A PLIOCENE GRAY WHALE ( ESCHRICHTIUS SP.) FROM THE EASTERN NORTH ATLANTIC

The gray whale Eschrichtius robustus, the only living member of the eschrichtiid lineage, currently inhabits only the North Pacific. Interestingly, however, the holotypes of both E. robustus and the late Miocene Archaeschrichtius ruggieroi (the oldest known eschrichtiid species) come from the North Atlantic and the Mediterranean, respectively. Here we describe a partial mysticete mandible from the Pliocene (3.71–2.76 Ma) of Belgium (Eastern North Atlantic). This new fossil displays a combination of morphological features that makes it nearly identical to modern E. robustus. Nevertheless, given... Mehr ...

Verfasser: CHENG-HSIU TSAI
ALBERTO COLLARETA
MARK BOSSELAERS
Dokumenttyp: Artikel
Erscheinungsdatum: 2020
Reihe/Periodikum: Rivista Italiana di Paleontologia e Stratigrafia, Vol 126, Iss 1 (2020)
Verlag/Hrsg.: Milano University Press
Schlagwörter: Cetacea / Mysticeti / Eschrichtiidae / evolution / paleobiogeography / Lillo Formation / Belgium / North Sea / Geology / QE1-996.5 / Paleontology / QE701-760
Sprache: Englisch
Permalink: https://search.fid-benelux.de/Record/base-26582477
Datenquelle: BASE; Originalkatalog
Powered By: BASE
Link(s) : https://doi.org/10.13130/2039-4942/13040

The gray whale Eschrichtius robustus, the only living member of the eschrichtiid lineage, currently inhabits only the North Pacific. Interestingly, however, the holotypes of both E. robustus and the late Miocene Archaeschrichtius ruggieroi (the oldest known eschrichtiid species) come from the North Atlantic and the Mediterranean, respectively. Here we describe a partial mysticete mandible from the Pliocene (3.71–2.76 Ma) of Belgium (Eastern North Atlantic). This new fossil displays a combination of morphological features that makes it nearly identical to modern E. robustus. Nevertheless, given its incomplete nature, the studied specimen is here identified in open nomenclature as belonging to Eschrichtius sp. The recognition of such an early record of Eschrichtius in the North Atlantic suggests that this genus developed a circum-Northern Hemisphere distribution not later than in Pliocene times, thus complicating our understanding of its origin, evolutionary history, and palaeobiogeographic patterns.