Where: Zaragoza, Spain (41.2° N, 1.1° W)
• Paleocoordinates: 79.8° S, 9.0° E (Wright 2013)
• coordinate estimated from map
• local area-level geographic resolution
When: Pena del Tormo Member (Fombuena Formation), Berounian to Berounian (457.9 - 455.8 Ma)
• Locally called the "Upper iron oolite and bryozoan marls"
• bed-level stratigraphic resolution
Environment/lithology: sand shoal; lithified, concretionary, ferruginous grainstone and lithified, shelly/skeletal, silty, conglomeratic shale
•
•At this section the Pefia del Tormo Member lacks the marly beds with bryozoans that characterize the unit southwest of this outcrop, including the two former sections. The basal ironstone is only 45 cm thick and is immediately succeeded by the alternating sandstones and shales of the Huerva Member.
Size classes: macrofossils, mesofossils
Preservation: cast
Primary reference: E. Villas. 1992. New Caradoc brachiopods from the Iberian Chains (northeastern Spain) and their stratigraphic significance. Journal of Paleontology 66(5):772-793 [A. Miller/P. Novack-Gottshall/P. Novack-Gottshall]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 166736: authorized by Pete Wagner, entered by Pete Wagner on 24.02.2015
Creative Commons license: CC0 (CC0)
Taxonomic list
Rhynchonellata | |