Pimenteira Formation
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| Pimenteira Formation | |
|---|---|
| Stratigraphic range: Late Eifelian-Famennian ~ | |
| Type | Geological formation |
| Unit of | Canindé Group |
| Sub-units | Picos Member Passagem Member |
| Underlies | Cabeças Formation |
| Overlies | Itaim Formation |
| Thickness | 20 m (66 ft) |
| Location | |
| Region | Piauí Tocantins |
| Country | Brazil |
| Extent | Parnaíba Basin |
| Type section | |
| Named for | Pimenteiras, Piauí |
The Pimenteira Formation, also known as Pimenteiras Formation,[1] is an Mid to Late Devonian geological formation of the Parnaíba Basin, northeastern Brazil. It mainly outcrops in the states of Piauí and Tocantins.[2] It is was deposited in a shallow sea, under the influence of currents and storm waves, as well as fluvio-deltaic influences.[3]
Being part of the Malvinokaffric Realm, it haboured a diverse fauna of invertebrates such as trilobites, brachiopods, bivalves, gastropods, and tentaculids, as well as elamobranches and plant remains.[3]
The name 'Pimenteira' was first proposed by Small (1914) to ascribe a shale sequence 20 m in thickness close to the municipality of Pimenteiras, Piauí.[2] Caster (1948), reported on the occurrence of several fossils in the area, like trilobites[1] and shark fin bones,[1] and Kegel (1953) later visited the region between Picos and Pimenteiras, collecting specimens and later describing them.[4][1]
Initially, Kegel (1952) divided the formation into the Itaim and Picos members. Blankennagel (1952) later considered that only the Picos Member is part of the formation, with the Itaim Member being the upper part of the Serra Grande Formation.[5]
































