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Caviomorph rodents from the Pampean region (Argentina) in the historical Santiago Roth Collection in Switzerland


Here I reviewed the Pleistocene caviomorphs collected by Santiago Roth (collection from Catalog No. 5) and housed at the paleontological collection of the Paläontologisches Institut und Museum, Universität Zürich, Zurich (Switzerland). The fossils were found in Pleistocene strata from Buenos Aires and Santa Fé provinces (Argentina) during the late nineteenth century. The material includes craniomandibular remains assigned to Lagostomus maximus (Chinchilloidea: Chinchillidae), craniomandibular and postcranial (thoracic and sacral vertebra, left scapula, left femur, and right tibia) bones identified as Dolichotis sp. (Cavioidea: Caviidae), and a fragmented hemimandible and isolated tooth of Myocastor sp. (Octodontoidea: Echimyidae). Other rodent specimens from this collection (Ctenomys sp. and Cavia sp.) are possibly sub-recent materials.


En este trabajo se estudian los caviomorfos del Pleistoceno colectados por Santiago Roth (colección del Catálogo Nro. 5) y conservados en la colección paleontológica del Paläontologisches Institut und Museum, Universität Zürich, Zurich (Switzerland). Los fósiles fueron recuperados de niveles del Pleistoceno de las provincias de Buenos Aires y Santa Fé (Argentina) hacia fines del siglo 19. Los materiales incluyen restos craniomandibulares asignados a Lagostomus maximus (Chinchilloidea: Chinchillidae), elementos craniomandibulares y postcraneanos (vértebras torácicas y sacras, escápula izquierda, femúr izquierdo y tibia derecha), identificados como Dolichotis sp. (Cavioidea: Caviidae), y un fragmento de una hemimandíbula y un diente aislado de Myocastor sp. (Octodontoidea: Echimyidae). Otros roedores de esta colección (Ctenomys sp. y Cavia sp.) posiblemente son materiales subrecientes.


The evolutionary history of the South American rodents—Caviomorpha—in deep time has been revealed through interpretations from the fossil record (Vucetich et al., 2015). These curious mammals have evolved on this continent probably since the Middle Eocene (Antoine et al., 2012; but see Campbell et al., 2021), and today they represent a significant part of the local endemic diversity of mammals, with almost 250 species (Patton et al., 2015). The high diversification of these rodents, associated with ecomorphological adaptations, promoted the colonization of most environments likely inhabited in this land mass (Patton et al., 2015; Upham & Patterson, 2015).

The diversity of extant and extinct crown Caviomorpha is included in four major clades: Erethizontoidea, Cavioidea, Chinchilloidea, and Octodontoidea (D’Elia et al., 2019; Fabre et al., 2015; Upham & Patterson, 2015). Fossils of caviomorphs indicate that these groups were already split during the Paleogene. At the same time, some enigmatic taxa are not included in such groups and probably represent extinct stem lineages (see Frailey & Campbell, 2004; Antoine et al., 2012; Bertrand et al., 2012; Vucetich et al., 2015; Boivin et al., 2016, 2017, 2018, 2019; Arnal et al., 2019, 2022). Neogene was an interval of time of great importance in the diversification of caviomorphs, evidenced by the disparity in body sizes that marked the evolution of several groups (Ferreira et al., 2020; Rinderknecht & Blanco, 2008; Sánchez-Villagra et al., 2003). Several groups became extinct in this continent during the Late Miocene and Pliocene, possibly associated with drastic environmental and biotic changes (Vucetich et al., 1999, 2015). In addition, during the Pliocene the fossil record is marked by the appearance of several fossils assigned to extant genera (e.g., Candela & Boinini, 2018; Madozzo-Jaén et al., 2021). Subsequently, during Pleistocene times, a significant part of the current caviomorph diversity was already established, at least at the generic level. However, some genera and species became extinct (some closely related to extant forms), and other taxa had a geographic distribution different from current biogeographic patterns (e.g., Tonni, 1981; Vucetich & Verzi, 1999, 2002; Vucetich et al., 1997, 1999, 2015; Ubilla & Rinderknecht, 2001, 2014, 2016; Ubilla et al., 2008; Kerber et al., 2011a, 2011b, 2014, 2016, 2020; Mayer et al., 2016; Kerber, 2017; Vezzozi & Kerber, 2017; Eduardo et al., 2018; Gomes et al., 2019).

