First detailed description of Hispanomys decedens (Rodentia) from the Middle Miocene of La Grive-Saint Alban (France)
Première description détaillée d’Hispanomys decedens (Rodentia) du Miocène moyen de La Grive-Saint Alban (France)
Swiss Journal of Geosciences volume 104, Article number: 345 (2011)
The material of Hispanomys decedens (Rodentia, Cricetodontinae) from La Grive-Saint Alban (France) is described in detail for the first time. H. decedens, which is one of the oldest species of the genus, shows the primitive character states that are typical of the Aragonian congeneric species, such as the mesolophs and labial cingula surrounding the upper molar valleys. The detailed examination of the teeth of H. decedens shows that this taxon is a good candidate ancestor for H. aragonensis.
Le matériel d’Hispanomys decedens (Rodentia, Cricetodontinae) de La Grive-Saint Alban (France) est décrit pour la première fois en détail. H. decedens est une des plus anciennes espèces du genre et montre des caractères primitifs typiques des espèces congénériques aragoniennes, tels que la présence de mésolophes et de cingulums labiaux sur les molaires supérieures. L’étude détaillée d’Hispanomys decedens montre que ce taxon est un bon candidat au titre d’ancêtre d’H. aragonensis.
La Grive–Saint Alban is the name used to refer to various Upper Aragonian (Middle Miocene) pits located on the territory of the municipality of Saint-Alban-de-Roche (Isère, France). These pits are constituted by fissures in Jurassic (Bajocian) oolitic limestones filled with fossiliferous siderolithic clays. Remains of Hispanomys have only been recovered from La Grive-Saint Alban L (quarry Lechartier), M (quarry Milliat), and P.B. (quarry Peyre et Beau, where a single m1 was found by P. Mein). La Grive-Saint Alban L has eight fissure-fillings numbered from L1 to L8, but the productive ones (from a palaeontological viewpoint) are only L3, L5, L5′, L6, and L7 (Mein & Ginsburg 2002).
In 1887, Depéret revealed the presence of two taxa of Cricetodon at La Grive-Saint Alban: C. medium and C. rhodanicum (Depéret, 1887a, b). In 1925, Schaub carried out a whole revision of the cricetine myomorph rodents. He included in the species C. sansaniensis Lartet, 1851 all the large-sized species of Cricetodon from Upper Aragonian localities: Sansan (Gers, France), La Grive-Saint Alban, various sites from the Swiss Molasse, and the Steinberg (=Spitzberg) in the Nördlinger Ries (Southern Germany). In this work he synonimized C. rhodanicum with C. sansaniensis because these taxa could not be differentiated neither by the morphology nor by the size (Schaub, 1925: p. 9). In addition, in the course of his revision of the material of C. sansaniensis housed in the Museum of Lyon, he noticed the presence of two morphotypes within the material of C. sansaniensis from La Grive-Saint Alban: the first, slightly larger and with less developed ectolophs corresponded to C. sansaniensis, whereas the smaller one, with better developed ectolophs, revealed a different variety (Schaub, 1925: p. 13), which he named Cricetodon sansaniensis var. decedens.
Later on, this variety was raised to the species level (Schaub, 1944: p. 454; Schaub, 1947: p. 60). Mein & Freudenthal (1971: p. 19) introduced the subgenus Hispanomys for a handful of allegedly derived Cricetodon, such as C. decedens. This subgenus was elevated to the genus level by Van de Weerd (1976): p. 106 et seq.). The holotype of H. decedens, which is a left maxillary fragment with M1 and M2, is housed in the MSNL (Schaub, 1925). It seems that the original findings of H. decedens are not the fruits of the field works carried out by Depéret in the mid-nineteenth century, but most likely of those carried out shortly later by Gaillard, which were taken up by Ennouchi in the beginning of the twentieth century. It is believed that Ennouchi worked in the “Carrière Lechartier” (called at that time “Carrière Chemin”) at the fissures L4, L5, L5′, and L7 (Ennouchi, 1930). The remains of H. decedens are supposedly from a now empty fissure, which is located between the fissure L5 and L7 and that is called L5′.
