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1.
    
Three fossils, a cranium of Papio, a cercopithecid frontal bone, and a mandible of juvenile Papio, have been recovered from cave deposits in the !Ncumtsa (Koanaka) Hills of western Ngamiland, Botswana. These specimens are significant because well‐preserved crania of Papio are extremely rare in the fossil record outside of South Africa and because this is the first report of fossil primate cranial remains from Botswana. Thermoluminescence dating of surrounding cave matrix indicates an age of ≥317 ± 114 ka, within the Middle Pleistocene, although it may be older. Based on univariate and multivariate analyses, the adult !Ncumtsa specimen falls within the range of variation seen in extant forms of Papio, yet is distinct from any living species/subspecies and represents a new taxon, named here as a new subspecies of Papio hamadryas—Papio hamadryas botswanae. Am J Phys Anthropol, 2012. © 2012 Wiley Periodicals, Inc.  相似文献   

2.
    
Terrestrial mammals are characterized by their digitigrade limb postures, which are proposed to increase effective limb length (ELL) to achieve preferred or higher locomotor speeds more efficiently. Accordingly, digitigrade postures are associated with cursorial locomotion. Unlike most medium‐ to large‐sized terrestrial mammals, terrestrial cercopithecine monkeys lack most cursorial adaptations, but still adopt digitigrade hand postures. This study investigates when and why terrestrial cercopithecine monkeys adopt digitigrade hand postures during quadrupedal locomotion. Three cercopithecine species (Papio anubis, Macaca mulatta, Erythrocebus patas) were videotaped moving unrestrained along a horizontal runway at a range of speeds (0.4–3.4 m/s). Three‐dimensional forelimb kinematic data were recorded during forelimb support. Hand posture was measured as the angle between the metacarpal segments and the ground (MGA). As predicted, a larger MGA was correlated with a longer ELL. At slower speeds, subjects used digitigrade postures (larger MGA), however, contrary to expectations, all subjects used more palmigrade hand postures (smaller MGA) at faster speeds. Digitigrade postures at slower speeds may lower cost of transport by increasing ELL and step lengths. At higher speeds, palmigrade postures may be better suited to spread out high ground reaction forces across a larger portion of the hand thereby potentially decreasing stresses in hand bones. It is concluded that a digitigrade forelimb posture in primates is not an adaptation for high speed locomotion. Accordingly, digitigrady may have evolved for different reasons in primates compared to other mammalian lineages. Am J Phys Anthropol 2009. © 2009 Wiley‐Liss, Inc.  相似文献   

3.
    
Nonprimate terrestrial mammals may use digitigrade postures to help moderate distal limb joint moments and metapodial stresses that may arise during high‐speed locomotion with high‐ground reaction forces (GRF). This study evaluates the relationships between speed, GRFs, and distal forelimb kinematics in order to evaluate if primates also adopt digitigrade hand postures during terrestrial locomotion for these same reasons. Three cercopithecine monkey species (Papio anubis, Macaca mulatta, Erythrocebus patas) were videotaped moving unrestrained along a horizontal runway instrumented with a force platform. Three‐dimensional forelimb kinematics and GRFs were measured when the vertical force component reached its peak. Hand posture was measured as the angle between the metacarpal segment and the ground (MGA). As predicted, digitigrade hand postures (larger MGA) are associated with shorter GRF moment arms and lower wrist joint moments. Contrary to expectations, individuals used more palmigrade‐like (i.e. less digitigrade) hand postures (smaller MGA) when the forelimb was subjected to higher forces (at faster speeds) resulting in potentially larger wrist joint moments. Accordingly, these primates may not use their ability to alter their hand postures to reduce rising joint moments at faster speeds. Digitigrady at slow speeds may improve the mechanical advantage of antigravity muscles crossing the wrist joint. At faster speeds, greater palmigrady is likely caused by joint collapse, but this posture may be suited to distribute higher GRFs over a larger surface area to lower stresses throughout the hand. Thus, a digitigrade hand posture is not a cursorial (i.e. high speed) adaptation in primates and differs from that of other mammals. Am J Phys Anthropol 2010. © 2009 Wiley‐Liss, Inc.  相似文献   

4.
    
StW 114/115, from Sterkfontein, South Africa, is the earliest complete hominin fifth metatarsal. Comparisons of StW 114/115 to modern humans, extant apes, and partial hominin metatarsals AL 333‐13, AL 333‐78, SKX 33380, OH 8, and KNM‐ER 803f reveal a similar morphology in all six fossils consistent with habitual bipedality. Although StW 114/115 possesses some primitive characters, the proximal articular morphology and internal torsion of the head are very human‐like, suggesting a stable lateral column and the likely presence of lateral longitudinal and transverse tarsal arches. We conclude that, at least in the lateral component of the foot of the StW 114/115 individual, the biomechanical pattern is very similar to that of modern humans. This, however, may not have been the case in the medial column of the foot, as a mosaic pattern of hominin foot evolution and function has been suggested. The results of this study may support the hypothesis of an increased calcaneo‐cuboid stability having been an early evolutionary event in the history of terrestrial bipedalism. Am J Phys Anthropol 2009. © 2009 Wiley‐Liss, Inc.  相似文献   

5.
    