Fossils from the Pampean region of Argentina (including rodents) have been fundamental for understanding the Pleistocene biota of South America. The Swiss/Argentinean paleontologist Santiago Roth (1850–1924) was one of the main contributors to the rapid increase of knowledge on these fossils during the late 1800s and early 1900s (Machon, 1925; Weigelt, 1951; Giacchino & Gurovich, 2001; Sánchez-Villagra et al., 2023). Here I reviewed the fossils of caviomorph rodents collected by Roth and housed at the Paläontologisches Institut und Museum, Universität Zürich, Zurich (Switzerland) (collection nº 5) (Roth, 1889).

Material and methods

Collection and provenance

The analyzed specimens were collected from Pleistocene strata in the Buenos Aires and Santa Fé provinces (Argentina) (see below). They are housed at the paleontological collection of the Paläontologisches Institut und Museum, Universität Zürich, Zurich (Switzerland). The specimens, originally numbered in Roth (1889), have recently been assigned new collection numbers with the acronym PIMUZ A/V. The stratigraphic provenance of the specimens is imprecise. Roth (1889) identified the strata as “Pampéen inférieur, Moyen, and Supérieur”, which would be rougly equivalent to the Early, Middle, and Upper Pleistocene (Cione & Tonni, 1999). See Voglino et al. (2023) for further details.

Nomenclature and measurements

For cranial anatomy, I employed the set of terms compiled by Kerber et al. (2019a) from several sources (e.g., Moore, 1981; Novacek, 1985, Wahlert, 1985; Wilson & Sánchez-Villagra, 2009; Nasif & Abdala, 2015). Description of the auditory region follows the recent study of the caviomorph ear by Arnaudo et al. (2020), who compiled anatomical terms from different contributions (i.e., Wible et al., 2005, Wible, 2010), and Wible and Shelley (2020). For the dentary and lower cheek teeth of the caviids, I followed Pérez (2010). Postcranial anatomy was based on Candela and Picasso (2008) and references therein. Regarding terms of direction, I followed the recommendations of Nomina Anatomica Veterinaria (NAV, 2017): rostral, caudal, dorsal, and ventral for head structures. Measurements were taken with a digital caliper, following Kerber et al., (2019b) for the chinchillid cheek teeth, and Candela and Picasso (2008) for postcranial bones.

Institutional abbreviations. MACN-A, paleontological collection (Ameghino Collection) of the Museo Argentino de Ciencias Naturales Bernardino Rivadavia, Buenos Aires, Argentina; PIMUZ/AV, Paläontologisches Institut und Museum, Universität Zürich, Zurich, Switzerland.

Systematic paleontology

Mammalia Linnaeus, 1758.

Rodentia Bowdich, 1821.

Hystricognathi Tullberg, 1899.

Chinchilloidea Kraglievich, 1940.

Chinchillidae Bennet, 1833.

Lagostomus Brookes, 1828.

Lagostomus maximus (Desmarest, 1817).

Referred specimens. PIMUZ A/V 4147, cranium and mandible, preserving the upper and lower cheek teeth series (Catalog No. 5, specimen 253); PIMUZ A/V 4235a, right dentary with cheek teeth (Catalog No. 5, specimen 254); PIMUZ A/V 4235b, right dentary with cheek teeth (Catalog No. 5, specimen 255); PIMUZ A/V 4202, fragmented left hemimandible with cheek teeth (Catalog No. 5, specimen 255).

Provenance. PIMUZ A/V 4147, Arroyo Pergamino, Buenos Aires, Argentina (Pampéen Supérieur, Roth, 1889); PIMUZ A/V 4235 a and b, Barranca Villa Constitución, Santa Fé, Argentina (Pampéen Moyen, Roth, 1889); PIMUZ A/V 4202, Barranca Villa Constitución, Santa Fé, Buenos Aires, Argentina (Pampéen Moyen, Roth, 1889).

General description. Cranium. The dorsal portion of the cranium is quite damaged (Fig. 1A1). The rostrodorsal region of both premaxillae is not preserved, and the nasals and zygomatic arches are missing (Fig. 1A1–A4). There are frontal fragments in which the suture between both bones (interfrontal) and the frontoparietal suture are discernible (Fig. 1A1). This latter is interdigitated and laterally oriented. Parietal bones are cracked, and it is not possible to describe them. The specimen conserves a portion of the right squamosal, forming the caudodorsal limit of the orbit (Fig. 1A4).

