Fortune Head

Fortune Head is a headland located about 1.6 km from the town of Fortune on the Burin Peninsula, southeastern Newfoundland.

A 410 m thick section of rock along its cliffs is designated the Global Boundary Stratotype Section and Point (or GSSP) representing the boundary between the Precambrian era and the Cambrian period, 542 million years ago. Because of its accessibility and abundance of fossils, Fortune Head was selected in 1992 over similar rock sections in Siberia, Russia, and Meischucum, China.cite web | url = http://www.k12.nf.ca/lakeacademy/fossil2.htm | title = Fortune Head Ecological Reserve | accessdate = 2006-03-21]

Fortune Head Ecological Reserve

Fortune Head was established as a provisional reserve in 1990, and then given full ecological reserve status in 1992 following Fortune Head’s selection as the global stratotype. The reserve is 2.21 km² in size. The Fortune Head lighthouse, which is operated by the Canadian Coast Guard, is also on the reserve and functions as a visitor center. [cite web | url = http://www.env.gov.nl.ca/parks/wer/r_fhe/ | title = Fortune Head Ecological Reserve | publisher = The Government of Newfoundland and Labrador | accessdate = 2006-03-21]

Geology

The Burin Peninsula is part of the Avalon Zone of the Appalachian Orogen, the geology of which chronicles the late Precambrian Alleghenian Orogeny. The stratigraphy is not uniform throughout the region, however. The southern end of the peninsula includes a series of mafic pillow lavas, volcanigenic sediments, shales and limestones, collectively known as the "Burin Group", as well as a 1500 m thick sill of gabbro about 760 million years old. The northern end of the peninsula is defined by the "Marystown Group", primarily carbon-lacking Silica-based sediments which span the Precambrian-Cambrian boundary. The sediments were probably deposited in shoreline environments along the former Iapetus Ocean.

The global stratotype at Fortune Head is composed of the uppermost part of member 1 and all of member 2 of the Chapel Island Formation of the Marystown Group. The Chapel Island Formation consists primarily of sandstones, siltstones, and limestones. Some of these rocks exhibit mud cracks and stromatolites, suggesting that deposition occurred in tidal or, at deepest, continental shelf environments.

Fossils

The boundary between the Precambrian and Cambrian is demarcated by the presence of trace fossils of "Trichophycus pedum", one of the earliest animals. Without any hard anatomical features, "Trichophycus" is known only by its distinctive burrow pattern, which can be seen at Fortune Head.

Fortune Head records the beginning of a period of increasing biological diversity known as the "Cambrian explosion", and it exhibits a number of other Cambrian and Precambrian fossils, including early shell fossils, vendotaenid algae, soft-bodied megafossils, and microfossils. Below "Trichophycus", the stratotype at Fortune Head includes traces of the arthropod "Monomorphichnus", vertical dwelling burrows from Skolithes and ArenicolitesVerify source|date=December 2007 , cnidarian resting burrows from "Conichnus" and "Bergauria", and more intricate feeding burrows from Gyrolithes. More complex fossils appear later.

References