Translator Disclaimer
1 December 2010 The Oldest and Youngest Records of Afrosoricid Placentals from the Fayum Depression of Northern Egypt
Erik R. Seiffert
Author Affiliations +
Abstract

Tenrecs (Tenrecoidea) and golden moles (Chrysochloroidea) are among the most enigmatic mammals alive today. Molecular data strongly support their inclusion in the morphologically diverse clade Afrotheria, and suggest that the two lineages split near the K-T boundary, but the only undoubted fossil representatives of each superfamily are from early Miocene (∼20 Ma) deposits in East Africa. A recent analysis of partial mandibles and maxillae of Euchrysuchloris, Jawharia, and Widanelfarasia, from the latest Eocene and earliest Oligocene of Egypt, led to the suggestion that the derived “zalambdomorph” molar occlusal pattern (i.e., extreme reduction or loss of upper molar metacones and lower molar talonids) seen in tenrecoids and chrysochloroids evolved independently in the two lineages, and that tenrecoids might be derived from a dilambdomorph group of “insectivoran-grade” placentals that includes forms such as Widanelfarasia. Here I describe the oldest afrosoricid from the Fayum region, ∼37 Ma Dilambdogale gheerbranti gen. et sp. nov., and the youngest, ∼30 Ma Qatranilestes oligucaenus gen. et sp. nov. Dilambdugale is the most generalized of the Fayum afrosoricids, exhibiting relatively broad and well-developed molar talonids and a dilambdomorph arrangement of the buccal crests on the upper molars, whereas Qatranilestes is the most derived in showing relatively extreme reduction of molar talonids. These occurrences are consistent with a scenario in which features of the zalambdomorph occlusal complex were acquired independently and gradually through the later Paleogene. Phylogenetic analysis places Dilambdogale and Widanelfarasia as sister taxa to the exclusion of crown afrosoricids, but derived features that these taxa share with early Miocene Protenrec hint at the possibility that both taxa might be stem tenrecoids. Late Paleocene Todralestes and Afrodon from Morocco are similarly placed as stem afrosoricids, indicating that African adapisoriculids (including Garatherium) might also be relevant to the origin of the tenrecoid and chrysochloroid clades.

Introduction

Paleocene and Eocene mammals of Afro-Arabia are very poorly documented relative to those of other major landmasses. Among the more rarely recovered members of Paleogene African mammal faunas are a variety of diminutive insectivorous placentals—generally represented solely by isolated teeth—that were originally placed in higher-level taxa such as Cimolesta and Lipotyphla, and the families Adapisoriculidae, Chambilestidae, Cimolestidae, Palaeoryctidae, and Todralestidae (e.g., Gheerbrant 1992, 1994, 1995; Gheerbrant et al. 1998). Lipotyphla are now widely considered to be diphyletic on the basis of nucleotide and other genomic data (Springer et al. 1997; Madsen et al. 2001; Murphy et al. 2001; Amrine-Madsen et al. 2003; Asher et al. 2003; Springer et al. 2004; Asher and Hofreiter 2006; Seiffert 2007; Asher 2007), and two former members of that group—the Afro-Malagasy tenrecs (herein treated together as a superfamily, Tenrecoidea, containing a monophyletic Potamogalidae (African otter-shrews) and Tenrecidae (Malagasy tenrecoids); see Asher and Helgen 2010, for an alternative classification, and African golden moles (Chrysochloroidea, Chrysochloridae) have come to be placed in their own order, Afrosoricida, within a larger endemic African clade, Afrotheria (Stanhope et al. 1998), that also includes elephants, sea cows, hyraxes, aardvarks, and sengis (Fig. 1). Molecular divergence estimates suggest that crown afrosoricids last shared a common ancestor in the latest Cretaceous or Paleocene (Douady and Douzery 2003; Springer et al. 2003), opening up the possibility that afrosoricid origins might be traced back to some of the poorly known “cimolestan” and/or “lipotyphlan” fossils that have been recovered from the Paleocene and Eocene of North Africa (Seiffert 2010).

At present there is, however, no unambiguous fossil evidence for this hypothesis. The crux of the issue is that all extant afrosoricids have a “zalambdomorph”* occlusal pattern on their molars—i.e., a condition in which upper molar metacones and lower molar talonids are greatly reduced or absent altogether (see also Asher and Sanchez-Villagra 2005). Optimization of zalambdomorphy onto a cladogram of extant placentals alone (e.g., Springer et al. 2004) would reconstruct this dental pattern as having been present in the last common ancestor of tenrecs and golden moles (Fig. 1). If this ancestor was in fact ∼66–63 Ma in age as estimated by molecular sequence data—and if Afrosoricida is indeed an endemic African clade—then zalambdodomorph fossil afrosoricids should have been present in Afro-Arabia during the time periods for which there is paleontological coverage on that landmass (i.e., latest Paleocene, early Eocene, early middle Eocene, late Eocene, and early Oligocene). Zalambdomorph species, are, however, completely absent from Afro-Arabian mammal faunas of these time periods (Seiffert 2010) suggesting that either (i) afrosoricids were not present in Afro-Arabia during the Paleogene, (ii) zalambdomorph afrosoricids were present in Afro-Arabia during the Paleogene, but not in the areas that have been sampled thus far, (iii) tenrecs and golden moles diverged much later (e.g., in the Oligocene) than suggested by molecular data, or (iv) zalambdodomorphy was not present in the last common ancestor of tenrecs and golden moles, and evolved convergently later in the Paleogene.

There is now a small but growing body of fossil evidence that has been interpreted by Seiffert et al. (2007) as supporting the latter scenario. The oldest definitive euzalambdomorph tenrecoids and chrysochlorids (i.e., forms that completely lack upper molar metacones) are from the early Miocene of Kenya and Uganda (Butler and Hopwood 1957; Butler 1969, 1984), but Seiffert et al. (2007) have recently identified tribosphenic latest Eocene (∼34 Ma; Seiffert 2006; Seiffert et al. 2007) Widanelfarasia and early Oligocene Jawharia as stem tenrecoids, and early Oligocene Eochrysochloris as a stem chrysochlorid (see Fig. 2). Because these genera all retain well-developed molar metacones and/or lower molar talonid basins, these identifications would require that euzalambdomorphy evolved convergently within Afrosoricida. In particular, Widanelfarasia's combination of a dilambdomorph M1 and protozalambdomorph M2–3 would suggest that the stem lineage leading to crown Tenrecoidea either passed through a dilambdodomorph phase prior to acquisition of zalambdomorphy, or that Widanelfarasia's dilambdomorphy is autapomorphic. Furthermore, it has long been known that the extant potamogalid tenrecoid Potamogale is protozalambdomorph (McDowell 1958; Butler 1972, 1988), lending additional support to the hypothesis that this condition might be plesiomorphic within Afrosoricida. Alternatively, this condition is simply an autapomorphy of Potamogale; this possibility is supported by the observation that the molar metacones of Potamogale's sister taxon, the smaller genus Micropotamogale, vary from being very reduced to absent.

Fig. 1.

Relationships of extant placental mammalian orders, based on the analysis of Roca et al. (2004), with zalambdomorph groups (Afrosoricida and Solenodontidae) highlighted.

f01_599.eps

Here I present additional evidence that contributes to the debate surrounding the homology of zalambdomorphy in tenrecs and golden moles. Recent work at the earliest Priabonian (earliest late Eocene, ∼37 Ma) Birket Qarun locality 2 (or BQ-2) has led to the recovery of the oldest Fayum afro- soricids, including a new genus described below that is evidently even more generalized than Widanelfarasia, and that appears to document an even more primitive dilambdomorph phase in either stem afrosoricid or stem tenrecoid evolution. The material also provides a clearer look at the upper molar and P4 morphology of a primitive afrosoricid, previously known solely from 3-D reconstructions derived from micro-CT scans of a damaged Widanelfarasia maxilla (Seiffert et al. 2007). A distal humerus from BQ-2 is also attributed to the new genus described here, providing the first look at one aspect of postcranial morphology in this poorly documented evolutionary radiation. In addition, less informative tenrecoid fossils that were collected in the 1960s at one of the youngest vertebrate fossil localities in the Fayum area (∼29.5–30 Ma Quarry I; Fig. 2) have recently been relocated in the collections of the Yale Peabody Museum, and these specimens are described, named, and figured here for the first time. Though fragmentary, it is clear that the Quarry I fossils more closely approximate the euzalambdomorph condition than any of the older afrosoricids from the succession, and provide support for gradual acquisition of zalambdomorphy through the later Paleogene.

Institutional abbreviations.—CGM, Egyptian Geological Museum, Cairo, Egypt; DPC, Duke Lemur Center Division of Fossil Primates, Durham, North Carolina, USA; YPM, Yale Peabody Museum, New Haven, Connecticut, USA.

Systematic paleontology

Supercohort Afrotheria Stanhope, Waddell,
Madsen, de Jong, Hedges, Cleven, Kao, and
Springer, 1998
Order Afrosoricida Stanhope, Waddell, Madsen, de
Jong, Hedges, Cleven, Kao, and Springer, 1998
Suborder ?Tenrecomorpha Butler, 1972
Genus Dilambdogale nov.

  • Type species: Dilambdogale gheerbranti sp. nov., see below.

  • Etymology: From Greek di, two and lambda, eleventh letter of the Greek alphabet (L)—in reference to the dilambdomorph arrangement of the buccal crests on the genus' first upper molar; and gale, weasel—a common suffix in generic names of extant tenrecoids.

  • Diagnosis.—Same as for the species.

  • Dilambdogale gheerbranti sp. nov.
    Figs. 37.

  • Etymology: In honor of the French paleontologist Emmanuel Gheerbrant, for his numerous contributions to the study of Paleogene Afro-Arabian placental mammals, including “insectivoran-grade” placentals.

  • Holotype: CGM 66005, a maxillary fragment preserving the distal alveolus for P3, the crowns of P4 and M1, the mesiobuccal root of M2, and the infraorbital foramen (Fig. 3).

  • Type locality: Birket Qarun locality 2 (BQ-2), northern Egypt.

  • Type horizon: Earliest Priabonian (earliest late Eocene), Umm Rigl Member of Birket Qarun Formation.