Fig. 1
figure 1

Cranial and mandibular remains of Lagostomus maximus (A PIMUZ A/V 4147). A1A4 cranium in dorsal (A1), ventral (A2), right lateral (A3), and left lateral (A4) views. A5 upper cheek teeth series, in occlusal view. A6A7 mandibular remains, in occlusal and lateral views. A8 detail of the right cheek teeth series. Abbreviations: ch, choana (or mesopterygoid fossa); cp, coronoid process; fps, frontoparietal suture; Fr, frontal; g, groove; I, upper incisor; ifo, incisive foramen; ifs, interfrontal suture; ipf, interpremaxillary foramen; nmpi, notch for the insertion of the muscle masseter medialis pars infraorbitalis; Mx, maxilla; M1–M3, first to third upper molars; m1-m3, first to third lower molars; Pa, parietal; Pl, palatine; pms, premaxillo-maxillary suture; Pmx, premaxilla; P4, upper fourth premolar; p4, lower fourth premolar; Sq, squamosal; rfm, rostral masseteric fossa; vrz, ventral zygomatic root

In the rostral region of the cranium, the diastema is long (Table 1), and its ventral surface is concave. However, the concavity is not accentuated (Fig. 1A2–A4). The premaxilla is one of the best preserved cranial bones. On its lateral face is a well-marked rostral masseteric fossa, which is deeper in its rostral region (Fig. 1A4). Dorsally, this fossa is delimited by a pronounced rostral masseteric crest. This crest is slightly curved and is rostroventrally oriented. Ventrally, in the rostral region of the diastema, between both premaxillae, there is a lenticular, rostrocaudally oriented, interpremaxillary foramen (Fig. 1A2). Caudally to this foramen is a wide incisive foramen. This foramen is oval in outline but laterally compressed. The premaxillo-maxillary suture crosses the foramen at its middle portion (Fig. 1A2). Lateral to the caudalmost region of the foramen, there is a shallow fossa on the maxilla’s ventral surface.

Table 1 Measurements (in mm) of the fossils of Lagostomus maximus

On the lateral face of the maxilla, the ventral zygomatic root is at the level of the P4-M1. It is broken at its base (Fig. 1A2). Dorsally to this structure, there is a groove delimited laterally by a thin lamina (Fig. 1A4).

The palatal region, composed of the palatal processes of the maxilla and palatine, is concave (Fig. 1A2). This region preserves both dental series (see below), which are caudally divergent, forming an angle of ~ 26º concerning the sagittal plane. Rostrally, lateral to the suture between both maxillae, there is a rostrocaudally oriented palatal sulcus (Fig. 1A2). On the caudal region of the palate, the specimen preserves part of the palatines (Fig. 1A2), and the maxillo-palatine suture can be partially observed.

MandiblePIMUZ A/V 4147 and PIMUZ A/V 4235 a and b preserve the rostral portion of the dentary bodies, missing the region caudal to the m3 (Fig. 1A6–A7, 2A1–B2). At the same time, PIMUZ A/V 4202 is more complete, but its surface is damaged (Fig. 2C1–C2). On the right dentary of PIMUZ A/V 4147, which is better preserved, the notch for the insertion of the muscle masseter medialis pars infraorbitalis is placed at the level of the m1-m2 (Fig. 1A6). The base of the coronoid process is lateral to the distal region of the m3 (Fig. 1A6). Ventrally to the coronoid process is the rostralmost region of the masseteric fossa and a portion of the horizontal crest delimiting it laterally.

Fig. 2
figure 2

Mandibular remains and lower teeth of Lagostomus maximus (A PIMUZ A/V 4235a, B PIMUZ A/V 4235b, C PIMUZ A/V 4202). A1A2 right hemimandible, in lateral and occlusal views. B1B2 right hemimandible, in lateral and occlusal. C1C2 left hemimandible, in lateral and occlusal views. Abbreviations: I, lower incisor; nmpi, notch for the insertion of the muscle masseter medialis pars infraorbitalis; m1-m3, first to third lower molars; p4, fourth lower premolar

Teeth. In PIMUZ A/V 4147, the upper incisors are complete (Fig. 1A1–A4). They are proodont and have a subtriangular section. The enamel covers the labial surface, which is flat and marked by fine longitudinal striations. The distal corner of the incisor is curved, while the mesial forms a right border. The lower ones are broken, remaining only their base.

The cheek teeth (Table 1) of the analyzed specimens are euhypsodont (sensu Mones, 1982). The upper series of PIMUZ A/V 4147 preserves the P4–M2 series (Fig. 1A5). The P4, M1, and M2 are morphologically similar to each other. They comprise two oblique laminae separated by a very thin lingual flexus. The angle of the tooth laminae concerning the sagittal plane is 48.8º. The mesial enamel layer that surrounds each lamina is thicker than the distal. Only the first lamina is preserved in both teeth from the M3.