Using a geometric morphometric approach, we explored the variation in skull size and skull shape in banded newts (genus Ommatotriton). The genus Ommatotriton is represented by two allopatric, genetically well‐defined species: Ommatotriton ophryticus and O. vittatus. Within each species, two subspecies have been recognised. The samples used in this study cover the geographical and genetic variation within each species. We found statistically significant variation in skull size between species and among populations within species. When corrected for size, there was no significant variation in shape between species. Our results indicate that the variation in skull shape within the genus Ommatotriton is almost entirely due to size‐dependent, allometric shape changes. The exception is the shape of the ventral skull in males. Males of O. ophryticus and O. vittatus significantly diverge in the shape of the ventral cranium. The ventral skull, more precisely the upper jaw and palate, is directly functionally related to feeding. In general, our results indicate that allometry is a significant factor in the morphological variation of banded newts. However, the divergence in the ventral skull shape of males indicates that sexual selection and niche partitioning may have influenced the evolution of skull shape in these newts.  相似文献   

6.
It has been hypothesized that most morphological evolution occurs by allometric differentiation. Because rodents encapsulate a phenomenal amount of taxonomic diversity and, among several clades, contrasting levels of morphological diversity, they represent an excellent subject to address the question: how variable are allometric patterns during evolution? We investigated the influence of phylogenetic relations and ecological factors on the results of the first quantification of allometric disparity among rodents by exploring allometric space, a multivariate morphospace here derived from, and encapsulating all, the ontogenetic trajectories of 34 rodent species from two parallel phylogenetic radiations. Disparity was quantified using angles between ontogenetic trajectories for different species and clades. We found an overlapping occupation of allometric space by muroid and hystricognath species, revealing both clades possess similar abilities to evolve in different directions of phenotypic space, and anatomical diversity does not act to constrain the labile nature of allometric patterning. Morphological features to enable efficient processing of food serve to group rodents in allometric space, reflecting the importance of convergent morphology, rather than shared evolutionary history, in the generation of allometric patterns. Our results indicate that the conserved level of morphological integration found among primates cannot simply be extended to all mammals.  相似文献   

7.
    
The relationship between locomotor behavior and long bone structural proportions is examined in 179 individuals and 13 species of hominoids and cercopithecoids. Articular surface areas, estimated from linear caliper measurements, and diaphyseal section moduli (strengths), determined from CT scans, were obtained for the femur, tibia, humerus, radius, and ulna. Both within-bone (articular to shaft) and between-bone (forelimb to hindlimb) proportions were calculated and compared between taxa. It was hypothesized that: 1) species emphasizing slow, cautious movement and/or more varied limb positioning (i.e., greater joint excursion) would exhibit larger articular to cross-sectional shaft proportions, and 2) species with more forelimb suspensory behavior would have relatively stronger/larger forelimbs, while those with more leaping would have relatively stronger/larger hindlimbs. The results of the analysis generally confirm both hypotheses. Several partial exceptions can be explained on the basis of more detailed structural-functional considerations. Associations between locomotion and structural proportions can be demonstrated both across major groupings (hominoids and cercopithecoids) and between relatively closely related taxa, e.g., mountain and lowland gorillas, siamangs and gibbons, and Trachypithecus and other colobines. Furthermore, structure and function do not always covary with taxonomy. For example, compared to cercopithecoids, mountain gorillas have relatively larger joints, like other hominoids, but do not have relatively stronger forelimbs, unlike other hominoids. This is consistent with a locomotor repertoire emphasizing relatively slow movement but with very little forelimb suspension. Proportions of Proconsul nyanzae, Proconsul heseloni, Morotopithecus bishopi, and Theropithecus oswaldi are compared with modern distributions to illustrate the application of the techniques to fossil taxa.  相似文献   

8.
    
The Sterkfontein fossil site in South Africa has produced the largest concentration of early hominin fossils from a single locality. Recent reports suggest that Australopithecus from this site is found within a broad paleontological age of between 2.5-3.5 Ma (Partridge [2000] The Cenozoic of Southern Africa, Oxford: Oxford Monographs, p. 100-125; Partridge et al. [2000a], The Cenozoic of Southern Africa, Oxford: Oxford Monographs, p. 129-130; Kuman and Clarke [2000] J Hum Evol 38:827-847). Specifically, the hominin fossil commonly referred to as the \"Little Foot\" skeleton from Member 2, which is arguably the most complete early hominin skeleton yet discovered, has been magnetostratigraphically dated to 3.30-3.33 Ma (Partridge [2000] The Cenozoic of Southern Africa, Oxford: Oxford Monographs, p. 100-125; Partridge et al. [2000a], The Cenozoic of Southern Africa, Oxford: Oxford Monographs, p. 129-130). More recent claims suggest that hominin fossils from the Jacovec Cavern are even older, being dated to approximately 3.5 Ma. Our interpretation of the fauna, the archeometric results, and the magnetostratigraphy of Sterkfontein indicate that it is unlikely that any Members yet described from Sterkfontein are in excess of 3.04 Ma in age. We estimate that Member 2, including the Little Foot skeleton, is younger than 3.0 Ma, and that Member 4, previously dated to between 2.4-2.8 Ma, is more likely to fall between 1.5-2.5 Ma. Our results suggest that Australopithecus africanus should not be considered as a temporal contemporary of Australopithecus afarensis, Australopithecus bahrelghazali, and Kenyanthropus platyops.  相似文献   

9.
We explored the phylogenetic signal of skull size and shape in alpine newts from the Balkans, a group of European newts that, in spite of their considerable phylogeographic substructuring (as inferred from previous DNA analyses), maintain a conserved phenotype. In terms of skull shape disparity, geometric morphometrics show that the dorsal cranium carries a significant phylogenetic signal, the most notable evidence in this present study. On the contrary, no phylogenetic signal in the shape of the ventral cranium was found. This result indicates that the variation in the shape of the ventral cranium is more prone to other factors and processes, such as adaptations to local environments rather than phylogenetic constraints. Variation in skull size within alpine newts seems to be independent from phylogenetic constraints.  相似文献   