Although H. decedens from La Grive-Saint Alban has been mainly found in the fissure-filling L5′, it has also been recorded in fissures L5, L7, as well as in La Grive-Saint Alban M (Mein and Ginsburg 2002). Additional material of this species has been mentioned by Alba et al. (2006) and Casanovas-Vilar (2007) from various MN7/8 sites of the Can Mata series (Barcelona, Spain).
The other species of Hispanomys found in La Grive-Saint Alban is H. bijugatus, which has been recorded from fissures L3 and L5 and has been described in detail in López-Antoñanzas and Mein (2009).
Hispanomys decedens is to date the less-known species of Hispanomys. Actually, no complete description or photographs of this important material have been made available so far. Therefore, the aim of the present work is to offer a detailed description of this taxon, which has been neglected until now.
Materials and methods
The systematic study presented here is based on the examination of original specimens of the MNCN, RUU, IPS, and FSL collections, and data from the literature. We examined the teeth of the following species: Hispanomys bijugatus and H. decedens from La Grive-Saint Alban (Isère, France), H. mediterraneus from the localities of Montredon (Hérault, France), Soblay (Ain, France), and Dionay (Isère), H. aguirrei from Escobosa (Soria, Spain), H. daamsi from Can Missert (Barcelona, Spain), H. dispectus from Hostalets de Pierola and Castell de Barbera (Barcelona), H. lavocati from Hostalets de Pierola, of H. aragonensis from Pedregueras 2A (Saragossa, Spain), H. nombrevillae from Molina de Aragón (Guadalajara, Spain), H. peralensis from Peralejos 4, Peralejos C, Peralejos D, Masía del Barbo 2A, and Masía del Barbo 2B (Teruel, Spain), H. moralesi from Batallones 1, Batallones 3, Batallones 5, and Batallones 10 (Madrid, Spain), H. thaleri from Can Llobateres (Barcelona), H. freudenthali from Puente Minero (Teruel), and H. adroveri from Casa del Acero (Murcia, Spain).
Measurements of the occlusal surface of the teeth (maximum length and maximum width) have been taken following the method of van de Weerd (1976) for all dental e1ements except for the second upper molars, for which the maximum length has been taken parallel to the labial side of the tooth. Measurements were obtained with a Nikon digital counter CM-6S measuring device (Table 1, Electronic Supplementary Material).
The first, second, and third lower molar are designed as m1, m2, and m3, respectively, whereas the first, second, and third upper molar are designed as M1, M2, and M3, respectively. The terminology used in the tooth descriptions follows that of Freudenthal, Hugueney, & Moissenet (1994) and López-Antoñanzas et al. (2010).
Since de Bruijn et al. (1992), the biozones MN7 and MN8 have been grouped into a single unit MN7/8 due to the impossibility to distinguish them. However, Mein and Ginsburg (2002), based on the different species of Democricetodon recorded in the different fissure-fillings of La Grive-Saint Alban, were able to differentiate them in this area. They considered La Grive-Saint Alban M and La Grive-Saint Alban L3 as reference sites for the biozones MN7 and MN8, respectively, a conclusion with which López-Antoñanzas and Mein (2009) agreed. Thus, in this work, we apply the biozonation given by Mein and Ginsburg (2002) for the fissure fillings of La Grive-Saint Alban.
Order Rodentia Bowdich, 1821
Subfamily Cricetodontinae Schaub, 1925
Genus Hispanomys Mein and Freudenthal, 1971
Type species Hispanomys aragonensis (Freudenthal, 1966)
Holotype ML-Lgr 130: left maxillary fragment with M1 and M2 (Schaub 1925: fig. 2, plate III).
