Rectifying a substantial biostratigraphic error: There are no Hauterivian calpionellids in Busot (Alicante, Spain)

Earlier misidentifications of ammonites from Busot (SE Spain) led to two incorrect hypotheses regarding calpionellids, which are today attributed to the Calpionellopsis Zone (D) of the upper Berriasian. The first hypothesis suggested that some calpionellid species survived into Hauterivian times, while the second hypothesis proposed that these calpionellids were reworked into Hauterivian strata. However, the revision of the ammonitic material collected in 1993-1994, along with the study of new material collected in 2024, suggests a late Berriasian age, as the ammonite assemblages likely correspond to the Fauriella boissieri and Tirnovella alpillensis Standard Ammonites zones. Nannofossil assemblages and the presence of Octahedronoides tethysianus further support this dating. This reassessment calls for a reexamination of claims regarding the occurrence of calpionellids in strata younger than the Valanginian in the literature.

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Publication Details

Journal
Carnets de géologie (Notebooks on geology)
Published
2024-12-22
DOI
https://doi.org/10.2110/carnets.2025.2502
Primary Topic
Pleistocene-Era Hominins and Archaeology
Type
article
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article

Rectifying a substantial biostratigraphic error: There are no Hauterivian calpionellids in Busot (Alicante, Spain)

Bruno Ferré, Antonio Estévez Rubio, Bernard C. Lambert, Bruno Granier et al.
Carnets de géologie (Notebooks on geology)
Pleistocene-Era Hominins and Archaeology
article

Rectifying a substantial biostratigraphic error: There are no Hauterivian calpionellids in Busot (Alicante, Spain)

Bruno Ferré, Antonio Estévez Rubio, Bernard C. Lambert, Bruno Granier, José Miguel Andreu Rodes, Joachim Blau, Eric Monteil, Stéphane Reboulet, Aurélien Virgone, Mohamed Benzaggagh, Alfonso Marini, Éric Böker
article en

Abstract

Earlier misidentifications of ammonites from Busot (SE Spain) led to two incorrect hypotheses regarding calpionellids, which are today attributed to the Calpionellopsis Zone (D) of the upper Berriasian. The first hypothesis suggested that some calpionellid species survived into Hauterivian times, while the second hypothesis proposed that these calpionellids were reworked into Hauterivian strata. However, the revision of the ammonitic material collected in 1993-1994, along with the study of new material collected in 2024, suggests a late Berriasian age, as the ammonite assemblages likely correspond to the Fauriella boissieri and Tirnovella alpillensis Standard Ammonites zones. Nannofossil assemblages and the presence of Octahedronoides tethysianus further support this dating. This reassessment calls for a reexamination of claims regarding the occurrence of calpionellids in strata younger than the Valanginian in the literature.

Carnets de géologie (Notebooks on geology)Vol. 25(2)
Université Claude Bernard Lyon 1 (FR), École Normale Supérieure de Lyon (FR), Centre National de la Recherche Scientifique (FR), Laboratoire de Géologie de Lyon : Terre, Planètes et Environnement (FR), Université Jean Monnet (FR)
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Pleistocene-Era Hominins and Archaeology
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Rectifying a substantial biostratigraphic error: There are no Hauterivian calpionellids in Busot (Alicante, Spain) — Bruno Ferré, Antonio Estévez Rubio, et al. · Carnets de géologie (Notebooks on geology) (2024) | TGRS Research Map | TGRS