  • Material.—The type specimen; DPC 23306E, left M2; DPC 23307A, right M3; DPC 23007H, left m2; DPC 23736A, right mandibular fragment with ml and talonid of p4; DPC 23780C, left m2; DPC 23784D, right M1; DPC 23983C, right mandibular fragment with p4–m1; DPC 24001A, left P4; DPC 24081B, right mandibular fragment with p2–4; DPC 24103A, right mandibular fragment with m1–3; uncatalogued specimens at the CGM.

  • Diagnosis.—Differs from Miocene-to-Recent tenrecoids primarily in retaining a well-developed metacone and protocone on M1–3, small conules on M1–2, a cuspate (rather than crestiform) stylocone on M1–3, and well-developed talonid and hypoconulid cusps on the lower molars. Further differs from tenrecoids other than Protenrec in having the distal root of P3 placed lingual to the mesiobuccal root of P4. Differs from Widanelfarasia in having a relatively well-developed P4 ectostyle; a shorter postmetacrista on M1; well-developed and cuspate (rather than crestiform) metacone, stylocone, and parastyle on M3; a cuspate, rather than crestiform, stylocone on M2; and in having an m1 with a relatively broad talonid and more buccally placed cristid obliqua, delimiting a relatively poorly-developed hypoflexid. Differs from late Paleocene Todralestes in having a “w”-shaped arrangement of the buccal crests on M1–2, relatively broad stylar shelves, no pre- or postcingula on M1–3, and a P4 ectostyle, -crista, and -fossa. Differs from late Paleocene Afrodon chleuhi in having a dilambdodont M2, relatively broad stylar shelves, and slightly taller molar trigonids. Differs from ?Garatherium todrae (known only from upper molars) in lacking distinct upper molar premetaconule cristae and postpara- and premetacristae that contact the mesostyle buccally.

  • Description.—The dental morphology of D. gheerbranti is known from four upper tooth loci (P4, M1, M2, M3) and six lower tooth loci (p2, p3, p4, m1, m2, m3) (Figs. 36). Measurements for upper and lower teeth are provided in Table 1 and Table 2, respectively. The holotype partial maxilla (CGM 66005, Fig. 3) contains P4–M1 and preserves the infraorbital foramen, the alveolus for the distal root of P3, and the mesial halves of the lingual and mesiobuccal alveoli for M2; P4, M1, M2, and M3 are also known from isolated teeth (Fig. 6). Partial mandibles together preserve p2–m3 in place (Figs. 4, 5), and most of these loci are also known from isolated teeth (Table 1). Though found in isolation, the M2–3 are assigned to this species because (i) they are of similar size to, and occlude well with, the m2–3 in the hypodigm, and (ii) they bear a strong resemblance to the upper teeth of younger Widanelfarasia, P2–M3 of which are preserved in place in a single maxilla (Seiffert et al. 2007).

    A partial alveolus that is preserved mesial to the double-rooted p2 (Fig. 4A) is relatively large, and, as in Widanelfarasia, was presumably for the lower canine. If this interpretation is correct, then (d)p1 was absent in Dilambdogale, as in Widanelfarasia and all extant afrosoricids (Seiffert and Simons 2000). The p3 and p4 both bear tall protoconids; that of p3 is mesially inclined, and has a long postprotocristid on its gradually sloping distal face. There is a tiny paraconid at the base of the p3 protoconid which is slightly lingual to the mesiodistal long axis of the tooth, and a larger hypoconid that is present at the distal terminus of the postprotocristid. There is a very faint and short lingual cingulum just distal to the paraconid, but it does not continue across the rest of the crown. The base of the crown is somewhat staggered with respect to the alveolar plane; the distal aspect of the crown base, above the distal root, extends closer to the alveolar plane than the mesial part of the crown base.

    The p4 also has a small paraconid at the base of the protoconid (Fig. 4A, C); this cusp is relatively large and robust when compared with the p3 paraconid, but is nevertheless still very small in comparison to the tall p4 protoconid (Fig. 4C2). The metaconid is approximately half the height of the protoconid (Fig. 4C2), and is placed lingual, and slightly distal, to that cusp (Fig. 4C). A faint protocristid extends from the protoconid to the metaconid. Distinct and closely situated entoconid and hypoconid cusps are present on the lingual aspect of the talonid, with the hypoconid being slightly larger than the entoconid. There are very faint entocristid and hypocristid crests, but no cristid obliqua, and the p4 hypoflexid is deep. There are no lingual or buccal cingulids.

    On m1 (Fig. 4B, C, E), the paraconid is large, mesially oriented, and is placed slightly buccal and far mesial to the metaconid. There is no premetacristid descending mesially from the metaconid, leaving the trigonid broadly open lingually. The paraconid is connected to the protoconid by an elongate paracristid that bears a distinct notch along its midpoint. The protocristid connecting the metaconid and protoconid varies from being perpendicular to the long axis of the tooth, to being slightly oblique. The metaconid is slightly lower than the protoconid. The talonid is preserved on DPC 23736A (Fig. 4E); the basin is subequal in width to the trigonid, has a relatively shallow hypoflexid, and distinct entoconid, hypoconid, and hypoconulid cusps, the latter of which projects distally. The cristid obliqua meets the posterior wall of the trigonid slightly buccal to its midpoint. The m2–3 (Fig. 4B, D) differ from m1 in having oblique cristids that terminate midway between the protoconid and metaconid cusps, protocristids that are consistently transversely oriented, and relatively deep hypoflexids. All lower molars have talonids that are slightly longer than trigonids, oblique cristids and hypocristids that meet at a sharp angle, and distinct precingulids.

    The mesiobuccal aspect of P4 is missing on all of the specimens that have been recovered thus far, but the alveolus for the mesiobuccal root is placed mesial to the preserved part of the crown, suggesting that Dilambdogale probably had a prominent parastyle on P4, as has been documented for Todralestes (Gheerbrant 1991b) and Widanelfarasia (Seiffert et al. 2007). The P4 bears a tall paracone cusp and a very small and mesially placed protocone. Like many crown tenrecoids, Dilambdogale also has a distinct ectostyle cusp distal and buccal to the apex of the paracone. DPC 24001A has a very faint ectocrista descending from the buccal face of the paracone to meet the ectostyle. Together with the elongate post-paracrista, these structures delimit a shallow distolabial ectofossa. The P4 has no conules and no pre- and postcingula, but a tiny crestiform hypocone is present, and is connected to the protocone by a weak postprotocrista. Though the parastylar region is missing, it is clear that it would have protruded from a very low point on the mesial face of the paracone.

    A relatively unworn M1 is present in the holotype specimen (Fig. 3). This locus is also represented by an isolated tooth with a more worn stylar region (DPC 23784D; Fig. 6D). The Ml resembles Widanelfarasia in having a “W”-shaped arrangement of the pre- and postparacristae and pre- and postmetacristae. In mesial and distal view, the paracone, metacone, and protocone are approximately equal in height. The paracone and metacone show some “fusion” of their bases. The stylar region of the M1 in the holotype specimen exhibits some wear, but it is clear that the stylocone would have been the largest and tallest cusp on the buccal aspect of the tooth, followed by the parastyle. It appears that there was also a very small mesostyle at the trough of the ectoflexus, and a similarly small cusp “D” on the periphery of the metastylar lobe. This interpretation is supported by the clear presence of these cusps on M2 (see below). The trigon is restricted due to encroachment of the centrally placed para- and metacone and is bordered lingually by distinct pre- and postprotocristae. A small, lingually-placed paraconule is present and bears a postparaconule crista on DPC 23784D but not on CGM 66005; the preprotocrista bypasses the lingual aspect of the paracone and is continuous with the parastylar area. There is a short but distinct hypoparacrista that connects the paraconule and the lingual face of the paracone on DPC 23784D, but this is absent on the holotype specimen. A small metaconule is present but is more buccally placed than the paraconule. A distolabially oriented postmetaconule crista leaves the trigon open distally on DPC 23784D, but this crest is not present on CGM 66005. There is no premetaconule crista, and no pre- or postcingula, on either specimen.

    M2 is represented by two isolated specimens (DPC 23306E, Fig. 6B; DPC 23780C, Fig. 6C). The M2 is much broader (buccolingually) than M1. Of the two primary buccal cusps, the paracone is closest to the protocone (and is placed farther from the buccal margin than is the metacone). In lingual and buccal view, the paracone is taller than the metacone (Fig. 6C2). When compared with Ml, the protocone is relatively prominent, but the trigon is more constricted mesiodistally. The stylar shelf bears a tall and distinct stylocone and a much smaller mesostyle and cusp “D” (Fig. 6C2). The parastyle is prominent, and the parastylar lobe forms a prominent mesial “hook” which, based on the placement of the mesiobuccal root of M2 implanted in the holotype partial maxilla, would have curved around the buccal aspect of the metastylar lobe of M1, as in Widanelfarasia (Seiffert et al. 2007). A paraconule is not evident on DPC 23780C, but is present, though minute, on DPC 23306E; on the latter specimen the paraconule is connected to the base of the paracone by a short postparaconule crista. As on M1, the paraconule is situated closer to the protocone than is the metaconule, there is no premetaconule crista, and there are no pre- or postcingula.

    M3 (represented solely by DPC 23307A, Fig. 6A) has well-developed paracone and metacone cusps, the postparaand premetacristae of which are slightly buccally oriented in a weakly “W”-shaped arrangement. The metacone is smaller than the paracone, both in height and in volume. The post-metacrista is buccally (rather than distally) oriented and is continuous with the buccal aspect of a very broad stylar shelf. The stylocone and parastyle are distinct and well-developed, and, at least on DPC 23307A, an accessory cuspule is present on the buccal face of the tooth just distal and labial to the parastyle. A crestiform metaconule is present but no paraconule is evident, perhaps due to wear. It is clear that there is no postparaconule crista and no pre- or postcingula.

    Various fragments of the mandibular corpus are preserved (see, e.g., Figs. 4A, B, 5). The corpus is fairly shallow, being only slightly taller than trigonid height, and bears a mental foramen below ml (Fig. 5) and p2. Little is preserved of the distal part of the mandible but the anterior part of the masseteric fossa appears to have been well-developed.

