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Vol. 96, Issue 13, 7604-7609, June 22, 1999 (Neandertals / mandible / postcrania / dentition / radiocarbon
dating)
* Instituto Português do Património
Arquitectónico, Divisão de Conservação e
Restauro, Palácio da Ajuda, 1400-206 Lisbon, Portugal;
Contributed by Erik Trinkaus, April 26, 1999
The discovery of an early Upper Paleolithic human burial at the
Abrigo do Lagar Velho, Portugal, has provided evidence of early modern
humans from southern Iberia. The remains, the largely complete skeleton
of a During the past decade it has become apparent that the human
biological and cultural evolutionary transitions between late archaic
(Neandertal) and early modern humans and between the Middle and Upper
Paleolithic occurred relatively late throughout most of Iberia (1-4).
It is now certain that the Middle Paleolithic of most of Iberia south
of the Pyrenees lasted until about 30,000 years B.P., perhaps as late
as 28,000 years B.P., and that the initial stages of the Upper
Paleolithic known to have occurred further north (the
Châtelperronian and the early Aurignacian) were never present in
this region. Moreover, human paleontological evidence from Zafarraya in
southeastern Spain indicates that late Middle Paleolithic technology
from this region was the product of Neandertal populations (5). This
evidence has led to hypotheses as to why Middle Paleolithic Neandertals
endured in the cul-de-sac of Iberia between 5,000 and 10,000 years
after they had been replaced (by whatever historical processes)
elsewhere in Europe (4, 6, 7). The "Ebro Frontier" model (3,
6-8) suggests that the basin of the Ebro river of northern Spain
represented a biogeographical and ecological barrier to the diffusion
of the Upper Paleolithic innovations developed by late Neandertal
populations to the north (the Châtelperronian) and, subsequently,
to the dispersal of the first modern human groups in western Europe.
Even though both the late Middle Paleolithic and early Upper
Paleolithic are increasingly well known and chronologically situated south of the "Ebro Frontier" (4, 6, 9), diagnostic human remains
associated with early Upper Paleolithic industries in this region have
been elusive. The discovery of a largely intact early Upper Paleolithic
child's burial at the Abrigo do Lagar Velho in Portugal therefore adds
significantly to our knowledge of the biology and burial practices of
the earliest Iberian modern humans and sheds light on the nature of the
transition from Neandertals to their successors in one of the last
archaic human frontiers.
The archeological site consists of deposits within horizontal
fissures and along the current base of a limestone cliff on the south
side of the Lapedo Valley near Leiria, central western Portugal (lat
39° 45' 25" N, long 8° 43' 58" W). The site was damaged by earth
removal in 1992, exposing an Upper Paleolithic sequence and coming
within a few centimeters of the burial along the base of the cliff. On
November 28, 1998, the site was discovered by J.M. and P.S., who also
found the left hand and forearm bones of the child in a burrow. The
following week C.D. and J.Z. confirmed the presence of Paleolithic
deposits and a human burial. A salvage excavation directed by J.Z.
ensued from December 12 to January 7, 1999, in the framework of which
the burial was excavated by C.D. Paleontological analysis by C.D. and
E.T. commenced on January 4, 1999.
The child's skeleton, Lagar Velho 1 (Fig.
1), was on its back parallel to
the cliff base, with the head to the east and left side against the
cliff. The cranium and mandible were damaged by earth removal, but the
preservation of the left temporal bone and mandible indicates that the
head had tilted toward the cliff face. The collapse and folding
in situ of the right ribs suggest that the thorax was
similarly tilted. The pelvis was horizontal, and the feet were
plantar-flexed and crossed. The skeleton and the containing sediment
are heavily stained with red ochre, but the alteration of the sediment
stopped at the outer border of the skeleton, suggesting a wrap around
the body. Vertically oriented animal bones and stones outlined the
ochre-stained sediments; radiocarbon dating of one such bone yielded a
result that is consistent with the hypothesis that these represent
intentional burial features and not a natural disposition of deposit
components caused by digging a burial pit.
