Revisiting the Developmental Stage and Age-at-Death of the Mrs. Ples Э Sts 5 and Sts 14 Specimens from Sterkfontein South AfricaDo They Belong to the Same Individualкод для вставкиСкачать
THE ANATOMICAL RECORD 291:1707–1722 (2008) Revisiting the Developmental Stage and Age-at-Death of the ‘‘Mrs. Ples’’ (Sts 5) and Sts 14 Specimens from Sterkfontein (South Africa): Do They Belong to the Same Individual? ALEJANDRO BONMATÍ,1,2* JUAN-LUIS ARSUAGA,1,2 AND CARLOS LORENZO1,3 1 Centro de Investigación (UCM-ISCIII) de Evolución y Comportamiento Humanos, c/Sinesio Delgado 4, 28029 Madrid, Spain 2 Dpto. de Paleontologı́a, Facultad de Ciencias Geológicas, Universidad Complutense de Madrid, Ciudad Universitaria, 28040 Madrid, Spain 3 Institut Català de Paleoecologia Humana i Evolució Social, Área de Prehistoria, Facultat de Lletres, Universitat Rovira i Virgili, Pl Imperial Tarraco 1, 43005 Tarragona, Spain ABSTRACT During the 1947 ﬁeldwork season, Member 4 (2-3 My) of the South African Sterkfontein site yielded two important Australopithecus africanus fossils: a cranium popularly nicknamed ‘‘Mrs. Ples" (Sts 5), and a partial skeleton (Sts 14). Previous reports have proposed that Sts 5 was a nonfully grown adolescent individual (Thackeray et al., S Afr J Sci 2002a;98:21–22), and that Sts 14 was a sub-adult specimen (according to various signs of immaturity in the skeleton) (Berge and Gommery, C R Acad Sci Paris, Sciences de la terre et des planètes 1999;329:227–232; Häusler and Berger, J Hum Evol, 2001;40:411–417; Thackeray et al., S Afr J Sci, 2002b;98:211–212). It was subsequently proposed that these fossils actually belonged to the same individual (Thackeray et al., S Afr J Sci, 2002b;98:211–212), a proposition supported by their spatial positions within the site. The present work attempts to revise these different assertions. The results obtained: (i) show that the Sts 5 fossil represents a fully grown adult cranium; (ii) provide new evidence of immaturity in the Sts 14 skeletal elements (sustaining the proposed young adult age of this specimen), and (iii) suggest that although the revised ages-at-death for these fossils are partially compatible, there is no evidence to support the idea that they represent a single individual. Finally, the encephalization quotient associated with a hypothetical union of Sts 5 and Sts 14 (calculated using data from both specimens) lies between the upper and lower limits of the currently estimated range for this species and H. habilis, respectively. Anat Rec, 291:1707–1722, 2008. Ó 2008 Wiley-Liss, Inc. Key words: Sts 5; Sts 14; Australopithecus africanus; development; age-at-death; Sterkfontein *Correspondence to: Alejandro Bonmatı́ Lasso, Centro UCMISCIII de Evolución y Comportamiento Humanos, c/ Sinesio Delgado 4, Pabellón 14, 28029 Madrid, Spain. Fax: 134918222855. E-mail: email@example.com. Grant sponsor: Spanish Ministry of Education and Science; Grant number: CGL2006-13532-C03-02 and 01; Grant sponsor: Duques de Soria Foundation/Atapuerca Foundation. Ó 2008 WILEY-LISS, INC. Received 26 December 2008; Accepted 14 July 2008 DOI 10.1002/ar.20795 Published online 24 October 2008 in Wiley InterScience (www. interscience.wiley.com). 1708 BONMATÍ ET AL. Fig. 1. (a) Location of the Sterkfontein site (modiﬁed from Partridge et al., 1999) where the (b) Sts 5 cranium and (c) Sts 14 partial skeleton were discovered. Scale bar 5 2 cm. INTRODUCTION The Sterkfontein site lies in northeastern South Africa, 10 km NNW of Krugersdorp in the Gauteng province (Fig. 1a). Located within a complex endokarstic system formed by the dissolution of Precambrian dolomite limestone along bedding planes and vertical joints via the action of weakly acidic groundwater (Kuman and Clarke, 2000, p. 829), the cavities at the site became ﬁlled with calcareous bone-bearing breccia. As a consequence of its land-use history and the repeated collapseﬁll sequences involved in its genesis, great efforts were required to ascertain the spatial and temporal sequences of the site (see Brain, 1957, 1958; Robinson, 1962; Robinson and Manson, 1962; Howell, 1967; Tobias and Hughes, 1969; Wilkinson, 1973, 1983; Partridge, 1978; Stiles and Partridge, 1979; Tobias, 1979; Clarke, 1985, 1994; Partridge and Watt, 1991; Kuman and Clarke, 2000). Six lithostratigraphic members were originally identiﬁed (Partridge, 1978; Partridge and Watt, 1991), numbered 1 to 6 (oldest to youngest). Post Member 6, the Stw 53 Inﬁll and the Oldowan Inﬁll were described at a later date (Kuman and Clarke, 2000). Since 1936 about 500 hominid fossil specimens have been recovered from this site (Partridge et al., 2003), the bulk coming from Member 4 (MNI 5 87 individuals; Pickering