Las especies del género Chasicotatus Scillato–Yané (Eutatini, Dasypodidae)

Gustavo Juan Scillato–Yané¹, Cecilia Mariana Krmpotic¹,*, and Graciela Irene Esteban²

¹ Consejo Nacional de Investigaciones Científicas y Técnicas. División Paleontología de Vertebrados, Museo de La Plata, Paseo del Bosque s/n, 1900, La Plata, Argentina. *E–mail: ckrmpotic_pv@fcnym.unlp.edu.ar.

² Instituto Superior de Correlación Geológica (INSUGEO), Facultad de Ciencias Naturales e Instituto Miguel Lillo, Miguel Lillo 205, 4000, San Miguel de Tucumán, Argentina.

Manuscript received: October 7, 2009. ]]> Corrected manuscript received: November 30, 2009.
Manuscript accepted: December 12, 2009.

ABSTRACT

Chasicotatus was originally described as a monotypic genus based on Chasicotatus ameghinoi Scillato–Yané, 1979, from the upper member of Arroyo Chasicó Formation (Las Barrancas Member, late Chasicoan). An additional species, Chasicotatus peiranoi , was erected by Esteban and Nasif (1996). This work presents the description of two new species previously recognized but never published by Scillato–Yané (1982), with a study and description of the osteoderm's internal structure from three of four species of the genus. On this basis, the genus is revised and expanded diagnoses are provided for the previously known taxa, so that the species are clearly differentiated by internal and external osteodermal features. The geographical distribution of the species of genus Chasicotatus supports advanced palaeoenvironmental hypotheses previously proposed by different authors.

Key words: Xenarthra, Eutatini, Chasicotatus, systematic, palaeohistology, Arroyo Chasicó Formation, Argentina.

RESUMEN

Chasicotatus fue reconocido como un género monotípico, con Chasicotatus ameghinoi Scillato–Yané, 1979, procedente del miembro superior de la Formación Arroyo Chasicó (Miembro Las Barrancas, Chasiquense tardío). Además, posteriormente fue fundada la especie Chasicotatus peiranoi por Esteban y Nasif (1996). En este trabajo se describen dos especies nuevas, previamente reconocidas pero no publicadas por Scillato–Yané (1982) y se desarrolla un estudio y descripción de la estructura interna de los osteodermos de tres de las cuatro especies del género. Sobre esta base se realiza una revisión del género y se amplían las diagnosis de los taxones previamente conocidos, quedando las especies claramente diferenciadas por caracteres externos e internos de los osteodermos. La distribución geográfica de las especies del género Chasicotatus, avala las hipótesis paleoambientales planteadas previamente por distintos autores.

Palabras clave: Xenarthra, Eutatini, Chasicotatus, sistemática, paleohistología, Formación Arroyo Chasicó, Argentina.

INTRODUCTION

The tribe Eutatini, included in the subfamily Euphractinae (Scillato–Yané, 1980, 1982; McKenna and Bell, 1997), comprises exclusively extinct taxa. This is one of the best represented dasypodid tribes in the stratigraphic units of the Cenozoic in southernmost South America, very frequently found in Argentina (Scillato–Yané, 1980; Scillato–Yané et al., 1995) and to a lesser extent in Uruguay (Mones and Francis, 1973; Mones, 1986; Perea–Negreira, 1998; Bostelmann et al., 2008), Chile (Croft et al., 2007) and Bolivia (Croft et al., 2009). In contrast, they have not been recorded in southern Brazil, even though other faunal elements typical of the Pleistocene of the Pampean Region are abundant in that area.

The eutatines had one of the most extreme southern distribution ranges among dasypodids (Stenotatus Ameghino, 1891a and Proeutatus Ameghino 1891b, south of Santa Cruz province) and they evolved the most abundant hair of any dasypodid, probably in connection with the adaptation to colder climates (Scillato–Yané et al., 1995; Carlini et al., 2005). They are recorded in since the Casamayoran (Barrancan, late Eocene) to Platan (early Holocene). At the locality Gran Barranca Sur, near Colhue–Huapi Lake (Chubut province, Argentina), the diversity and abundance of Eutatini shows a remarkable increase from the Tinguirirican (Carlini et al., 2004, 2005, 2009).