Anthropology
The early Upper Paleolithic human skeleton from the Abrigo do
Lagar Velho (Portugal) and modern human emergence in Iberia
,
,
,
,**,
, and
Department of Anthropology, 13-15 Henry Marshall Tory Building,
University of Alberta, Edmonton T6G 2H4, AB, Canada;
Sociedade
Torrejana de Espeleologia e Arqueologia, Quinta da Lezíria,
2350 Torres Novas, Portugal; § Radiocarbon Accelerator Unit,
Research Laboratory for Archaeology and the History of Art, University
of Oxford, 6 Keble Road, Oxford OX1 3QJ, England; ¶ Department of
Anthropology, Campus Box 1114, Washington University, St. Louis, MO
63130;
Unité Mixte de Recherche 5809 du Centre National
de la Recherche Scientifique, Laboratoire d'Anthropologie,
Université de Bordeaux I, 33405 Talence, France;

Centrum voor Isotopen Onderzoek, Faculteit der Wiskunde
en Natuurwetenschappen, Rijksuniversiteit Groningen, Nijenborgh 4, 9747 AG Groningen, The Netherlands; and 
Instituto
Português de Arqueologia, Avenida da India 136, 1300 Lisbon,
Portugal
![]()
ABSTRACT
TOP
ABSTRACT
INTRODUCTION
THE ABRIGO DO LAGAR...
AGE AND BODY SIZE
MORPHOLOGICAL CONSIDERATIONS
DISCUSSION
CONCLUSION
REFERENCES
4-year-old child buried with pierced shell and red ochre, is
dated to ca. 24,500 years B.P. The cranium, mandible,
dentition, and postcrania present a mosaic of European early modern
human and Neandertal features. The temporal bone has an
intermediate-sized juxtamastoid eminence. The mandibular mentum osseum
and the dental size and proportions, supported by mandibular ramal
features, radial tuberosity orientation, and diaphyseal curvature, as
well as the pubic proportions align the skeleton with early modern
humans. Body proportions, reflected in femorotibial lengths and
diaphyseal robusticity plus tibial condylar displacement, as well as
mandibular symphyseal retreat and thoracohumeral muscle insertions,
align the skeleton with the Neandertals. This morphological mosaic
indicates admixture between regional Neandertals and early modern
humans dispersing into southern Iberia. It establishes the complexities
of the Late Pleistocene emergence of modern humans and refutes strict
replacement models of modern human origins.
![]()
INTRODUCTION
TOP
ABSTRACT
INTRODUCTION
THE ABRIGO DO LAGAR...
AGE AND BODY SIZE
MORPHOLOGICAL CONSIDERATIONS
DISCUSSION
CONCLUSION
REFERENCES
![]()
THE ABRIGO DO LAGAR VELHO
TOP
ABSTRACT
INTRODUCTION
THE ABRIGO DO LAGAR...
AGE AND BODY SIZE
MORPHOLOGICAL CONSIDERATIONS
DISCUSSION
CONCLUSION
REFERENCES

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Fig. 1.
Lagar Velho 1 in situ, with
damaged skull and left forearm elements already removed.
The only diagnostic archeological item in the burial was a pierced
Littorina obtusata shell found near the cervical vertebrae; it is identical to those from Level Jb of the nearby site of Gruta do
Caldeirão (Tomar) dated to 26,020 ± 320 years B.P.
(OxA-5542; ref. 6). Similar burials with pierced shells and/or teeth
and a covering of ochre are known particularly from the Gravettian of
Europe, especially from Britain (Paviland), Italy (Arene Candide, Barma
Grande, Caviglione, Ostuni), and the Czech Republic (Brno, Dolní V
stonice; refs. 10-12).
The uppermost 2-3 m of the shelter's fill were largely removed and
current ground level represents the surface of an estimated 3- to 4-m
sequence of early Upper and possibly Middle Paleolithic strata. A
60-cm thick hanging remnant is preserved within a fissure running along the back wall of the shelter and contains a
Proto-Solutrean (level 6) through Middle Solutrean (level 9) sequence.
In Portugal, assemblages with diagnostic laurel-leaf point fragments
date to ca. 20,000-20,500 years B.P., and the
Proto-Solutrean dates to ca. 21,500 years B.P. (6, 13).
Radiocarbon dating of charcoal from level 9 yielded a date of
20,200 ± 180 years B.P. (OxA-8419), and samples of charcoal from
level 6 yielded results of 21,180 ± 240 years B.P. (OxA-8420) and
21,380 ± 810 years B.P. (Sac-1561); a stratigraphically less
reliable level 6 sample yielded 22,180 ± 180 years B.P.