et al., 2004). Among the most famous of these fossils are the cranium Sts 5 (commonly known as ‘‘Mrs. Ples’’; Fig. 1b) and the partial skeleton Sts 14 (Fig. 1c). Both specimens were discovered during the 1947 ﬁeldwork season within the same lithostratigraphic unit (Member 4C). After having originally been attributed to different species, by the early 1950s the entire Sterkfontein collection (Member 4) was commonly assigned to Australopithecus africanus (Schwartz and Tattersall, 2005). Member 4 broadly corresponds to the Type Site but its geological age has been widely debated. According to Clark (2002), the stratigraphic position and the archaeological and palaeontological content of Member 4 indicate it to encompass the age interval of 2–3 My. Partridge (2005) proposed an age for the Sts 5 cranium of between 2.14 and 2.15 My. According to the original description of Sts 5 by Broom et al. (1950), the degree of closure of the cranial sutures STS 5 AND STS 14: AGE-AT-DEATH REVISITED is in agreement with an individual who was ‘‘no longer young’’ (Broom et al., 1950, p. 14). However, Thackeray et al. (2002a) later identiﬁed immature traits in the dentition. In particular (thanks to the use of high-quality CT scan techniques) they indicated that the apical ends of the roots of the right third molar (RM3) were not fully closed. Similarly, Sts 14 was also originally considered to represent an adult (Robinson, 1972), but again, subsequent studies revealed signs of immaturity in the iliac crest, the ischial tuberosity, the pubic spine, the anterior superior iliac spine (ASIS), the synchondrosis between the ﬁrst and the second sacral vertebrae, and the epiphyseal plate of the sacro-iliac joint (Berge and Gommery, 1999; Häusler and Berger, 2001; Thackeray et al., 2002b). All these latter studies consider Sts 14 to be a subadult individual. In particular, Berge and Gommery (1999) established its owner’s age-at-death to be little more than 12 years from the ossiﬁcation stage of the sacrum. On the basis of their very similar developmental stages and matching sex attributions, Thackeray et al. (2002b) and Gommery and Thackeray (2006) proposed that Sts 5 and Sts 14 might belong to the same individual, a gravitational slump explaining their relative spatial positions within the site. The aim of this study was to reassess the developmental stage and the biological and chronological ages-atdeath of the Sterkfontein Sts 5 and Sts 14 fossils, using developmental information for chimpanzees and extant humans. The results were then used to test whether these specimens are developmentally compatible, and therefore might represent a single individual. Finally, the consistency of the encephalization quotient (EQ) of this hypothetical individual with that currently estimated for A. africanus was investigated. To date, no other Australopithecus skeletons recovered have been well enough preserved to make an accurate assessment of this key aspect of the biology of extinct hominins. Development of Australopithecus africanus Numerous studies have addressed the maturation pattern and growth rate of the extinct species A. africanus, focusing mainly on the calciﬁcation and incremental histological patterns of the dentition and the sequence of tooth emergence and facial growth, but also on the development of the postcranial skeleton. Although some authors (Mann, 1975, 1988; Mann et al., 1987, 1990; Lampl et al., 1993) have supported the idea that the developmental pattern for South African Australopithecus is essentially human-like, it is currently widely accepted that the pattern and timing of postnatal maturation in this species is essentially ape-like (Bromage, 1985, 1986, 1987; Bromage and Dean, 1985; Beynon, 1986; Smith, 1986, 1987, 2004; Conroy and Vannier, 1987, 1988, 1991; Beynon and Wood, 1987; Dean, 1987a,b, 1988, 2000; Beynon and Dean, 1988; Berge, 1998; Dean et al., 2001; Anemone, 2002). Relative Maturation of the Cranial and Postcranial Systems Sts 5 is edentulous; only indirect information on the length of the roots can be gleaned from the depths of the alveoli (see later). Therefore, to test the consistency between Sts 5 cranial and Sts 14 postcranial develop- 1709 ment, skeletal traits were examined. In particular, by taking into account the preservation of these specimens and making use of information in the literature, the slightly earlier closure of the spheno-occipital synchondrosis (SOS) relative to the ossiﬁcation of the epiphysis of the iliac crest was conﬁrmed (Stewart, 1934; Zilhman, 2007). However, the time span between these maturational events is quite small and reversals of this sequence are not uncommon in modern