Fractal analysis and its applications in human palaentology

Fractal analysis was applied in human palaentology by Gibert and Palmqvist to estimate the value of the fractal dimension obtained from the cranial sutures preserved in the fragment of occipital bone (VM-0) found at the Venta Micena site. This paper also estimated the values of fractal dimension for different specimens in order to establish a taxonomy. Although that initial study demonstrated that the technique could be useful in human palaentology, the large variability of sutures observed in the VM-0 sample requires a mechanism that makes it possible to automatically obtain an objective plot of the suture to be analyzed.     

Linking form and function of the fibrous joints in the skull: a new quantification scheme for cranial sutures using the extant fish Polypterus endlicherii

The aim of this study is to connect specific sutural morphologies with the specific types of deformation they experience. To meet this goal, we quantified the morphologies of the interfrontal (IF), interparietal (IP), and frontoparietal (FP) sutures in the extant fish Polypterus endlicherii, and used our published measurements of in vivo deformation of these sutures during feeding to infer how suture morphology and function are connected. Specifically, we found that three relatively simple measures of cross-sectional suture complexity (i.e., the ratio of total sutural length to its shortest end-to-end length; amount of sutural overlap; and size of the largest interdigitation) can be used to distinguish between the IF, FP, and IP sutures, which exhibit very different cross-sectional shapes and responses to loading. Interestingly, these differences in cross-sectional morphology are not reflected by the linear traces of these sutures on the surface of the skull, implying that cross-sectional shape of a suture must be known to infer the loading conditions it experiences. Plotting the three cross-sectional metrics against one another to yield a sutural morphospace shows that the IF, IP, and FP sutures define regions that are largely distinct from one another. Our previous measurements of strain across these sutures suggested that the FP region would lie between the IF and IP regions; instead, the FP region is largely set apart from the other two fields. Based on this discovery, and on the locations of cranial muscles, we propose a new model of deformation in the skull of P. endlicherii during feeding, in which rotation parallel to the skull roof is combined with bending, subjecting the FP suture to complex shearing. Finally, although the sutures of P. endlicherii appear to be significantly less complex than those of mammals, these fish sutures show a similar range of morphologies and perform similar functions as do mammalian sutures.     

Assessment of the role of sutures in a lizard skull: a computer modelling study

Sutures form an integral part of the functioning skull, but their role has long been debated among vertebrate morphologists and palaeontologists. Furthermore, the relationship between typical skull sutures, and those involved in cranial kinesis, is poorly understood. In a series of computational modelling studies, complex loading conditions obtained through multibody dynamics analysis were imposed on a finite element model of the skull of Uromastyx hardwickii, an akinetic herbivorous lizard. A finite element analysis (FEA) of a skull with no sutures revealed higher patterns of strain in regions where cranial sutures are located in the skull. From these findings, FEAs were performed on skulls with sutures (individual and groups of sutures) to investigate their role and function more thoroughly. Our results showed that individual sutures relieved strain locally, but only at the expense of elevated strain in other regions of the skull. These findings provide an insight into the behaviour of sutures and show how they are adapted to work together to distribute strain around the skull. Premature fusion of one suture could therefore lead to increased abnormal loading on other regions of the skull causing irregular bone growth and deformities. This detailed investigation also revealed that the frontal-parietal suture of the Uromastyx skull played a substantial role in relieving strain compared with the other sutures. This raises questions about the original role of mesokinesis in squamate evolution.     

Eyasi 1 and the suprainiac fossa

A reexamination of Eyasi 1, a later Middle Pleistocene east African neurocranium, reveals the presence of a suite of midoccipital features, including a modest nuchal torus that is limited to the middle half of the bone, the absence of an external occipital protuberance, and a distinct transversely oval suprainiac fossa. These features, and especially the suprainiac fossa, were considered to be uniquely derived for the European and western Asian Neandertals. These observations therefore indicate that these features are not limited to Neandertal lineage specimens, and should be assessed in terms of frequency distributions among later archaic humans.     

Insights into the evolution of child growth from Lower Pleistocene humeri at Venta Micena (Orce, Granada province, Spain)

Well-defined human anatomical characteristics are present on humeral fragments of a child (VM-1960) and an adult (VM-3691) from early Lower Pleistocene sediments at Venta Micena: both have narrower medullary cavities than in AfricanHomo erectus/ergaster (KNM-ER 1808), and the child’s humeral shaft is longer than in recent 8-to-9-year-olds even though its muscle markings are less pronounced than theirs. We infer that exposure of growing children to high mechanical loading favoured Plio-Pleistocene skeletal evolution inHomo of humeral robusticity and elongation. Precocious childhood arm-bone development, occurring before pubertal growth-spurt increments in shoulder and arm muscularity, implies a different balance from today between prepubertal hormonal influences exerted on ossification (growth hormone and somatomedin C) and the adolescent gonadal hormones of our modern growth spurt which may have still been in the process of evolution by natural selection.     

