ABSTRACT
The Galericinae are a group of Erinaceidae that are currently distributed in Southeast and Eastern Asia. Although galericines have an Asian origin, their fossil record in this region is scarce, which greatly limits the knowledge of the evolutionary history of this group. We describe here the first fossils of Eulipotyphla from the middle Miocene (13.4–13.2 Ma) of the Mae Moh Basin of northern Thailand, and assign the material to three taxa of Erinaceidae attributable to the Galericinae (Galerix rutlandae, Lantanotherium anthrace, sp. nov., and Lantanotherium sp.). The Mae Moh erinaceids present a Lantanotherium-Galerix association that is uncommon in the Miocene of Asia. Galerix rutlandae is a species formerly described in the Siwaliks of Pakistan and India, which reaffirms the strong affinities during the middle Miocene between the mammalian faunas of Southeast and Southern Asia. The discovery of two species of Lantanotherium in Mae Moh provides additional knowledge about the evolution in Asia of this widespread Miocene genus that had never been recorded in Southeast Asia. The presence of three Galericinae in Mae Moh Basin reinforces the hypothesis of a mainly closed and wet environment during the deposition of the K and Q lignite layers.
http://zoobank.org/urn:lsid:zoobank.org:pub:BDE7F01C-360C-4D4B-988C-01633F1AB722
ACKNOWLEDGMENTS
We thank the EGAT authorities for access to the mine of Mae Moh and scientific assistance, M. Rugbumrung (Department of Mineral Resources, Bangkok, Thailand) for field work and preparation, K. Suraprasit (Chulalongkorn University, Thailand) for field work, A. Mazurier (Platform PLATINA, IC2MP, University of Poitiers) for CT-scan acquisitions, X. Valentin (PALEVOPRIM, University of Poitiers) for preparation, S. Passot (University of Lyon 1, France) for providing bibliographic resources, E. Béré (ImageUP, University of Poitiers) for SEM imaging, E. Robert (University of Lyon 1) and S. Jiquel (ISEM, University of Montpellier, France) for giving access to comparative material. We wish to express our deep gratitude to M. Furió and an anonymous reviewer who greatly improved the manuscript. This work has been supported by the Department of Mineral Resources (Thailand), the ANR-05-BLAN-0235, the ANR-09-BLAN-0238-02-EVAH, the Fyssen foundation (grant to O.C.) and the UMR 7262 PALEVOPRIM (CNRS and University of Poitiers, France).
Correction Statement
This article was originally published with errors, which have now been corrected in the online version. Please see Correction (https://doi.org/10.1080/02724634.2020.1851510)