Title
A rhinopristiform sawfish (Genus pristis) from the middle eocene (lutetian) of southern Peru and its regional implications
Other title
[Un poisson-scie rhinopristiforme (genre Pristis) de l'Éocène moyen (Lutétien) du Pérou méridional et ses implications régionales]
Date Issued
01 January 2020
Access level
open access
Resource Type
journal article
Author(s)
Collareta A.
Landini W.
Urbina-Schmitt M.
Bianucci G.
Publisher(s)
Carnets de Geologie
Abstract
Modern sawfishes Rhinopristiformes: Pristidae are circumglobally distributed in warm waters and are common in proximal marine and even freshwater habitats. The fossil record of modern pristid genera i.e., Pristis and Anoxypristis dates back to the early Eocene and is mostly represented by isolated rostral spines and oral teeth, with phosphatised rostra representing exceptional occurrences. Here, we report on a partial pristid rostrum, exhibiting several articulated rostral spines, from middle Eocene strata of the Paracas Formation Yumaque Member exposed in the southern Peruvian East Pisco Basin. This finely preserved specimen shows anatomical structures that are unlikely to leave a fossil record, e.g., the paracentral grooves that extend along the ventral surface of the rostrum. Based on the morphology of the rostral spines, this fossil sawfish is here identified as belonging to Pristis. To our knowledge, this discovery represents the geologically oldest known occurrence of Pristidae from the Pacific Coast of South America. Although the fossil record of pristids from the East Pisco Basin spans from the middle Eocene to the late Miocene, sawfishes are no longer present in the modern cool, upwelling-influenced coastal waters of southern Peru. Given the ecological preferences of the extant members of Pristis, the occurrence of this genus in the Paracas deposits suggests that middle Eocene nearshore waters in southern Peru were warmer than today. The eventual disappearance of pristids from the coastal waters off southern Peru might be interpreted as reflecting the late Cenozoic trend of strengthening of the Humboldt Current.
Start page
91
End page
105
Volume
20
Issue
5
Language
English
OCDE Knowledge area
Geología
Subjects
Scopus EID
2-s2.0-85083425900
Source
Carnets de Geologie
ISSN of the container
17652553
Sponsor(s)
This research was supported by a grant by Università di Pisa to Giovanni BIANUCCI (PRA_2017_0032). The present paper is a contribution of the "Programa de Paleontología" of the Regional Geology Department, INGEMMET, and a result of the "Convenio Específico" between the INGEMMET and the Museo de Historia Natural de la Universidad Nacional Mayor de San Marcos.
sery grounds for these highly idiosyncratic rays wan) for their valuableandthorougheditorialle),andBrianR.PRATT(UniversityofSaskatche- (SIMPFENDORFER, 2007). Present-day seagrasses support. are mostly known from tropical and subtropical This research was supported by a grant by environments; modern seagrass patches along Università di Pisa to Giovanni BIANUCCI (PRA_ the southeastern Pacific margin are limited to a 2017_0032). The present paper is a contribution few occurrences near Coquimbo, Chile (KUO, of the "Programa de Paleontología" of the Regio-mighthavebeenmorewidespreadalongthe2005,andreferencestherein),butmeadows nal Geology Department, INGEMMET, and a result
Sources of information:
Directorio de Producción Científica
Scopus
Instituto Geológico Minero y Metalúrgico