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(Squamata: Mosasauridae) from the Late Cretaceous Of C. R. Palevol 14 (2015) 483–493 Contents lists available at ScienceDirect Comptes Rendus Palevol www.sci encedirect.com General Palaeontology, Systematics and Evolution (Vertebrate Palaeontology) An halisaurine (Squamata: Mosasauridae) from the Late Cretaceous of Patagonia, with a preserved tympanic disc: Insights into the mosasaur middle ear Un halisauriné (Squamata : Mosasauridae) du Crétacé supérieur de Patagonie, à disque tympanique conservé : un aperc¸ u de l’oreille moyenne des mosasaures a,∗ b Marta S. Fernández , Marianella Talevi a CONICET - División Paleontología Vertebrados, Museo de La Plata, Paseo del Bosque s/n, 1900 La Plata, Argentina b CONICET - Instituto de Investigación en Paleobiología y Geología, Universidad Nacional de Río Negro, Isidro Lobo y Belgrano, 8332 General Roca, Río Negro, Argentina a b s t r a c t a r t i c l e i n f o Article history: Halisaurinae is a subfamily of enigmatic, small- to medium-sized mosasauroids, which Received 15 September 2014 retain a mosaic of primitive and derived features. The first record of a South American Hal- Accepted after revision 13 May 2015 isaurus with precise stratigraphic information includes a quadrate carrying a tympanic disc together with twelve vertebrae, collected in the Late Maastrichtian of Jagüel Formation Handled by Nathalie Bardet in northern Patagonia (Argentina). The preservation of a tympanic disc allows exploring and discussing the mechanisms of sound transmission in these mosasauroids. The loca- Keywords: tion of the tympanic disc resembles that one formed by the extracolumella of aquatic Halisaurus turtles and at least one extant lizard. Based on morphological comparison of the middle Patagonia ear we discuss previous hypotheses on the modification of the tympanic middle ear system Late Maastrichtian of mosasauroids for underwater hearing, in a manner similar to that observed in aquatic Cretaceous turtles. Tympanic disc Mosasauroidea © 2015 Académie des sciences. Published by Elsevier Masson SAS. All rights reserved. r é s u m é Mots clés : Les Halisaurinae représentent un clade énigmatique de mosasauroïdés de taille petite à Halisaurus moyenne. Un os carré avec un disque tympanique conservé et des vertèbres, découverts Patagonie dans la Formation Jagüel d’âge Maastrichtien supérieur, Nord de la Patagonie (Argentine), Maastrichtien supérieur représentent la première occurrence à provenance stratigraphique précise d’Halisaurus Crétacé d’Amérique du Sud. La préservation d’un disque tympanique permet d’explorer et de dis- Disque tympanique Mosasauroidea cuter le mécanisme de transmission des sons chez ces mosasauroïdés. L’emplacement du ∗ Corresponding author. E-mail addresses: [email protected] (M.S. Fernández), [email protected] (M. Talevi). http://dx.doi.org/10.1016/j.crpv.2015.05.005 1631-0683/© 2015 Académie des sciences. Published by Elsevier Masson SAS. All rights reserved. 484 M.S. Fernández, M. Talevi / C. R. Palevol 14 (2015) 483–493 disque tympanique ressemble à ceux formés par les extracolumella des tortues aquatiques. Sur la base de la comparaison morphologique, nous émettons l’hypothèse que, comme proposé précédemment, le système de l’oreille moyenne tympanique des mosasauroïdés a été modifié pour une audition subaquatique, d’une manière similaire à celle des tortues aquatiques. © 2015 Académie des sciences. Publié par Elsevier Masson SAS. Tous droits réservés. 1. Introduction or even in a more basal position as the sister taxon to Natantia (Mosasaurines + Tylosaurines + Plioplatecarpines) Mosasauroids were squamates that invaded marine (Bardet et al., 2003, 2005a; Polcyn et al., 2012). The taxo- environments during the Late Cretaceous. The earliest nomic diversity of the clade is low, not only in comparison record is from the Cenomanian of Israel (Polcyn et al., with the other clades but also in absolute terms: four gen- 1999) while the youngest records have been recovered erally accepted nominal species are known, included in from Late Maastrichtian deposits from numerous localities two or three genera according to different authors. These in both hemispheres, including Antarctica (Bardet et al., are Eonatator sternbergii (Wiman, 1920) Bardet and Pereda 2014; Fernández and Gasparini, 2012; Gallagher, 2005; Suberbiola in Bardet et al., 2005a; Halisaurus platyspondy- Kiernan, 2002; Martin, 2006; Mulder et al., 1998). The lus Marsh, 1869; Halisaurus arambourgi Bardet and Pereda fossil records indicate that they rapidly radiated within Suberbiola in Bardet et al., 2005a; and Phosphorosaurus the marine realm to achieve an almost worldwide dis- ortliebi Dollo, 1889. A fifth species – Halisaurus walkeri tribution (Polcyn and Everhart, 2008). Their extinction (Lingham-Soliar, 1998) from the Maastrichtian