10.
The depositional history of the Name Chamber at the Sterkfontein early hominid site is complex, as is the case with most such cavities. Unravelling this history may therefore benefit from the input of less usual lines of evidence to complement baseline geological investigations. In this case, micromammalian remains from the Western Talus of the Name Chamber provide tentative evidence for the depositional history of these deposits. Correlation of samples based on minimum numbers of individuals referred to genera occurring in one third or more of the samples suggests that a large proportion of the Western Talus material, particularly that from the area infiltrated by the Eastern Talus deposit, originated in the vicinity of squares P54, Q54 and Q55 in the main excavation, from a depth spanning the boundary between Acheulean and Oldowan levels in Member 5. Differences in general diversity between the samples from the main excavation and some from the Name Chamber support the proposal that surface sediments of the homogeneous deposits have been contaminated by material entering the cavern during the 1994 opening of the feeder shaft. Initial taphonomic analysis indicates that all samples, both the original and those from the Name Chamber, were accumulated by the same avian predator, that is, one or more of three owl species (barn owl Tyto alba, grass owl Tyto capensis and marsh owl Asio capensis).  相似文献   

11.
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This paper presents a comprehensive comparative study between Dali cranium and other human fossils of Middle Pleistocene and those of later time.The non-metric and metrical features are classified into 9 categories as follows:<br>1.The features of Dali which are similar to other Middle Pleistocene humans(MPH) and quite different from those of early modern humans(EMH).<br>The brow ridges are robust and connect each other in glabellar region.<br>The bregma and vertex coincide in position.<br>There is angular turn on the occipital portion of mid-sagittal contour.<br>The cranial wall is thick.<br>The lacrimal fossa is shallow.<br>The left infraorbital fissure communicates with the infratemporal fossa through a downward passage instead of a horizontal one.<br>The infratemporal surface of sphenoid bone locates at a lower level than the orbital floor.<br>The auricular height of Dali cranium is 102mm. It falls within the variation range (v.r.) of Homo erectus (H.e.) from Zhoukoudian (ZKD) (93.5mm~107mm)[9] and shorter than that of Kabwe (105mm) [9] and Neanderthals (103-122 mm, totally including 7 cases, the sites from which the fossils were enearthed can be checked in the references cited, similarly hereinafter) [9-10]and EMH of China (108~119 mm, including Liujiang, Lijiang, Chuandong and Upper Cave) [11-14].<br>The length-height index I (ba-b/g-op) of Dali cranium is 57.1. It falls within the v.r. of Plio/Pleistocene humans of Africa (50.4~67.5, including KNM-ER1813; OH 9, KNM-ER 3733, 3883) [5, 15] and that of Dmanisi (55.4~65.4) [16]. The value of Dali is slightly higher than that of the recontructed skull of Yunxian 55.8[16], and lower than that of the reconstructed skull of H.e. from ZKD (59.9)[9] and that of Kabwe (60.2) [15] as well as that of most of MPH of Europe (58.6~69.9, including Petralona, Steinheim, Swanscombe; Ceprano; Atapuerca SH 4,5,6) [15-17] except Ehringsdorf (the index is 55.9)[15]. It is much lower than that of EMH of China (66.7~77.7, including Liujiang and Upper Cave) [11,12] and Europe (65.8~71, including 6 cases) [10].<br>The length-height index II (po-b ht/g-op) of Dali is 49.6. It falls within the v.r. of that of Dmanisi (46.38~53.59[16]) and Plio/Pleistocene humans of Africa (46.6~53.3, including OH 9, KNM-ER 3733, 3883) [15]. The value of Dali is close to the lower limit of H.e. from ZKD (49.0~53.3) [9]. It is lower than that of H.e. from Hexian (50) [18] and close to the lower limit of the v.r. of MPH of Europe (51.0~65.1, including Petralona, Steinheim; Arago, Ceprano; Atapuerca SH) [15,16,17]. The index of Dali is much lower than that of EMH of China (57.1~72.5, including Liujiang, Upper Cave, Lijiang and Chuandong) [11,12,13,14] and Europe (58~62.3, including 6 cases) [10].<br>Transverse cranial curvature (au-au/po-b-po) of Dali cranium is 47.2. It is lower than that of H.e.of China (47.4~54.8) [9,18,19] and is between two specimens of Pithecanthropus from Trinil ( I, 52.3 and II, 45.6) [9]. It is lower than that of Kabwe (48.3) [9] and higher than that of Petralona (44.8) [10]. The value of Dali is much higher than that of EMH of China (39.2~42.2, measured by the author on Liujiang and casts of Upper Cave) and Europe (36.5~43.6, including 3 cases)[10].<br>The ratio of b-ast to occipital breadth (ast-ast) of Dali cranium is 113.9. It is within the v.r. of H.e. of China (103.5~119.8, including those of Hexian and cast of ZKD which are all measured by the author) and MPH of Europe (97.8~117.5, including Atapuerca SH, Petralona and Swanscombe) [17]as well as that of MPH of Africa (107.1~116.3, including Kabwe; Eliye Springs, Omo 2)[17, 20]. It is much lower than those in EMH of China (121.5~132.7, including those of Liujiang, Ziyang and casts of Upper Cave which are all measured by the author).<br>The angle, l-i-o of Dali is 105°. It is close to the highest value of the v.r. of H.e. of China (98°~106°, those of ZKD are according to Weidenreich 1943[9]; that of Nanjing is measured by the author) and lowest value of that of MPH of Europe (107°~129.1°, including Ehringsdorf, Steinheim ; Atapuerca SH) [10, 17]. It is much lower than that of modern humans (117°~127.3°) [10].<br>Angle l-op-o of Dali cranium is 98°. It equals the lowest value of the v.r. of H.e. of China (98°~108°, including ZKD and Nanjing) [16, 19],much lower than that of Petralona (106°)[16] and much lower than that of modern humans (128°~138°) [16].<br>The ratio of d-d to fm: a-fm: a of Dali cranium is 22.8. It is between the values of H.e. from ZKD XII (21) and Nanjing (26)(those of ZKD and Nanjing are measured and calculated by the author) and very close to that of Kabwwe (22.6, measured by the author on cast). The value of Dali is much lower than that of Petralona(28.7) [21]and Atapuerca SH 4 and 5 (33.1 and 29.5 respectively) [17] and higher than that in EMH of China (15.5~18.6, measured by the author on fossil from Liujiang and casts of the fossils from Upper Cave).<br>2. Features similar or close to that in modern humans<br>The contour in hind view appears as an even curve with the broadest part locating at the temporal squama.