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Genetics and Molecular Biology

Print version ISSN 1415-4757

Genet. Mol. Biol. vol.22 n.4 São Paulo Dec. 1999

http://dx.doi.org/10.1590/S1415-47571999000400001 

LAPA VERMELHA IV HOMINID 1: MORPHOLOGICAL AFFINITIES OF THE EARLIEST KNOWN AMERICAN

 

Walter A. Neves1, Joseph F. Powell2, Andre Prous3, Erik G. Ozolins2 and Max Blum1
1Laboratório de Estudos Evolutivos Humanos, Departamento de Biologia, Instituto de Biociências, Universidade de São Paulo, Caixa Postal 11461, 05422.970 São Paulo, SP, Brasil. Send correspondence to W.A.N. Fax: +55-11-818-7533. E-mail: waneves@ib.usp.br
2Department of Anthropology, University of New Mexico, Albuquerque, NM 87131-1086, USA.
3Setor de Arqueologia, Museu de História Natural, Universidade Federal de Minas Gerais, Belo Horizonte, MG, Brasil.

 

 

ABSTRACT

Several studies concerning the extra-continental morphological affinities of Paleo-Indian skeletons, carried out independently in South and North America, have indicated that the Americas were first occupied by non-Mongoloids that made their way to the New World through the Bering Strait in ancient times. The first South Americans show a clear resemblance to modern South Pacific and African populations, while the first North Americans seem to be at an unresolved morphological position between modern South Pacific and Europeans. In none of these analyses the first Americans show any resemblance to either northeast Asians or modern native Americans. So far, these studies have included affirmed and putative early skeletons thought to date between 8,000 and 10,000 years B.P. In this work the extra-continental morphological affinities of a Paleo-Indian skeleton well dated between 11,000 and 11,500 years B.P. (Lapa Vermelha IV Hominid 1, or "Luzia") is investigated, using as comparative samples Howells' (1989) world-wide modern series and Habgood's (1985) Old World Late Pleistocene fossil hominids. The comparison between Lapa Vermelha IV Hominid 1 and Howells' series was based on canonical variate analysis, including 45 size-corrected craniometric variables, while the comparison with fossil hominids was based on principal component analysis, including 16 size-corrected variables. In the first case, Lapa Vermelha IV Hominid 1 exhibited an undisputed morphological affinity firstly with Africans and secondly with South Pacific populations. In the second comparison, the earliest known American skeleton had its closest similarities with early Australians, Zhoukoudian Upper Cave 103, and Taforalt 18. The results obtained clearly confirm the idea that the Americas were first colonized by a generalized Homo sapiens population which inhabited East Asia in the Late Pleistocene, before the definition of the classic Mongoloid morphology.

 

 

INTRODUCTION

It is widely accepted that modern Homo sapiens appeared in Africa around 120,000 years B.P. and spread throughout the Old World, arriving in the Near East soon after appearing in Africa, spreading to Europe around 45,000 years B.P., and to Australia by at least 50,000 years ago (Stringer and Andrews, 1988; Stringer,1989a,b, 1990; Lahr, 1994, 1996; see O'Connell and Allen, 1998, for a recent review). Modern humans soon replaced archaic forms of hominids in those regions (Stringer, 1985, 1990), although there are some scholars who suggest that anatomically modern humans lived in sympatry with Homo erectus in Southern Asia until late in time (Swisher et al., 1996).

In this scenario, the settlement of Australia is seen as the result of a natural expansion of Homo sapiens eastward, who probably took a southern path following the more tropical regions of Asia (Stringer, 1985; Lahr, 1996). We also know that the settlement of modern human populations in Australia implied the use of some aquatic means of transportation, since Australia was never connected to mainland Asia by a terrestrial bridge (Allen and Kershaw, 1996).