PIMUZ A/V 4147 preserves the p4–m3 series (Table 1) (Fig. 1A6–A8), better preserved on the right side. PIMUZ A/V 4235a preserves the p4–m3 series (Table 1) (Fig. 2A), except for the broken first lophid of the p4. In PIMUZ A/V 4235b, the m1 is broken ( Fig. 2B). The lower cheek teeth are bilophododont and a labial flexid separates the laminae. The distal enamel layer is thicker than the mesial. The angle of the laminae (following Rasia & Candela, 2013) is 25º. PIMUZ A/V 4202 conserves the p4–m3 series (Fig. 2C). However, only the second lophid of the left p4 and the m1 and m2 have the occlusal surfaces preserved.

Fig. 3
figure 3

Cranial and mandibular remains of Dolichotis sp. (A PIMUZ/AV 4131; B PIMUZ/AV 4194). A1A6 rostral region of the cranium, in dorsal (A1), ventral (A2), right lateral (A3), left lateral (A4), and caudal (A5) views. A6, occipital region of the cranium, in caudal view. A7A9 right ear region, in lateral (A7), medial (A8), and rostral (A9) views. B1B3 right dentary, in lateral (B1), medial (B2), and occlusal (B3) views (with the cheek teeth series in detail). Abbreviations: aa, anterior apex; al, anterior lobe; ap, anterior projection; ch, choana; cp, crista petrosa; crp, cribriform plate; cs, cerebellar surface; csq, crista squamosa; cts, cheek teeth alveolar series (P4-M3); eam, external acoustic meatus; ef, ethmoidal fossa; Ex, exoccipital; Fr, frontal; I, upper incisor; ias, incisive alveolar sheath; if, interprismatic furrow; ifo, incisive foramen; hc, horizontal crest; hy, hypoflexid; La, lacrimal; laf, lacrimal foramen; lp, lacrimal process; Na, nasal; nfs, nasofrontal suture; me, mastoid exposure; nmpi, notch for the insertion of the muscle masseter medialis pars infraorbitalis; Mx, maxilla; saf, subarcuate fossa; sf, stylomastoid foramen; sp, styliform process; oc, occipital condyle; pa, posterior apex; pfc, prefacial commissure; pl, posterior lobe; pms, premaxillo-maxillary suture; Pmx, premaxilla; pp, paroccipital process; ps, palatal sulcus; Sq, squamosal; tb, tympanic bulla (ectotympanic); vzr, ventral zygomatic root

Remarks. Lagostomus maximus, the vizcacha, is a chichillid rodent that inhabits open areas in central, north, and northwest Argentina, western Paraguay, and southern Bolivia (Jackson et al., 1996; Llanos & Crespo, 1952; Spotorno & Patton, 2015). This taxon is also present in the Pleistocene fossil record of Argentina, including some places that they do not inhabit today, such as Uruguay and southern Brazil (e.g., Tonni & Fidalgo, 1982; Prado et al., 1987; Tonni et al., 1988; Gómez et al., 1999; Sarrat, 2009; Cruz et al., 2009; Kerber et al., 2011a; Ubilla & Rinderknecht, 2016). According to the comprehensive review of the Pleistocene fossil record of Lagostomus by Ubilla and Rinderknecht (2016), the species L. maximus is the only confidently valid taxon (however, according to Rasia, 2021, L. incisus is recorded in the Raigón Formation, at levels that could be of Pleistocene age). The material reported here is assigned to the L. maximus based on the presence of bilaminar and euhypsodont cheek teeth, and angle of the lamina of the upper cheek teeth concerning the sagittal plane compatible with the species (Rasia & Candela, 2013, 2017a, 2007b; Ubilla & Rinderknecht, 2016; Rasia et al., 2020; Rasia, 2021).

Cavioidea (Fischer, 1817) sensu Kraglievich 1930

Caviidae (Fischer, 1817) sensu Waterhouse 1839

Dolichotinae Pocock, 1922

Dolichotis Desmarest, 1820

Dolichotis sp.

Referred specimens. PIMUZ/AV 4131, cranium without teeth and postcranial remains (thoracic and sacral vertebra, left scapula, left femur, and right tibia) (Catalog No. 5, specimen 252); PIMUZ/AV 4194, right dentary with p4–m2 (Catalog No. 5, specimen 257).

Provenance. PIMUZ/AV 4131, San Nicolas, Buenos Aires, Argentina (Pampéen Moyen, Roth, 1889); PIMUZ/AV 4194, Arroyo Pergamino, Buenos Aires, Argentina (Pampéen Supérieur, Roth, 1889).

General description. Cranium. The rostral half of the cranium of PIMUZ/AV 4131 is preserved (Fig. 3A1–A9; Table 2). The region caudal to the palate is missing, but isolated left and right ears, and a portion of the occiput are preserved.