  • Humerus.—A small distal humerus (Fig. 7) from locality BQ-2 (DPC 24108A) is attributed to Dilambdogale gheerbranti on the basis of size, morphology, and relative abundance. The only other small mammals known from BQ-2 that the humerus could be attributable to (on the basis of size alone) is the chiropteran Qarunycteris (Gunnell et al. 2008) and the anomaluroid rodent Shazurus (Sallam et al. 2010a). DPC 24108A exhibits none of the distinctive derived features of chiropteran distal humeri (see, e.g., Simmons and Geisler 1998), excluding the possibility that the specimen is attributable to Qarunycteris. The morphology of a distal humerus of the large anomaluroid Kabirmys from BQ-2 (Sallam et al. 2010b, c) is radically different from that of DPC 24108A, suggesting that its smaller relative Shazurus is unlikely to exhibit the morphology observable on DPC 24108A.

    DPC 24108A does bear clear morphological resemblance to the distal humeri of some extant tenrecoids, particularly species of Microgale, which lends additional support for its attribution to Dilambdogale. Features shared with many species of Microgale, such as the presence of an entepicondylar foramen, a moderately developed brachioradialis flange, a deep radial fossa, a shallow olecranon fossa, and an ovoid capitulum with a proximodistally tall but laterally tapering capitular tail, are, however, presumably primitive within Afrosoricida, and possibly within Afrotheria. Perforation of the bony lamina separating the olecranon and radial fossae, as occurs in DPC 24108A, also occurs variably in species of Microgale (Salton and Sargis 2008). The medial aspect of the trochlea is missing, but in distal view there is a distinct notch separating the capitulum from the lateral aspect of the trochlea, as in species such as Microgale talazaci. DPC 24108A also preserves the distal part of a sharp deltopectoral crest, the more proximal part of which trends laterally. DPC 24108A bears no special resemblance to the humeri of Malagasy Geogale and African potamogalids, which are likely to be autapomorphic in lacking entepicondylar foramina and having relatively reduced brachioradialis flanges. The humeri of golden moles reflect their highly fossorial existence in having features such as elongate medial epicondyles, globular capitula, mediolaterally long trochleae, and humeral shafts that are strongly laterally canted relative to the long axis of the distal articulation (e.g., Asher and Avery 2010). None of these features are seen in DPC 24108A.

    The morphology of DPC 24108A is consistent with Dilambdogale having been a very generalized terrestrial quadruped. The combination of a shallow olecranon fossa and a deep radial fossa suggest that Dilambdogale habitually maintained postures in which the forearms were typically held in acute flexion. DPC 24108A bears none of the structural features of the distal humerus that are typically correlated with saltatory locomotion, habitual fossoriality, arboreality, or dedicated aquatic behavior in extant mammals.

  • Comparisons.—As already noted, the fossil record of small mammals is relatively poor in Afro-Arabia (Seiffert 2010), and as such it is rare for “insectivoran-grade” placentals (sensu Asher 2005) to be documented by more than a few tooth loci. Therefore Dilambdogale, despite being represented solely by P4–M3 and p2–m3 and a distal humerus, actually allows for more extensive comparisons than many other important taxa from Afro-Arabian Paleogene, some of which are only documented by upper teeth (e.g., Garatherium, Chambilestes).

    The genus that is best-documented from older horizons in Africa is latest Paleocene Todralestes variabilis (Gheerbrant 1991b, 1994). Todralestes differs from Dilambdogale in retaining upper molar features which, based on their occurrence in other afrotherians (e.g., Seiffert 2007), may be primitive within that clade—e.g., relatively narrow stylar shelves, short prepara- and postmetacristae, linear centrocristae, absence of deep ectoflexi, presence of pre- and postcingula, and, in some individuals, small hypocones on M1–2 (Fig. 8F). Stylar cusps are also poorly-developed and crestiform in Todralestes, but are much more prominent in Dilambdogale, and Todralestes lacks an ectostyle on P4, whereas this cusp is very prominent in Dilambdogale. The morphology of P4 in Todralestes is otherwise also very similar to that of Dilambdogale in having a long postparacrista and a very low, small, and mesially positioned protocone. Dilambdogale is more similar to Todralestes in the lower dentition, differing primarily in having larger para- and hypoconid cusps on p3, an entoconid on p4, relatively broad lower molars with more distinct talonid cusps, and molar protocristids that tend to be less obliquely oriented with respect to the long axis of the molar crown.

    Seiffert et al. (2007) noted that Todralestes, Widanelfarasia, and Protenrec all have an odd configuration of the maxilla and P3–4 complex, in which the distal root of P3 is lingually placed, being mesial to the lingual root of P4, rather than being mesial to the mesiobuccal root as in other afrotherians. This feature is also seen in Dilambdogale (Fig. 3). This morphology appears to be related to the placement of the rostral aperture of the infraorbital foramen; in all of the aforementioned taxa, the rostral aperture is placed just dorsal to the mesiobuccal root of P4, and the alveolar process of the maxilla lateral to the P3 is similarly offset medially, leading to a distinctive constriction of the palate at the junction between P3 and P4. This morphology is also seen in the extant Malagasy tenrec Geogale (Butler 1984), and, interestingly, the early Eocene hyaenodontid Koholia from Algeria (Crochet 1988). These taxa also all have a greatly enlarged paracone on P4, a mesiobuccal root of P4 that is widely exposed in lateral view, and, in those taxa that preserve a P3 in place (Widanelfarasia, Protenrec, and Geogale) there is a distinctly “stepped” transition from the apex of the P4 to that of P3 (Fig. 3) This surely would have also been the case in Dilambdogale and Todralestes, given the small size of the occluding p3, and the position of the distal P3 alveolus far dorsal to the base of the P4 crown. As strange as this overall pattern may be, its presence in a variety of early Paleogene African mammals with very different dental morphology suggests that this condition may be plesiomorphic at a high taxonomic level within Afrotheria.

    The upper dentition of the alleged adapisoriculid Afrodon chleuhi, from the same latest Paleocene deposits that yielded remains of Todralestes variabilis (Gheerbrant 1988, 1995; Gheerbrant et al. 1998), is more similar to Dilambdogale than is Todralestes in having relatively broad stylar shelves, longer and more buccally oriented prepara- and postmetacristae, more pronounced ectoflexi, a relatively lingually placed paraconule, and absence of pre- and postcingula. However A. chleuhi is not as derived as Dilambdogale in that it retains a linear centrocrista and a stylar shelf that is not as broad (Fig. 8E); the stylar cusps are also more crestiform in A. chleuhi. The lower molars and p4 of A. chleuhi are also relatively broad, with deep hypoflexids (as in Dilambdogale), and its p4 talonid is more complex than that of Todralestes. Afrodon tagourtensis, from the earliest Eocene of Morocco (Gheerbrant 1993; Gheerbrant et al. 1998), is even more similar to Dilambdogale than is A. chleuhi in having a relatively elongate buccal margin on M1, and, on p4, a distinct entoconid.

    Of all other older Afro-Arabian mammals, Dilambdogale is most similar in its occlusal morphology to Garatherium mahboubii from the early Eocene of Algeria (Crochet 1984; Mahboubi et al. 1986). A similar species that has been referred to as ?Garatherium todrae is also known from the latest Paleocene localities that preserve remains of Afrodon chleuhi and Todralestes variabilis (Gheerbrant et al. 1998). Unlike Afrodon and Todralestes, but as in Dilambdogale, Garatherium exhibits well-developed dilambdomorphy, with a “W”-shaped arrangement of crests connecting the paracone and metacone (Fig. 8D). Like Dilambdogale, Garatherium has distinct parastyle, stylocone, mesostyle, and “D” cusps along the buccal margin, but in Garatherium the mesostyle and cusp “D” are even more prominent, and the mesostyle is met by the postpara- and premetacristae. Further resemblances include the lack of pre- and postcingula. At present no lower teeth or upper premolars have been attributed to Garatherium, limiting comparisons with Dilambdogale, however the distinctive upper molar features shared by the two taxa increase the likelihood that the two species may be closely related, and that G. mahboubii is indeed a placental as argued by Gheerbrant (1991a), and not a peradectine marsupial as was initially suggested (Crochet 1984; Mahboubi et al. 1986).

    The enigmatic genus Chambilestes from the early or early middle Eocene of Tunisia (Gheerbrant and Hartenberger 1999; Fig. 8C) differs from Dilambdogale in having distinct pre- and postcingula, small hypocones on M1–2, well-developed postpara- and premetaconule cristae, and a relatively narrow stylar shelf. On the basis of predicted occlusal relationships, Seiffert and Simons (2000) suggested that Chambilestes might have affinities with Widanelfarasia, but now that the upper dentition of Widanelfarasia is known (Seiffert et al. 2007), this possibility appears remote. Chambilestes might be more closely related to Todralestes (Seiffert 2010), specifically early Eocene Todralestes butleri (Gheerbrant 1993).

    Of all Paleogene Afro-Arabian taxa, Dilambdogale is most similar to latest Eocene Widanelfarasia (Seiffert and Simons 2000; Seiffert et al. 2007). The upper and lower teeth of these genera exhibit a series of striking resemblances, but Dilambdogale appears to be more primitive in having relatively broad lower molar talonids (Fig. 9), a larger metacone on M2, and a distinct and cuspate metacone on M3. In each of these features, Dilambdogale is similar to early African “adapisoriculids” such as Afrodon, while Widanelfarasia exhibits derived features that arguably align the genus with later tenrecoids (Seiffert et al. 2007).

  • Stratigraphic and geographic range.—Earliest Priabonian, northern Egypt.

  • Fig. 2.

    Stratigraphic placement of afrosoricid-bearing localities in the later Paleogene rocks exposed in the Fayum area, and proposed correlation of local polarity zones to the Geomagnetic Polarity Timescale (GPTS), following Seiffert (2006) and Seiffert et al. (2008). Locality BQ-2, which yielded the remains of Dilambdogale gheerbranti described here, is estimated to be ∼37 Ma; Quarry I, which produced remains of Qatranilestes oligocaenus, is estimated to be ∼29.5–30 Ma.

    f02_599.eps

    Fig. 3.

    Holotype maxilla of the afrosoricid placental Dilambdogale gheerbranti gen. et sp. nov., from the earliest late Eocene (earliest Priabonian) locality BQ-2, Birket Qarun Formation, Fayum Depression, northern Egypt. A. Occlusal view of CGM 66005, left maxillary fragment preserving the alveolus for the distal root of P3, crowns of P4–M1, and partial alveoli for the mesiobuccal and lingual roots of M2. B. Line drawing of CGM 66005 in lateral view, showing the position of the infraorbital foramen and the orbital rim.

    f03_599.eps

    Table 1.