<br>The vertical line passing the most lateral point of mandibular fossa passes through the lateral cranial wall lateral to the joining point between the inner surface of cranial base and lateral cranial wall.<br>The ratio of calvarium height above g-i chord to g-i chord of Dali cranium is 50.4. It is much higher than those in H.e. from ZKD(34.8~41.2)[9], Pithecanthropus from Trinil(33.3~37.4)[9] that of Kabwe (40.5) [10], Saldanha (45.0) [10] and Jebel Irhoud (43.7) [10], and higher of that of Steinheim (46) [10]. The value of Dali falls into the v.r. of EMH of Europe (49-61, including 5 cases) [10].<br>The ratio of arc n-i to n-i chord of Dali cranium is 189.9. It is higher than that of Neanderthals (5 cases, 145.1~178.1) [10], between that of male (181.2) and female (203.7) of Obercassel[10]. Dali’s value is close to the average of Middle Age Japanese (200.0) [10].<br>Angle b-n-op (i) of Dali is 54°. It is much higher than that of H.e. from ZKD (42°~46.5°) [9], Kabwe(48°) [9] and Neanderthals (including 5 cases, 39°~50°) [9]. It is higher than that of Ehringsdorf (52°)[9] and falls into the v.r. of modern humans (45°~59°)[9].<br>Angle g-i-l of Dali cranium is 82°. It is much higher than that t of H.e. of China (57°~68°)(those of ZKD are from Weidenrech[9]; that of Nanjing is measured by the author), Ehringsdorf (63°) [10], Kabwe (68°) [10], and Neanderthals of Europe (including 7 cases, 59°~69°) [10]. Dali’s value falls within the v.r. of modern humans (80.2°~88.6°) [10].<br>Upper facial height (fmt-fmt) of Dali cranium is 121mm. It is much longer than those of H.e. from ZKD(III, 109mm; XI, 111mm?)[16] and Nanjing (107mm,measured by the author) and Hexian (113mm). Dali’s value is very close to that of Maba(126mm) and Upper Cave 101(122mm), and much longer than those in Upper Cave 102 and 103 (113mm and 100mm respectively) as well as that in Liujiang(107mm)(All specimens of China except those from ZKD are measured by the author). Dali’s value is shorter than MPH of Europe(125~130mm, including Arago, Atapuerca SH5, Petralona and Ceprano)[16], and much shorter than those from Bodo(136mm) [16]and Kabwe(139mm)[16].<br>The depth of facial bones (ba-pr) is 105mm. It is much shorter than that of Atapuerca SH 5 (115mm) [16], Petralona (119 mm) [16], Bodo (118 mm) [16] and Kabwe (117.5mm) [16]. Dali’s value falls within the v.r. of EMH of China (100~113.6 mm, including Liujiang and Upper Cave) [11, 12] and is close to the average of that of modern humans (including 60 cases, 97.2 mm) [16].<br>The ratio n-ba/ba-pr of Dali cranium is 100.5. It is much higher than that in Bodo (88.4) [16]; Kabwe (93.1) [16], Atapuerca SH 5(87.8) [16] and Petralona (94.8) [16]. It falls within the v.r. of EMH of China (99.3~112.0 , including Liujiang and Upper Cave) [11, 12] and is close to the average of modern humans (101.7) [16].<br>Cheek height(WMH) of Dali cranium is 23mm. It is within the v.r. of early modern humans of China(21.7~27.2mm, including 7 sides of 4 cases of Upper Cave and Liujiang, measured by the author). Dali’s value is shorter than that in H.e. from ZKD(XII, 28mm, measured by the author), and those in MPH of Europe(26.7~37.1mm, including 7 sides of 6 cases) [17]. It is close to the H.e. from Nanjing(24.3mm, measured by the author) and Zuttiyeh(24mm)[17], but the dimensions of H.e. from Nanjing are generally shorter than H.e. from ZKD.<br>The prosthion angle (n-pr-ba) of Dali cranium is 69.5°. It is very close to the average of that of modern humans (71.4°±3.1°) [24] and much higher than that in Kabwe ( 62.1°) [24], Bodo( 59°, calculated by the author based on the data in Rightmire, 1996[23]), Atapuerca SH 5 (60.9°) [17] and Petralona (62.0°) [24].<br>3. Features far from that in H.e. of China and within the v.r. of that in EMH of China and /or modern humans. These features are also close to that in MPH of Europe and/or Africa<br>Dali cranium has no supraorbital process.<br>The maximum cranial length (g-op) is 16.5 mm longer than glabella-inion length (g-i) in Dali cranium. The difference between these two measurements is very short or none in H.e. of China and is between 4 mm and 17 mm in EMH of China (including Liujiang[11] ,Upper Cave[12], Lijiang[13] and Chuandong 2[14]). The difference is larger than 5 mm in Petralona[15], Steinheim[15], Jebel Irhoud [10] and Narmada[15].<br>Transverse fronto-parietal index (100 x ft-ft/eu-eu) is 69.6 in Dali cranium. It is higher than that of H.e. of China (55.9~64.5, including ZKD, Hexian, and Nanjing) [9, 18, 19, 25] and falls in the v.r. of EMH of China (66.9~77.1, including Liujiang , Upper Cave and Lijiang)[11, 12, 13]. Dali’s value is higher than that of Kabwe(64.3) [15] and Salé (57.5) [15]. It is within the v.r. of MPH of Europe (67.0~77.9, including Ehringsdorf, Steinheim; Arago, Ceprano, Petralona; Atapuerca SH) [15,16,17].<br>The total cranial arc (n-o arc) is 379 mm in Dali cranium. It is much longer than those in H.e. from ZKD (321 mm~337 mm)[9] and H.e. from Hexian (340 mm?) [18]. It falls within the v.r. of EMH of Chna (335 mm~388.5 mm, including Liujiang, Upper Cave, Lijiang, Chuandong and Ziyang) [11-14, 28] and that of MPH of Europe and Africa (340 mm~380 mm , including Ehringsdorf [9]Atapuerca SH, Petralona, and Kabwe [9]) (the values of Atapuerca SH and Petralona are calculated by the author based on the data presented in Arsuaga et al. [17] and Stringer et al. [21],respectively).<br>The cranial curvature on the n-o chord is 37.7 in Dali cranium. It is lower than that of H.e. from ZKD (43.2-44.9) [9], Nanjing (48.8) (by the author)and Hexian (38.5) [18]. It falls within the v.r. of EMH of China (36.4~40.3, including Liujiang , Upper Cave and Ziyang ) [11, 12, 28] and v.r. of modern humans (35.2~39.9) [9]. Dali’s value is close to the average of that of modern humans (36.6) [9], Kabwe (37.1) [9]and slightly lower than that of Ehringsdorf (40.1) [9].<br>The ratio of maximum frontal breadth to occipital breadth (co-co/ast-ast) is 103.5 in Dali cranium. It is much higher than those of H.e. of China (including ZKD, Nanjing and Hexian: 83.9~99.1?)(ZKD is from Weidenreich, 1943[9], Nanjing and Hexian are by the author) and that of Kabwe(90.5, calculated by the author based on Weidenreich, 1943[9]). Dali’s value falls within the v.r. of MPH of Europe (93.6~108.8, including Arago, Atapuerca SH 4 and 5, Petralona, Steinheim and Swanscombe) [29]. Dali’s value falls within the v.r. of EMH of China (including Upper Cave, Liujiang and Ziyang: 100~114, by the author) and is close to the average of Mesolithic humans of Europe (male, 102.9; female, 103.3) and Sepúlveda population (male, 103.0; female, 105.6)[29].