(OxA-8418).
The position of the burial,
2.5 m below the Proto-Solutrean remnant,
as well as its archeological resemblances to Gravettian burials
elsewhere, suggests an age several millennia earlier. This inference is
supported by accelerator mass spectrometry radiocarbon dating of
charcoal [24,860 ± 200 years B.P. (GrA-13310)] and Cervus elaphus remains [24,660 ± 260 years B.P. (OxA-8421) and
24,520 ± 240 years B.P. (OxA-8423)] directly associated with the
burial and of a vertebra from a semiarticulated section of a
Oryctolagus cuniculus vertebral column [23,920 ± 220 years B.P. (OxA-8422)] immediately overlying the legs. The burial
therefore occurred between 24,000 and 25,000 years B.P. and probably
between 24,500 and 25,000 years B.P.
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AGE AND BODY SIZE |
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The remains are those of a juvenile (Figs. 1 & 2). All of the deciduous teeth
(right di2 to left dm2 plus left
dc1 and dm2) have apically
closed roots, indicating a median minimum age of
3.0 years. The
I2 is almost at Crc; the
C1 is
C3/4; the
P4 is
Cco; the
M1 and M1 are
R1/4; and the M2 is
Coc (nomenclature established by Moorrees
et al.; ref. 14). The levels of calcification for the latter
four teeth provide median ages (male/female) of 3.4/3.5, 3.9/3.9,
4.9/4.8, and 4.9/4.5 years, by using Euro-American standards (15).
The average estimate is 4.2 years postnatal, and the probable range is
3.5-5.0 years.
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The more complete right femur has an intermetaphyseal length of 198 mm
plus proximal and distal epiphyseal thicknesses of 10.0 mm and 13.3 mm,
respectively. Adding these and rounding up because of the absence of
the epiphyseal cartilages provides an interepiphyseal length of
225
mm. Estimates from the ratios of 4- to 18-year-old modern Euro-American
mean femoral lengths (16) predict adult femoral lengths of
450 mm
(male) and
410 mm (female). These values are below the means for
adult European earlier Upper Paleolithic males (478.0 ± 21.4 mm;
n = 13) and females (427.3 ± 19.0 mm;
n = 9) but within their ranges of variation; the values are close to the means for Neandertal males (443.3 ± 18.7 mm; n = 11) and females (400.3 ± 14.2 mm;
n = 3).
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MORPHOLOGICAL CONSIDERATIONS |
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Materials and Methods. This preliminary assessment of Lagar Velho 1 is concerned with its morphological affinities to northwestern Old World late archaic humans (Neandertals) versus early modern humans. The latter sample consists predominantly of Aurignacian and Gravettian remains between 20,000 and 30,000 years B.P. Given the dearth of earlier Upper Paleolithic juvenile human remains, the comparisons also involve Near Eastern Middle Paleolithic (Qafzeh-Skhul) early modern humans. Recent human comparative data are included as appropriate, the samples deriving from temperate European and North American samples (17-19). The relative positions of the fossil specimens in the postcranial proportional assessments are based on distributions of raw residuals from the reduced major axis lines for the recent human samples and are expressed as z scores.
The Temporal Bone. The mastoid region in the left temporal bone is preserved with little damage. It has a clear juxtamastoid eminence, which extends to the same level as the mastoid process tip. The relative sizes of these two processes is intermediate between Neandertal juveniles with their larger juxtamastoid eminences (20) and early modern humans with their more projecting mastoid processes (21, 22).
The Mandible. The anterior mandibular symphysis has the full development of a mentum osseum (Fig. 3). There is a very prominent tuber symphyseos with an exceptionally protruding tuberculum laterale on each side. These combine to create a deeply excavated incisura mandibulae anterior. The midline of the tuber symphyseos extends superiorly toward the alveoli. By any criteria, this symphyseal configuration is a prominent development of a "chin," clearly distinct from the modest development of these elements in similarly aged Neandertals (19, 23) and pronounced even for a developmentally comparable modern human (21, 24).