From late Miocene to early Holocene, the eutatines are represented by the following genera: Chasicotatus (Chasicoan–Huayquerian), Doellotatus Bordas, 1932 (Huayquerian–Vorohuean), Ringueletia Reig, 1958 (Huayquerian–Barrancalobian) and Eutatus Gervais, 1867 (Chapadmalalan–Platan). Eutatus has the largest geographical range in Argentina and is also the taxon most frequent found, followed by Chasicotatus. At present, the records for the tribe in Uruguay comprise the genera Eutatus, Doellotatus and Ringueletia (Mones and Francis, 1973; Perea–Negreira, 1998; Bostelmann et al., 2008).

Chasicotatus was originally recognized as a monotypic genus: Chasicotatus ameghinoi Scillato–Yané, 1979, from the upper (Las Barrancas Member) of the Arroyo Chasicó Formation (late Chasicoan). In his doctoral thesis, Scillato–Yané (1982) recognized two new species, which are only now being published as part of the present work. Later on, another species was erected for northwestern Argentina (Catamarca province), namely Chasicotatus peiranoi Esteban and Nasif, 1996, which was later recorded in the southwest of Buenos Aires province (Deschamps, 2005). Likewise, the species Chasicotatus ameghinoi was also recorded in the provinces of Catamarca (Esteban and Nasif, 1999) and La Pampa (Esteban et al., 2001, 2003; Urrutia, 2004, Urrutia et al., 2008).

This work provides a revision of the genus and the description of two new species, which were originally recognized by Scillato–Yané (1982), but not subsequently published. In addition, the morphology and the internal structure of osteoderms from three of four species of the genus Chasicotatus is studied in comparison with other Eutatini studied previously.

ABBREVIATIONS

MLP: División de Paleontología de Vertebrados, Facultad de Ciencias Naturales y Museo de La Plata, Universidad Nacional de La Plata.

UNSGH: Cátedra de Geología, Universidad Nacional de Sur, Bahía Blanca.

MATERIALS AND METHODS

Materials

Chasicotatus ameghinoi . Holotype: MLP 76–VI–12–11. Hypodigm: holotype and MLP 28–X–11–43, 28–X–11–64, 30–XII–10–13, 55–IV–28–47, 60–VI–18–67, 60–VI–18–75, 76–VI–12–19, 76–VI–12–26, 76–VI–12–27, 76–VI–12–38, 76–VI–12–58, 76–VI–12–111, 76–VI–12–136, 76–VI–12–137. Chasicotatus peiranoi . Holotype: PVL 4796. Hypodigm: the holotype and UNSGH 57. Chasicotatus powelli n. sp. Holotype: PVL 3212. Paratype: PVL 3213. Chasicotatus spinozai n. sp. Holotype: MLP 69–VIII–4–5.

Methods

Practically no endoskeletal remains are known for the genus Chasicotatus. Because of this, the species of this genus have been erected on the basis of variations in the morphological features from the caparace (of the single fairly complete specimen) and articulated or isolated osteoderms. In this work the internal structure of the osteoderms was investigated in order to conduct as thorough as possible an analysis of the previously existing taxa and one of the new species erected here.

Osteoderms were cleaned with 100 volume hydrogen peroxide as 1:10 dilution in distilled water to remove the sediment lodged in pores, foramina and cavities. They were subsequently embedded in colored polyester resin and placed in a vacuum chamber to ensure complete perfusion of the resin. Once the resin solidified, the pieces were progressively ground using a disc metallographic grinder. Digital photographs were taken every 200 μ (on average) between grinding stages. The observations were compared with the results of previous histological and palaeohistological works.