Referred specimens FSL67000-FSL67003, FSL67005, FSL67006, FSL67099-FSL67101, FSL67103, FSL67105-FSL67108, FSL67118, FSL67121, FSL67122, FSL67142 (mandibular ramus with m1-m3); FSL67004, FSL67021, FSL67102, FSL67120 (mandibular ramus with m1–m2); FSL67098 (mandibular ramus with m2–m3); FSL67111 (mandibular ramus with m3); FSL67093-FSL67097, FSL67104, FSL67133 (isolated m1); FSL67047-FSL67052, FSL67060-FSL67065 (isolated m2); FSL67053-FSL67059 (isolated m3); FSL67007, FSL67009-FSL67011, FSL67046, FSL67110, FSL67113, FSL67115, FSL67116, FSL67119, FSL67135, FSL67136, FSL67138, FSL67140, FSL67143, FSL67144, FSL67146 (maxilla with M1-M3); FSL67008, FSL67109, FSL67112, FSL67114, FSL67117, FSL67123, FSL67124, FSL67126, FSL67129, FSL67134, FSL67137, FSL67139, FSL67141, FSL67145, FSL67147 (fragmentary maxilla with M1-M2); FSL67125, FSL67128 (fragmentary maxilla with M1); FSL67127 (fragmentary maxilla with M2-M3); FSL67012-FSL67017, FSL67022-FSL67045, FSL67130-FSL67132 (isolated M1); FSL67018-FSL67020, FSL67066-FSL67084 (isolated M2); FSL67085-FSL67092 (isolated M3). Measurements are given in Table 1, Electronic Supplementary Material and Fig. 4.
Type locality La Grive-Saint Alban (fissure L5′) (López-Antoñanzas and Mein 2009: fig. 1).
Age Probably MN 7 (see below).
Other localities La Grive-Saint Alban (Carrière Milliat, fissure M; Carrière Lechartier, fissure L5 and L7), Isère, France (Mein and Ginsburg 2002); Hostalets de Pierola, Barcelona, Spain (Alba et al. 2006; Casanovas Vilar 2007).
Extended diagnosis Hispanomys species of medium size with low hypsodonty; having low values of the mean LM1/mean LM3 (=1.74) and mean Lm1/mean Lm3 (=1.16) ratios (third lower and upper molars not reduced); lower molars usually lacking the cingula on the lingual valleys; with some m1 having a double metalophulid or a short mesolophid or even both; three rooted m2 with a short, but distinct, mesolophid; m3 having a long or short, but distinct, mesolophid; M1 and M2 having labial cingula surrounding their valleys and usually having a mesoloph and an enamel-coated valley; four-rooted M1 having one or two anterior cusps on the prelobe, with the anterior ectoloph well developed, but lacking the forward paracone spur and usually having prominent protostyles and entostyles; M2 with lingual anteroloph, having the anterosinus usually open, but having sometimes anterior ectoloph and forward paracone spur, less M2 than M1 with mesoloph and enamel-coated valley, and all of them having well-developed backward paracone spur and posterior ectoloph; M3 with distinct anteroloph and posteroloph and having backward paracone spur, but lacking the anterior ectoloph, the forward paracone spur, and the posterior ectoloph.