    Measurements (in mm) of upper teeth of Dilambdogale gheerbranti gen. et sp. nov. BL, buccolingual breadth; MD, mesiodistal length.

    t01_599.gif

    Table 2.

    Measurements (in mm) of lower teeth of Dilambdogale gheerbranti gen. et sp. nov. MD, mesiodistal length.

    t02_599.gif

    Fig. 4.

    Lower dentition of the afrosoricid placental Dilambdogale gheerbranti gen. et sp. nov. from the earliest late Eocene (earliest Priabonian) locality BQ-2, Birket Qarun Formation, Fayum Depression, northern Egypt. A. Oblique lingual view of DPC 24081B, a right mandibular fragment preserving the alveolus for the lower canine and the crowns of p2–4. B. DPC 24103A, right mandibular fragment preserving the worn crowns of m1–3 in oblique lingual (B1) and occlusal (B2) views. C. DPC 23983C, a right mandibular fragment preserving p4-m1 in occlusal (C1) and lingual (C2) views. D. DPC 23783B, a left mandibular fragment preserving m2–3 in occlusal (D1) and lingual (D2) views. E. Occlusal view of DPC 23736A, a right mandibular fragment preserving the talonid of p4 and the complete crown of m1. F. DPC 23307H, a left m2 in occlusal view.

    f04_599.eps

    Fig. 5.

    Buccal view of DPC 23783B, a left mandibular fragment of the afrosoricid placental Dilambdogale gheerbranti gen. et sp. nov., from the earliest late Eocene (earliest Priabonian) locality BQ-2, Birket Qarun Formation, Fayum Depression, northern Egypt, preserving m2–3.

    f05_599.eps

    Fig. 6.

    Upper dentition of the afrosoricid placental Dilambdogale gheerbranti gen. et sp. nov. from the earliest late Eocene (earliest Priabonian) locality BQ-2, Birket Qarun Formation, Fayum Depression, northern Egypt. A. DPC 23307A, right M3, in occlusal (A1) and distal (A2) views. B. DPC 23306E, left M2, in occlusal view. C. DPC 23780C, left M2, in occlusal (C1) and buccal (C2) views. D. DPC 23784D, right M1, in occlusal (D1) and mesial (D2) views. E. DPC 24001A, left P4, in distal (E1) and occlusal (E2) views.

    f06_599.eps

    Fig. 7.

    DPC 24108A, right distal humerus attributed to the afrosoricid placental Dilambdogale gheerbranti gen. et sp. nov., from the earliest late Eocene (earliest Priabonian) locality BQ-2, Birket Qarun Formation, Fayum Depression, northern Egypt.

    f07_599.eps

    Fig. 8.

    Comparison of occlusal morphology of the upper second molar (scaled to the same approximate buccolingual width) in a series of Paleogene African mammals with possible afrosoricid affinities. A. Widanelfarasia bowni (latest Eocene, Jebel Qatrani Formation, Egypt), based on Seiffert et al. (2007). B. Dilambdogale gheerbranti (earliest late Eocene, Birket Qarun Formation, Egypt). C. Chambilestes fousstmensis (late early or early middle Eocene, Chambi, Tunisia), based on Gheerbrant and Hartenberger (1999). D. ?Garatherium todrae (late Paleocene, Jebel Guersif Formation, Morocco), based on Gheerbrant et al. (1998). E. Afrodon chleuhi (late Paleocene, Jbel Guersif Formation, Morocco), based on Gheerbrant (1988). F. Todralestes variabilis (late Paleocene, Jbel Guersif Formation, Morocco), based on Gheerbrant (1991b).

    f08_599.eps

    Suborder Tenrecomorpha Butler, 1972
    ?Superfamily Tenrecoidea Gray, 1821
    Genus Qatranilestes nov.

  • Type species: Qatranilestes oligocaenus sp. nov., see below.

  • Etymology: From Arabic qatran, tar—in reference to the dark basalt capping the Jebel Qatrani Formation, cobbles of which drape the hills north of Quarry I and which give that Formation its name (Jebel Qatrani = “tar hill”), and from Greek lestes, robber—a common suffix in generic names of insectivoran-grade placentals.

  • Diagnosis: Same as for the species.

  • Qatranilestes oligocaenus sp. nov.
    Figs. 10, 11B.

  • Holotype: YPM 24203, a right mandibular fragment preserving the talonids of m2–3 (Fig. 10B).

  • Etymology: In reference to the Oligocene age of the species.

  • Type locality: Quarry I, northern Egypt.

  • Type horizon: Late early Oligocene, upper sequence of Jebel Qatrani Formation, northern Egypt (∼29.5–30 Ma).

  • Diagnosis.—Small species (about 65% the size of Dilambdogale gheerbranti) that differs from other Fayum afrosoricids (Dilambdogale, Widanelfarasia, and Jawharia) in having relatively reduced talonid basins and capacious hypoflexids on m2–3 (Figs. 9, 10); differs from Dilambdogale in having very reduced molar entoconids.

  • Description.Qatranilestes is only known from very fragmentary material, notably the holotype mandible preserving the talonids of m2–3, the horizontal ramus distal to p4, and the base of the ascending ramus (Fig. 10B). A complete but badly abraded and worn m3 is implanted in another partial mandible (YPM 24200, Fig. 10A). Even from such poorly preserved material, it is clear that Qatranilestes is unique among Fayum tenrecoids in having very reduced talonids (Figs. 9, 11) and capacious hypoflexids (m2 talonid width = 0.45 mm; m3 talonid width = 0.45 mm). The m2 talonid preserves a concave cristid obliqua and small hypoconid, hypoconulid, and entoconid cusps. The trigonid of m3 on YPM 24200 is very worn, but clearly would have had well-developed metaconid, paraconid, and protoconid cusps, and was elevated high above the very low and mediolaterally narrow talonid basin, which shows little clear differentiation of cusps aside from the hypoconid. The m3 of the holotype specimen is not as worn and damaged, but similarly shows only very small and indistinct talonid cusps, with the hypoconid and hypoconulid closely approximated. Relative to trigonid breadth, the m3 talonid of Qatranilestes is very reduced relative to those of Widanelfarasia and Jawharia. Seiffert et al. (2007) noted that Widanelfarasia exhibits slight external rotation of the long axis of the lower molar crowns, leading to an arrangement in which the lower molar paraconids are situated distal to the hypoconulid (rather than the entoconid) of the adjacent molar.

    This orientation decreases the size of the trough for the occluding upper molar metacone, and increases the buccal exposure of the paracristid for occlusion with the upper molar postmetacrista. Judging from the orientation of the m2 talonid, Qatranilestes had a similar external rotation of the molar crowns. The preserved morphology and orientation of Qatranilestes' m2–3 suggests that the occluding M2 would have had a greatly enlarged paracone (to occlude in the large hypoflexid), a reduced metacone, and an elongate postmetacrista, and probably more closely approximated the “euzalambdomorph” occlusal pattern than did any of the older species that have been recovered thus far.

  • Fig. 9.

    Relative talonid breadth in Paleogene afrosoricids. Plot of the distance from the entoconid to hypoconid on m2 divided by the maximum breadth of the m2 trigonid. Note that relative talonid breadth decreases through the later Paleogene.

    f09_599.eps

    Fig. 10.

    Dental morphology of the afrosoricid placental Qatranilestes oligocaenus, gen. et sp. nov., from the late early Oligocene (late Rupelian) Quarry I, upper sequence of the Jebel Qatrani Formation, northern Egypt. A. YPM 24200, right mandibular fragment with crown of m3 in occlusal (A1) and lingual (A2) views. B. YPM 24203, holotype right mandible with talonids of m2–3 in occlusal stereo view (B1 and B2).

    f10_599.eps

    Fig. 11.

    Comparison of talonid morphology, in lingual view of two Egyptian afrosoricid placentals. A. Dilambdogale gheerbranti (DPC 24103A), from the earliest late Eocene (earliest Priabonian; ∼37 Ma) locality BQ-2, Birket Qarun Formation, Fayum Depression, northern Egypt. B. Qatranilestes oligocaenus (YPM 24203), from the late early Oligocene (late Rupelian; ∼30 Ma) Quarry I, upper sequence of the Jebel Qatrani Formation, northern Egypt. Specimens are scaled to the same approximate m2–3 length to facilitate comparison. Note the much larger hypoconid and relatively capacious and concave talonid basin in Dilambdogale. Also note that the m2 entoconid is broken in DPC 24103A, but is relatively well-developed in other specimens.

    f11_599.eps

    Phylogenetic analysis

    Afrodon chleuhi, Dilambdogale gheerbranti, and Todralestes variabilis were added to the character-taxon matrix of afrotherian mammals that was originally compiled by Seiffert (2007), and which was recently augmented by Barrow et al. (2010). Although Eochrysochloris, Jawharia, and Qatranilestes may prove to be key taxa for understanding afrosoricid interrelationships, available specimens preserve too few characters to be included in the analysis. The matrix now includes 403 morphological characters, 18 369 nucleotide characters (from three mitochondrial genes and 20 nuclear genes) derived from the analysis of Amrine-Madsen et al. (2003), ten chromosomal association presence/absence characters derived from various analyses (Yang et al. 2003; Robinson et al. 2004; Kellogg et al. 2007), and eight SINE presence/absence characters derived from the analysis of Nikaido et al. (2003). See Seiffert (2007) for additional information, including character descriptions; the modified matrix, in NEXUS format, is available at  http://www.morphobank.org.