The internal structure of mobile osteoderms was only studied in C. ameghinoi because the very few complete mobile osteoderms known for C. powelli n.sp. and C. peiranoi could not be used for palaeohistological sections, and in the case of C. spinozoai n. sp., no osteoderms from that region are preserved. Fixed osteoderms of C. spinozai n. sp. were not studied because only two of these are known.

PALAEOHISTOLOGY

Internal morphology of Chasicotatus osteoderms

Palaeohistological sections were made from a mobile osteoderm belonging to Chasicotatus ameghinoi and fixed osteoderms from C. ameghinoi, C. peiranoi and C. powelli n. sp. Morphologically diverse cavities were recognized. In order to make inferences about the type of soft tissues that originally occupied these cavities, they were compared with histological sections from living individuals described in the literature (Fernández, 1931; Krmpotic et al., 2005, 2009a; Hill, 2006; Vickaryous and Hall, 2006; Ciancio et al., 2007), in an attempt to recognize homologous structures (Figure 1).

The osteoderms of Chasicotatus show three well–defined zones, in particular a very well developed middle zone (Figure 1) that seems to be typical of the Euphractinae, since it occurs in Chaetophractus villosus (Desmarest, 1804) Fitzinger, 1871 (Fernández, 1931; Krmpotic et al., 2005, 2009a) and in several eutatine genera, but not in Dasypus Linné, 1758 (Dasypodinae) (Hill, 2006; Ciancio et al., 2007). The Eutatini are hypothesized to have a more developed piliary apparatus compared with the Euphractini, as indicated by the genera Eutatus (Krmpotic et al., 2007a, 2007b, 2009a, 2009b), Ringueletia (Krmpotic et al., 2007c), Sadypus Ameghino, 1902 and Meteutatus Ameghino, 1902 (Ciancio and Carlini, 2007), Doellotatus, Stenotatus (Deseadan, late Oligocene–Colloncuran, early middle Miocene) and Chasicotatus in the present work. The greater piliary development is inferred not only from the number of superimposed hair follicles on each palaeohistological section , but also from the extension and total volume occupied by each hair follicle within the osteoderm (Figure 1).

Chasicotatus ameghinoi

The mobile osteoderms of C. ameghinoi (Figure 2) have a proportionally less developed middle zone when compared with Doellotatus chapadmalensis Bordas, 1933 (Figure 3), and are more similar to Stenotatus patagonicus (Ameghino, 1887) Scott, 1903–1905 (Figure 4). The glandular cavities are smaller than those of Doellotatus chapadmalensis, much smaller than those of Stenotatus patagonicus, never more than two per palaeohistological section and with narrow ducts (one duct per glandular cavity). The hair follicle cavities (like the glandular cavities) are located on the posterior half of the ornamented part; the cranial portion (overlapping region) has a middle zone with large cavities that contain adipose tissue, and the outer and inner zones are proportionally thicker than in Doellotatus chapadmalensis and Ringueletia simpsoni (Bordas, 1933) Reig 1958, similar to those of S. patagonicus. The fixed osteoderms of C. ameghinoi (Figure 5) have large glandular cavities, larger than those of C. peiranoi (Figure 6), but smaller than those of C. powelli n. sp. (Figure 7), never more than two per palaeohistological section; the gland ducts are narrow (one per glandular cavity). The hair follicle cavities are well developed and lodged in a zone that is thicker than the rest of the osteoderm. Analysis of its internal structure shows that this greater thickness is due to the large size of the cavities corresponding to hair follicles and to the presence of a relatively thicker outer zone (Figure 5).

Chasicotatus peiranoi

Chasicotatus powelli n. sp.

The internal structure of the fixed osteoderms shows the inner and outer zones are thinner than those of C. ameghinoi and C. peiranoi (Figure 7). The glandular cavities are large, larger than those of C. ameghinoi; they may even occupy the entire thickness of the middle zone reaching the inner zone, and possess a single duct. Up to three gland cavities are present per cross–section (unlike the condition in C. ameghinoi and C. peiranoi that have only two).