<br>The minimum frontal breadth of Dali cranium is 104 mm. It is much longer than those of H.e.of China (80.0 mm~93 mm including ZKD, Hexian and Nanjing) [9, 18, 19] and falls within the v.r. of EMH of China (83 mm~110 mm , including Upper Cave, Liujiang, Ziyang, Longlin and Maludong) [1, 12, 28, 30]. It falls also in the v.r. of EMH of Europe (91 mm~111 mm) [30] and West Asia (96 mm~110 mm) [30]. The mean values of last two groups are 105±5mm and 103±5 mm respectively). Dali’s value falls also in the v.r. of MPH of Europe (102 mm~117 mm , including Arago, Steinheim; Ceprano, Petralona ; Atapuerca SH) [15, 16, 17]and is close to that of Bodo (103 mm) [16] , but is longer than that of Kabwe (96) [16].<br>The ratio of minimum frontal breadth to maximum frontal breadth (ft-ft/co-co) is 87.4. It is higher than those of H.e. of China (77.8~84.3, including ZKD [9], Nanjing [19] and Hexian which is measured and calculated by the author)and falls within the v.r. of MPH of Europe (86.1~100, including Arago, Petralona, Steinheim; Ceprano , Atapuerca SH,) [15, 16, 17] and that of African MPH ( 78.3~89.6, including Bodo, Kabwe and Salé) [16, 31]. It falls also within the v.r. of EMH of China (76.0~90.5, including Upper Cave, Liujiang, Ziyang, and Maludong which is from Curnoe et al., 2012[30]; U.C., Liujiang and Ziyang are measured and calculated by the author).<br>The bistaphanic breadth (st-st) of Dali cranium is 108 mm. It is longer than those of H.e. of China ( 78mm~103mm , including ZKD [9], Nanjing and Hexian, latter two are measured by the author), and falls within the v.r. of EMH of Chian(105~119.5, including Upper Cave 101, 103, Liujiang and Ziyang, all of these are measured by the author). The mean value of modern humans (110.42mm) [16] is close to that of Dali’s value which falls also within the v.r. of MPH of Europe (102mm~130mm, including Arago, Petralona, Ceprano; Atapuerca SH) [16, 17].<br>Length-height index of temporal squama is 64.6 in Dali cranium. It is higher than those in H.e.of Chinna (45.2~60, including ZKD and Hexian) [9, 18], and slightly lower than those in Atapuerca SH (including 5 cases, 69.3~79.7) [32]. Dali’s value is close to the average of that of modern man (65.2) and well within his v.r. (49.4~87.5). [9]<br>The frontal profile (angle m-g-i) of Dali cranium is 74°. It is much larger than those of H.e. of China (56°~63°,including ZKD, Hexian, and Nanjing ) [9, 18, 19], Pithecanthropus from Trinil (47°and 55°) [9] and MPH of Africa (including Jebel Irhoud, 67°[10]; Saldanha, 61°[10]; Kabwe, 60°[9]). Dali’s value is very close to that of Ehringsdorf (73.5°) [9] and falls in the v.r. of mordern man (70°~96°)[9].<br>4. Features intermediate between MPH and EMH<br>Dali cranium has a weak bregmatic eminence, a fusiform median sagittal ridge at the middle part of frontal bone, and a tympanic plate the thickness of which is intermediate between that of H.e.from ZKD and modern man.<br>An angular torus presents at the outer surface of parietal bone.<br>Tranverse cranial curvature (au-au / arc po-b-po) of Dali cranium is 47.2. The comparsions between Dali cramium and other specimens have been persented among the features of Group 1. <br>5. Features intermediate between H.e. and EMH of China and close to those in MPH of Europe and/or Africa<br>The cranial curvature above chord n-op of Dali cranium is 51.8. It is much lower than those in H.e. from ZKD (55.7~57.3) [9], slightly lower than that in H.e. from Hexian (52.9, measured by the author). It is slightly higher than the upper limit of the v.r. of EMH of China (including Upper Cave, Liujiang, and Ziyang, 47.2~51.0, by the author) and is well within the v.r. of MPH of Europe (49.5~54.4, including Ehringsdorf[9], Atapuerca SH[17] and Petralona[21]). That of Kabwe (54.2) [9] is also within the v.r. of MPH of Europe.<br>The ratio of maximum frontal breadth to maximum cranial breadth (co-co/eu-eu) is 79.3 in Dali cranium. It is intermediate between those in H.e. of China (68.5~76.9, including ZKD [9], Nanjing and Hexian which are measured and calculated by the author) and those in EMH of China (79.7~93.1, including Upper Cave, Liujiang and Ziyang, measured by the author). It falls in the v.r. of MPH of Europe (Atapuerca SH: 75.0~87.9) [17] and v.r. of Neanderthals of Europe (including 11 cases, 75.5~83.4) [29]. It is much lower than the averages of early Upper Paleolithic man of Europe (male: 87.9; female: 85.2) [29]and within the v.r. of Sepúlveda population (male, 41 cases: 72.9~90.1; female, 57 cases: 77.7~90.8) [29].<br>6. Features close to those in fossil humans of East Asia and distant to those of MPH of Europe and / or Africa<br>The median sagittal ridge of frontal bone is higher and has narrower base than those in MPH of Europe and Africa.<br>The ratio of nasion subtense fraction of n-b chord to n-b chord is 43.5 in Dali cranium. It is slightly lower than those in H.e. from ZKD(45.3~48.7) [16] and slightly higher than that of H.e from Nanjing(42.4, by the author). It falls in the v.r. of EMH of China ( 43.0~46.0, including Upper Cave and Liujiang, all are measured and calculated by the author). On the contrary, Dali’s value is much lower than those in MPH of Europe (including Petralona, 50.0[16]; Arago, 49.6, based on the data presented by de Lumley[16]) and is lower than those in MPH of Africa (44.9~54.1, including Laetoli OH18, Eliye Springs , Omo 1, Jebel Ithoud 1 and 2 and Singa) [3].<br>The occipital angle of Dali cranium is 96°. It is within the v.r. of H.e. of China (including ZKD and Nanjing, 95°~108°, measured on the Figures in Weidenreich[9] and Wu et al. [19] respectively) and is much lower than those of Atapuerca SH (106.5°~126.1°) [17]. Dali’s value is also much lower than those of Plio/Pleistocene huamns of Africa( 101°~114°, including KNM-ER 3883, 3733, 1813?) [34], Dmanisi (115.6° and 108°) [34] and Sangiran (105° and 100°) [34].<br>The anterior interorbital breadth (mf-mf) of Dali cranium is 21.5 mm. It is close to that in EMH of China (including Upper Cave and Liujiang: 19.1mm~21.2mm, by the author), H.e. from ZKD(No.XII, 22.5mm), Nanjing(19mm) and slightly shorter than that of EMH of Europe (including 7 cases: 23.4±2.9 mm) [22]. Dali’s value is much shorter than that in MPH of Europe, Africa and West Asia (including 5 cases, 29.5±2.2 mm) [22].