203
Views
16
CrossRef citations to date
0
Altmetric
ARTICLES

On the Eocene cichlids from the Lumbrera Formation: additions and implications for the Neotropical ichthyofauna

, &
Pages 49-58 | Received 06 Aug 2012, Accepted 24 Feb 2013, Published online: 07 Jan 2014
 

ABSTRACT

The Lumbrera Formation is an Eocene unit cropping out in northwestern Argentina from which three cichlid species were recently described and represent the oldest Neotropical cichlid records: Proterocara argentina, Gymnogeophagus eocenicus, and Plesioheros chauliodus. The fossils come from a level interpreted as a perennial, low-energy, freshwater lake surrounded by low relief and sporadically flooded vegetated areas. Sedimentological, paleontological, and absolute U/Pb zircon dating studies suggest a lower Eocene age (∼48.6 Ma). Phylogenetic analyses place these cichlids as nested in the modern Geophagini and Heroini clades and attest to early differentiation from the basal cichlid lineages and a morphological conservatism since at least the early Eocene (∼48.6 Ma). Molecular phylogenies calibrated with the Lumbrera Formation fossils suggest that the age of cichlids may be considerably older than the minimum age provided by currently known fossils. In combination with well-established family-level phylogenetic relationships compatible with Gondwanan fragmentation, the origin of the Cichlidae likely dates back to the Cretaceous. The occurrence of Eocene cichlid fossils in the same geographical area as that of related modern lineages suggests that patterns of distribution and endemism of the Neotropical Cichlidae have an ancient history. Here we describe additional cichlid specimens from the Lumbrera assemblage and evaluate their implications for cichlid phylogeny and paleobiogeography.

ACKNOWLEDGMENTS

The authors thank O. Zuleta for collecting the material of the Lumbrera Formation presented here, and C. Del Papa (UNC) for loaning the material and for the critical reading of a previous version of this paper. This work was partially funded by CNPq (M.C.M. and L.R.M.) grants. H.L.F. was supported by a Discovery Grant from the National Sciences and Engineering Research Council of Canada. Comments by P. Chakrabarty and an anonymous reviewer helped to significantly improve the manuscript.

Handling editor: Matt Friedman

Reprints and Corporate Permissions

Please note: Selecting permissions does not provide access to the full text of the article, please see our help page How do I view content?

To request a reprint or corporate permissions for this article, please click on the relevant link below:

Academic Permissions

Please note: Selecting permissions does not provide access to the full text of the article, please see our help page How do I view content?

Obtain permissions instantly via Rightslink by clicking on the button below:

If you are unable to obtain permissions via Rightslink, please complete and submit this Permissions form. For more information, please visit our Permissions help page.