SYSTEMATIC PALEONTOLOGY

Superorder Xenarthra Cope, 1889
Order Cingulata Illiger, 1811
Superfamily Dasypodoidea Gray, 1821
Family Dasypodidae Gray, 1821
Subfamily Euphractinae Pocock, 1924 ]]> Tribe Eutatini Bordas, 1933

Genus Chasicotatus Scillato–Yané, 1979

Type species. Chasicotatus ameghinoi Scillato–Yané, 1979.

Included species. Chasicotatus peiranoi Esteban and Nasif, 1996; Chasicotatus powelli n. sp., this paper; Chasicotatus spinozai n. sp., this paper.

Amended diagnosis (Scillato–Yané, 1979). Small size, intermediate between that of Zaedyus Ameghino, 1889 and Doellotatus. Osteoderms smooth, not rugose. Mobile osteoderms with a smooth region separating the cranial portion from the caudal portion, and ornamentation similar to that of fixed osteoderms, but without anterior figures; margin posterior to hair foramina much less extended than in Eutatus. Fixed osteoderms with central figure more elongated than in Eutatus and with sharp tips, surrounded by two anterior and two lateral figures at each side; figures globose, separated by deep sulci. Internal structure with up to three superimposed hair follicle cavities per palaeohistological section; conspicuous glandular cavities with narrow gland ducts, one per glandular cavity.

Chronological and stratigraphical distribution. Late Miocene (early Chasicoan–late Huayquerian).

Geographical distribution. Argentina (Buenos Aires, La Pampa, Catamarca and Entre Ríos provinces) (Figure 8).

Chasicotatus ameghinoi Scillato–Yané, 1979

Holotype. Large portion of the carapace.

Repository. MLP 76–VI–12–11 (Figure 9). Provenance: Chasicó creek, Villarino Department (Partido), Buenos Aires province; Arroyo Chasicó Formation, Las Barrancas Member (late Chasicoan, late Miocene).

Hypodigm. The holotype and MLP: 28–X–11–43, 28–X–11–64, 30–XII–10–13, 55–IV–28–47, 60–VI–18–67, 60–VI–18–75, 76–VI–12–19, 76–VI–12–26, 76–VI–12–27, 76–VI–12–38, 76–VI–12–58, 76–VI–12–111, 76–VI–12–136, 76–VI–12–137.

Amended diagnosis (Scillato–Yané, 1982). Small size, slightly smaller than that of the remaining species of the genus. Pelvic shield proportionally smaller than in Stenotatus, Doellotatus, and Eutatus. Posterior end of mobile and fixed osteoderms with large hair foramina arranged mediolaterally in a single row as in C. powelli n. sp. Mobile osteoderms with margin posterior to hair foramina more extended than in the other species. Fixed osteoderms with central figure shaped like a narrow elevated keel, both central and peripheral figures more globose than in C. powelli n. sp. and C. peiranoi ; foramina on exposed surface (glandular foramina) as fine punctuations, as in C. peiranoi ; osteoderms thicker posteriorly. Internally the mobile osteoderms have a less developed middle zone than those of Doellotatus chapadmalensis; glandular cavities small, never more than two per palaeohistological section and with narrow ducts (one per glandular cavity), hair follicle cavities (as the glandular cavities) located on the posterior half of the ornamented part and no more than two per palaeohistological section, cranial (overlapping region) portion with thick inner and outer zones, unlike the species of Doellotatus chapadmalensis. Fixed osteoderms with large glandular cavities, larger than those of C. peiranoi , but smaller than those of Chasicotatus powelli n. sp., never more than two per palaeohistological section; well developed hair follicle cavities, lodged in a zone thicker than the rest of the osteoderm.

Chronological and stratigraphic distribution. Late Miocene (early Chasicoan–late Huayquerian).

Geographical distribution. Argentina (Buenos Aires, La Pampa, and Catamarca provinces) (Figure 8).