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The Dentition. The deciduous dental remains have no macroscopic pathological alterations and minimal incisor attrition. The first molar crown diameters (Table 1) are similar to those of Neandertals and early modern humans, who are not significantly different in these dimensions. The I2 breadth shows a gradual decrease from Neandertals to Qafzeh-Skhul humans to earlier Upper Paleolithic humans to recent Europeans, and Lagar Velho 1 falls between the means of the last two samples. Late archaic and early modern humans differ more in their anterior-to-posterior dental proportions than in absolute dental dimensions (26), and the relative I2 versus M1 breadths of Lagar Velho 1 fall with the early modern humans and separate from the Neandertals.
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The Postcranial Remains. At least one of each of the major long bones was preserved in the appendicular skeleton of Lagar Velho 1, with only the radius lacking a complete intermetaphyseal length (Fig. 4). The intermetaphyseal maximum lengths (left side for all but the femur) are, for the humerus, 143 mm; for the ulna, 122.5 mm; for the femur, 198 mm; and for the tibia, 155 mm. The clavicles are not sufficiently preserved to provide lengths, and major portions of the pelvis remain.
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128°. This value is
similar to the values of juvenile (Roc de Marsal 1, 130°; La Ferrassie 6, 132°) and early adolescent (Teshik-Tash 1, 128°) Neandertals and the juvenile Skhul 1 early modern human (131°). Neck-shaft angles decrease with normal locomotor loading during development (27), such that (based on a recent Native American sample;
ref. 28) it should decrease
2% between the juvenile and adult
years. The predicted adult value for Lagar Velho 1 (125°) is similar
to the values of Neandertals (121.0° ± 4.7; n = 9) and earlier Upper Paleolithic Europeans (118.8° ± 6.0;
n = 13) but below the Qafzeh-Skhul values (133.2° ± 2.6; n = 6). The right femur has a metaphyseal
bicondylar angle (29) of 8°. The greater medial distal epiphyseal
thickness (13.3 mm versus 12.7 mm) suggests that the articular
bicondylar angle was slightly higher. These values are attained by
recent humans at about 4-5 years of age (29). This pattern is echoed
in the proximal tibial metaphyseal orientation; the medial metaphyseal
retroversion angle (12°) is close to articular angles of mature
Neandertal (15.0° ± 2.2; n = 5) and earlier Upper
Paleolithic (15.8° ± 5.3; n = 8) tibiae.
These angles indicate that locomotor loading levels were similar to
those of European Late Pleistocene hominids and nonurban recent humans
(29, 30). In combination with the apparent absence of pathological
lesions on the dental and leg remains, these angles imply normal and
active locomotor behavior for Lagar Velho 1 in the context of little or
no systemic developmental stress. As a result, it is possible to
consider other proportions of its lower limbs as reflections of normal
skeletal morphology.
Early and recent modern humans are largely distinct from archaic humans
in the relative mediolateral shortness of their pubic bones (31), and
this contrast appears early in development (18). A comparison of pubic
(acetabulosymphyseal) breadth to femoral length shows a regular pattern
of development (r2 = 0.857) with the
La Ferrassie 6 Neandertal falling significantly above the recent human
distribution (Table 2). The Lagar
Velho 1 pubic length is within the recent human distribution but is still relatively high for a modern human.
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2-8 years) in a cool-temperate modern
human sample (r2 = 0.983), with Skhul
1 falling above the line and both La Ferrassie 6 and Lagar Velho 1 falling significantly below the recent humans (Table 2). Given the
hyperarctic versus tropical proportions of Neandertal versus
Qafzeh-Skhul adult remains (38), the separation of the La Ferrassie and
Skhul specimens is expected. However, the low position of Lagar Velho 1 is unexpected, given the relatively long tibiae of all known European
earlier Upper Paleolithic humans (32).
These contrasts in adult limb-segment proportions are combined with the
Neandertals having very broad trunks and the Qafzeh-Skhul and European
earlier Upper Paleolithic trunks being quite slender (32, 38). As a
result of the contrasting body masses (and hence baseline
weight-bearing loads) relative to femoral and especially tibial
lengths, Neandertals seem to have robust leg diaphyses, whereas these
early modern humans seem gracile (39). The apparent differences in
structural hypertrophy, however, disappear once body proportions are
taken into account (40-43). Consequently, given that mature diaphyseal
hypertrophy reflects in large part developmental trajectories (44), it
is expected that immature Neandertals and early modern humans had
similar femoral and tibial diaphyseal hypertrophy once body proportions
were incorporated into the analysis. In other words, any significant
differences in diaphyseal hypertrophy should primarily reflect
contrasts in body proportions (relative trunk size for the femur and
relative trunk size plus leg segment proportions for the tibia) and
only secondarily differences in lower limb robusticity.