of Niger – has been associated with the K/Pg crisis brought about could be recognized as valid according to Lindgren and by the collapse of the marine food web driven by the Siverson (2005) and Bardet (2012). Most recently, a new Chicxulub asteroid impact (Gallagher et al., 2012; Jouve species, Eonatator coellensis, was described from Columbia et al., 2008; Polcyn et al., 2014). Disparity in cranio- on the basis of a mostly articulated skeleton (Páramo- dental anatomy and body size, among and within major Fonseca, 2013). In spite of the comparatively scarce record, clades, suggests foraging niche partitions (Polcyn et al., their geographic distribution reveals that halisaurines 2014). Advanced forms (i.e. hydropedal and hydroplevic were widely distributed, at least during the Maastrichtian. mosasauroids) rapidly radiated during the Late Turonian They have been documented from both paleogeographic reaching a cosmopolitan distribution until their extinc- provinces of the Mediterranean Tethys, from the Western tion at the K/Pg boundary (Bardet et al., 2015). Knowledge Interior seaway, Gulf Coast and East Pacific of North Amer- on mosasauroid biology has increased significantly in ica, from the Iullemmenden basin (Niger-Nigeria), and recent years. This was triggered by new findings, re- from the Kristianstad Basin in southern Sweden (Bardet, examination of historical collections, and re-analysis of 2012; Lindgren and Siverson, 2005; Lindgren, 2007). A fossils by means of new tools and/or within new concep- new halisaurine has been recently reported from the Low- tual frameworks. Growing consensus considers them as est Maastrichtian of northern Japan (Konishi et al., 2013) obligatory aquatic, viviparous, probably endotherm, and extending their spatial distribution to the northwestern fast sustained swimmers (e.g., Bell et al., 1996; Bernard Pacific. The South American records of halisaurines has et al., 2010; Caldwell and Lee, 2001; Houssaye and Bardet, been until now restricted to an isolated Late Cretaceous 2012; Konishi et al., 2012; Lindgren et al., 2009, 2010, (probably Santonian) vertebra from Peru (Caldwell and 2013). Within mosasauroids, most of the phylogenetic Bell, 1995), and to a fragmentary jaw with teeth from the analyses recovered four major clades formally named as Maastrichtian central Chile tentatively identified as a Hal- subfamilies Halisaurinae, Mosasaurinae, Plioplatecarpinae, isaurinae (Jimenez Huidobro et al., 2014). and Tylosaurinae (Bell, 1997; Bell and Polcyn, 2005; Recent field trips carried out in the area of Los Bajos de Polcyn and Bell, 2005; Polcyn et al., 2014) (Fig. 1A). Trapalcó and Santa Rosa (Río Negro province, Argentina) Palci et al. (2013) recognized two other clades, formally resulted in the recovery of mosasauroid remains from named Tethysaurinae and Yaguarasaurinae. The subfamily Late Maastrichtian rocks assigned to the Jagüel Forma- Halisaurinae represents an enigmatic and still poorly tion (Fernández et al., 2008; Gasparini et al., 2003). Among known group of small- to medium-sized mosasauroids them there are a quadrate preserving a tympanic disc, and which range from the Santonian to the Maastrichtian. 12 vertebrae of a small mosasaur. The same bed yielded Although they are consistently found as a monophyletic remains of Plioplatecarpus, Mosasaurus and Prognathodon group, formally defined by Bardet et al. (2005a) as a previously reported by Fernández et al. (2008). The main subfamily, there is no generalized agreement on the phy- purpose of this contribution is to describe this newly dis- logenetic relationships of halisaurines with the rest of the covered mosasauroid, herein indentified as Halisaurus sp., mosasauroids. Thus, some phylogenetic analyses recover and to discuss the meaning of a tympanic disc in its middle them as basal members of Plioplatecarpines (Lingham- ear. Soliar, 1988), or as the sister taxon of Mosasaurinae (Palci The finding reported herein is significant for the fol- et al., 2013) (Fig. 1B); or as the sister taxon to Rus- lowing reasons: it documents the first stratigraphically and sellosaurina (= Tylosaurinae + Plioplatecarpinae) (Bell and taxonomically precise occurrence of a halisaurine in South Polcyn, 2005; Caldwell and Palci, 2007; Makádi et al., 2012), America; it represents the southernmost occurrence of the M.S. Fernández, M. Talevi / C. R. Palevol 14 (2015) 483–493 485 Fig. 1. (Color online). Mosasauroids phylogenetic trees simplified and modified from Polcyn et al., 2014 (A) and Palci et al., 2013 (B). A. Letters above the nodes indicate the clades Halisaurinae (a), Mosasaurinae (b), Plioplatecarpinae (c), and Tylosaurinae (d). Black square, genera with extreme bony enclosure of middle ear by means of elongation, confluence and/or fusion of the suprastapedial and
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