    The matrix was analyzed under two assumption sets using the maximum parsimony algorithm in PAUP* 4.0b10 (Swofford 1998); results are presented in Figs. 12 and 13. In one analysis (Fig. 12A), some multistate characters were ordered and scaled; in the other assumption set all multistate characters were unordered and equally weighted (Fig. 12B). Analysis of the matrix with some multistate characters ordered and scaled recovered a single tree of length 18745.188 (Fig. 12A). Despite very minor perturbations to the matrix of Seiffert (2007) in terms of character and taxon addition, afrotherian superordinal relationships are remarkably different from those recovered in his original analysis—i.e., instead of a ([Macroscelidea + Afrosoricida], [Tubulidentata + Paenungulata]) arrangement, Afrosoricida is instead placed as the sister group of all other afrotherians, a Macroscelidea + Tubulidentata clade is placed as the sister group of Paenungulata, and, within the latter group, Sirenia joins Hyracoidea rather than Proboscidea. These results reinforce Seiffert's (2007) conclusion that two bursts of superordinal cladogenesis—one at the base of crown Afrotheria, and one at the base of Paenungulata—occurred so rapidly that interordinal relationships might not be convincingly resolved by parsimony analyses of combined molecular-morphological data sets. Within Afrosoricida, Protenrec was placed as the nearest sister group of chrysochloroids and tenrecoids, followed by a DilambdogaleWidanelfarasia clade. Todralestes was placed as the most basal stem afrosoricid. Analysis of all characters unordered recovered 63 MPTs of length 19568 (Fig. 12B). The strict consensus of these trees provides no resolution among crown afrosoricids or Paleogene taxa, apparently due to Early Cretaceous Prokennalestes and Montanalestes, which acted as “wild-card” taxa by falling either as a sister group of placentals, or as a sister group of Todralestes, Dilambdogale, and Widanelfarasia across the 63 equally most parsimonious trees. An Adams consensus of the 63 MPTs reveals that a (Todralestes, [Dilambdogale, Widanelfarasia]) clade was nevertheless consistently placed with afrosoricids, though in various positions, and in most of the trees this clade was placed as the sister group of Protenrec, followed by Potamogale. When the poorly-known genus Afrodon was added to the matrix (Fig. 13), the phylogenetic relationships among afrotherians remained the same, and Afrodon was placed as a sister group of a Dilambdogale-Widanelfarasia clade whether certain multistates were treated as ordered and scaled, or as unordered.

    Discussion

    In many ways, the dentitions of Dilambdogale and Widanelfarasia are morphologically intermediate between those of the highly derived euzalambdomorph afrosoricids from the early Miocene of East Africa, and those of the much more generalized protodilambdomorph adapisoriculids and todralestids from the latest Paleocene of northern Africa. An intermediate phylogenetic position is supported by parsimony analyses with some multistate characters ordered and scaled (Figs. 12, 13), but analyses with all characters unordered sometimes nest Afrodon, Dilambdogale, Todralestes, and Widanelfarasia deep within Tenrecoidea as sister taxa of Protenrec, or alternatively as stem afrosoricids joined by Early Cretaceous Montanalestes and Prokennalestes (the latter of which are generally considered to be basal eutherians [e.g., Kielan-Jaworowska et al. 2004]). These results must be interpreted with considerable caution, because the matrix employed here was originally compiled in order to test hypotheses of superordinal relationships among the morphologically diverse afrotherian crown group, and might not be sufficiently detailed to accurately resolve relationships among stem and crown afrosoricids.

    Certain aspects of occlusal morphology in Dilambdogale and Widanelfarasia are somewhat unexpected given their position as possible “intermediate” taxa—for instance, despite exhibiting features that are typical of protozalambdomorphs (e.g., transversely broad molar crowns, broad sty lar shelves with elongate and buccally oriented prepara- and postmetacristae, reduced metacones that are placed buccal to paracones, a deep ectoflexus on M1–2, and complete absence of pre- and postcingula), the buccal crests of the Fayum afrosoricids are nevertheless arranged in a typically dilambdomorph “W” shape. This odd combination of molar features either suggests that tenrecoid (or afrosoricid) zalambdomorphy is derived from dilambdomorphy, or that Dilambdogale and Widanelfarasia are merely highly derived sister taxa that are members of a dilambdomorph stem afrosoricid clade. By placing Dilambdogale and Widanelfarasia as sister taxa to the exclusion of all other afrotherians, parsimony analysis favors an interpretation in which their dilambdomorph arrangement of the buccal crests is simply a specialization of an extinct side branch (Figs. 12, 13).

    Fig. 12.

    Phylogenetic analysis of living and extinct afrotherians, with Dilambdogale and Todralestes added to a modified version of the matrices employed by Seiffert (2007) and Barrow et al. (2010). A. Single most parsimonious tree derived from analysis with some multistate characters ordered and scaled; tree length = 18746.434, consistency index excluding uninformative characters = 0.49, retention index = 0.44, rescaled consistency index = 0.28. B. Adams consensus of 63 equally parsimonious trees derived from analysis with all multistate characters unordered, and Afrodon excluded; tree length = 19579, consistency index excluding uninformative characters = 0.49, retention index = 0.44, rescaled consistency index = 0.28. Dashed lines indicate branches that are present in the Adams tree, but not in the strict consensus of all MPTs.

    f12_599.eps

    Parsimony analyses provide a simple and straightforward directional explanation for the distribution of molar occlusal features among afrosoricids through time, and are also highly consistent with stratigraphic ordering of the taxa concerned —i.e., older taxa generally exhibit primitive dental features, while successively younger taxa acquire features of the euzalambdomorph dental pattern through the later Paleogene. The only undoubted fossil afrosoricid in the analysis, early Miocene Protenrec—a genus that has consistently been interpreted as a tenrecoid, despite its relatively generalized dental morphology (Butler and Hopwood 1957; Butler 1969, 1972, 1978, 1984; Asher and Hofreiter 2006)—is surprisingly most parsimoniously placed as a sister taxon of crown Afrosoricida when some multistate characters are ordered and scaled (Figs. 12A, 13A). In the absence of contradictory evidence, a logical interpretation of this phylogenetic pattern would be that the absence of euzalambdomorphs in the Paleogene of Afro-Arabia is best explained by a very late divergence of chrysochloroids and tenrecoids, possibly in the later Oligocene.

    Fig. 13.

    Phylogenetic analysis with the poorly-known latest Paleocene genus Afrodon included. A. Single most parsimonious tree derived from analysis with some multistate characters ordered and scaled; tree length = 18748.435, consistency index excluding uninformative characters = 0.49, retention index = 0.44, rescaled consistency index = 0.28. B. Adams consensus of 97 equally parsimonious trees derived from analysis with all multistate characters unordered, and Afrodon included; tree length = 19582, consistency index excluding uninformative characters = 0.49, retention index = 0.45, rescaled consistency index = 0.28. Dashed lines indicate branches that are present in the Adams tree, but not in the strict consensus of all MPTs.

    f13_599.eps

    The possibility of such a late origin for crown Afrosoricida is strongly contradicted, however, by molecular divergence estimates that place the chrysochloroid-tenrecoid split about 40 million years earlier—in either the latest Cretaceous or earliest Paleocene (Springer et al. 2003; Gilbert et al. 2006; Poux et al. 2008). Indeed, the relationship between tenrecs and golden moles is distant enough that the two have not consistently been recovered as sister taxa in molecular phylogenetic analyses (Murata et al. 2003; Waddell and Shelley 2003; Kitazoe et al. 2007; Arnason et al. 2008). It is unlikely that the timing of the chrysochloroid-tenrecoid divergence has been dramatically overestimated by these molecular analyses, because dating of other splits within Afrotheria, particularly those within Paenungulata, are generally remarkably consistent with that group's much better fossil record.

    When one of the topologies recovered by the parsimony analyses presented here (Fig. 13A) is plotted against time within the context of a latest Cretaceous divergence of chrysochloroids and tenrecoids (Fig. 14), and rooted with the oldest known paenungulate, Eritherium (Gheerbrant 2009), the picture becomes much more complicated, and the topology arguably becomes far less likely, because such an ancient split implies extraordinarily long Paleogene “ghost lineages” for all of crown Afrosoricida, and an unsampled >45 Ma-long interval for the lineage leading to Protenrec. The extremely short internodes along the afrosoricid stem lineage also leave very little time for the evolution of zalambdomorphy. As such, when metacone loss is reconstructed within Afrosoricida using a maximum likelihood approach on the time-calibrated phylogeny (Fig. 14), the last common ancestor of crown Afrosoricida, and even the last common ancestor of crown Tenrecoidea, is optimized as having had distinct but reduced M2 metacones. Parsimony analysis cannot incorporate these considerations as background information, but such evidence calls into question the likelihood of the topology itself, at least as it relates to the origin of zalambomorphy.

    Fig. 14.

    Implied ghost lineages and maximum likelihood reconstructions of M2 metacone size (treated as an ordered character with four states), given one of the topologies (Fig. 12A) recovered by parsimony analysis of morphological data. Here the topology is plotted against time, with major divergences among clades with extant representatives based on the molecular estimates of Douady et al. (2003) for Macroscelidea, Poux et al. (2008) for Tenrecoidea, and Gilbert et al. (2006) for the origin of crown Chrysochloroidea. The depth of the PotamogaleMicropotamogale divergence has not been estimated using molecular data, and is here arbitrarily placed at half the time depth of Potamogalidae. An origin of crown Afrotheria at ∼80 Ma is supported by various studies (e.g., Springer et al. 2003). Although parsimony reconstructs metacone loss as homologous in tenrecs and golden moles, note that when branch lengths are taken into account for maximum likelihood reconstructions (“MLR”, computed in Mesquite v. 2.72; Maddison and Maddison 2005), the common ancestors of crown Afrosoricida and crown Tenrecoidea are reconstructed as having had a reduced but distinct M2 metacone, the former with high proportional likelihood (0.779). These data, combined with the numerous zalambdomorph Paleogene ghost lineages that are required by the parsimony-based topology, arguably call into question the likelihood of the topology itself.

    f14_599.eps

    There are additional taxa from the Fayum succession that are currently too fragmentary to be included in the parsimony analysis, but that nevertheless might come to bear decisively on this issue should more material be recovered. Notably, the tiny species Eochrysochloris tribosphenus—at present represented solely by mandibular fragments, a partial p3, and crowns of p4 and m2 (Seiffert et al. 2007)—exhibits an m2 talonid morphology in which the cristid obliqua is oriented only slightly lingually, leaving a relatively shallow hypoflexid for an occluding paracone when compared with those of Dilambdogale, Widanelfarasia, Jawharia, and Qatranilestes. Eochrysochloris also has a very tall trigonid, and the occlusal pattern of M2 is predicted to be associated with an occluding m2 that would be transversely broad, but not dilambdomorph (Seiffert et al. 2007). This poorly-known but very distinctive genus reveals that there are two groups of probable afrosoricids in the Paleogene of northern Africa, the other being represented by Dilambdogale, Widanelfarasia, Jawharia, and Qatranilestes, all of which have deep hypoflexids. It was previously argued by Seiffert et al. (2007) that the latter group documents gradual acquisition of tenrecoid zalambdomorphy from dilambdomorphy through the later Paleogene, while Eochrysochloris documents acquisition of chrysochloroid zalambdomorphy through a very different transformation of upper molar occlusal morphology. This scenario is, however, still highly speculative, and must be tested by the recovery of much more complete fossil material.