Chasicotatus peiranoi Esteban and Nasif, 1996

Figures 6 and 10

Holotype. 77 fixed osteoderms, five complete mobile osteoderms (11 with missing cranial portion) and numerous fragments of both types, all from a single specimen.

Hypodigm. The holotype and UNSGH 57.

Amended diagnosis (Esteban and Nasif, 1996). A Chasicotatus species slightly larger than C. ameghinoi, similar in size to C. powelli n. sp and C. spinozai n sp. Posterior end of the most osteoderms with a double row of hair foramina arranged mediolaterally, the anterior one with 2–4 smaller foramina, and the posterior one with 4 to 5 foramina. Compared with those of C. ameghinoi, the mobile osteoderms are the same length but wider, and they are slightly shorter and broader compared to those of C. powelli n. sp.; central figures oval, with sharp tips, unlike those of C. ameghinoi (not sharp cornered). Fixed osteoderms with central figure broad, sharpened at its tips, less so than in C. ameghinoi and C. spinozai n. sp.; less convex than in C. ameghinoi. Internally, the inner and outer zones of the osteoderm are more developed than in C. powelli n. sp., similar to those of C. ameghinoi; glandular cavities smaller than those of C. ameghinoi and much smaller than those of C. powelli n. sp., arranged in the upper half of the thickness of the middle zone; in those areas where a second row of hair foramina is evident externally, the internal structure shows that these are divided by a bony septum along their entire length.

Chronological and stratigraphic distribution. Late Miocene (Huayquerian).

Geographical distribution. Argentina (Catamarca and Buenos Aires provinces) (Figure 8).

Chasicotatus powelli n. sp.

Figures 7 and 11

Holotype. 155 fixed osteoderms from the pelvic shield, some of them incomplete, and 20 mobile osteoderms, almost all very fragmented.

Paratype. 32 fixed osteoderms from the pelvic shield and left astragalus, same provenance.

Repository. PVL 3213.

Hypodigm. The holotype and paratype.

Derivatio nominis. In honor of palaeontologist Dr. Jaime Powell.

Amended diagnosis (Scillato– Yané, 1982). Size slightly larger than that of C. ameghinoi, similar to that of C. peiranoi . Astragalus with fused ectal and sustentacular facets, as in Eutatus. Posterior end of mobile and fixed osteoderms with large hair foramina arranged mediolaterally in a single row, as in C. ameghinoi; foramina on exposed surface more conspicuous than in the remaining species of the genus, sometimes extending to the sulci that separate peripheral figures from each other. Central figure of mobile osteoderms flatter, narrower and with shallower delimiting sulci than in C. ameghinoi. Fixed osteoderms with subelliptical central figure, less narrow anteriorly and posteriorly than in C. ameghinoi, similar to that of C. peiranoi ; delimiting sulcus shallower than in the remaining species. Internally, the inner and outer zones are thinner than those of C. ameghinoi and C. peiranoi ; large glandular cavities, larger than those of C. ameghinoi; they may even occupy the entire thickness of the middle zone and contact the inner zone; up to three glandular cavities per section (unlike C. ameghinoi and C. peiranoi , which have only two).

Chronological and stratigraphic distribution. Late Miocene (Huayquerian).

Geographical distribution. Argentina (Catamarca province) (Figure 8).

Chasicotatus spinozai n. sp.

Figure 12

Derivatio nominis. In honor of Dutch–Jewish philosopher Baruch de Spinoza (1632–1677).

Holotype. Two articulated osteoderms from the pelvic shield. Repository. MLP 69–VIII–4–5. Provenance: Vicinity of Paraná, Entre Ríos Province, "Ossiferous Conglomerate" of Ituzaingó Formation, Huayquerian Age, late Miocene.