<br>The upper facial index (n-pr/zy-zy) of Dali cranium is 53.2. It is close to that of Jinniushan(50.1)[26], H.e. of Nanjing (49.9) [19] and ZKD XII (54.5, measured by the author on cast). Dali’s value is within the v.r. of EMH of China(48.5~53.8) [11, 12] , but is lower than those in MPH of Europe (56.0~59.0, including Petralona, Steinheim; Atapuerca SH) [10, 17] and Africa (54.2~64.7, including Jebel Irhoud, Kabwe; Bodo) [10, 35].<br>The distance between infraorbital foramen and inferior border of orbit is 8.3 in Dali cranium. It is close to that in H.e. of Nanjing (7.5 mm, measured by the author) and much shorter than those in Atapuerca SH (14.1 mm~17.7 mm) [17] and Petralona (16.4 mm) [17].<br>The ratio d-d to fm:a of Dali cranium is 22.8 mm. The comparisons between Dali cranium and other specimens have been presented among the features of Group 1.<br>7. Features quite different from those in H.e. of China and are close to those in MPH of Europe and/or Africa<br>In Dali cranium supraorbital process is absent, the middle part of the supraorbital torus is much thicker than the medial and lateral part, and there is a bulge between the orbit and pyriform aperture.<br>The l-ast chord of Dali cranium is 94 mm. It is within the v.r. of MPH of Europe (74.5 mm~95.6 mm , including 10 cases, 17 sides of Atapuerca SH and Petralona) [17, 21] and much longer than those in H.e. of China (77 mm~87 mm, including ZKD[9] and Hexian which is measured by the author).<br>The bifrontal breadth (fm: a-fm: a) of Dali cranium is 114 mm. It is much longer than the MPH of China (96 mm~104 mm, inluding H.e. from ZKD, Naanjing and Hexian, Maba , all of these are measured by the author) and close to those in MPH of Europe, Africa and West Asia ( mean value of 6 cases: 114.7±8.5) [22].<br>The EQ of Dali cranium, average of H.e. from ZKD and MPH of Europe and Africa are 5.30, 4.6 and 5.3±1.29 respectively, as estimated by Rightmire[36].<br>8. Feature close to those in MPH of Africa and distant from other MPH of China and Europe<br>The ratio of glabella subtense fraction of g-b chord to g-b chord is 43.4 in Dali cranium. It is lower than those of H.e. from ZKD (47~50.9, measured and calculated by the author based on the figures in Black[37] and Weidenreich[9]), Nanjing (49.7, by the author ) and Maba (45.1, by the author). But it is within the v.r. of EMH of China (41~48.5, including Huanglong[40], Upper Cave, Liujiang and Ziyang, that of the latter three are made by the author), Dali’s value is within the v.r. of MPH of Africa (42.6~58.5, including Florisbad, Jebel Irhoud, Kabwe, Laetoli, Omo 1 and Saldanha) [3]. But it is much lower than those in Arago (51, calculated by the author based on the cast and the data presented in Spitery [38]), and Ceprano (60.8, measured and calculated by the author based on the figure presented in Ascenzi et al [39]).<br>9. Features rarely seen in other MPH or uniquely seen in Dali<br>A quadrangular shaped process of the size of 10×7 mm, extending from the antero-superior part of temporal squama and connects with frontal bone. This makes the sutures in pteryon region obliquely posited ∏ shape.<br>The crista galli is thin and low with a large transverse diameter. The angle g-i-o of Dali is 21°. It is much smaller than those in H. e. from ZKD (37°~44°,measured by the author on the figures presented in Weidenreich [9]) and Nanjing (49°, measured by the author on cast) , Neanderthals of Europe and Asia (31°~54°, including 7 cases) [10] and modern man (31°~40°) [10].<br>Discussion and conclusion<br>The features including in Group 1 confirm the position of Dali cranium in Middle Pleistocene. Features of Group 2 show that this cranium is one of the specimens closer to EMH than H.e. if not also MPH of Europe and Africa. Part of the features of Group 2, 3, 4 and 5 suggest that thepopulation represented by Dali cranium provides more contribution to the formation of modern man than H.e. of China, if not also the MPH of west part of Old World. The features of Groups 1 and 2 and some features of other Groups indicate that Dali cranium represents a mosaic with primitive and progressive characters. Features of Group 6 and part features in Group 1, 2, 3 and 5 suggest close relation of Dali cranium to populations of East Asia. Many features presented in Groups 2, 3, 4, 5, 7, 8 and 9 indicate that Dali cranium probably belong to a population different from H.e. Thhe features of Group 3, 5, 7, 8 and part of Group 4 suggest that Dali may have close relation with the populations in the western part of Old World. So Dali cranium is a mosaic joining some features of H.e. of China, MPH of Europe and Africa as well as some modern features. This cranium belongs to neither H.e., nor H.heidelbergensis. The population represented by Dali cranium have made more contribution in the formation of EMH of China than H.e. of China and MPH of Africa. Considering the geographical factor and the association with the Paleoliths of Mode I of Dali cranium, more reasonable inference may be that the root of the population represented by Dali cranium is in East Asia and the antecessors of this population originally had higher affinity with the populations of Europe or had absorbed the gene flow from the West before evolving to Dali population.<br> With regards to the relation between the humans of Middle and Late Pleistocene Rightmire (1995)[41] has proposed four hypotheses, the evidence exhibited in the present paper are more favourable to the fourth hypothesis of him, namely the recent humans are most closely related with Archaic Asians.<br> In spite of the limitation of the data for comparison the present author would like to say that the complexity of the morphology shown in Dali cranium suggeats that the human evolution in East Asia is not as simple as we thought until present. The Middle Pleistocene humans may be classified into several morphs: Dali morph, erectus morph, Narmada morph, Zuttiye morph, Rhodesia morph (for Africa), Heidelberg morph (for Europe) etc. Hexian specimens may represent a submorph of erectus morph, Jinniushan, Maba and Quyuan River Mouth may represent separate submorphs of Dali morph or separate morphs for themselves. Atapuerca SH and Arago may represent separate submorphs. The model of human evolution in Middle Pleistocene is like a river network.<br>The above mentioned comparisons are based on limited information available. The author looks forward to the accumulation of new data to renew the preliminary conclusion based on this study.  相似文献   