In the comparison of femoral midshaft circumference to length (Fig.
5), Lagar Velho 1 and the three
Neandertal specimens (La Ferrassie 6, Roc de Marsal 1, and Teshik-Tash
1) fall significantly above the recent human distribution (Table 2).
The Qafzeh-Skhul early modern humans are more modest in their
positions. In the tibial comparison (Fig. 5), the early modern Skhul 1 is in the middle of the recent human distribution (reflecting the
competing effects of linear body proportions and Pleistocene
Homo hypertrophy), and La Ferrassie 6 is well above the
recent human distribution (reflecting the combination of hypertrophy
and hyperarctic body proportions). Lagar Velho 1 is beyond the
Neandertal specimen, clearly separate from the recent humans.
Therefore, either Lagar Velho 1 had exceptionally robust femora and
tibiae, or more likely, it shared the hyperarctic trunk and lower limb
proportions of the Neandertals.
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DISCUSSION |
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These morphological considerations provide a mixed impression of the Lagar Velho 1 juvenile early Upper Paleolithic human skeleton relative to northwestern Old World Neandertals and early modern humans. It is buried in a distinctively early Upper Paleolithic pattern, but its morphology is a mosaic of Neandertal and early modern human features.
The temporal juxtamastoid eminence development is intermediate between these two groups. The mandibular mentum osseum and dental proportions align it completely with the early modern humans. This alignment is supported by mandibular ramal discrete traits, orientation of the radial tuberosity, radial curvature, and relative pubic breadth. The femorotibial length proportions and lower limb hypertrophy (femoral and tibial diaphyseal robusticity and tibial condylar posterior displacement) indicate hyperarctic Neandertal body proportions distinct from those of European earlier Upper Paleolithic humans. In addition, the mandibular symphysis retreats at an archaic angle, and the thoracohumeral muscle insertions are most similar to those of the Neandertals.
The body proportions of Iberian Neandertals are not known, but all European Neandertals, including the Châtelperronian St. Césaire 1, have hyperarctic body proportions (41, 50). It is therefore likely that the Iberian Neandertals either had similar body proportions or, given the more temperate glacial climate of coastal southern Iberia (6), had less extreme cold-adapted proportions. All of the European earlier Upper Paleolithic human remains have subtropical body proportions, whether measured directly or inferred from femoral and tibial diaphyseal scaling (32, 42, 43). The more moderate oxygen-isotope stage 3 climate of southern Iberia versus the climate known for southwestern France or central Europe makes it unlikely that the inferred cold-adapted body proportions of Lagar Velho 1 were the product of regional climatic selection. They can only indicate affinities to the Neandertals.
Although some of these features are developmentally plastic, the mandibular and dental patterns as well as the ecogeographically related body proportions seem to be resistant to environmental perturbations and to be evolutionarily stable over at least the millennia of concern. They are therefore appropriate markers for assessing the ancestry of Lagar Velho 1.
There are two logical explanations for the morphological mosaic seen in Lagar Velho 1. It could represent the ancestral (plesiomorphous) pattern for Late Pleistocene European humans, or it could be the result of admixture between European late archaic and early modern humans. The first explanation can be rejected by the presence of a uniquely derived (autapomorphous) feature of modern humans, its mentum osseum development, supported by its chronological position after the presence of both Neandertals and early modern humans in Europe.
The morphological mosaic of the Lagar Velho 1 child therefore indicates admixture between early modern humans spreading through Iberia and local Neandertal populations. Such morphological mosaics, with character states distinctive to each parental group (directional dominance), plus intermediate (additive) or divergent (overdominance or underdominance) configurations, characterize hybrids between subspecies, species, and genera of primates and carnivores (51-55). It is not known whether any one mosaic pattern would be expected, given specified ancestral morphological patterns, nor is it known how stable the pattern is likely to have been over time. However, the mosaic seen in Lagar Velho 1 conforms to the known patterns of hybridization.