Table 2 Measurements (in mm) of the fossils of Dolichotis sp. (femur dimensions taken according to Candela & Picasso, 2008)

PIMUZ/AV 4131 shows a narrow rostrum with a long diastema, larger than the upper dental series (Table 2) (Fig. 3A2–A4). The lateral face of the rostrum is damaged (Fig. 3A3–A4). On the right side of the rostrum, there is a fragment of the caudalmost region of the premaxilla, contacting the frontal (Fig. 3A1). The rostral part of the nasal is transversely curved, and its caudal end has a flat surface. Its extension is uniform in width except at its rostralmost point, in which it tapers to form the nasal process. The nasal suture is straight and rostrocaudally elongated (Fig. 3A1). On the ventral region of the rostrum, there is a long incisive foramen (possibly confluent with the interpremaxillary foramen). It is narrow and lenticular in shape. The premaxillo-maxillary suture crosses the foramen transversely at is caudal portion (Fig. 3A2).

On the lateral side of the maxilla, the base of the ventral zygomatic root is at the level of the P4–M1 (Fig. 3A2–A4). This root is laterocaudally oriented. On the dorsal face of the ventral zygomatic root, there is a groove limited laterally by a ridge.

The palatal region is triangular, and the dental series are divergent caudally (Fig. 3A2). The maxillo-palatine suture is visible parallel to the dental series. The palatine forms the caudal end of the palatal region and the rostral edge of the choana or mesopterygoid fossa. This one is V-shaped, and its rostralmost point is at the level of the M2 (Fig. 3A2).

The orbital region is wide. Medially, this region is formed by the frontal, ventrally by the maxilla, and the lacrimal forms its rostrolateral edge. The lacrimal is well preserved on both sides of the cranium (Fig. 3A3–A5). It displays a well-developed lacrimal process that is laterocaudally oriented. The lacrimal foramen is on the caudal face of this process (Fig. 3A5). The frontal is wide and flat and forms the roof of the orbital region. The suture between the frontals is artificially opened by the taphonomic processes. A triangular frontal projection penetrates between the nasal and premaxilla on its anteriormost region.

The ethmoidal fossae of PIMUZ/AV 4131 for the olfactory bulbs are visible in the caudal aspect of the preserved portion of the cranium (Fig. 3A5). They have the shape of an inverted right triangle. The dorsal and lateral limits of these fossae are formed by the frontal, and rostrally they are enclosed by the cribriform plate.

Both tympanic bullae (ectotympanic) of PIMUZ/AV 4131 are preserved (Fig. 3A2, A7–A9). The bulla is rounded and presents an external acoustic meatus surrounded by a bony tube laterodorsally oriented (Fig. 3A7). The stylomastoid foramen is placed caudoventrally to the external acoustic meatus but is filled by matrix. The rostralmost region of the styliform process of the ectotympanic is broken, and its tip is missing (Fig. 3A8). Caudally, the styliform process is continuous, with a curved crest that marks the limit between the mastoid exposure of the petrosal and the ectotympanic bulla.

Rostrally, the cerebellar surface of the petrosal is smooth, and there is a dorsoventrally tenuous ridge at the middle line of this surface (Fig. 3A9). In medial view, the subarcuate fossa is at the dorsal level of the mastoid exposure of the petrosal (Fig. 3A8). Most of it is filled by the sedimentary matrix. Caudally, it is delimited by the crista squamosa. Laterally, the fossa is delimited by a marked crista petrosa lateromedially oriented that extends from the caudalmost region of the subarcuate fossa, almost reaching the area of the styliform process of the ectotympanic (Fig. 3A8). This crest delimits the cerebellar surface medially. Rostrally to the subarcuate fossa and medially to the crista petrosa, the prefacial commissure is wide. The region of the internal acoustic meatus is damaged by an artificial hole (probably made for inserting a support) (Fig. 3A8).

The left bulla is associated with a fragment of the squamosal and with a part of the occiput preserving part of the exoccipital (Fig. 3A7). There is a thin paroccipital process that extends ventrally, surpassing the ventral most limit of the bulla. However, its tip is broken.

Dentary. PIMUZ/AV 4194 preserves the rostral region of the dentary (Fig. 3B1–B3; Table 2). The portion caudal to the m2 is missing. Laterally, this dentary shows a strong horizontal crest, and its rostralmost point is at the level between p4 and m1 (Fig. 3B1). Medially, the incisive alveolar sheath forms a protuberance on the surface of the dentary that extends to the posterior lobe of the m1 (Fig. 3B2).

Teeth. Only the base of the incisors are preserved in PIMUZ/AV 4131 (Fig. 3A2–A3). Their mesial surface is flat, but the distal corner is rounded. Cheek teeth are not preserved, but the alveolar outline indicates the presence of P4–M2 formed by two lobes and the M3 with two lobes plus a posterior projection (Fig. 3A2).