The occupation of the Americas, however, has not generally been viewed as part of this early expansion of our species. The view traditionally held is that anatomically modern humans arrived in the New World only very late in time, much after the initial expansion out of Africa, and, most importantly, after Northern Asian populations had made significant adaptations to their environment. As exemplified in the Three Migration Model, the biological source of the first Americans is Northern Asia, with the earliest Americans being just an extension of the spread of Mongoloid people at the end of the Pleistocene (Turner, 1983; Greenberg et al., 1986; Lahr, 1995). Recent comparative studies of the cranial morphology of Paleo-Indian and Early Archaic skeletons from North and South America, however, have shown that the occupation of the New World could have been a much more complex biological process than the waves of expansion depicted in the Three Migration model.

In a series of previous publications (Neves and Pucciarelli, 1989, 1991, 1998; Neves and Blum, in press; Munford et al., 1995; Munford, 1999; Neves et al., 1996a,b, 1997, 1999; Powell et al., in press) we have demonstrated that the cranial morphology of the earliest South Americans cannot be classified as typical Mongoloid and that, in fact, it closely resembles the craniofacial morphology typically seen in modern South Pacific populations and in Africa. In these several comparisons, multivariate statistical analyses have demonstrated a strong morphological similarity between the oldest Americans and modern Australians and only a slightly weaker morphological similarity to modern Africans. When the comparisons are made using Pleistocene fossil hominids as comparative samples, the same pattern of biological resemblance is obtained.

A similar phenomenon seems to occur with the earliest North American skeletons. In a series of contributions, Steele and Powell demonstrated that the morphology of the North American Paleo-Indian and Early Archaic populations in no way resembles that of modern Mongoloid populations of North Asia (Steele and Powell, 1992, 1993, 1994; Powell and Steele, 1992). The oldest North American remains, when treated with multivariate analytical tools, seem to occupy an unresolved morphological position between modern South Pacific and European populations.

All this information indicates that the Americas were first occupied by a generalized population of Homo sapiens very similar to the one that departed from East Asia to Australia around 50,000 B.P., and whose remote origins ultimately can be traced back to Africa (Lahr, 1995; Munford et al., 1995; Neves et al., 1997). This morphology is primarily characterized by very long and narrow skulls, short and narrow faces, with short orbits and noses. A process of in situ microevolution leading to mongolization cannot be ruled out to explain what is seen in terms of cranial morphology in later native American populations, namely broad faces and vaults, tall faces with tall orbits and noses. As Lahr (1995) emphasized, this would have implicated a tremendous amount of convergent evolution in Asia and in the Americas. This becomes even more difficult to accept if we recall that Sutter (1997) has suggested that dental morphology has also changed from a sundadont to a sinodont pattern in prehistoric coastal Chile and Peru during the Middle Holocene. Another indicator that weakens the local microevolution argument is that, at least in South America, the evidence seems to point to a major population replacement around 8,000 to 9,000 years B.P., when the generalized morphology was abruptly replaced by the classic Mongoloid morphology (Munford et al., 1995; Neves et al., 1996a).

The central idea of this paper is to strengthen our recent discoveries about the extra-continental biological similarities of the first Americans, bringing into the analysis what we think is the oldest known American skeleton: Lapa Vermelha IV Hominid 1, also known as "Luzia". Most of our previous works were based on cranial samples not pre-dating 10,000 years B.P. It is our belief that the older the skeletal material used in the comparative analysis, the more we can learn about the ancestral populations of the first Americans in the Old World.

 

MATERIAL AND METHODS

The material used in this work consists of a South American Paleo-Indian skeleton recovered in 1974 and 1975 from the site of Lapa Vermelha IV, during excavations carried out by the French-Brazilian mission under the leadership of the late Annette Laming-Emperaire.

The rock-shelter of Lapa Vermelha IV is located in the county of Pedro Leopoldo, Lagoa Santa region, State of Minas Gerais, central Brazil (Figure 1), and is part of a karstic complex of caves, shelters and underground water channels (Laming-Emperaire et al., 1975). The scientific excavation of Lapa Vermelha IV started in 1971 and was interrupted suddenly in 1976 with the unexpected death of Laming-Emperaire (Prous, 1986, 1991). For this reason, the published material regarding the site is meager (Laming-Emperaire et al., 1975; Laming-Emperaire, 1979; Prous, 1986), and few archaeologists outside Brazil are aware of the site, its stratigraphy, or dating.