Moreover, the dating of the burial to several millennia after the probable period of transition from Neandertal to early modern human in southern Iberia (28,000-30,000 years B.P.), and hence the persistence of a morphological mosaic for that time period, indicates that this child was not the result of a rare Neandertal/early modern interbreeding but the descendant of extensively admixed populations. There does not seem to be a better means of explaining why, in spite of sharing a similar material culture and identical burial practices with the Gravettian elsewhere in Europe, Lagar Velho 1 is anatomically so distinct.
The presence of such admixture supports the hypothesis (56, 57) of variable admixture between early modern humans dispersing into Europe and local Neandertal populations. It runs counter to the interpretation (58, 59) that, in western Europe, this transition involved the extinction without descent of the Neandertals and their complete replacement by dispersing early modern humans with more elaborate technological and sociocultural systems.
The broader implications of this finding are multiple. First, it means that the degree of abruptness in sociocultural and technological complexes around the time of the transition from the Middle to Upper Paleolithic need say little about the degree of human biological population continuity. Second, the geographical location and temporal position of the transition need not constrain the degree to which there was admixture between local archaic and early modern human populations. Third, it is inappropriate to apply a species distinction with strict implications of reproductive isolation to the Neandertals versus early modern humans. And fourth, hypotheses (60-63) that full population replacement of late archaic humans by early modern humans took place everywhere outside of the (presumably African) core area of modern humans can be rejected. It is therefore necessary to go beyond the categorical models that have been used commonly to characterize the late archaic to early modern human and the Middle to Upper Paleolithic transitions and to recognize the complex regional, temporal, human biological, and cultural processes as well as historical trajectories that took place.
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CONCLUSION |
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The early Upper Paleolithic human burial at Lagar Velho, Portugal, provides evidence of the burial practices and human biology of these Late Pleistocene human populations. The burial, with pierced shell ornamentation and red ochre, is similar to Gravettian ones elsewhere in Europe. The facial and appendicular remains provide a morphological mosaic, with the mandibular mentum osseum and dental proportions, as well as mandibular ramal, antebrachial features, and pubic size, aligning the specimen with European early modern humans. The mastoid region is intermediate; however, the femorotibial length proportions and lower limb hypertrophy reflect arctic body proportions, and these features, along with the mandibular symphyseal retreat and thoracohumeral muscle hypertrophy, indicate affinities to the Neandertals. This mosaic indicates admixture between late archaic and early modern humans in Iberia, refuting hypotheses of complete replacement of the Neandertals by early modern humans and underlining the complexities of the cultural and biological processes and events that were involved in modern human emergence.
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ACKNOWLEDGEMENTS |
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We are grateful to the many curators who have permitted analysis of human remains in their care and to the L. S. B. Leakey, National Science, and Wenner-Gren Foundations for related support. The Lagar Velho project is carried out under the auspices of the Instituto Português de Arqueologia, Ministry of Culture, Portugal.
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FOOTNOTES |
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** To whom reprint requests should be addressed. e-mail: trinkaus{at}artsci.wustl.edu.
A Commentary on this article begins on page 7117.
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REFERENCES |
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|---|
| 1. | Vega Toscano, L. G. (1990) Mem. Mus. Prehist. Ile France 3, 169-176 . |
| 2. | Villaverde, V. & Fumanal, M. P. (1990) Mem. Mus. Prehist. Ile France 3, 177-183 . |
| 3. | Zilhão, J. (1993) in El Origen del Hombre Moderno en el Suroeste de Europa, ed. Cabrera, V. (Univ. Nacl. Educ. Distancia, Madrid), pp. 127-145. |
| 4. | Hublin, J. J., Barroso Ruiz, C., Lara, P. M., Fontugne, M. & Reyss, J. L. (1995) C. R. Acad. Sci. Ser. II 321, 931-937 . |
| 5. | Garcia Sanchez, M. (1986) Homenaje a Luis Siret (Consejeria Cult. Junta Andalucia, Granada, Spain), pp. 49-56. |
| 6. | Zilhão, J. (1997) O Paleolítico Superior da Estremadura Portuguesa (Colibri, Lisbon). |
| 7. | d'Errico, F., Zilhão, J., Julien, M., Baffier, D. & Pelegrin, J. (1998) Curr. Anthropol. 39, S1-S44 [CrossRef]. |
| 8. | Zilhão, J. (1998) in XIII International Congress of Prehistoric and Protohistoric Sciences: Proceedings, eds. Facchini, F., Palma di Cesnola, A., Piperno, M. & Peretto, C. (Abaco, Forli, Italy), Vol. 2, pp. 299-312. |
| 9. | Zilhão, J. (1999) in Gibraltar and the Neanderthals, eds. Stringer, C. B. & Findlayson, J. C. (Oxbow Books, Oxford), in press. |
| 10. |
Svoboda, J., Lo ek, V. & Vl ek, E.