Concerning the lower teeth, PIMUZ/AV 4194 preserves the p4–m2 (Fig. 3B3). They are euhypsodont, constituted of two main labially connected lobes and lanceolate lingual tips. The p4 shows the two main lobes (anterior and posterior) plus an anterior projection. This anterior projection is lingually rounded and separated from the anterior lobe by the interprismatic furrow (Fig. 3B3). The anterior and posterior lobes are transversely oriented. The anterior lobe is linguolabially shorter than the posterior. The hypoflexid, which separates both lobes, almost crosses the occlusal surface of the tooth. The labial side of the posterior lobe is slightly rounded. The m1 and m2 are similar. They are composed of two lobes with lanceolate lingual tips (anterior and posterior apexes, sensu Pérez, 2010) connected by a thin isthmus. Their apexes are slightly distally oriented compared to the lingual ones of the p4, which are transverse. The hypoflexid almost crosses the occlusal surface. Hence, both lobes are connected only by a thin and short isthmus. On the labial face, the lobes have a rounded outline and are separated by a shallow furrow (Fig. 3B3).

Postcranial skeleton. PIMUZ/AV 4131 preserves a thoracic vertebra and a sequence of three sacral vertebrae (Fig. 4A1–A5). The thoracic vertebra is almost complete, missing only the tip of the neural spine (Fig. 4A1–A3).

Fig. 4
figure 4

Postcranial remains of Dolichotis sp. (A PIMUZ/AV 4131). A1A3 thoracic vertebra, in cranial (A1), caudal (A2), and lateral (A3) views. A4A5 sacral vertebrae, in left lateral (A4) and right lateral (A5) views. A6-A7 left scapula in lateral and distal views. A8A11 left femur, in cranial (A8), caudal (A9), medial (A10), and distal (A11) views. A12-A14 right tibia, in cranial (A12), caudal (A13), and proximal (A14) views. Abbreviations: ce, centrum; cp, coracoid process; di, diaphysis; gc, gluteal crest; gf, glenoid fossa; gt, great trochanter; he, femoral head; ic, intertrochanteric crest; if, intertrochanteric fossa; iff, infraspinous fossa; it, intercondilar tuberosities; lc, lateral condyle; lt, lesser trochanter; ltc, lateral tibial condyle; mc, medial condyle; nc, neural canal; ne, neck; ns, neural spine; mtc, medial tibial condyle; pg, patellar groove; poz, postzygapophysis; prz, prezygapophysis; suf, supraspinous fossa; tp, transverse process; tt, tibial tubercle

The scapula of PIMUZ/AV 4131 does not preserve most of the scapular blade (Fig. 4A6–A7; Table 2). The coracoid process is short, and it is rostromedially oriented. A portion of the spine is preserved, observed in the external (or lateral) view. Caudally to the spine, PIMUZ/AV 4131 preserves part of the infraspinous fossa, which forms a depression on the scapular blade surface, distinct from the supraspinous fossa, in which there is no depression (Fig. 4A6). The glenoid fossa is shallow and has a pyriform outline, with a narrower region cranially (Fig. 4 A7).

The femur of PIMUZ/AV 4131 is complete (Fig. 4A8–A11; Table 2). In the proximal region of the femur, the femoral head is globose (Fig. 4 A8–A10). The fovea capitis is located on the mediocaudal region of the femoral head. The great trochanter is well-developed and surpasses the femoral head proximally. It is slightly laterally oriented. On its lateral side, there is a crest (gluteal crest) protruding laterally (Fig. 4A8–A9). The trochanteric fossa is deep. The lesser trochanter forms a rounded tuberosity that is mediocaudally oriented but is not visible in cranial view (Fig. 4A8). The intertrochanteric crest limits the trochanteric fossa caudally and is connected to the lesser trochanter (Fig. 4A9). No third trochanter is present. The diaphysis is long, gracile, and shows a slight variation in diameter in its extension (Fig. 4A8–A10). It is predominantly straight but has a slight craniocaudal curvature (Fig. 4A10). In the distal region, the patellar groove is slightly medially tilted (Fig. 4A8). Both lateral and medial condyles have approximately the same size. The craniocaudal diameter of the distal region of the femur is larger than the transverse diameter (Fig. 4A11).

The tibia only preserves its proximalmost region (Fig. 4A12–A14; Table 2). The lateral tibial condyle is broken on its lateral face. Both are transversely concave, but the lateral is more accentuated than the medial tibial condyle. The lateral condyle's tibial spine or intercondylar tuberosity projects more proximally than the medial one (Fig. 4A12–A13). In its cranial face, there is a preserved portion of the tibial tuberosity (Fig. 4A12).