12.
    
Body mass estimation equations are generated from long bone cross-sectional diaphyseal and articular surface dimensions in 176 individuals and 12 species of hominoids and cercopithecoids. A series of comparisons is carried out to determine the best body mass predictors for each of several taxonomic/locomotor groupings. Articular breadths are better predictors than articular surface areas, while cross-sectional shaft strengths are better predictors than shaft external breadths. Percent standard errors of estimate (%SEEs) and percent prediction errors for most of the better predictors range between 10-20%. Confidence intervals of equations using sex/species means are fairly representative of those calculated using individual data, except for sex/species means equations with very low %SEEs (under about 10%), where confidence intervals (CIs) based on individuals are likely to be larger. Given individual variability, or biological \"error,\" this may represent a lower limit of precision in estimating individual body masses. In general, it is much more preferable to determine at least broad locomotor affinities, and thus appropriate modern reference groups, before applying body mass estimation equations. However, some structural dimensions are less sensitive to locomotor distinctions than others; for example, proximal tibial articular M-L breadth is apparently \"locomotor blind\" regarding body mass estimation within the present study sample. In other cases where locomotor affiliation is uncertain, mean estimates from different reference groups can be used, while for some dimensions no estimation should be attempted. The techniques are illustrated by estimating the body masses of four fossil anthropoid specimens of Proconsul nyanzae, Proconsul heseloni, Morotopithecus bishopi, and Theropithecus oswaldi.  相似文献   