human populations (Stewart, 1934). Therefore, it was considered that both events take place at roughly the same time, and that small advances or delays of one relative to the other are within the normal range of variation. These advances/delays occur because certain sets of bones are more sensitive to factors affecting skeletal development (see Tanner, 1962), causing some degree of variability in the ossiﬁcation sequence. MATERIALS AND METHODS The Sts 5 specimen is a near complete cranium with some parts of the cranial vault and the dentition missing (Fig. 1b). Sts 14, on the other hand, is a partial skeleton composed of six lumbar (Sts 14a, Sts 14b, Sts 14c, Sts 14d, Sts 14e, Sts 14f, caudo-cranially oriented) and nine thoracic (Sts 14g, Sts 14h, Sts 14i, Sts 14k, Sts 14l, Sts 14m, Sts 14n, Sts 14o, Sts 14p, caudo-cranially oriented) vertebrae (in different states of preservation), several rib fragments (MNE 5 9, Pickering et al., 2004), both innominate bones (Sts 14r, Sts 14s; quite complete in their preservation), a partial sacrum (Sts 14q), and the proximal half of the left femur (Sts 14t) (Robinson, 1972) (Fig. 1c). Data were collected from the Sts 5 and Sts 14 original fossils housed in the Transvaal Museum in Pretoria. Morphological descriptions, photographs of these specimens, and a high-resolution computer tomography (CT) (0.2-mm slice thickness, 120 kV, 299 mA, 512 3 512 matrix, 0.152 mm pixel size) scan of Sts 5 (conducted at the Little Company of Mary Hospital, Pretoria) were made. A commercial tomography scan of Sts 5 (Weber et al., 1997a) was also used as a data source. The comparative sample was composed of a set of CT scans from nine specimens of Pan troglodytes from Equatorial Guinea but of unknown age-at-death (all held at the Estación Biológica de Doñana [EBD], Spain) (0.5 mm slice thickness, 170–160 kV, 4.0–3.75 mA, 1024 3 1024 matrix, 0.217–0.253–0.289 mm pixel sizes) (Table 1). The original specimen of the partial adult cranium Sts 71 (A. africanus) from Sterkfontein, held at the Transvaal Museum in Pretoria, was also examined. A commercial CT scan of this specimen (Weber et al., 1997b) was also used as an information source. The comparative sample was completed with information from the literature on the pattern and schedule of development of the traits studied in chimpanzees and modern humans. The reason for including extant humans was the incomplete data regarding the maturation of certain features in the chimpanzee essays. Tables 2 and 3 show most of the information used, pertaining to chimpanzees and humans. The patterns and timing of closure of the cranial sutures were obtained from Krogman (1930), Schultz (1940) and Ashley-Montagu (1935, 1937 in Chopra, 1957) for chimpanzees, and from Todd and Lyon (1924, 1925a,b,c), Krogman (1939), Wood Jones (1946 in 1710 BONMATÍ ET AL. TABLE 1. Developmental stages of the cranial features of the chimpanzee sample (EBD) Sample 6877 17140 17957 6842f 15772 6845g 15774 709 708 Dental emergencea Tooth calciﬁcationb Spheno-occipital synchondrosisc Petro-exoccipital synchondrosisd Sphenoidal sinuse 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 3 2 – 3 3 3 3 3 3 2 2 3 3 2 3 2 2 3 3 1 3 3 3 2 4 3 EBD, Estación Biológica de Doñana. Stage 1—M2 erupted and fully functional; M3 close to eruption or recently erupted. Stage 2—M3 erupted but not functional. Stage 3—M3 fully functional. b Stage 1—Incomplete M3 root length (funnel-shaped openings). Stage 2—Complete M3 root length (parallel walls); open apical ends. Stage 3—Complete M3 apical closure. c Stage 1—No evidence of ossiﬁcation. Stage 2—Partial ossiﬁcation. Stage 3—Complete ossiﬁcation. d Stage 1—No evidence of ossiﬁcation. Stage 2—Partial ossiﬁcation and/or evidence of osseous bridging on one side. Stage 3—Complete ossiﬁcation on one side. Stage 4—Complete ossiﬁcation on both sides. e Based on the posterior extension of the sinus in the sagittal plane. Stage 1—Sella turcica. Stage 2—Dorsum sellae. Stage 3—First half of the clivus. Stage 4—Second half of the clivus. f Most of the basisphenoid and occipital bone are missing. g Part of the occipital bone is missing. The jugular synchodronsis score was assessed with reference only to the left side. a Chopra, 1957), Abbie (1950 in Chopra, 1957), Singer (1953 in Chopra, 1957), Acsádi and Nemeskéri (1970), Meindl and Lovejoy (1985), Mann et al. (1991), Gruspier and Mullen (1991) and Key et al. (1994) for humans. Taking into account the degree of preservation of Sts 5 and Sts 14, the features studied are those of developmental signiﬁcance. These features were scored in the chimpanzee comparative sample (for stage deﬁnitions see footnote in Table 1) and for the