    While it appears increasingly likely that the Fayum afrosoricids are of relevance for understanding the origins of Tenrecoidea and Chrysochloroidea, these taxa also provide some interesting clues that might help to explain the higherlevel affinities of older insectivoran-grade placentals from Afro-Arabia such as Afrodon, Garatherium, and Todralestes. Garatherium was originally identified as a peradectine marsupial on the basis of an isolated upper molar from the early Eocene E1 Kohol locality in Algeria (Crochet 1984), but was subsequently reinterpreted as a dilambdomorph adapisoriculid (Gheerbrant 1991a, 1995). The well-developed dilambdomorphy seen on the M1 of Dilambdogale and Widanelfarasia is similar to, though less extreme than, that of Garatherium, and all three taxa have broad stylar shelves, restricted trigons, elongate postmetacristae, no pre- or postcingula, and small conules. Like Garatherium, Dilambdogale has relatively distinct (as opposed to crestiform) stylar cusps, and variably exhibits a postparaconule crista, which was not previously clearly present in the micro-CT reconstructions of Widanelfarasia. In many ways therefore Dilambdogale appears to be structurally intermediate between Garatherium and Widanelfarasia, while Widanelfarasia is in turn structurally intermediate between the older dilambdomorphs and tenrecoids. If Garatherium is an early stem tenrecoid, its age (∼56–54 Ma) would be in line with molecular estimates for the timing of the chrysochlorid-tenrecoid divergence.

    Dilambdogale's position as a morphological and phylogenetic intermediate between tenrecoids and adapisoriculids takes on new significance in light of a recent analysis that has suggested a close relationship between Afrodon and the enigmatic Late Cretaceous placental Deccanolestes from India (Prasad et al. 2010). Analysis of adapisoriculid tarsals from the late Paleocene of Europe has also suggested that Deccanolestes is closely related to European adapisoriculids (Smith et al. 2009). On the basis of tarsal morphology, Deccanolestes has, however, been interpreted as a possible “archontan” or euarchontan (Prasad and Godinot 1994; Kielan-Jaworowska et al. 2004; Smith et al. 2009), and not as a possible afrotherian. If Deccanolestes is in fact allied with adapisoriculids as argued by Prasad et al. (2010), this interpretation would appear to be consistent with Storch's (2008) recent analysis of adapisoriculid humeri, which led him to suggest that the family has plesiadapiform (and hence euarchontan, and possibly even primate) affinities. Notable exceptions to the interpretation of Deccanolestes as a basal euarchontan are the studies of Wible et al. (2007), which placed Deccanolestes as a stem placental, and that of Rana and Wilson (2003), who considered Deccanolestes to be of uncertain affinities within Placentalia. Most recently, Boyer et al. (2010) described a distal humerus and proximal ulna of Deccanolestes, and concluded that its distal humerus is more primitive than the adapisoriculid humeri described by Storch (2008), and morphologically intermediate between Late Cretaceous Protungulatum and Procerberus, and definitive euarchontans. Breakage of the distal humerus that is here attributed to Dilambdogale does not allow for extensive comparison, but in preserved morphology the humeral morphology of Dilambdogale appears to be quite similar to that of Deccanolestes, and both are similar to generalized tenrecoids such as Microgale.

    Given the enormous amount of homoplasy that has occurred in the dentition of placental mammals, the meaning of the occlusal similarities shared by Deccanolestes, adapisoriculids, and afrosoricids is by no means clear at the moment. There can be little doubt, however, that the dental morphology of Deccanolestes closely approximates the primitive morphotype for crown placentals; as was argued by Kielan-Jaworowska et al. (2004: 505): “molar morphology of Deccanolestes differs substantially from that of Cimolestes and similar taxa...mainly in the presumed retention of plesiomorphies”. Primitive adapisoriculids such as Afrodon and Bustylus are similarly generalized, to the extent that the latter was first described as a marsupial by Crochet and Sigé (1983). The fact that adapisoriculids have been proposed as possible marsupials, basal euarchontans, and herein as possible basal afrosoricids—the latter two of which are now known to be very distantly related within Placentalia (Fig. 1)—could indicate that many, if not most, aspects of dental morphology in Afrodon, Bustylus, and Deccanolestes were present in the last common ancestor of crown Placentalia (a hypothesis that is supported by the very basal placement of Deccanolestes in Wible et al.'s [2007] phylogenetic analysis), and that the most basal members of Afrotheria, Euarchontoglires, Laurasiatheria, and Xenarthra might be identified as “adapisoriculid” on the basis of dental features. This possibility is particularly compelling in light of the results of the phylogenetic analyses presented here, which consistently placed Afrosoricida as the sister group of all other afrotherians, rather than as the sister group of Macroscelidea and/or Tubulidentata as in many molecular studies (Fig. 1). This phylogenetic arrangement implies an insectivoran-grade (and perhaps dentally adapisoriculid-like), rather than condylarthran-grade, ancestor for crown Afrotheria (see discussion in Seiffert 2002; Robinson and Seiffert 2004; Seiffert 2007; Tabuce et al. 2008; Asher and Seiffert 2010). Paleontological sampling in the Late Cretaceous of Africa, ideally from horizons near the estimated time of origin of Afrotheria (i.e., ∼80 Ma, early to mid-Campanian) is now desperately needed to test these and other hypotheses bearing on afrotherian origins.

    Acknowledgements

    I would like to thank the staff of the Egyptian Mineral Resources Authority and the CGM for supporting and facilitating paleontological research in the Fayum area; Elwyn L. Simons and Prithijit Chatrath (both DPC) for providing access to the Duke collections and facilitating fieldwork in the Fayum area; Hesham Sallam (University of Oxford, Oxford, UK), Michelle Gignac (Duke University, Durham, USA), and Owen Green (University of Oxford, Oxford, UK) for assistance with scanning electron micrography; Emmanuel Gheerbrant (Muséum National d'Histoire Naturelle, Paris, France), Bernard Marandat (Université Montpellier 2, Montpellier, France), and Rodolphe Tabuce (Université Montpellier 2, Montpellier, France) for providing access to comparative fossil material from Algeria and Morocco; Walter Joyce (YPM) for relocating, and providing access to, the specimens of Qatranilestes housed in the Yale Peabody Museum; and 2001–2009 Fayum field crews for work at locality BQ-2 that led to the recovery of fossils described here. Robert Asher (Cambridge University, Cambridge, UK), Richard L. Cifelli (Sam Noble Oklahoma Museum of Natural History, Norman, USA), and an anonymous reviewer provided helpful comments that improved the manuscript. This research was funded by the US National Science Foundation and The Leakey Foundation. This is Duke Lemur Center publication No. 1182.

    References

    1.

    H. Amrine-Madsen , K.-P. Koepfli , R.K. Wayne , and M.S. Springer 2003. A new phylogenetic marker, apolipoprotein B, provides compelling evidence for eutherian relationships. Molecular Phylogenetics and Evolution 28: 225–240.  http://dx.doi.org/10.1016/S1055-7903 (03)00118-0 Google Scholar

    2.

    U. Arnason , J.A. Adegoke , A. Gullberg , E.H. Harley , A. Janke , and M. Kullberg 2008. Mitogenomic relationships of placental mammals and molecular estimates of their divergences. Gene 421: 37–51.  http://dx.doi.org/10.1016/j.gene.2008.05.024 Google Scholar

    3.

    R.J. Asher 2005. Insectivoran-grade placentals. In : K.D. Rose and J.D. Archibald (eds.), The Rise of Placental Mammals: Origins and Relationships of the Major Extant Clades , 50–70. Johns Hopkins University Press, Baltimore. Google Scholar

    4.

    R.J. Asher 2007. A web-database of mammalian morphology and a reanalysis of placental phylogeny. BMC Evolutionary Biology 7 (108): 1–10. Google Scholar

    5.

    R.J. Asher and D.M. Avery 2010. New golden moles (Afrotheria, Chrysochloridae) from the Pliocene of South Africa. Paleontologica Electronica 13 (1): 3A. Google Scholar

    6.

    R.J. Asher and K.M. Helgen 2010. Nomenclature and placental mammal phylogeny. BMC Evolutionary Biology 10 (102): 1–9. Google Scholar

    7.

    R.J. Asher and M. Hofreiter 2006. Tenrec phylogeny and the noninvasive extraction of nuclear DNA. Systematic Biology 55: 181–194.  http://dx.doi.org/10.1080/10635150500433649 Google Scholar

    8.

    R.J. Asher and M.R. Sanchez-Villagra 2005. Locking yourself out: diversity among dentally zalambdodont therian mammals. Journal of Mammalian Evolution 12: 265–282.  http://dx.doi.org/10.1007/s10914-005-5725-3 Google Scholar

    9.

    R.J. Asher and E.R. Seiffert 2010. Systematics of endemic African mammals. In : W.J. Sanders and L. Werdelin (eds.), Cenozoic Mammals of Africa , 911–928. University of California Press, Berkeley. Google Scholar

    10.

    R.J. Asher , M.J. Novacek , and J.H. Geisler 2003. Relationships of endemic African mammals and their fossil relatives based on morphological and molecular evidence. Journal of Mammalian Evolution 10: 131–194.  http://dx.doi.org/10.1023/A:1025504124129 Google Scholar

    11.

    E. Barrow , E.R. Seiffert , and E.L. Simons 2010. A primitive hyracoid (Mammalia, Paenungulata) from the early Priabonian (late Eocene) of Egypt. Journal of Systematic Palaeontology 8: 213–244. Google Scholar

    12.

    D.M. Boyer , G.V.R. Prasad , D.W. Krause , M. Godinot , A. Goswami , O. Verma , and J.J. Flynn 2010. New postcrania of Deccanolestes from the Late Cretaceous of India and their bearing on the evolutionary and biogeographic history of euarchontan mammals. Naturwissenschaften 97: 365–377.  http://dx.doi.org/10.1007/s00114-010-0648-0 Google Scholar

    13.

    P.M. Butler 1969. Insectivores and bats from the Miocene of East Africa: new material. In : L.S.B. Leakey (ed.), Fossil Vertebrates of Africa , 1–37. Academic Press, London. Google Scholar

    14.

    P.M. Butler 1972. The problem of insectivore classification. In : K.A. Joysey and T.S. Kemp (eds.), Studies in Vertebrate Evolution , 253–265. Oliver and Boyd, Edinburgh. Google Scholar

    15.