Remarks. The genus Dolichotis encompasses two extant species: Dolichotis patagonum, from austral Argentina (Patagonia), and Dolichotis salinicola, from the Chaco ecoregion of Argentina, Paraguay, and Bolivia (Cabrera, 1961; Campos et al., 2001; Eisenberg & Redford, 1989; Madozzo-Jaén, 2019). The inclusion of both species in Dolichotis has been discussed over the years and recently confirmed by the comprehensive review by Madozzo-Jaén et al. (2021), who employed cladistic analysis, including morphological data of extant and extinct data and molecular data to analyze the phylogenetic relationships of dolichotines. Other four Quaternary species (D. platycephala, D. intermedia, D. major, and D. minor) were recognized by Ameghino (1889) from central Argentina. However, according to Madozzo-Jaén et al. (2021), these taxa were not studied after their original descriptions or other materials were not reported. Other Pleistocene records of Dolichotis are scarce and mainly represented by specimens not confidently identified at specific level. Most of these records of Dolichotis are from deposits in Argentina (Sarrat, 2009; Scillato-Yané et al., 1998; Tonni, 1981), but similar to the case of Lagostomus (see above), fossils out of the current distribution area are known from Uruguay and southern Brazil (Kerber et al., 2011a; Rodrigues & Ferigolo, 2004; Ubilla et al., 2004, 2009). Considering these facts, a taxonomic review of the Quaternary fossil record of Dolichotis is necessary to test if there are reliable extinct Quaternary taxa, or alternatively, if they are within the variation of the extant taxa, as in the case of Lagostomus extinct species (Ubilla & Rinderknecht, 2016).

The material described here shares morphological traits (e.g., expanded frontals, upper diastema longer than the cheek teeth series, choana reaching the M2, external acoustic meatus dorsolaterally oriented) with the species of the genus Dolichotis (Dunnum, 2015; Madozzo-Jaén, 2019; Madozzo-Jaén et al., 2021; Quintana, 1998; Ubilla & Rinderknecht, 2003), the largest non-hydrochoerine caviid. The length of the upper cheek teeth series is similar to the dimension of the specimen MACN-A 556 (Dolichotis platycephala) reported by Madozzo-Jaén et al. (2021), which is slightly larger than the average length in D. patagonum and smaller than the Pliocene D. chapalmalense. Dolichotis salinicola is the smallest species. The dimensions of the lower teeth of PIMUZ/AV 4194 are comparable with the data presented by Kerber et al. (2011a) and Madozzo-Jaén et al. (2021). They are compatible with D. patagonum (which has larger dimensions than D. salinicola), and with the extinct D. improla and D. intermedia from central Argentina. The extinct Pliocene species D. chapalmalense has cheek teeth mesiodistally longer than our material and other specimens. Only one measure of D. major is comparable with our sample (length of the m2), being slightly larger. As the analyzed sample does not preserve the upper cheek teeth series (where important traits are present) and a taxonomic review of the extinct Quaternary species is needed, the specimens are not identified at specific level.

Octodontoidea Waterhouse, 1839

Echimyidae Gray, 1825

Myocastor Kerr, 1792

Myocastor sp.

Referred specimens. PIMUZ A/V 4204a, left dentary with fragmented m1 and m2 (Catalog No. 5, specimen 256); PIMUZ A/V 4204b, right m3. The isolated tooth may not be of the same individual as the dentary because there are differences in the preservation and ontogenetic differences.

Provenance. PIMUZ A/V 4204a and b, San Pedro, Buenos Aires Province, Argentina (Pampéen Supérieur, Roth, 1889).

General description. PIMUZ A/V 4204 comprises a damaged left dentary that misses the region caudal to the m2 (Fig. 5A1–A2). The incisor (width: 6.42 mm) shows a flat surface and is still orange (Fig. 5A1). The m1 shows a broken occlusal surface, but the m2 (Mesiodistal length: 8.01, Labiolingual width: 6.50 mm) is partially preserved (Fig. 5A1–A3). Its lingual mesiolingual corner is broken. It is tetralophodont, with lophids oriented linguodistally (Fig. 5A3). The hypoflexid penetrates the tooth distolingually and almost reaches the midline of the tooth. Its tip is opposite to the posterofossetid. The lingual flexid are closed, forming fossetids. The first one is labiolingually shorter than the second and third. The m3 (PIMUZ A/V 4204b) is a protohypsodont teeth, tetralophodont, and shows the three lingual flexids open (Fig. 5B1–B2). The posteroflexid is confluent with the hypoflexid, and the posterolophid is isolated from the other lophids.

