekwi Formation, Northwest Territories, Canada: Implications for ocean chemistry and secular curve generation". Palaeogeography, Palaeoclimatology, Palaeoecology. 256 (3–4): 174–194. doi:10.1016/j.palaeo.2007.02.031.
- Various Contributors to the Paleobiology Database. "Fossilworks: Gateway to the Paleobiology Database". Retrieved 17 December 2021.