 

 

The rock-shelter was filled by a thick layer of Pleistocene and Holocene sediments, of which 13 meters were excavated. Radiocarbon dates from these deposits revealed a long process of deposition, extending from modern times to at least 25,000 years B.P. Unquestionable evidence of human occupation of the site, as indicated by the presence of a quartz flake, scattered charcoal and a human skeleton, was observed in deposits dating as far back as the Pleistocene-Holocene boundary (around 12,000 years B.P.), as is also the case with several other sites in central Brazil (Prous, 1980, 1986, 1991; Schmitz, 1984, 1987; Dillehay et al., 1992). An isolated scraper and a few flakes of questionable provenience were also found in a layer dated to between 15,000 and 20,000 years B.P.

The site is significant in a number of ways. In addition to indicating the presence of humans in Central Brazil as early as the beginning of the Holocene, the excavations carried out in Lapa Vermelha IV also generated the first incontestable evidence of contemporary humans and extinct fauna in the region. Bones and coprolites of a giant sloth (Glossoterium gigas) were found in deposits as deep as 11 meters, and dated to 9,580 ± 200 years B.P. (uncalibrated) (Laming-Emperaire, 1979).

Approximately 2 meters below the remains of the giant sloth, unarticulated scattered remains of a human skeleton were found bracketed by two archaeological levels which produced radiocarbon dates on charcoal of 10,220 and 12,960 B.P. (uncalibrated), respectively. Although Laming-Emperaire (1979) and Prous (1986) described the skeleton as in situ, Cunha and Guimarães (1978) questioned its original position because the bones were not found in total articulation. Recent trials to directly date the skeleton by AMS methods proved unsuccessful, due to the absence of collagen in the sample (Darden Hood, personal communication, 1996; Thomas Stafford, personal communication, 1997). However, an AMS date run on carbon found in the acid washes of the sample generated a minimum date of 9,330 ± 60 B.P. (uncalibrated) (Beta Analytic sample 84439). For this reason, and accepting the original stratigraphic position described by the archaeologists responsible for the excavation, Hominid 1 of Lapa Vermelha IV is presented here as the oldest human remains found in the Americas, dating between 11,000 and 11,500 years B.P.*

Recently, two of us (W.A.N. and J.F.P.) were able to study the specimen, and concluded that all of the bones belonged to a single individual, a female aged 20 and 25 years, confirming previous independent assessment carried out by Alvim (1977). The nearly complete skull was metrically characterized using the standard measurements and points of reference recommended by Howells (1973). The morphology of Lapa Vermelha IV Hominid 1 was compared with modern human cranial variation and also with morphological variation in Late Pleistocene fossils from the Old World.

For the first comparison we used the Howells (1989) female craniometric data bank and for the second case we employed data adapted from Habgood (1985), with males and females pooled. The comparison with Howells' (1989) data was carried out by means of a canonical variate analysis, using 45 craniometric variables as input. This procedure minimizes within-group variation and maximizes between-group variation, making regional groups as distinct as possible (Manly, 1994). Individuals were grouped by population rather than region in this analysis, and the resulting population centroids were plotted using the first three canonical variates. Because the "population" of fossil hominid material was often represented by a single specimen, we were unable to carry out a canonical variate analysis on these data. Instead, we performed a principal component analysis on 16 craniofacial variables (Tables I and II). This descriptive technique, which employs the pooled variance-covariance matrix for all samples regardless of their geographic origin, attempts to summarize the variation present in the total data set into a series of orthogonal vectors (Manly, 1994). In both cases, the initial raw craniometric data were size-corrected, using the strategy recommended by Darroch and Mosimann (1985).

 

0929t1.gif (25250 bytes)

 

RESULTS

Table III presents the main parameters of the canonical variates with eigenvalues greater than 1.000, while Table IV presents the scores for the centroid of each population. The scores regarding the first three canonical variates were used for the construction of the graph in Figure 2. As can be seen in Table III, the first three canonical variates account for approximately 61% of the total dispersion. The first canonical variate is mainly influenced by the projection of glabella and alveolar prognathism. So individuals with large positive scores show very projecting glabellae and very prognathic maxillae. The second canonical variate is also very influenced by glabella projection. However, in this case, individuals with high positive scores exhibit a flatter glabella. The third canonical variate relies heavily on the projection of the face in relation to the transmeatal plane. Individuals with large positive scores for this axis show very projecting prosthions.