(1996)
Hunters Between East and West
(Plenum, New York).
|
| 11. | Aldhouse-Green, S. & Pettitt, P. B. (1998) Antiquity 72, 756-772 . |
| 12. | Giacobini, G. (1999) Congr. Prehist. France 24, 29-39 . |
| 13. | Zilhão, J. (1991) Etud. Rech. Archeol. Univ. Liege 42, 485-501 . |
| 14. |
Moorrees, C. F. A., Fanning, E. A. & Hunt, E. E.
(1963)
J. Dent. Res.
42,
1490-1502
|
| 15. | Smith, B. H. (1991) in Advances in Dental Anthropology, eds. Kelley, M. A. & Larsen, C. S. (Wiley, New York), pp. 143-168. |
| 16. |
Anderson, M., Messner, M. B. & Green, W. T.
(1964)
J. Bone Joint Surg. Am.
46,
1197-1202
|
| 17. | Brabant, H. & Twiesselmann, F. (1967) Bull. Group. Int. Rech. Sci. Stomatol. 10, 5-180 [Medline] . |
| 18. | Tompkins, R. L. & Trinkaus, E. (1987) Am. J. Phys. Anthropol. 73, 233-239 [Medline] . |
| 19. | Mallegni, F. & Trinkaus, E. (1997) J. Hum. Evol. 33, 651-668 [Medline] . |
| 20. | Tillier, A. M. (1987) in Préhistoire de Poitou-Charentes, ed. Vandermeersch, B. (Comité des Travaux Historiques et Scientifiques, Paris), pp. 201-206. |
| 21. |
Matiegka, J.
(1934)
Homo P edmostensis, Fosilní lov k z P edmostí na Morav I
( eské Akad. V d a Um ní, Prague).
|
| 22. | McCown, T. D. & Keith, A. (1939) The Stone Age of Mount Carmel II (Clarendon, Oxford). |
| 23. | Tillier, A. M. (1981) C. R. Acad. Sci. Ser. II 293, 725-727 . |
| 24. | Schutkowski, H. (1993) Am. J. Phys. Anthropol. 90, 199-205 [Medline] . |
| 25. | Stefan, V. H. & Trinkaus, E. (1999) Bull. Mém. Soc. Anthropol. Paris 10, 87-118 . |
| 26. | Stefan, V. H. & Trinkaus, E. (1998) J. Hum. Evol. 34, 443-468 [CrossRef][ISI][Medline] . |
| 27. | Houston, C. S. & Zaleski, W. A. (1967) Radiology 89, 59-66 [Medline] . |
| 28. | Trinkaus, E. & Ruff, C. B. (1996) J. Hum. Evol. 30, 299-314 [CrossRef]. |
| 29. | Tardieu, C. & Trinkaus, E. (1994) Am. J. Phys. Anthropol. 95, 183-195 [Medline] . |
| 30. | Anderson, J. Y. & Trinkaus, E. (1998) J. Anat. 192, 279-285 . |
| 31. | Trinkaus, E. (1984) Curr. Anthropol. 25, 509-514 [CrossRef]. |
| 32. | Holliday, T. W. (1997) J. Hum. Evol. 32, 423-447 [CrossRef][ISI][Medline] . |
| 33. | Schultz, A. H. (1923) Am. J. Phys. Anthropol. 4, 389-399 . |
| 34. | y'Edynak, G. (1978) Am. J. Phys. Anthropol. 45, 569-574 . |
| 35. |
Vl ek, E.