Differential diagnosis Differing from Hispanomys daamsi, H. thaleri, H. freudenthali and H. adroveri, in being smaller; differing from H. bijugatus, H. thaleri, H. moralesi, H. peralensis, H. baixasi, H. freudenthali, and H. adroveri in having strong labial cingula surrounding the valleys on the M1; differing from H. bijugatus, H. aragonensis, H. thaleri, H. moralesi, H. peralensis, H. baixasi, H. freudenthali, and H. adroveri in having strong labial cingula surrounding the valleys on the M2; differing from H. mediterraneus, H. moralesi, H. peralensis, H. freudenthali, and H. adroveri in having four-rooted M1; differing from H. dispectus, H. thaleri, H. mediterraneus, H. moralesi, H. peralensis, H. freudenthali, and H. adroveri in having incomplete ectolophs on the M1 and M2; differing from H. castelnovi, H. bijugatus, H. daamsi, H. aguirrei, H. nombrevillae, H. lavocati, H. mediterraneus, H. moralesi, H. peralensis, H. freudenthali, and H. adroveri in having an enamel-coated valley on many M1–M2; differing from H. castelnovi, H. bijugatus, H. nombrevillae, H. mediterraneus, H. moralesi, H. peralensis, H. freudenthali, and H. adroveri in having usually a mesoloph on the M1; differing from H. castelnovi, H. dispectus, H. nombrevillae, H. thaleri, H. mediterraneus, H. moralesi, H. peralensis, H. freudenthali, and H. adroveri in having the M3 less reduced; differing from H. moralesi, H. peralensis, H. freudenthali, and H. adroveri in having labial anterolophid in all m1; differing from H. castelnovi, H. daamsi, H. dispectus, H. thaleri, H. baixasi, H. aragonensis, H. moralesi, H. peralensis, H. freudenthali, and H. adroveri in having a double metalophid on some m1; differing from H. thaleri, H. nombrevillae, and H. aguirrei in having three-rooted m2; differing from H. nombrevillae, H. aguirrei, H. moralesi, H. peralensis, H. freudenthali, and H. adroveri in having the m3 less reduced.
i: The incisor enamel bears in its labial side two feeble longitudinal ridges.
m1: The outline of these teeth in occlusal view is sub-rectangular, longer than wide, with its anterior part somewhat rounded and narrower than the posterior one. The lingual anterolophid is usually lacking, but in few specimens (e.g. FSL 67005) it is present, but weak. The labial anterolophid is long and prominent and can even reach the anterior side of the protoconid, closing thereby the protosinusid. The m1 have a double metalophulid (e.g. FSL 67003, Fig. 1d) or a short mesolophid (FSL 67005, FSL 67001, Fig. 1a, c). Some teeth clearly show both structures (e.g. FSL 67002, Fig. 1b). Even when the mesolophid is lacking, there is a slight inflation at the end of the posterior arm of the protoconid. The hypolophulid is transverse. A few teeth have an ectomesolophid (FSL 67000, Fig. 2). All the specimens have a labial cingulum surrounding the sinusid. This cingulum is constituted by the junction of two ridges: the first emerging from the posterior wall of the protoconid and the second from the anterior wall of the hypoconid. It can bear an ectostylid. Some m1 also show a thin, low ridge surrounding the lingual valley. The sinusid is antero-lingually directed. The posterolophid is short and constricted behind the hypoconid; it does not reach the posterior wall of the entoconid. These teeth are two-rooted.
m2: These teeth are rectangular in shape, though they are anteriorly and posteriorly slightly rounded. They show a prominent labial anterolophid that reaches the anterolabial side of the protoconid, closing thereby the protosinusid. The metalophulid is anterolabially directed and the hypolophulid is transverse. The mesolophid is usually short and ends free. The m2 have rarely lingual cingula surrounding the valleys (e.g. FSL 67006), but all of them have strong labial cingula closing the sinusid. These cingula are constituted by two ridges; the first (which is stronger) emerging from the posterior wall of the protoconid and the second from the anterior wall of the hypoconid. The sinusid is transverse. The posterolophid is short and constricted behind the hypoconid; it does not reach the posterior side of the entoconid. The posterior root splits into two and, therefore, these teeth are three-rooted. The posterolabial root is stronger than the posterolingual one.