Sts 5 and Sts 14 fossils. Using the chimpanzee data, a modal pattern was established for the development of the petro-exoccipital synchondrosis and the pneumatization of the sphenoidal sinus relative to the dentition (tooth calciﬁcation and dental emergence) and the SOS. However, the chronological age-of-death of the chimpanzees studied was unknown; thus, only the relative development of these features was recorded. The gathered data allowed the developmental status of both fossil specimens to be established, followed by the biological age-at-death of the individual(s) represented. This procedure was also used to attempt an approximation of the chronological age-at-death. To show that Sts 5 and Sts 14 belong to a single individual requires that the corresponding ages-at-death be compatible and that the relative development between the iliac crest epiphysis of Sts 14 and the SOS of Sts 5 be consistent within the framework of the chimpanzee and human patterns (as mentioned earlier). RESULTS Chimpanzee Sample Table 1 reveals a common pattern of relative development between the cranial traits of the chimpanzee sample. Once the dentition is erupted and completely calciﬁed, the SOS appears fused (or about to fuse) (Fig. 2a). With respect to the sphenoidal sinus, the pneumatization of the greater wings and the area beyond the dor- sum sellae occurs with the complete fusion of the SOS and the fully developed dentition (Fig. 2). These statements are in agreement with the pattern described by some authors for chimpanzees and humans (see references in Tables 2 and 3). Finally, the petro-exoccipital synchondroses show partial or complete ossiﬁcation on one side at the time of completion of the dentition and SOS closure. Sts 5 Dentition. External inspection of the Sts 5 maxilla reveals no evidence of dentition (Tables 2 and 3). The commercial axial CT images (Weber et al., 1997a) show some rounded and homogeneous structures with a brighter signal than the surrounding areas in what appears to be the position of the dental roots within the maxilla (Fig. 3a). In contrast, the CT scan images of the teeth of Sts 71 (Weber et al., 1997b) show one lingual and two oral roots in the maxillary molar series to have rounded and structured morphologies, that is, a bright external layer (cementum), a darker internal area (dentine), and a central white area (root canal) resembling the cementum in shade (Fig. 3b). In comparison with the tomography of the roots of Sts 71, the apparent tooth cavities of Sts 5 have an irregular outline and are poorly structured internally (Fig. 3). The formations seen in Sts 5 are therefore probably casts of the alveolar sockets, formed as a result of mineralization and/or sedimentary ﬁlling after the complete loss of the dentition. Sts 5 was therefore concluded to be edentulous (contrasting with Thackeray et al., 2002a).. Alveoli are perfect natural casts of the root of each tooth, and their size and shape change as the roots grow. In the sagittal tomogram of Sts 5, the suggested natural casts of all the alveoli cut through most of the alveolar bone of the maxilla (Fig. 4a). Further, when compared to Sts 71, these alveoli show similar develop- Stage 2e Sphenoidal sinus Unfused Partially fused Sacrum: sacro-iliac joint epiphysis Ridge and furrow structure attenuation. Welllimited borders Completely fused Sacrum: S1-S2 annular epiphysis Sacrum: S1-S2 costal elements Pubic symphysis Ribs: articular region epiphyses Iliac crest epiphysis Ranging from the beginning of union to almost complete union Almost completely fused Partially fused Stage 3d Petro-exoccipital synch. Vertebrae: annular rings Stage 3c Spheno-occipital synch. (SOS) Developmental stage Stage 2b Feature Tooth calciﬁcation Biological age Chronological age – – – 14.5 years (Zilhman, 2007). 10.1 6 0.84 years (Anemone, 2002). Young adult or older. These elements fuse before the sacral vertebral bodies (Schutlz, 1940). No precise age can be obtained. It may remain unfused in fully grown individuals (Schutlz, 1940). – Between 13 and 35 years, since the sacrum fuses between these ages (Kerley, 1966). Young adult, with slight dental attrition From 11 to 17 years (Schutlz, 1940; (Schultz, 1940; Schultz, 1942 in Curgy, Schultz, 1942 in Curgy, 1965; 1965; Zilhman, 2007). Kerley, 1966; Zilhman, 2007). No correlation with Pan was seen due to progressive symphyseal ankylosis (Schultz, 1940; Schultz, 1942 in Curgy, 1965; Kerley, 1966). Early adulthood or later. Root completion occurs shortly after M3 eruption (Anemone et al., 1991, 1996; Anemone and Watts, 1992; Kuykendall 1996, 2002; Anemone, 2002). From the attainment of adulthood, that is, just before the eruption of