Contents - Fossils sites in Ireland
Section 1-1 - Fossil collecting in IrelandSection 1-2 - Where are the dinosaurs?Section 1-3 - The good news
Section 2-1 - Precambrian/CambrianSection 2-2 - OrdovicianSection 2-3 - SilurianSection 2-4 - DevonianSection 2-5 - Carboniferous/MississippianSection 2-6 - Carboniferous/Pennsylvanian
Chapter 3 - Fossil sites in Ireland
Section 3-4 - County Sligo - Streedagh Point - Mississippian
Section 1-1 - Fossil collecting in IrelandSection 1-2 - Where are the dinosaurs?Section 1-3 - The good news
Section 2-1 - Precambrian/CambrianSection 2-2 - OrdovicianSection 2-3 - SilurianSection 2-4 - DevonianSection 2-5 - Carboniferous/MississippianSection 2-6 - Carboniferous/Pennsylvanian
Section 3-4 - County Sligo - Streedagh Point - Mississippian
Chapter 3 - Fossil sites in Ireland
Section 3-4 - County Sligo - Streedagh Point - Mississippian
Fig. 3-4.1 - Location of Streedagh Point, county Sligo. |
The prominent landmark of Benbulben in county Sligo comprises many of the Mississippian fossil-rich limestones and shales which also occur in the surrounding landscape, for example the Benbulben Shale Formation, the Glencar Limestone Formation and the Dartry Limestone Formation (GSI, Benbulben, undated).
Fig. 3-4.2 - The mountain Benbulben is visible from many locations in county Sligo, including Streedagh Point. Image © Michael O'Connell 2022, used with permission of the author. |
Fig. 3-4.3 - Corals Siphonophyllia samsonensis, Glencar Limestone Formation at Streedagh Point, county Sligo. |
Fig. 3-4.4 - Corals Siphonophyllia samsonensis, Glencar Limestone Formation at Streedagh Point, county Sligo. |
The typical 'elbow curvature' of the coral Siphonophyllia samsonensis is probably due to an adaptation of the corals to short-term changing living conditions at this location (pers. comm. Ian Sanders, 2022).
Fig. 3-4.5 - Corals Siphonophyllia samsonensis, Glencar Limestone Formation at Streedagh Point, county Sligo. |
The daily, monthly and annual growth bands of corals reveal that years on Earth in the Palaeozoic had more months than today (for example, 13 months in the Devonian) and the Earth's axial rotation is continuously slowing down (Scrutton, 1965) (Wyse Jackson, 2019, pp 72-73).
Fig. 3-4.6 - Growth bands of Siphonophyllia samsonensis, Glencar Limestone Formation at Streedagh Point, county Sligo. Length of the specimen is 21cm. |
Fig. 3-4.7 - Longitudinal section through a Siphonophyllia samsonensis, Glencar Limestone Formation at Streedagh Point, county Sligo. |
Fig. 3-4.8 - graphic - transverse section of a rugose coral. Image credit: geological-digressions.com |
Fig. 3-4.9 - Transverse sections of Siphonophyllia samsonensis, Glencar Limestone Formation at Streedagh Point, county Sligo. |
Fig. 3-4.10 - Siphonodendron colony, Glencar Limestone Formation at Streedagh Point, county Sligo. |
Fig. 3-4.11 - Brachiopod Gigantoproductus, Glencar Limestone Formation at Streedagh Point, county Sligo. |