m3: The occlusal outline of these teeth is rounded, longer than wide, with its posterior part narrower than the anterior one. They show a long and strong labial anterolophid that connects with the anterior wall of the protoconid, closing the protosinusid. The lingual anterolophid is absent. Most of the specimens have a short mesolophid (FSL 67002, FSL 67003, Fig. 1b, d). However, 4 out of 27 have it long (e.g. FSL 67001, FSL 67005, FSL 67054, FSL 67057 Fig. 1a, c). From these, three specimens (FSL 67001, FSL 67005, FSL 67054) have the mesolophid connected to the anterior side of the entoconid. The posterosinusid and mesosinusid are open; there are no lingual cingula surrounding the valleys. The sinusid is slightly posteriorly directed; it may be partially closed by two ridges: the strongest emerges from the posterior wall of the protoconid, whereas the other one comes out from the anterior wall of the hypoconid. The posterolophid is short and does not join the posterior wall of the entoconid. These teeth are three-rooted.
M1: These teeth show a pronounced groove between the two lobes of the anterocone. Most of the specimens show either a strong cusp (even two) in the prelobe or a low anterior ridge in front of the anterocone (e.g. Fig. 3h). The anterolophule connects the lingual lobe of the anterocone with the protocone. The protosinus is closed by a large protostyle (Fig. 3d, h, i, l) or by a low and strong ridge (Fig. 3a). The protolophule is anterolabially directed. The anterior ectoloph is well developed and ends free most of the time. It can be parallel to the longitudinal axis of the tooth or postero-lingually directed. The forward paracone spur is usually absent. The long and strong backward paracone spur connects to the posterior ectoloph closing the mesosinus, but it ends free in some specimens. The backward paracone spur emerges at about the midpoint between the labial side of the tooth and the entoloph. Most of the specimens have a short or medium mesoloph. In some of them, the mesoloph connects labially to a lingual spur of the backward paracone spur that points towards the mesoloph (Fig. 3l), isolating a circular valley (called enamel-coated valley), which disappears through wear. Otherwise these structures are too short to be connected (Fig. 3h, i, k). The M1 of Hispanomys decedens have strong, low cingula surronding the labial valleys; some of which bears a mesostyle. The anteriorly directed sinus is usually partially closed by a strong entostyle or by a ridge, which emerges from the hypocone towards the posterolabial side of the protocone. Some specimens (e.g. FSL 67015, Fig. 3i, j) and FSL 67017 (Fig. 3h) show a vertical ridge emerging from the posterior wall of the protocone towards the lingual side of the tooth (a sort of vestigial entomesoloph). In the less worn specimens, it is possible to observe that both lingual and labial posterolophs are short, but distinct. These teeth are four-rooted.
M2: The outline of these teeth in occlusal view is sub-rectangular, longer than wide, with its posterior part somewhat rounded and narrower than the anterior one. They have quite developed lingual anteroloph and a small, but distinct, protosinus in the anterior margin of the teeth. The labial anteroloph is well developed. The anterosinus is usually open due to the absence of anterior ectoloph, forward paracone spur or both (e.g. Fig. 3e, g, m). However, some of the M2 have the anterior ectoloph connected to the forward paracone spur, closing the anterosinus (e.g. Fig. 3d, f). The backward paracone spur is long and strong and usually reaches the posterior ectoloph (a small anterior ridge of the metacone) and, in so doing, entirely closes the mesosinus. Nevertheless, some specimens lack the posterior ectoloph and, therefore, have a backward paracone spur that ends free (e.g. Fig. 3m) or the two crests are not connected (e.g. Fig. 3f). All teeth have the mesosinus much larger than the anterosinus and they have a cingulum surrounding the main labial valley. A lesser number of M2 than M1 shows the mesoloph. When present, it is short or of medium length; in some specimens it reaches the backward paracone spur forming an enamel-coated valley (e.g. Fig. 3m). The enamel-coated valley is formed by the connection of the mesoloph with a lingual spur emerging from the backward paracone spur. In some specimens, the mesoloph and the backward paracone spur are too short and, therefore, they are disconnected (Fig. 3e). The presence of a mesoloph on the M2 is related to the presence of a mesoloph on the M1. Every M2 that lacks the mesoloph shows a slight inflation at the beginning of the anterior arm of the hypocone (Fig. 3d, f). The backward paracone spur is long and usually posterolabially oriented; in some specimens (Fig. 3d) it emerges practically at the midpoint of the protolophule. The protolophule is slightly oblique and anterolabially directed. The sinus is nearly closed by a low ridge that emerges from the anterior side of the hypocone towards the posterior side of the protocone. These teeth show short labial and lingual posterolophs. They have four roots.