    P.M. Butler 1978. Insectivora and Chiroptera. In : V.J. Maglio and H.B.S. Cooke (eds.), Evolution of African Mammals , 56–68. Harvard University Press, Cambridge, Mass. Google Scholar

    16.

    P.M. Butler 1984. Macroscelidea, Insectivora and Chiroptera from the Miocene of east Africa. Palaeovertebrata 14: 117–200. Google Scholar

    17.

    P.M. Butler 1988. Phylogeny of the insectivores. In : M.J. Benton (ed.), The Phylogeny and Classification of the Tetrapods, Volume 2: Mammals , 117–141. Clarendon Press, Oxford. Google Scholar

    18.

    P.M. Butler and A.T. Hopwood 1957. Insectivora and Chiroptera from the Miocene rocks of Kenya colony. Fossil Mammals of Africa 13: 1–35. Google Scholar

    19.

    J.-Y. Crochet 1984. Garatherium mahboubii nov. gen., nov. sp., marsupial de l'Eocène inférieur d'El Kohol (Sud Oranais, Algérie). Annales de Paléontologie 70: 275–294. Google Scholar

    20.

    J.-Y. Crochet 1988. Le plus ancien Créodonte africain: Koholia atlasense nov. gen., nov. sp. (Eocène inférieur d'El Kohol, Atlas saharien, Algérie). Comptes Rendus de l'Académie des Sciences Paris, Ser. II 307: 1795–1798. Google Scholar

    21.

    J.-Y. Crochet and B. Sigé 1983. Les Mammifères montiens de Hainin (Paléocène de Belgique). Part III. Marsupiaux. Palaeovertebrata 13: 51–64. Google Scholar

    22.

    C.J. Douady , F. Catzeflis , J. Raman , M.S. Springer , and M.J. Stanhope 2003. The Sahara as a vicariant agent, and the role of Miocene climatic events, in the diversification of the mammalian order Macroscelidea (elephant shrews). Proceedings of the National Academy of Sciences, USA 100: 8325–8330.  http://dx.doi.org/10.1073/pnas.0832467100 Google Scholar

    23.

    C.J. Douady and E.J.P. Douzery 2003. Molecular estimation of eulipotyphlan divergence times and the evolution of “Insectivora”. Molecular Phylogenetics and Evolution 28: 285–296.  http://dx.doi.org/10.1016/S1055-7903 (03)00119-2 Google Scholar

    24.

    E. Gheerbrant 1988. Afrodon chleuhi nov. gen., nov. sp., “insectivores” (Mammalia, Eutheria) lipotyphlé (?), du Paléocène marocain: données préliminaires. Comptes Rendus de l'Académie des Sciences Paris II 307: 1303–1309. Google Scholar

    25.

    E. Gheerbrant 1991a. Bustylus (Eutheria, Adapisoriculidae) and the absence of ascertained marsupials in the Palaeocene of Europe. Terra Nova 3: 586–592.  http://dx.doi.org/10.1111/j.1365-3121.1991.tb00200.x Google Scholar

    26.

    E. Gheerbrant 1991b. Todralestes variablis n. g., n. sp., nouveau Proteuthérien (Eutheria, Todralestidae fam. nov.) du Paléocène du Maroc. Comptes Rendus de l'Académie des Sciences Paris, Ser. II 312: 1249–1255. Google Scholar

    27.

    E. Gheerbrant 1992. Les mammifères paléocenes du Bassin d'Ouarzazate (Maroc). I. Introduction général et palaeoryctidae. Palaeontographica, Abteilung A 224: 67–132. Google Scholar

    28.

    E. Gheerbrant 1993. Premières données sur les mammifères “insectivores” de l'Yprésian du Bassin d'Ouarzazate (Maroc: site de N'Tagourt 2). Neues Jahrbuch für Geologie und Paläontologie Abhhandlungen 187:225–242. Google Scholar

    29.

    E. Gheerbrant 1994. Les mammifères paléocenes du Bassin d'Ouarzazate (Maroc). II. Todralestidae (Proteutheria, Eutheria). Palaeontographica, Abteilung A 231: 133–188. Google Scholar

    30.

    E. Gheerbrant 1995. Les mammifères paléocènes du Bassin d'Ouarzazate (Maroc). III. Adapisoriculidae et autres mammifères (Carnivora, ?Creodonta, Condylarthra, ?Ungulata et incertae sedis). Palaeontographica, Abteilung A 237: 39–132. Google Scholar

    31.

    E. Gheerbrant 2009. Paleocene emergence of elephant relatives and the rapid radiation of African ungulates. Proceedings of the National Academy of Sciences USA 106: 10717–10721.  http://dx.doi.org/10.1073/pnas.0900251106 Google Scholar

    32.

    E. Gheerbrant and J.-L. Hartenberger 1999. Nouveau mammifère insectivore (?Lipotyphla, ?Erinaceomorpha) de l'Eocène inférieur de Chambi (Tunisie). Paläontologische Zeitschrift 73: 143–156. Google Scholar

    33.

    E. Gheerbrant , J. Sudre , S. Sen , C. Abrial , B. Marandat , B. Sigé , and M. Vianey-Liaud 1998. Nouvelles données sur les mammifères du Thanétien et de l'Yprésian du Bassin d'Ouarzazate (Maroc) et leur contexte stratigraphique. Palaeovertebrata 27: 155–202. Google Scholar

    34.

    C. Gilbert , P.C. O'Brien , G. Bronner , F. Yang , A. Hassanin , M.A. Ferguson-Smith , and T.J. Robinson 2006. Chromosome painting and molecular dating indicate a low rate of chromosomal evolution in golden moles (Mammalia, Chrysochloridae). Chromosome Research 14: 793–803.  http://dx.doi.org/10.1007/s10577-006-1091-0 Google Scholar

    35.

    T. Gill 1883. On the classification of the insectivorous mammals. Bulletin of the Philosophical Society of Washington 5: 118–120. Google Scholar

    36.

    J.E. Gray 1821. On the natural arrangement of vertebrose animals. London Medical Repository 15: 296–310. Google Scholar

    37.

    G.F. Gunnell , E.L. Simons , and E.R. Seiffert 2008. New bats (Mammalia: Chiroptera) from the late Eocene and early Oligocene, Fayum Depression, Egypt. Journal of Vertebrate Paleontology 28: 1–11.  http://dx.doi.org/10.1671/0272-4634 (2008)28[1:NBMCFT]2.0.CO;2 Google Scholar

    38.

    M.E. Kellogg , S. Burkett , T.R. Dennis , G. Stone , B.A. Gray , P.M. McGuire , R.T. Zori , and R. Stanyon 2007. Chromosome painting in the manatee supports Afrotheria and Paenungulata. BMC Evolutionary Biology 7: 6. Google Scholar

    39.

    Z. Kielan-Jaworowska , R.L. Cifelli , and Z.-X. Luo 2004. Mammals from the Age of Dinosaurs: Origins, Evolution, and Structure. 630 pp. Columbia University Press, New York. Google Scholar

    40.

    Y. Kitazoe , H. Kishino , P.J. Waddell , N. Nakajima , T. Okabayashi , T. Watabe , and Y. Okuhara 2007. Robust time estimation reconciles views of the antiquity of placental mammals. PLoS ONE 2 (4): e384.  http://dx.doi.org/10.1371/journal.pone.0000384 Google Scholar

    41.

    A. Lopatin 2006. Early Paleogene insectivore mammals of Asia and establishment of the major groups of Insectivora. Paleontological Journal 40, supplement 3: S205–S405.  http://dx.doi.org/10.1134/S0031030106090012 Google Scholar

    42.

    W.P. Maddison and D.R. Maddison 2005. Mesquite: A modular system for evolutionary analysis, Version 1.06.  http://mesquiteproject.org/ Google Scholar

    43.

    O. Madsen , M. Scally , C.J. Douady , D.J. Kao , R.W. DeBry , R. Adkins , H.M. Amrine , M.J. Stanhope , W.W. de Jong , and M.S. Springer 2001. Parallel adaptive radiations in two major clades of placental mammals. Nature 409: 610–614.  http://dx.doi.org/10.1038/35054544 Google Scholar

    44.

    M. Mahboubi , R. Ameur , J.-Y. Crochet , and J.-J. Jaeger 1986. El Kohol (Saharan Atlas, Algeria): A new Eocene mammal locality in northwestern Africa. Palaeontographica, Abteilung A 192: 15–49. Google Scholar

    45.

    S.B. McDowell 1958. The Greater Antillean insectivores. Bulletin of the American Museum of Natural History 115: 115–214. Google Scholar

    46.

    Y. Murata , M. Nikaido , T. Sasaki , Y. Cao , Y. Fukumoto , M. Hasegawa , and N. Okada 2003. Afrotherian phylogeny inferred from complete mitochondrial genomes. Molecular Phylogenetics and Evolution 28: 253–260.  http://dx.doi.org/10.1016/S1055-7903 (03)00035-6 Google Scholar

    47.

    W.J. Murphy , E. Eizirik , S.J. O'Brien , O. Madsen , M. Scally , C.J. Douady , E. Teeling , O.A. Ryder , M.J. Stanhope , W.W. de Jong , and M.S. Springer 2001. Resolution of the early placental mammal radiation using Bayesian phylogenetics. Science 294: 2348–2351.  http://dx.doi.org/10.1126/science. 1067179 Google Scholar

    48.

    M. Nikaido , H. Nishihara , Y. Hukumoto , and N. Okada 2003. Ancient SINEs from African endemic mammals. Molecular Biology and Evolution 20: 522–527.  http://dx.doi.org/10.1093/molbev/msg052 Google Scholar

    49.

    C. Poux , O. Madsen , J. Glos , W.W. de Jong , and M. Vences 2008. Molecular phylogeny and divergence times of Malagasy tenrecs: Influence of data partitioning and taxon sampling on dating analyses. BMC Evolutionary Biology 8: 16.  http://dx.doi.org/10.1186/1471-2148-8-102 Google Scholar

    50.

    G.V.R. Prasad and M. Godinot 1994. Eutherian tarsal bones from the late Cretaceous of India. Journal of Paleontology 68: 892–902. Google Scholar

    51.