all teeth (Krogman, 1930), to young adult, that is, early after the eruption of all teeth and around the time of ﬁrst reproduction (Schultz, 1940; Zilhman, 2007) (Table 1), or older. Adult, showing completion of the permanent dentition and closed SOS (Table 1). Adult, with the completion of the permanent dentition and closed SOS (Table 1). No precise age can be obtained. Union occurs in adults, that is, after the completion of the permanent dentition (Schultz, 1940). – All data are for pooled sex samples. In the blank cells no current data are available. The value after the (6) symbol refers to the standard deviation. (b–e) Feature stages deﬁned in Table 1 (see footnote). Sts 14 skeleton Sts 5 cranium TABLE 2. Chimpanzee biological and chronological ages-at-death for the developmental stage of the features studied in Sts 5 and Sts 14 STS 5 AND STS 14: AGE-AT-DEATH REVISITED 1711 Sts 14 skeleton Sts 5 cranium Partially fused Ridge and furrow structure attenuation. Welllimited borders Iliac crest epiphysis Pubic symphysis Ribs: articular region epiphyses Ranging from the beginning of union to the achievement of almost complete union Almost completely fused Stage 2e Sphenoidal sinus Vertebrae: annular epiphyses Stage 3d Stage 3c b Stage 2 Developmental stage Petroexoccipital synch. Tooth calciﬁcation Sphenooccipital synch. (SOS) Feature Young to fully adult (Todd, 1920, 1921a,b,c; Meindl et al., 1985). From the adolescent period to the onset of full adulthood (see adjoining chronological ages). Just older than the latter stages of adolescence, according to ﬁrst rib ossiﬁcation (Kunos et al., 1999). No precise age can be obtained; no data on unilateral fusion are available. Bilateral fusion ranges from late adolescence-young adulthood through to fully adult individuals (Maat and Mastwijk, 1995; Hershkovitz et al., 1997). Juvenile or older. Most probably fully adult due to nondetectable SOS (Scuderi et al., 1993; Spaeth and Krugelstein, 1996; Weiglein, 1999; Yonetsu et al., 2000; Barghouth et al., 2002). From late adolescence to young adulthood (Albert and Maples, 1995). Adolescence to early adulthood or older (Scheuer and Black, 2000). From the end of the adolescent growth period, that is, before, but more commonly after, M3 eruption (Stewart, 1934; Melsen, 1969, in Scheuer and Black, 2000), or later. Biological age From above 17 to around 25 years according to ﬁrst rib ossiﬁcation: fusion occurs from 14 to 17–19 years. The rounded edges and lenticular proﬁle of the facet might be expected until 21 years. The dense surface with smooth irregularities suggests 20–25 years (Kunos et al., 1999). Remaining ribs: poorly documented, the onset of fusion to the tubercle suggests an age 18 years (Fawcett, 1911; Stevenson, 1924, in Scheuer and Black, 2000). From 15 to 26 years (Galstaun, 1937, Lurie et al., 1943, Mckern and Stewart, 1957, Jit and Singh, 1971, Birkner, 1978, Webb and Suchey, 1985, in Scheuer and Black, 2000; Veschi and Facchini, 2002; Coqueugniot and Weaver, 2007), but most probably in the 19–22 years range (80% of the population would be expected to show this from data in Veschi and Facchini, 2002). Around mid-late 20s: moderate to slight billowing and active rampart formation suggests 24–37 years. Appearance of distinct lower extremity suggests 25 to about 30 years. Reduced billowing together with full lower extremity deﬁnition suggests an age older than 29 (Meindl et al., 1985) to 25–30 years (Phase IV/V; Todd 1920, 1921a,b,c) From 17 (youngest age of early Stage 2; Albert and Maples, 1995) to 27 years (oldest age of late Stage 2; Albert and Maples, 1995). From 15 years (Scuderi et al., 1993; Spaeth and Krugelstein, 1996) to the end of the third decade of life (this occurs in 93% of the population by this time; Yonetsu et al., 2000) From 13 to 25 years, as determined by direct inspection or from CT scans studies (Hrdlička, 1920, in Chopra 1957; Madeline and Elster, 1995; Sahni et al., 1998; Veschi and Facchini, 2002; Coqueugniot and Weaver, 2007). Probably at the end of the second decade or in the ﬁrst half of the third decade, when high percentages of the population _ can, would normally show full closure (Krogman and Is 1986; Sahni et al., 1998; Veschi and Facchini, 2002). No precise age can be obtained; no data on unilateral fusion are available. Bilateral fusion occurs from mostly above 20 years of age (this occurs in 90%–93% of the population by this time; Hershkovitz et al., 1997), or 22–36 years according to Maat and Mastwijk (1995). 