 

 

 

 

 

0929f2.gif (17732 bytes)

 

The analysis of Figure 2 allows us to conclude that Lapa Vermelha IV Hominid 1 presents a strong similarity firstly with Africans and secondly with South Pacific populations. It is also important to note that one of the Polynesian populations (Easter Island) approximates the area occupied by Lapa Vermelha IV Hominid 1, Africans and Australians, especially if only variates 1 and 2 are considered. No resemblance was found between Lapa Vermelha IV Hominid 1 and either Asians or Late Holocene American Indians.

Table V presents the main parameters of the principal components with eigenvalues greater than 1.000, while Table VI presents the scores for each hominid included in the analysis. The scores regarding the first three components were used to build the graph presented in Figure 3. As can be seen in Table V, the first three components reflect approximately 62% of the total variance contained in the 16 original variables. The first principal component can be described as a direct relation of cranial breadth with facial height. In other words, individuals with large positive values for PC1 have relatively broad skulls and short faces. PC2 can be synthesized as a direct relation of cranial height and length against orbital and nasal breadth. So individuals with large positive scores for this component exhibit long high skulls and narrow noses and orbits. The third component shows a relationship of cranial base breadth and occipital length versus overall cranial length and orbital height. So individuals with large positive values have broad cranial bases, short skulls and short eyes.

 

 

 

 

 

 

The analysis of Figure 3 indicates that Lapa Vermelha IV Hominid 1 is surrounded by the following fossil hominids: Early Australians, Taforalt 18, Keilor and Zhoukoudian Upper Cave 103. This relation is even more clear when only principal components 1 and 2 are taken into account. Lapa Vermelha IV Hominid 1 presents a very peculiar PCA score for the third component.

 

DISCUSSION

Richard Shutler, Jr. (1983) argued more than 10 years ago that the occupation of the New World could parallel the peopling of Australia in several aspects. There are, however, two main constraints to this view: time of entry and the ancestral Old World populations involved. In the beginning of this paper we stated that the settlement of the Australian continent is currently seen as a direct expansion of early modern people from Africa (Lahr, 1996), while the settlement of the Americas is viewed as part of a much later colonization event, namely the expansion of the specialized Mongoloids from North Asia in relatively recent times (Turner, 1983; Greenberg et al., 1986).

If this view is accepted, it becomes clear that Native Americans had an ancestral population in mainland Asia which was not shared with Native Australians. While the first Australians were derived from a generalized Homo sapiens population in East Asia, whose ultimate ancestors can be traced back to Africa, the first Americans have been thought to be derived from an already specialized population of H. sapiens (Mongoloids) from northern Asia. While humans seem to have entered Australia during the middle part of the Late Pleistocene, archaeologists have been unable so far to present incontestable evidence for the presence of man in the Americas at the same time, although the timing of genetic differentiation of American Indians from populations in Asia may have occurred as early as 26,000 to 43,000 years ago (Torroni et al., 1992).

Despite the fact that our research, past and present, does not address time of entry, it has significant consequences for the problem of the ancestral populations involved. The results obtained in this work confirm our previous findings that the first Americans have no special biological resemblance to modern northern Asians. As can be seen in Figure 2, the oldest human skeleton of the Americas shows a strong similarity with modern Africans and Australians. When the comparison is made with Late Pleistocene and Early Holocene fossil hominids (Figure 3), the first known American is surrounded by early Australians and Zhoukoudian Upper Cave Hominid 103.

There is no necessity of invoking the occurrence of trans-oceanic migrations to explain the pattern of biological affinities we have been finding for the first Americans. The best way of reconciling the pattern of morphological similarities found in this work with common knowledge about human evolution in East Asia is to assume that both the first Australians and the first Americans shared a common ancestral population in mainland Asia. This ancestral population could well be represented by hominids similar to the Zhoukoudian Upper Cave people (Kamminga and Wright, 1988; Wright, 1995; Neves and Pucciarelli, 1998) and its ultimate origin can be traced back to Africa.

