Fortunian

From Wikipedia, the free encyclopedia
Jump to: navigation, search
Key events in the Cambrian
view • discuss • edit
-550 —
-540 —
-530 —
-520 —
-510 —
-500 —
-490 —
Fortunian
 
 
 
 
* * * * * * * * * * * *
* * * * * * * * * * * * * * * * * * * * * * * * *
Baykonur
glaciation
Baykonur
glaciation
* * * * * * * * * * * *
* * * * * * * * * * * * * * * * * * * * * * * * *
Orsten Fauna
Archaeocyatha extinction
SSF diversification, first brachiopods & archaeocyatha
Treptichnus pedum trace
Large negative peak δ 13Ccarb excursion
First Cloudina & Namacalathus mineral tubular fossils
Stratigraphic scale of the ICS subdivisions and Precambrian/Cambrian boundary.

Coordinates: 47°04′34″N 55°49′52″W / 47.0762°N 55.8310°W / 47.0762; -55.8310

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. The boundary is defined on the appearance of the complex, vertical trace fossil Treptichnus (formerly Phycodes) pedum.

The Fortunian stage marks the beginning of the Phanerozoic, the Paleozoic, and the Cambrian. 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 541.0 ± 1.0 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 ~529 million years ago.[1]

The name Fortunian is derived from a part of the Burin Peninsula, the village Fortune near the GSSP and Fortune Bay.[2]

GSSP[edit]

The type locality (GSSP) of the Fortunian stage is in Fortune Head, at the northern edge of the Burin Peninsula, Newfoundland, Canada (47°04′34″N 55°49′52″W / 47.0762°N 55.8310°W / 47.0762; -55.8310). This GSSP coincides with the beginning 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 1400 m above the boundary which corresponds to the beginning of the Branchian Series.[3]

See also[edit]

References[edit]

  1. ^ "Global Boundary Stratotype Section and Point". International Commission of Stratigraphy. Retrieved 2 November 2012. 
  2. ^ Landing, E. "THE BASE OF THE CAMBRIAN: TERRENEUVIAN SERIES AND FORTUNIAN STAGE". Retrieved 2 November 2012. 
  3. ^ Brasier, Martin; John Cowie; Michael Taylor (1994). "Decision on the Precambrian-Cambrian boundary stratotype". Episodes 17 (1-2): 95–100. Retrieved 14 September 2012. 

External links[edit]

Preceded by Proterozoic Eon Phanerozoic Eon
Paleozoic Era Mesozoic Era Cenozoic Era
Cambrian Ordovician Silurian Devonian Carboniferous Permian Triassic Jurassic Cretaceous Paleogene Neogene 4ry