Amended diagnosis (Scillato– Yané, 1982). Size similar to that of C. powelli n. sp. and C. peiranoi . Fixed osteoderms proportionally longer than those of C. ameghinoi. Central figure of fixed osteoderms forming a keel narrower and more prominent than in the remaining species. Sulci delimiting central and peripheral figures deep, more so than in C. powelli n. sp. and C. peiranoi and slightly less so than in C. ameghinoi. Hair follicle foramina much smaller than in the remaining species of the genus. Very noticeable foramina, probably for hair follicles, on both lateral margins of the osteoderms. The foramina on the exposed surface appear as fine punctuations, as in C. ameghinoi and C. peiranoi .

Chronological and stratigraphic distribution. Huayquerian.

Geographical distribution. Argentina (Entre Ríos province).

GEOGRAPHIC AND STRATIGRAPHIC PROVENANCE OF CHASICOTATUS SPECIES

Pampean region

Later, C. ameghinoi was reported from the Cerro Azul Formation of Chasicoan–Huayquerian age (late Miocene; Verzi, 1999; Verzi et al., 2003, 2004; Montalvo et al., 2005; Verzi et al., 2008). This Formation outcrops mainly in eastern La Pampa province and western Buenos Aires province (as "Epecuén formation" sensu Pascual, 1961; see Linares et al., 1980 and Goin et al., 2000). The lithological similarity between the deposits of Cerro Azul Formation and those of Arroyo Chasicó Formation is very high, and they can only be distinguished when the Río Negro Formation occurs between them (Linares et al., 1980). The first localities of Cerro Azul Formation that yielded remains of Chasicotatus ameghinoi were Telén, Quehué, Loventué, Naicó, Salinas de Hidalgo, Laguna Chillhué, Bajo Giuliani and El Guanaco (Esteban et al., 2001), although additional remains were later found in the localities Caleufú (Esteban et al., 2003) and Cerro La Bota (Urrutia, 2004), all within La Pampa province. According to the most recent biostratigraphic scheme presented by Verzi et al. (2008), Chasicotatus ameghinoi was recorded in the following Biozones: Chasichimys bonaerense, Chasichimys scagliai, Xenodontomys simpsoni and X. elongatus. Thus, the biochron of the species in this formation extends from the early Chasicoan to the late Huayquerian (early late Miocene), and for this reason Verzi et al. (2008) suggested that the old Chasicotatus ameghinoi Biozone be changed, since it would not be an exclusive taxon.

Chasicotatus peiranoi was recorded in the southwest of Buenos Aires province, at the Relleno Sanitario quarry (5 km southeast from Bahía Blanca, near the Grünbein township), with late Huayquerian (late Miocene) age (Deschamps, 2005).

Northwestern Argentine

Chasicotatus powelli n. sp. and Chasicotatus peiranoi come from El Cajón valley (Catamarca province). In this area, the Tertiary is represented by an assemblage of continental sediments that were originally described and named as El Bolsón Group (Turner, 1973); in particular, the fossil–bearing strata corresponds to the El Morterito Formation (Turner, 1973). Bossi et al. (1993) studied the sedimentology of the Neogene in this valley and established a new stratigraphic scheme based on alloformations. Within this scheme, the El Monterito Formation would approximately correspond to sequence II of Playa del Zorro Alloformation (Bossi et al., 1993). Stratigraphically, the Chasicotatus peiranoi remains come from the sequences IIb and IIc of the latter Alloformation (Esteban and Nasif, 1996). In turn, these sequences would correspond to the Andalhuala Formation, in the Santa María Valley (Catamarca province, Bossi et al., 1993), of Huayquerian Age.

Subsequently, Esteban and Nasif (1999) reported remains of Chasicotatus ameghinoi from the "A" Member of the Chiquimil Formation, belonging to the Santa María Group, at the locality Villavil (Catamarca province), which would be upper Chasicoan (Barrancan) in age.