The idea that East Asia was occupied by an Australian-like population by the end of the Pleistocene has gained more support recently. Matsumura and Zuraina (1999) described a very well-preserved skeleton from Gua Gunung, Malaysia. The specimen is aged 10,200 B.P. and is said to be a late representative of a non-specialized morphology, similar to Australian Aborigines, in East Asia.

If our inferences are correct, the Americas could ultimately be seen as part of the first expansion of anatomically modern humans out of Africa, which started during the beginning of the Upper Pleistocene. Recent acceptance of Late Pleistocene dates for the occupation of the site of Monte Verde, Chile (Meltzer et al., 1997), now suggests that populations colonizing the New World may have crossed the Bering Strait earlier than previously thought. This makes our suggestion still more plausible.

 

ACKNOWLEDGMENTS

Research supported by FAPESP (Brazil) and the University of New Mexico (USA). One of the authors (W.A.N.) held a scholarship from CNPq (Brazil) while preparing the manuscript. A grant-in-aid-of-research from Sigma-Xi enabled one of us (E.G.O.) to be in Brazil for the preparation of the final version of the paper. We also want to acknowledge Ricardo Santos, curator of Biological Anthropology of Museu Nacional, Rio de Janeiro, for allowing us to measure and date Lapa Vermelha IV, Hominid I. Acknowledgments are also extended to Roberta Hall for inviting us to present an earlier version of this paper at the 67th Annual Meeting of the AAPA, and also for several insightful comments made on this first version. We want to dedicate this work to Jose Inbelloni and Paul Rivet, in memorian, for arriving at similar conclusions about the first Americans, in a time when samples were scantier and methods much simpler. Publication supported by FAPESP.

 

 

RESUMO

Diversos estudos sobre afinidades morfológicas extra-continentais de esqueletos paleoíndios, executados independentemente na América do Sul e do Norte, têm indicado uma ocupação inicial do continente americano por não-mongolóides. Os primeiros sul-americanos demonstram uma clara semelhança com populações sul-pacíficas e africanas, enquanto os primeiros norte-americanos parecem encontrar-se em uma posição indefinida entre sul-pacíficos e europeus. Em nenhuma destas análises os primeiros americanos demonstraram qualquer similaridade com populações modernas do nordeste asiático ou com índios americanos atuais. Até então, estes estudos haviam incluído esqueletos datados de 8,000 a 10,000 anos atrás. Neste trabalho, as afinidades extra-continentais de um esqueleto paleoíndio bem contextualizado entre 11,000 e 11,500 anos atrás (Lapa Vermelha IV Hominídeo 1, ou Luzia) são investigadas, usando como amostras de referência as séries mundiais de Howells (1989) e a coleção de fósseis de hominídeos do Pleistoceno tardio de HabGood (1985). A comparação entre Lapa Vermelha IV Hominídeo 1 e as séries de Howells baseou-se em análises de variáveis canônicas incluindo 45 variáveis craniométricas corrigidas quanto ao tamanho, enquanto a comparação com hominídeos fósseis foi baseada em análise de componentes principais incluindo 16 variáveis também corrigidas. No primeiro caso, Lapa Vermelha IV Hominídeo 1 exibiu afinidade morfológica indiscutível, primariamente com africanos e, em seguida, com populações sul-pacíficas. Na segunda comparação, o mais antigo esqueleto americano conhecido apresentou maior similaridade com os primeiros australianos, Zhoukoudian UC103 e Taforalt 18. Os resultados obtidos confirmam claramente a idéia de que o continente americano foi inicialmente colonizado por uma população de Homo sapiens generalizados que habitaram o leste asiático no final do Pleistoceno, antes da definição da morfologia mongolóide clássica.

 

 

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(Received October 27, 1999)

 

 

* In fact Laming-Emperaire (1979: 71) states that "Un crâne humanie fut trouvé à la cote -12 m 90 qui peut être considéré comme vieux de plus de 12000 annés (A.P.)".