M3: The outline of these teeth in occlusal view is rounded, longer than wide, with the posterior part narrower than the anterior one. The labial anteroloph is long; the lingual one is much less developed, but distinct (except in worn specimens). The anterior ectoloph and the forward paracone spur are lacking and the anterosinus is open. A true mesoloph is lacking in all M3 of Hispanomys decedens, but some show a small inflation corresponding to this ridge (Fig. 4d). The teeth have a short, but distinct, posteroloph and a posterosinus. The well-developed backward paracone spur ends usually free due to the absence of the posterior ectoloph. The posterolabial side of the protocone generally has a strong ledge, which is directed towards the hypocone. This ledge closes the sinus partially. The sinus is directed backwards. These teeth are not reduced; actually, the value of the ratio mean LM1/mean LM3 of the teeth is very low (=1.736), one of the lowest ones obtained for any Hispanomys species known to date (López-Antoñanzas and Mein 2009). These molars are three-rooted.
In 1966, Freudenthal based on his studies of the cricetodontine material from the localities of Nombrevilla and Pedregueras 2C (Zaragoza, Spain) established two new subspecies of Cricetodon decedens in addition to C. decedens decedens: C. decedens aragonensis and C. decedens nombrevillae. Later on, Mein and Freudenthal (1971: 19) introduced the new subgenus Hispanomys and raised these subspecies to the species level.
Freudenthal’s (1966) decision of regarding the two taxa as subspecies of C. decedens was the result of the lack of information available at that time about the “typical” decedens from La Grive-Saint Alban. Actually, Freudenthal (1966) did not discard the possibility that, once the material from La Grive-Saint Alban is studied in detail, one of the two subspecies he named could turn out to be a synonym of decedens. However, he thought more likely that the Spanish subspecies were different from the French one, a conclusion that the present work supports.
The detailed study of Hispanomys decedens from La Grive-Saint Alban shows that this taxon is, in fact, very different from H. nombrevillae and, even though it seems closely related to H. aragonensis from Pedregueras, both species can be easily differentiated (see below).
The main characters usually used to establish the evolutionary stage of the Hispanomys species are: (1) the different development of the ectolophs; (2) the degree of reduction of the mesolophs and mesolophids; (3) the presence or loss of labial anterolophids; (4) the presence or loss of cingular structures; (5) the acquisition or not of extra roots; (6) the degree of reduction of the third molars; and (7) the degree of hypsodonty (van de Weerd 1976; Agustí 1981, 1982; López-Antoñanzas and Mein 2009; López-Antoñanzas et al. 2010). The most archaic morphologies of Hispanomys would be characterized by having lower molars with well-developed labial anterolophids, lingual anterolophids, lingual cingula surrounding the valleys, two-rooted m2, and unreduced m3. Besides, the most primitive upper molars would be characterized by having mesolophs, labial cingula surrounding the valleys, quite incomplete ectolophs, four-rooted M1, and unreduced M3 (van de Weerd, 1976; Agustí 1981, 1982; López-Antoñanzas and Mein 2009; López-Antoñanzas et al. 2010).