17.5 years (Smith, 1991). Chronological age TABLE 3. Modern human biological and chronological ages-at-death for the developmental stage of the features studied in Sts 5 and Sts 14 1712 BONMATÍ ET AL. SOS. The basisphenoidal region shows no sclerotic remnants of this synchondrosis in either the CT scans or on the external surface of the fossil, indicating that its full closure was far from being recent (in agreement with Broom et al., 1950) (Fig. 5a). Sphenoidal air sinus. The sphenoidal aeration extends to the border between the dorsum sellae and the clivus, the sphenoidal wings and the anterior pterygoid processes. It is partially ﬁlled with what are probably calcite crystals, since the brain case is lined with this material (Broom et al., 1950). The pattern of pneumatization of this sinus in humans and chimpanzees and the absence of traces of the SOS in Sts 5, suggest that the sinus of Sts 5 had reached this synchondrosis and exceeded it dorsally (Fig. 5a,b). All data for pooled sex samples. The value after the (6) symbol refers to the standard deviation. (b–e) Feature stages deﬁned in Table 1 footnote. Juvenile to full adulthood (see adjoining chronological ages). Partially fused Unfused 1713 ment relative to the maxillary sinus (Fig. 4b). Although the alveoli of Sts 5 could have been broken, allowing the loss of the teeth, their deep ends are not likely to have been affected. This would imply that the roots of the third molars were completely developed. Likely under 27 years (Mckern and Stewart, 1957, in Scheuer and Black, 2000; Coqueugniot and Weaver, 2007). From 16 to 30 years (Johnston, 1961; Szilvássy 1988 in Berge and Gommery, 1999; Berge and Gommery, 1999; Rogers and Cleaves, 1935, Bollow et al., 1997, in Scheuer and Black, 2000). 19 years (ﬁrst occurrence of complete fusion; Coqueugniot and Weaver, 2007). Late adolescence to full adulthood or later (see adjoining chronological ages). Juvenile to young adult (see adjoining chronological ages). Completely fused Sacrum: S1-S2 costal elements Sacrum: S1-S2 annular epiphysis Sacrum: sacroiliac joint epiphysis Chronological age Biological age Developmental stage Feature TABLE 3. Modern human biological and chronological ages-at-death for the developmental stage of the features studied in Sts 5 and Sts 14 (continued) STS 5 AND STS 14: AGE-AT-DEATH REVISITED Petro-exoccipital synchondrosis. This stage was only assessed on the left side, where the occipital and temporal bones are continuous, signifying at least unilateral complete fusion (Fig. 5c). Cranial sutures. The dynamite blast that uncovered Sts 5 left portions of bone adhered to the calciﬁed matrix of the breccia, making it difﬁcult to observe most of the sutures (Broom et al., 1950; Thackeray, 1997; Prat and Thackeray, 2001). Most of the facial and palatal group of sutures are unidentiﬁable to the naked eye. However, the right side of the fronto-zygomatic—the left side is affected by a fracture that prevents observation of the suture—and the naso-premaxillary sutures are closed although still recognizable on the ectocranial surface (in agreement with Broom et al., 1950). In the cranial vault, only a small ectocranial portion of the sagittal suture within the bregma-lambda region is visible; it is closed (in agreement with Broom et al. 1950; Thackeray, 1997; Prat and Thackeray, 2001). The parieto-squamosal, the spheno-temporal, and the spheno-frontal sutures (belonging to the circum-meatal group of sutures) are fused but remain noticeable ectocranially on both sides (in agreement with Broom et al., 1950). Finally, in basal view, most of the occipito-mastoid suture is somewhat perceptible endocranially on the right side, and identiﬁable but closed ectocranially on both sides (in agreement with Broom et al., 1950), whereas in the splanchnocranium, the anterior and posterior median palatines and the spheno-palatine sutures are closed but still recognizable. Developmental stage and age-at-death of Sts 5. The lack of signs of recent closure of the SOS and the high degree of obliteration of the cranial sutures, especially those of the vault, are indicative that Sts 5 represents a fully grown cranium. Irrespective of whether the chimpanzee or human pattern is used as a model for Sts 5 (Tables 2 and 3), the state of these features signify that this cranium was part of an adult individual with a fully developed dentition. Moreover, the aerated portions 1714 BONMATÍ ET AL. Fig. 2. Basicranium of Pan troglodytes (EBD 17957). (a) Sagittal and (b) transversal CT-scans. BO, basiocciput; BS, basisphenoid; CL, clivus; DS, dorsum sellae; FM, foramen magnum; MF, middle fossa; OP, olivary process; PET, petrous bone; SO, supraocciput; SOS, spheno-occipital synchondrosis; SS, sphenoidal sinus; ST, sella turcica. Scale bar 5 2 cm. of the sphenoidal sinus, the fusion status of the petroexoccipital