13.
14.
    
Cranial discrete or 'epigenetic\" traits have been analyzed for interrelationships with measurements of the skull in a sample of American Negro males. Univariate t and multivariate T2 tests are used. It has been the previous consensus view that nonmetric and metric characters are unrelated. Statistically significant associations between the total of 50 discrete and 23 metrical characters, however, are much more frequent than would be expected through random distribution. Multivariate analysis supplements simpler statistics by synthesizing patterns of variation within regions of the skull, identifying many interrelations of skull size and shape with discrete traits. A low but observable general influence is exerted upon nonmetric morphology by metrical variation of the human skull (or vice versa).  相似文献   

15.
SUMMARY

Two alien species and seven indigenous species, including two minnow species, were present in Sterkfontein Dam. Of the larger species, Barbus aeneus and Labco capensis were the dominant in terms of numbers.  相似文献   

16.
In this study, allometric trajectories for 51 rodent species, comprising equal representatives from each of the major clades (Ctenohystrica, Muroidea, Sciuridae), are compared in a multivariate morphospace (=allometric space) to quantify magnitudes of disparity in cranial growth. Variability in allometric trajectory patterns was compared to measures of adult disparity in each clade, and dietary habit among the examined species, which together encapsulated an ecomorphological breadth. Results indicate that the evolution of allometric trajectories in rodents is characterized by different features in sciurids compared with muroids and Ctenohystrica. Sciuridae was found to have a reduced magnitude of inter‐trajectory change and growth patterns with less variation in allometric coefficient values among members. In contrast, a greater magnitude of difference between trajectories and an increased variation in allometric coefficient values was evident for both Ctenohystrica and muroids. Ctenohystrica and muroids achieved considerably higher adult disparities than sciurids, suggesting that conservatism in allometric trajectory modification may constrain morphological diversity in rodents. The results provide support for a role of ecology (dietary habit) in the evolution of allometric trajectories in rodents.  相似文献   

17.
    
Two analyses conclude that Sts 19 cannot be accommodated within the Australopithecus africanus hypodigm (Kimbel and Rak [1993] In Kimbel and Martin [eds.]: Species, Species Concepts, and Primate Evolution. New York: Plenum, pp. 461–484; Sarmiento [1993] Am. J. Phys. Anthropol. [Suppl.] 16:173). Both studies exclude Sts 19 because it possesses synapomorphies with Homo. Furthermore, according to Kimbel and Rak (1993), including Sts 19 in A. africanus results in an unacceptably high degree of polymorphism. This study aims to refute the null hypothesis that Sts 19 belongs to A. africanus. Twelve basicranial characters, as defined and implemented in Kimbel and Rak's study, were scored for casts of seven A. africanus and seven Homo habilis basicranial specimens. These characters were also examined on specimens from a large (N = 87) sample of African pongids. Contrary to Kimbel and Rak's (1993) findings, the null hypothesis is not refuted. The degree of polymorphism among A. africanus with Sts 19 included is less than that seen in Pan troglodytes. In addition, Sts 19 shares only one apomorphy with Homo. However, when treated metrically, Sts 19's morphology for this character is not significantly divergent from other A. africanus specimens. Am J Phys Anthropol 105:461–480, 1998. © 1998 Wiley-Liss, Inc.  相似文献   

18.
吴新智 《人类学学报》2014,33(4):405-426
本文将大荔颅骨的一系列形态特征与中国的直立人、欧洲和非洲的中更新世人、欧洲和亚洲的尼安德特人、中国和欧洲的早期现代人以及现生现代人的数据进行比较,发现可以归纳为几种状况。大荔颅骨:1)与其他中更新世颅骨比较一致,而与早期现代人相去较远;2)与早期和现生现代人一致或接近,显得比其他中更新世人进步;3)在中国早期现代人或现代人变异范围内,也在欧洲中更新世人变异范围内或与之接近,却与中国直立人相距较远;4)处于一般中更新世人与早期现代人之间的中间状态;5)处于中国直立人与中国早期现代人之间的中间位置,而且比较接近欧洲/非洲中更新世人;6)与东亚多数化石人比较一致,而与旧大陆西部中更新世化石人相去较远;7)与中国直立人显然不同,而与欧洲/非洲中更新世人更加接近;8)与非洲中更新世人接近,而与中国直立人和欧洲中更新世人差距较大;9)与大多数中更新世人不同,似乎是自身独有或罕见的。基于这样复杂的状况,作者提出,大荔颅骨既不属于直立人,也不属于海德堡人,表现为兼具东亚的直立人、欧洲和非洲中更新世人的特征,而且是这些共有特征与早期现代人部分特征的镶嵌体,可能比中国的直立人对中国现代人的形成做出过更大的贡献。  相似文献   

19.
    
The first neutron diffraction data were collected from crystals of myoglobin almost 42 years ago using a step‐scan diffractometer with a single detector. Since then, major advances have been made in neutron sources, instrumentation and data collection and analysis, and in biochemistry. Fundamental discoveries about enzyme mechanisms, biological complex structures, protein hydration and H‐atom positions have been and continue to be made using neutron diffraction. The promise of neutrons has not changed since the first crystal diffraction data were collected. Today, with the developments of beamlines at spallation neutron sources and the use of the Laue method for data collection, the field of neutrons in structural biology has renewed vitality.  相似文献   

20.
    
Marmots are of great interest for both sociobiologists studying the evolution of mammal societies and conservationists trying to protect them from extinction. In contrast, their phylogeny and morphological evolution are poorly understood and studied. Recently, a phylogenetic analysis using cytochrome b provided the first reconstruction of marmot evolutionary history and suggested that a high level of sociality evolved at least twice independently in the two proposed marmot subgenera. A morphological analysis of the marmot mandible supported this subgeneric classification and showed interesting, and unexpected, patterns in the evolution of marmot skeletal characters. In the present study we investigated a more complex, and potentially informative structure, the ventral cranium. Geometric morphometric techniques were applied in the first analysis of cranial morphology including all marmot species. Three main phenetic groups were found, which reflect phylogeny (subgenus Petromarmota , and Palaearctic subgenus Marmota ) or geographical distribution (Palaearctic vs. Nearctic subgenus Marmota ). Convergence in skeletal characters due to size similarities, a common finding in the sciurid skeleton according to traditional morphological analyses, did not occur in the marmot ventral cranium. Despite a genetic distance between Marmota vancouverensis and Marmota caligata similar to that among different populations of the latter species, the Vancouver Island marmot had the most atypical ventral cranium in the subgenus Petromarmota . This finding confirmed results obtained with the mandible, and emphasized the uniqueness of M. vancouverensis and the usefulness of complementing molecular analyses with morphological studies for a thorough characterization of population divergence, and a careful planning of conservation strategies.  © 2004 The Linnean Society of London, Biological Journal of the Linnean Society , 2004, 82 , 385–407  相似文献   

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