Fig. 5
figure 5

Mandibular and lower teeth remains of Myocastor sp. (A PIMUZ A/V 4204a, B PIMUZ A/V 4204b). A1A2 left hemimandible, in lateral (A1) and occlusal (A2) views. A3 left m2, in occlusal view. B1B2 right m3, in occlusal (B1) and labial (B2) views. Abbreviations: hy, hypoflexid; m2, second lower molar; pf, posterofossetid; plf, posterolophid

Remarks. The natural distribution of Myocastor encompasses Argentina, Uruguay, Bolivia, Paraguay, and Brazil (Woods et al., 1992). Fossil records of M. coypus were reported from Brazil, northern Uruguay, Argentina, and Bolivia (Ameghino, 1902; Boule & Trevenin, 1920; Ferrero & Noriega, 2009; Hoffstetter, 1963; Kerber et al., 2014; Werdelin, 1991) (see Fig. 8 in Kerber et al., 2014). During Pleistocene times, the distribution of M. coypus was much wider than its current natural distribution, reaching northeast Brazil in areas where today semiarid conditions are predominant (Kerber et al., 2014; Fig. 8). Kerber et al. (2014) considered the Early Pleistocene species from Santa Fé Myocastor columnaris erected by Rusconi (1929) as a valid taxon. On the other hand, other Pleistocene species of Myocastor (e.g., M. minor, M. priscus, and M. perditus) were considered probable synonyms of M. coypus (Kerber et al., 2014). The material reported here is similar to the extant species. However, it is quite fragmented, and for this reason, we do not identify it at specific level.


In this work, fossils of three taxa of caviomorph rodents were reviewed. These materials were collected by Santiago Roth in the late nineteenth century in Pleistocene deposits in the Pampas region of Buenos Aires and Santa Fé provinces. The specimens are assigned to Lagostomus maximus (Chinchilloidea: Chinchillidae), Dolichotis sp. (Cavioidea: Caviidae), and Myocastor sp. (Octodontoidea: Echimyidae). Other materials (Ctenomys sp.—PIMUZ A/V 4243, Catalog No. 5, specimen 263; Cavia sp.—PIMUZ A/V 4218, Catalog No. 5, specimen 263) are not reported here as they probably correspond to sub-recent material.

The fauna of Pleistocene caviomorphs from the Pampean region of Argentina is characterized by the presence of taxa adapted to open environments. This fauna, in addition to the taxa mentioned here, includes the caviids Cavia, Galea, Microcavia and Neochoerus, and the ctenomyid Ctenomys (Vucetich & Verzi, 1999). Unfortunately, the stratigraphic information of the specimens here reviewed lacks further data, limiting paleoenvironmental and paleobiogeographical considerations. Nevertheless, these fossils emerge as a source of information about the morphology of these taxa during the Pleistocene. Additionally, due to its historical context, the revisiting of the material contributes to the history of one of the most important paleontologists who worked in South America during the second half of the nineteenth century.

Availability of data and materials

All data generated or analyzed during this study are included in this published article [and its supplementary information files]. 3D models of the specimens PIMUZ/AV 4131 and PIMUZ A/V 4147 are available as supplemental material. The models (.ply) were generated with a 3D Scanner Artec Spider.


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I thank Jorge Carrillo-Briceño and Marcelo R. Sánchez-Villagra for coordinating this project and other logistical matters that made this study possible; Gabriel Aguirre Fernández and Analia Forasiepi, editors of this Special Issue; the reviewers Luciano Rasia and Carolina Madozzo-Jaén for their useful comments that improved the first draft of this manuscript.


This work was funded by the Swiss National Science Foundation grants 31003A_169395 to Marcelo R. Sánchez-Villagra, the SNF-SPIRIT, IZSTZ0 208545, entitled 'South American Pleistocene Megafaunal Diversification and Extinction—An Evaluation of the Historical Roth collection in Zurich to Marcelo R. Sánchez-Villagra and Analía Forasiepi and with the funds provided for the project SWISSCOLLNET, SCN133-ZH to Gabriel Aguirre Fernández. LK is supported by Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPQ 422568/2018-0; 309414/2019-9; 309178/2022-3) and Fundação de Amparo a Pesquisa do Rio Grande do Sul (FAPERGS 21/2551-0002030-0).

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LK designed and wrote the manuscript, photographed the specimens and produced the figures, and identified all the specimens described herein. The author read and approved the final manuscript.

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Correspondence to Leonardo Kerber.

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Kerber, L. Caviomorph rodents from the Pampean region (Argentina) in the historical Santiago Roth Collection in Switzerland. Swiss J Palaeontol 142, 8 (2023).

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