synchondrosis, and the probable completion of the M3 roots, are all consistent with this statement. Thus, the Pan and modern human schedules of maturation support ages-at-death of 14.5 years or older, and older than around 20 years, respectively (Tables 2 and 3). Sts 14 Vertebrae. The annular rings of the spine of Sts 14 show a variety of stages of ossiﬁcation (Fig. 6a) (Tables 2 and 3). Following the scoring system of Albert and Maples (1995), these epiphyses appear to range from the early (beginning of union; Sts 14b, Sts 14h) to late (progressing union; Sts 14d, Sts 14e, Sts 14f, Sts 14g, Sts 14i, Sts 14k, Sts 14l, Sts 14m, Sts 14n, Sts 14o, Sts 14q) phases of Stage 1, through to the early (almost complete union; Sts 14a, Sts 14c) phase of Stage 2. Ribs. Those ribs with a preserved tubercle region (none of which were identiﬁed as a ﬁrst rib) show the articular epiphyseal plate with nearly complete fusion, though the suture is still identiﬁable (Fig. 6b). In addition, the proﬁle of the tubercle is no longer elliptical but distinctively lenticular, and its boundaries are mostly rounded and slightly raised above the shaft. The surface texture of the tubercle is dense with smooth depressions and ridges. Pelvis. The iliac crest is mostly fused on the left side (Sts 14r), showing only traces of the suture, while the right coxal (Sts 14s) bone shows partial loss of the anterior portion of the epiphysis, probably due to incomplete ossiﬁcation (in agreement with Berge and Gommery, 1999; Häusler and Berger, 2001) (Fig. 7a). The sacrum shows incomplete fusion of the S1-S2 annular epiphysis. Further, even though the epiphyseal plate of the left sacro-iliac joint is fragmentary, the suture with the sacral alae remains discernible (in agreement with Berge and Gommery, 1999) (Fig. 7b). The pubic symphysis of Sts 14 appears to have a characteristic ridge and furrow structure on its ventral STS 5 AND STS 14: AGE-AT-DEATH REVISITED 1715 Fig. 3. Maxilla. Transversal tomograms of (a) Sts 5 (Weber et al., 1997a) and (b) Sts 71 (Weber et al., 1997b). Circles surrounding teeth (Sts 71) or alveoli (Sts 5): RPM3, right third premolar; RPM4, right fourth premolar; RM1, right ﬁrst molar; RM2, right second molar; RM3, right third molar; LM1, left ﬁrst molar; LM2, left second molar; LM3, left third molar. Scale bar 5 5 cm. margin, albeit mostly attenuated along the dorsal border. Additionally, its dorsal, superior and inferior margins are well limited by a continuous rim, whereas its anterior wall shows the beginning of the formation of the ventral rampart (Fig. 7c). likely fully grown in terms of height (as shown by the ossiﬁed acetabulum, and the probably-fused long bone epiphyses) and close to—thought not completely—grown in terms of body breadth (as shown by the incomplete iliac crest and sacrum epiphyses) (in agreement with Berge and Gommery, 1999). Therefore, this fossil assemblage represents part of a young adult probably between 14.5 years to 17 years according to chimpanzee standards, or somewhere in its early mid-20s according to the modern human schedule of maturation (Tables 2 and 3). Femur. This lacks most of the greater trochanter and the most basal part of the lesser trochanter; they cannot, therefore be used for age diagnosis. Developmental stage and age-at-death of Sts 14. The several signs of immaturity in the ossiﬁcation of the epiphyses of Sts 14 show that this skeleton had not completed its development. With respect to both the Pan and Homo sapiens patterns (Tables 2 and 3) these epiphyses are among the last to complete ossiﬁcation. The individual to whom this skeleton belonged was DISCUSSION One and the Same Individual? According to the present results, the biological and chronological ages-at-death of both specimens are partially compatible. However, Sts 5 shows no sign of 1716 BONMATÍ ET AL. Fig. 4. Maxilla. Sagittal tomograms of (a) Sts 5 (Weber et al., 1997a) and (b) Sts 71 (Weber et al., 1997b). (1) maxillary sinus, (2) alveolar bone, (3) ﬁllings of the alveolar sockets, (4) roots of the maxillary dentition. Scale bar 5 5 cm. having recently reached adulthood. Since the SOS of Sts 5 is no longer detectable, its closure does not appear to have occurred recently before death. Even when considering the intrapopulation variation of chimpanzees and modern humans, such a degree of the SOS closure in Sts 5 does not seem to be consistent with the still fusing iliac crest in Sts 14. Although cranial vault closure may occur over an extended period of time in extant human populations, severe obliteration of this vault is common in fully adult individuals (Acsádi and Nemeskéri, 1970, Meindl and Lovejoy, 1985; Key et al., 1994). Therefore, against