(1973)
J. Hum. Evol.
2,
537-544
.
|
| 36. | Madre-Dupouy, M. (1992) L'Enfant du Roc de Marsal (Centre National de la Recherche Scientifique, Paris). |
| 37. | Golovanova, L. V., Hoffecker, J. F., Kharitonov, V. M. & Romanova, G. P. (1999) Curr. Anthropol. 40, 77-86 . |
| 38. | Ruff, C. B. (1994) Yearb. Phys. Anthropol. 37, 65-107 [CrossRef]. |
| 39. | Trinkaus, E. (1983) The Shanidar Neandertals (Academic, New York). |
| 40. |
Trinkaus, E.
(1997)
Proc. Natl. Acad. Sci. USA
94,
13367-13373
|
| 41. |
Trinkaus, E., Ruff, C. B., Churchill, S. E. & Vandermeersch, B.
(1998)
Proc. Natl. Acad. Sci. USA
95,
5836-5840
|
| 42. | Trinkaus, E., Stringer, C. B., Ruff, C. B., Hennessy, R. J., Roberts, M. B. & Parfitt, S. A. (1999) J. Hum. Evol., in press. |
| 43. | Trinkaus, E. & Ruff, C. B. (1999) J. Archaeol. Sci., in press. |
| 44. | Ruff, C. B., Walker, A. & Trinkaus, E. (1994) Am. J. Phys. Anthropol. 93, 35-54 [CrossRef][Medline] . |
| 45. | Trinkaus, E. & Rhoads, M. L. (1999) J. Hum. Evol. in press. |
| 46. | Trinkaus, E. (1999) in Gibraltar and the Neanderthals, eds. Stringer, C. B. & Findlayson, J. C. (Oxbow, Oxford), in press. |
| 47. |
Matiegka, J.
(1938)
Homo P edmostensis, Fosilní lov k z P edmostí na Morav II
( eské Akad. V d a Um ní, Prague).
|
| 48. | Churchill, S. E. (1994) Ph. D. Thesis (Univ. New Mexico, Albuquerque, NM). |
| 49. | Heim, J. L. (1982) Les Enfants Néandertaliens de La Ferrassie (Masson, Paris). |
| 50. | Holliday, T. W. (1997) Am. J. Phys. Anthropol. 104, 245-258 [CrossRef][ISI][Medline] . |
| 51. | Mengel, R. M. (1971) J. Mammal. 52, 316-336 [Medline] . |
| 52. | Nagel, U. (1973) Folia Primatol. 19, 104-165 . |
| 53. | Markarjan, D. S., Isakov, E. P. & Kondalov, G. I. (1974) J. Hum. Evol. 3, 247-255 . |
| 54. | Cheverud, J. M., Jacobs, S. C. & Moore, A. J. (1993) Am. J. Primatol. 31, 23-39 . |
| 55. | Peres, C. A., Patton, J. L. & da Silva, N. F. (1996) Folia Primatol. 67, 113-124 . |
| 56. | Bräuer, G. (1984) in The Origins of Modern Humans, eds. Smith, F. H. & Spencer, F. (Liss, New York), pp. 327-410. |
| 57. | Smith, F. H. & Trinkaus, E. (1991) in Aux Origines d'Homo sapiens, eds. Hublin, J. J. & Tillier, A. M. (Presses Univ. France, Paris), pp. 251-290. |
| 58. | Hublin, J. J., Spoor, F., Braun, M., Zonneveld, F. & Condemi, S. (1996) Nature (London) 381, 224-226 . |
| 59. | Krings, M., Stone, A., Schmitz, R. W., Krainitzid, H., Stoneking, M. & Pääbo, S. (1997) Cell 90, 1-20 [CrossRef][ISI][Medline] . |
| 60. |
Stringer, C. B. & Andrews, P.
(1988)
Science
239,
1263-1268
|
| 61. |
Vigilant, L., Stoneking, M., Harpending, H., Hawkes, K. & Wilson, A. C.
(1991)
Science
253,
1503-1507
|
| 62. |
Harpending, H. C., Batzer, M. A., Gurven, M., Jorde, L. B., Rogers, A. R. & Sherry, S. T.
(1998)
Proc. Natl. Acad. Sci. USA
95,
1961-1967
|
| 63. |
Cavalli-Sforza, L. L.
(1998)
Proc. Natl. Acad. Sci. USA
95,
11501-11503
|
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