Mesopotamia

As previously mentioned, the remains of Chasicotatus spinozai n. sp. come from the "Mesopotamian" (Ituzaingó Formation) of the vicinity of Paraná, Entre Ríos province. The outcroppings of the Ituzaingó Formation extend from the homonymous city (in Corrientes province) to the north of Paraná city (Entre Ríos province), along the steep bluffs of the Paraná River and several tributary rivers and creeks (Cione et al., 2000; Herbst, 2000; Brandoni, 2005). De Alba (1953) established the type locality of the Ituzaingó Formation in the vicinity of the town of Ituzaingó. The fossil vertebrate remains come almost exclusively from the lower levels of that formation, in particular from the basal stratum informally known as "Mesopotamian" or "ossiferous conglomerate" (Frenguelli, 1920, see Cione et al., 2000), which outcrops discontinuously along the Paraná river bluffs, from the vicinity of the homonymous city in the south, to the locality Pueblo Brugo in the north (Brandoni, 2005). Cione et al. (2000), on the basis of the vertebrate remains found in the "ossiferous conglomerate" and the existing stratigraphic relationships, proposed a greater affinity with the Huayquerian Age (Tortonian of the International scale), although part of the materials collected could suggest a Chasicoan Age. As in the case of the osteoderms of Chasicotatus spinozai n. sp., most of the collections from Paraná lack accurate provenance; however, practically all the terrestrial and freshwater vertebrates come from the "ossiferous conglomerate", at the base of the Ituzaingó Formation (Cione et al., 2000). In turn, Herbst (2000) considers that the base of the Ituzaingó Formation is middle–upper Pliocene in age, but it must be taken into account that this author's studies and chronological hypotheses were made for the area of Corrientes, not for Entre Ríos where these fossil vertebrates were found.

DISCUSSION

The internal morphology of osteoderms belonging to the different Chasicotatus species is characterized by the presence of glandular cavities of considerable size with very narrow ducts, one per glandular cavity. Within the internal morphological variations exhibited by the different species, it is noteworthy that the osteoderms of Chasicotatus ameghinoi are most similar to those of Stenotatus patagonicus (Figure 13). The fixed osteoderms of both species are thicker at the posterior area due to the implantation of hair follicles and the great depth of the outer zone of compact bone. However, the glandular cavities of Stenotatus patagonicus are much larger than those of C. ameghinoi, with a double duct, and present hair follicles arranged both vertically and horizontally, whereas the hair follicles of genus Chasicotatus are always arranged obliquely. On the other hand, the internal morphology of Chasicotatus powelli n. sp. resembles that of Doellotatus chapadmalensis in the thickness of the inner and outer zones and in the possession of up to three glandular cavities per palaeohistological section; however, the cavities of Chasicotatus powelli n. sp. are larger than those of Doellotatus chapadmalensis (Figure 14) and have a single duct per glandular cavity. Of the three Chasicotatus species, Chasicotatus peiranoi shows the greatest differences compared to the other two species in terms of internal morphology, due to the great development of its middle zone, smaller size of the glandular cavities and arrangement of hair follicles.

CONCLUSIONS

Two new species of this genus are described. These species are characterized using both the traditional criteria based on the external morphology of the osteoderms, and in addition, for the first time for this taxon, palaeohistological sections of the osteoderms were made allowing observation of numerous internal details (glandular cisterns, ducts that connect them to the exterior, insertion of hairs on the posterior margin, etc.).

A major faunal change took place between the pre–Chasicoan and Chasicoan units, and this change is particularly significant in the case of the Xenarthra Cingulata (Scillato–Yané and Carlini, 1998). Among the Dasypodidae, all the Eutatini and almost all the "pansantacrucian" Euphractini disappeared in the Chasicoan (Scillato–Yané et al., 1993). For the Eutatini, this change includes the definitive disappearance of Stenotatus and Proeutatus from the fossil record, and the first appearance of Chasicotatus.

ACKNOWLEDGEMENTS

The authors wish to express their gratitude to Dr. M. A. Reguero, curator of the División de Paleontología Vertebrados, MLP, and Dr. J. E. Powell curator of Palentología Vertebrados Lillo, PVL. To A. A. Carlini for his reviews and helpful suggestions. H. Gregory McDonald and an anonymous reviewer greatly improved the original manuscript through their critical review.

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