| Color | Fortunian |
|---|---|
| Time end prefix | ~ |
| Caption outcrop | Delegates from the Ichnia 2012 conference inspect the Global Boundary Stratotype Section and Point (GSSP) for the Ediacaran-Cambrian boundary at Fortune Head Ecological Reserve, Newfoundland, Canada. |
| Timeline | Cambrian |
| Name formality | Formal |
| Former names | Cambrian Stage 1 |
| Celestial body | earth |
| Usage | Global (ICS) |
| Timescales used | ICS Time Scale |
| Chrono unit | Age |
| Strat unit | Stage |
| Proposed by | Ed Landing, 2007[1] |
| Timespan formality | Formal |
| Lower boundary def | Appearance of the Ichnofossil Treptichnus pedum |
| Lower gssp location | Fortune Head section, Newfoundland, Canada |
| Lower gssp coords | 47.0762°N 55.8310°W |
| Upper boundary def | Not formally defined |
| Upper def candidates | First appearance of small shelly fauna or Archaeocyathids |
| Upper gssp candidates | None |
The Fortunian age marks the beginning of the Phanerozoic Eon, the Paleozoic Era, and the Cambrian Period. It is the first of the two stages of the Terreneuvian series. Its base is defined as the first appearance of the trace fossil Treptichnus pedum million years ago. The top of the Fortunian which is the base of the Stage 2 of the Cambrian has not been formally defined yet, but will correspond to the appearance of an Archeocyatha species or "Small shelly fossils" approximately million years ago.[2]
The name Fortunian is derived from the town of Fortune on the Burin Peninsula, near the GSSP and Fortune Bay.[1]
GSSP
The type locality (GSSP) of the Fortunian stage is in Fortune Head, at the northern edge of the Burin Peninsula, Newfoundland, Canada[1] (47.0762°N 55.8310°W). This GSSP coincides with the base of the Terreneuvian series, the Precambrian-Cambrian boundary and the beginning of the Phanerozoic. The outcrops show a carbonate-siliciclastic succession which is mapped as the Chapel Island Formation. The formation is divided into the following members that are composed of peritidal sandstones and shales (Member 1), muddy deltaic and shelf sandstones and mudstones (Member 2A), laminated siltstones (Member 2B and 3) and mudstones and limestones of the inner shelf (Member 4). The Precambrian-Cambrian boundary lies 2.4 m above the base of the 2nd member which is the lowest occurrence of Treptichnus pedum. The traces can be seen on the lower surface of the sandstone layers. The first calcareous shelled skeletal fossils (Ladatheca cylindrica) is 400 m above the boundary. The first trilobites appear 1,400 m above the boundary, which corresponds to the beginning of the Branchian Series.[3]
References
- ^ Landing, Ed (2007). "The Base of the Cambrian: Terreneuvian Series and Fortunian Stage". www.palaeontology.geo.uu.se. Retrieved October 21, 2025.
- ^ "Global Boundary Stratotype Section and Point". International Commission of Stratigraphy. Archived from the original on 15 November 2012. Retrieved 2 November 2012.
- ^ Brasier, Martin; John Cowie; Michael Taylor (1994). "Decision on the Precambrian-Cambrian boundary stratotype". Episodes. 17 (1–2): 3—8. doi:10.18814/epiiugs/1994/v17i1.2/002. Archived 2024-03-17 at the Wayback Machine.
External links
- Martin, Anthony (Tony) (27 August 2012). "Out of One's Depth in the Ediacaran". Archived 2022-11-21 at the Wayback Machine.
- Martin, Anthony (Tony) (23 August 2012). "Mistaken Point and the Limits of Actualism". Archived 2022-12-08 at the Wayback Machine.
- "Album of the Ichnia 2012 conference at Fortune Head". flickr.com. 13 August 2012. Archived 2024-03-17 at the Wayback Machine.
- "GSSP Table - Paleozoic Era". Geologic Timescale Foundation. Archived 2023-10-08 at the Wayback Machine.