    G.V.R. Prasad , O. Verma , E. Gheerbrant , A. Goswami , A. Khosla , V. Parmar , and A. Sahni 2010. First mammal evidence from the Late Cretaceous of India for biotic dispersal between India and Africa at the KT transition. Comptes Rendus Palevol 9: 63–71. Google Scholar

    52.

    R.S. Rana and G.P. Wilson 2003. New Late Cretaceous mammals from the Intertrappean beds of Rangapur, India and paleobiogeographic framework. Acta Palaeontologica Polonica 48: 331–348. Google Scholar

    53.

    T.J. Robinson and E.R. Seiffert 2004. Afrotherian origins and interrelationships: New views and future prospects. Currents Topics in Developmental Biology 63: 37–60.  http://dx.doi.org/10.1016/S0070-2153 (04)63002-X Google Scholar

    54.

    T.J. Robinson , B. Fu , M.A. Ferguson-Smith , and F. Yang 2004. Cross-species chromosome painting in the golden mole and elephant-shrew: support for the mammalian clades Afrotheria and Afroinsectiphillia but not Afroinsectivora. Proceedings of the Royal Society London, B 271: 1477–1484.  http://dx.doi.org/10.1098/rspb.2004.2754 Google Scholar

    55.

    A.L. Roca , G.K. Bar-Gal , E. Eizirik , K.M. Helgen , R. Maria , M.S. Springer , S.J. O'Brien , and W.J. Murphy 2004. Mesozoic origin for West Indian insectivores. Nature 429: 649–651.  http://dx.doi.org/10.1038/nature02597 Google Scholar

    56.

    H. Sallam , E.R. Seiffert , and E.L. Simons 2010a. A highly derived anomalurid rodent (Mammalia) from the earliest late Eocene of Egypt. Palaeontology 53: 803–813. Google Scholar

    57.

    H. Sallam , E.R. Seiffert , D.M. Boyer , and E.L. Simons 2010b. Postcranial morphology of an anomaluroid rodent from the late Eocene of Egypt. Journal of Vertebrate Paleontology 30 (Supplement): 155A. Google Scholar

    58.

    H.M. Sallam , E.R. Seiffert , E.L. Simons , and C. Brindley 2010c. A large-bodied anomaluroid rodent from the earliest late Eocene of Egypt: Phylogenetic and biogeographic implications. Journal of Vertebrate Paleontology 30: 1579–1593. Google Scholar

    59.

    J.A. Salton and E.J. Sargis 2008. Evolutionary morphology of the Tenrecoidea (Mammalia) forelimb skeleton. In : E.J. Sargis and M. Dagosto (eds.), Mammalian Evolutionary Morphology: A Tribute to Frederick S. Szalay , 51–71. Springer, New York. Google Scholar

    60.

    E.R. Seiffert 2002. The reality of afrotherian monophyly, and some of its implications for the evolution and conservation of Afro-Arabia's endemic placental mammals. Afrotherian Conservation 1: 3–6. Google Scholar

    61.

    E.R. Seiffert 2006. Revised age estimates for the later Paleogene mammal faunas of Egypt and Oman. Proceedings of the National Academy of Sciences, USA 103: 5000–5005.  http://dx.doi.org/10.1073/pnas.0600689103 Google Scholar

    62.

    E.R. Seiffert 2007. A new estimate of afrotherian phylogeny based on simultaneous analysis of genomic, morphological, and fossil evidence. BMC Evolutionary Biology 7: 224.  http://dx.doi.org/10.1186/1471-2148-7-224 Google Scholar

    63.

    E.R. Seiffert 2010. Paleogene “insectivores”. In : W.J. Sanders and L. Werdelin (eds.), Cenozoic Mammals of Africa , 253–260. University of California Press, Berkeley. Google Scholar

    64.

    E.R. Seiffert and E.L. Simons 2000. Widanelfarasia, a diminutive placental from the late Eocene of Egypt. Proceedings of the National Academy of Sciences, USA 97: 2646–2651.  http://dx.doi.org/10.1073/pnas.040549797 Google Scholar

    65.

    E.R. Seiffert , T.M. Bown , W.C. Clyde , and E.L. Simons 2008. Geology, paleoenvironment, and age of Birket Qarun locality 2 (BQ-2), Fayum Depression, Egypt. In : J.G. Fleagle and C.C. Gilbert (eds.), Elwyn L. Simons: A Search for Origins , 71–86. Springer, New York. Google Scholar

    66.

    E.R. Seiffert , E.L. Simons , T.M. Ryan , T.M. Bown , and Y. Attia 2007. New remains of Eocene and Oligocene Afrosoricida (Afrotheria) from Egypt, with implications for the origin (s) of afrosoricid zalambdodonty. Journal of Vertebrate Paleontology 27 (4): 963–972.  http://dx.doi.org/10.1671/0272-4634 (2007)27[963:NROEAO]2.0.CO;2 Google Scholar

    67.

    N.B. Simmons and J.H. Geisler 1998. Phylogenetic relationships of Icaronycteris, Archaeonycteris, Hassianycteris, and Palaeochiropteryx to extant bat lineages, with comments on the evolution of echolocation and foraging strategies in Microchiroptera. Bulletin of the American Museum of Natural History 235: 4–182. Google Scholar

    68.

    T. Smith , E. De Bast , and B. Sigé 2009. Adapisoriculid mammals from the Paleocene of Hainin (Belgium) shed light on the phylogenetic affinities of the enigmatic arboreal Cretaceous Deccanolestes from the Deccan Traps of India. Journal of Vertebrate Paleontology 29: 183A. Google Scholar

    69.

    M.S. Springer , G.C. eleven , O. Madsen , W.W. de Jong , V.G. Waddell , H.M. Amrine , and M.J. Stanhope 1997. Endemic African mammals shake the phylogenetic tree. Nature 388: 61–64.  http://dx.doi.org/10.1038/40386 Google Scholar

    70.

    M.S. Springer , W.J. Murphy , E. Eizirik , and S.J. O'Brien 2003. Placental mammal diversification and the Cretaceous-Tertiary boundary. Proceedings of the National Academy of Sciences, USA 100: 1056–1061.  http://dx.doi.org/10.1073/pnas.0334222100 Google Scholar

    71.

    M.S. Springer , M.J. Stanhope , O. Madsen , and W.W. de Jong 2004. Molecules consolidate the placental mammal tree. Trends in Ecology and Evolution 19: 430–438.  http://dx.doi.org/10.1016/j.tree.2004.05.006 Google Scholar

    72.

    M.J. Stanhope , V.G. Waddell , O. Madsen , W. de Jong , S.B. Hedges , G.C. Cleven , D. Kao , and M.S. Springer 1998. Molecular evidence for multiple origins of Insectivora and for a new order of endemic African insectivore mammals. Proceedings of the National Academy of Sciences, USA 95: 9967–9972.  http://dx.doi.org/10.1073/pnas.95.17.9967 Google Scholar

    73.

    G. Storch 2008. Skeletal remains of a diminutive primate from the Paleocene of Germany. Naturwissenschaften 95: 927–930.  http://dx.doi.org/10.1007/s00114-008-0401-0 Google Scholar

    74.

    D.L. Swofford 1998. PAUP* Phylogenetic Analysis Using Parsimony (*and Other Methods), Version 4. Sinauer Associates, Sunderland, MA. Google Scholar

    75.

    R. Tabuce , R.J. Asher , and T. Lehmann 2008. Afrotherian mammals: a review of current data. Mammalia 72: 2–14.  http://dx.doi.org/10.1515/MAMM.2008.004 Google Scholar

    76.

    P.J. Waddell and S. Shelley 2003. Evaluating placental inter-ordinal phylogenies with novel sequences including RAG1, ?-fibrinogen, ND6, and mt-tRNA, plus MCMC-driven nucleotide, amino acid, and codon models. Molecular Phylogenetics and Evolution 28: 197–224.  http://dx.doi.org/10.1016/S1055-7903 (03)00115-5 Google Scholar

    77.

    J.R. Wible , G.W. Rougier , M.J. Novacek , and R.J. Asher 2007. Cretaceous eutherians and Laurasian origin for placental mammals near the K/T boundary. Nature 447: 1003–1006.  http://dx.doi.org/10.1038/nature05854 Google Scholar

    78.

    F. Yang , E.Z. Alkalaeva , P.L. Perelman , A.T. Pardini , W.R. Harrison , P.C.M. O'Brian , B. Fu , A.S. Graphodatsky , M.A. Ferguson-Smith , and T.J. Robinson 2003. Reciprocal chromosome painting among human, aardvark, and elephant (superorder Afrotheria) reveals the likely eutherian ancestral karyotype. Proceedings of the National Academy of Sciences, USA 100 (3): 1062–1066.  http://dx.doi.org/10.1073/pnas.0335540100 Google Scholar

    Notes

    [1] * In what follows I employ the terminology recently proposed by Lopatin (2006), which is useful for distinguishing important differences between taxa that have been termed “zalambdodont” and “dilambdodont” (Gill 1883). The broad category of “zalambdomorphy” is defined by Lopatin (2006: S215) as follows: “the trigon of the upper molars is formed by a large lingually located paracone, a paracrista that is V-shaped in projection, and styles; the metacone and protocone are considerably reduced or absent, the conules are absent … in this pattern, the lower molars are characterized by reduced talonids and excessively developed trigonids, including the formation of the oblique paracristid and a very high and broad transverse protocristid”. “Euzalambdomorphy”, which is present in most extant afrosoricids, is described as “complete loss of the metacone and protocone, the lingual displacement of the paracone to the position of the protocone, excessive development of the stylar shelf, and appearance of supplementary cingular elements … the talonid is extremely reduced and resembles a postcingulid” (Lopatin 2006: S215) while in “protozalambdomorphy”, which occurs in extant Potamogale and early Miocene Protenrec, “the metacone is considerably reduced (however, its rudiment is preserved between a shortened centrocrista and postmetacrista), the paracone is displaced to the center, the protocone and talonid are reduced” (Lopatin 2006: S215).

    Erik R. Seiffert "The Oldest and Youngest Records of Afrosoricid Placentals from the Fayum Depression of Northern Egypt," Acta Palaeontologica Polonica 55(4), 599-616, (1 December 2010). https://doi.org/10.4202/app.2010.0023
    Received: 18 February 2010; Accepted: 14 June 2010; Published: 1 December 2010
    JOURNAL ARTICLE
    18 PAGES


    SHARE
    ARTICLE IMPACT
    Back to Top