the human standard, the high degree of vault obliteration shown by Sts 5 does not suggest a young adult age. In conclusion, no evidence supporting the idea that the studied fossils belong to a single individual was found; in fact, some data clearly suggest they belong to different individuals. The EQ Using previous estimates for the body mass for Sts 14 (27.6 kg by McHenry, 1976 and 34.8 kg by Jungers, 1988) and an endocranial volume for Sts 5 of 485 cm3 (Falk et al., 2000), the method of Ruff et al. (1997) was used to calculate the brain mass and EQ for a hypothetical association between Sts 5 and Sts 14. This resulted in an EQ value of 2.9–3.4, depending on the body mass estimate used. This interval lies between the uppermost estimates for A. africanus (2.4–3.0 as derived from data in McHenry and Cofﬁng, 2000) and the lowermost limits for Homo habilis (3.4–3.8 as derived from data in STS 5 AND STS 14: AGE-AT-DEATH REVISITED Fig. 5. Basicranium of Sts 5. (a) Sagittal, (b) transversal (Weber et al., 1997a) and (c) coronal tomograms of Sts 5. L EXO, left exoccipital portion of the occipital bone; L PETEXO, left petro-exoccipital 1717 synchondrosis (note its complete fusion); PF, post-depositional fracture (note its continuation with the dorsal border of the sphenoidal sinus). See Fig. 2 for other abbreviations. Scale bar 5 2 cm. 1718 BONMATÍ ET AL. Fig. 6. Sts 14 trunk. (a) Stages of ossiﬁcation of the ring epiphyses (arrows) in the Sts 14 spine: beginning of union (Sts 14b), progression of union (Sts 14m), and almost complete union (Sts 14a). (b) Articular region of one rib with the epiphyseal plate showing traces (arrows) of the suture. Scale bar 5 2 cm. McHenry and Cofﬁng, 2000). The result for the Sts 5-Sts 14 fossil assemblage is therefore only partially compatible with our current knowledge of the encephalization of A. africanus. If these fossils do represent a single specimen, the range for the relative brain capacity of this species would be necessarily increased. CONCLUSIONS A thorough re-evaluation of the developmental stage and age-at-death of the landmark Sts 5 and Sts 14 A. africanus fossils has been attempted in this work. Contrary to the conclusions of a previous assessment (Thackeray et al., 2002a), Sts 5 was found not to belong to an adolescent specimen but to a fully grown adult whose estimated chronological age-at-death was 14.5 years or above, or more than around 20 years, according to the chimpanzee and modern human schedules of development respectively. This conclusion rests upon the following evidence: the mostly obliterated cranial vault sutures, the complete closure of the spheno-occipital and petro-exocccipital synchondroses (as observed on the left side), the pneumatization of the sphenoidal sinus to the dorsum sellae, and the adult size of the alveolar sockets in the maxilla. Sts 14 shows signs of immaturity in the pelvis, ribs, and vertebrae. On the basis of data for chimpanzees and modern humans, the ossiﬁcation stage of the studied features in Sts 14 suggests this partial skeleton belonged to a young adult that died between 14.5 to around 17 years of age according to chimpanzee standards, or within the ﬁrst half of its third decade of life STS 5 AND STS 14: AGE-AT-DEATH REVISITED 1719 Fig. 7. Sts 14 pelvis. (a) Iliac crest. (b) Sacrum. (c) Pubic symphysis. Circles highlighting the stage of the traits above inspection. Scale bar 5 2 cm. according to extant human standards. Previous studies on the pattern of development in A. africanus suggest that the chronological ages of both Sts 5 and Sts 14 are best determined using the chimpanzee developmental pattern. These results also show the age-at-death of these two specimens to be partially consistent which one another. However, no evidence was found to support the idea that Sts 5 had just attained full growth, nor, therefore, that Sts 5 is the cranium of the young adult Sts 14 partial skeleton. Further, the stage of development of some of the Sts 5 features suggest it unlikely that this be the skull of a young adult. Finally, the lower value of the EQ range resulting from a hypothetical association between Sts 5 and Sts 14 lie at the top end of that currently supposed for A. africanus. Should future research conﬁrm such an association, the relative brain capacity of this species would necessarily increase, shortening the distance separating Homo and Australopithecus. 1720 BONMATÍ ET AL. ACKNOWLEDGMENTS The authors thank the staff of the Transvaal Museum (Pretoria, South Africa), especially Francis Thackeray, for allowing us to study the original fossils Sts 14, Sts 5, and Sts 71. 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