Where: Coimbra, Portugal (40.1° N, 8.8° W: paleocoordinates 30.2° N, 2.4° E)

• outcrop-level geographic resolution

When: spinatum ammonoid zone, Lemede Formation, Pliensbachian (190.8 - 182.7 Ma)

• Spinatum hawskerense subzone

• group of beds-level stratigraphic resolution

Environment/lithology: coastal; lithified limestone and lithified marl

Size class: macrofossils

Primary reference: R. Paredes, M. J. Comas-Rengifo, L.V. Duarte and A. Goy. 2018. Upper Pliensbachian–lowermost Toarcian macroinvertebrates (Ammonites, Bivalves) succession prior to the TOAE extinction interval. The example of Fonte Coberta section - Stop 2.1. In L.V. Duarte, R.L. Silva (eds.), The Toarcian Oceanic Anoxic Event in the Western Iberian Margin and its context within the Lower Jurassic evolution of the Lusitanian Basin. 2nd International Workshop on Toarcian Oceanic Anoxic Event, Field Trip Guidebook 63-70 [M. Aberhan/C. Reddin]more details

Purpose of describing collection: paleoecologic analysis

PaleoDB collection 225386: authorized by Martin Aberhan, entered by Carl Reddin on 06.05.2022

Creative Commons license: CC BY (attribution)