H. decedens and H. aragonensis share some primitive character states as the presence of a mesoloph forming an enamel-coated valley on the M1 and M2 and the presence of labial cingula surrounding the M1 as well as some derived ones like the absence of a mesoloph on the M3 and the splited posterior root on the m2. However, there are also differences between these species that makes H. decedens a reasonable forerunner of H. aragonensis. In the latter species, there is a trend towards the decrease in the proportion of M1 and M2 with the mesoloph and in that of M1 with either anterior cingulum or anterostyle in the prelobe. Besides, another progressive character distinguishing H. aragonensis from H. decedens is the lack of the labial cingulum surrounding the valley on M2. Therefore, H. aragonensis shows a trend to lose archaic characters so characteristic of H. decedens.
Moreover, if we compare the dental evolutionary stage of Hispanomys decedens and the Upper Aragonian and Lower Vallesian species of Hispanomys, it appears that the former shows a quite primitive morphology.
Thus, Hispanomys decedens is more primitive than H. castelnovi, H. bijugatus, H. aguirrei, H. daamsi, H. lavocati, and H. nombrevillae in having well-developed mesolophs on M1 and M2, which tend to form an enamel-coated valley. Well-developed mesolophs are also present, but in much lesser proportion, in H. thaleri (a few upper molars) and in H. aragonensis. Besides, H. decedens seems more primitive than H. castelnovi, H. bijugatus, and H. thaleri in having strong cingula surrounding the labial valleys of the first and second upper molars. Regarding the reduction of the third molars, this taxon is also quite primitive: H. decedens appears more primitive than H. castelnovi, H. dispectus, H. nombrevillae, and H. thaleri in having the M3 much less reduced (López-Antoñanzas et al., 2010: table 2). This character is shared with the other species of Hispanomys from La Grive-Saint Alban: H. bijugatus.
So far, Hispanomys includes 17 species with a stratigraphical distribution that encompasses nearly 10 my. Among them, ten taxa are known from the Upper Aragonian and Lower Vallesian: Hispanomys castelnovi, H. decedens, H. bijugatus, H. aguirrei, H. daamsi, H. dispectus, H. thaleri, H. lavocati, H. nombrevillae, and H. aragonensis.
Hispanomys decedens from La Grive-Saint Alban has most of the typically primitive dental characters of the Aragonian species of Hispanomys, such as the not reduced M3, the labial cingula surrounding the first and second molar valleys, and the presence of mesolophs on the upper molars forming an enamel-coated valley. This suggests that H. decedens is a quite primitive species with respect to the coeval congeneric taxa. In addition, the detailed study of H. decedens from La Grive-Saint Alban shows that this taxon could be an ancestor of H. aragonensis.
Université Claude Bernard, Villeurbanne, France
Instituto Catalán de Paleontología, Sabadell, Spain
Museo Nacional de Ciencias Naturales-CSIC, Madrid, Spain
Centre de Conservation et d’Etude des Collections, Lyon, France
Rijksuniversiteit Utrecht, Utrecht, The Netherlands
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J. van Dam and W. Wessels (Rijksuniversiteit Utrecht, Utrecht) kindly lent material of Hispanomys housed in their institution. L. Celià Gelabert and J. Galindo Torres (Instituto Catalán de Paleontología, Sabadell) allowed the examination of material under their care. Thanks to D. Marty (Office de la Culture de la République et Canton du Jura, Porrentruy), J. Prieto (Ludwig-Maximilians-Universität, Munich), and an anonymous reviewer for having improved this work through critical reading. Discussion with P. Peláez-Campomanes (Museo Nacional de Ciencias Naturales-CSIC, Madrid) was much appreciated. This study has been partly founded by research project CGL2008-05813-CO2-01 (MICINN, Spanish Government) conducted by J. Morales. R.L.A. is currently supported by a Ramón y Cajal research contract.
Editorial handling: Loïc Costeur & Daniel Marty.
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López-Antoñanzas, R., Mein, P. First detailed description of Hispanomys decedens (Rodentia) from the Middle Miocene of La Grive-Saint Alban (France). Swiss J Geosci 104, 345 (2011). https://doi.org/10.1007/s00015-011-0066-0
- La Grive-Saint Alban
- Mots clés
- La Grive-Saint Alban