群落均匀度分形分析

修正了Frontier和Ricotta等关于有效物种丰富度指数A与物种丰富度指数S之间幂律关系的定义．探讨了A与S之间分形关系的生态学意义．认为分形维数D是群落均匀度测度值在物种数S不断增加的过程中．向其逼近的一个理论值;提出了利用双对数坐标上建立的A与S拟合直线的方程．对群落均匀度的4种变化趋势进行描述的方法。以广东黑石顶自然保护区森林演替系列为例．研究了针阔叶混交林和常绿阔叶林样带上．随着样带观察长度的逐渐增加群落均匀度的变化情况。结果表明．230m长的混交林样带只存在一个线性无标度区间．群落均匀度随样带长度的不断增加而逐渐降低．向分形维数D=0．810趋近。170m长的常绿阔叶林样带存在两个线性无标度区问．在0～25m的尺度域内．随着样带长度的逐渐增加均匀度不断降低．向分形维数D=0．525逼近;在30～170m的尺度域内．随着样带观察长度的增加．群落均匀度也逐渐增加．向分形维数D=0．920趋近。     

Investigations into cut-marks on fossil bones of Lower Pleistocene age from Venta Micena (Orce,Granada province,Spain)

Fossil bones from the Lower Pleistocene site of Venta Micena bear cut-marks in a small proportion of specimens, similar to that of bones with cut-marks at East African sites at Olduvai and East Lake Turkana. Cut-marks are distinguishable from other surface marks on bone cortex in terms of metrical characteristics, anatomical location, grouping, and microscopical characteristics, particularly those such as microstriations which may be observed with the scanning electron microscope.     

Human remains from the Austrian Gravettian: the Willendorf femoral diaphysis and mandibular symphysis

Early excavations at the Willendorf site complex in Austria yielded a femoral diaphysis collected between 1883 and 1887 and a mandibular symphysis discovered in 1908--1909. The femoral section, Willendorf 1, derives from the Willendorf I site and direct AMS (14)C dating (24,250+/-180 years B.P.) assigns it to layer 9. The Willendorf 2 mandibular piece was excavated from layer 9 of the Willendorf II site, which is AMS (14)C dated to 24,000--23,900 years B.P. The Willendorf 1 femoral piece is relatively small and exhibits a pronounced pilaster and linear aspera, moderately elevated relative cortical area, and a level of diaphyseal robusticity in the middle of the European earlier Upper Paleolithic human range of variation, assuming similar body proportions. The Willendorf 2 mandibular symphysis has an inferior lingual torus, a planum alveolare, and a mental trigone with indistinct lateral tubercles, a clear fossa mentalis and a midline basilar rounding. In these features it is close to the majority of European earlier Upper Paleolithic mandibles.     

Transition analysis: a validation study with known-age modern American skeletons

Transition Analysis-a recent skeletal age-estimation procedure (Boldsen et al.: Paleodemography: age distributions from skeletal samples (2002) 73-106)-is evaluated using 252 known-age modern American males and females from the Bass Donated Collection and Mercyhurst forensic cases. The pubic symphysis worked best for estimating age, followed by the sacroiliac joint and cranial sutures. Estimates based on all skeletal characteristics are influenced by the choice of prior distribution, although its effect is dwarfed by both the inaccuracy and imprecision of age estimates. Age intervals are narrowest for young adults, but are surprisingly short in old age as well. When using an informative prior distribution, the greatest uncertainty occurs from the late 40s into the 70s. Transition Analysis estimates do not perform as well as experience-based assessments, indicating the existing procedure is too narrowly focused on commonly used pelvic and cranial structures.     

Shanidar 10: a Middle Paleolithic immature distal lower limb from Shanidar Cave, Iraqi Kurdistan

The analysis of the faunal remains from Shanidar Cave has identified an incomplete immature human distal leg and foot from the deepest levels of the Middle Paleolithic of Shanidar Cave, Iraq. The distal tibia, fibula, first metatarsal, and two tarsals, designated Shanidar 10, derive from a 1-2-year-old infant. The tibia exhibits a transverse line from a stress episode during the last quarter of its first year postnatal. The cross-sectional geometry of the tibial midshaft reveals modest cortical thickening and a level of diaphyseal robusticity similar to those of recent human infants of a similar developmental age.     

Morphological integration in the carnivoran skull

The correlated evolution of traits may be a principal factor in morphological evolution, but it is typically studied in genetic or developmental systems. Most studies examining phenotypic trait correlations, through analysis of morphological integration, consider only few taxa, with limited ability to test hypotheses of the influence of trait integration on morphological variation and diversity. The few comparative studies in less inclusive groups have yielded varying relationships of integration to the key factors of phylogeny and diet. In this paper, I present analyses of cranial morphological integration in 30 species from the mammalian order Carnivora, spanning eight extant families and a wide range of ecological and morphological diversity. Fifty-five cranial landmarks were captured through three-dimensional digitization of 15-22 specimens for each species. Using a node-based phylogenetic distance matrix, a significant correlation was found between similarity in patterns of integration and phylogenetic relatedness within Felidae (cats) and Canidae (dogs), but not within more inclusive clades, when size-related variation was removed. When size was included, significant correlations were found across all Caniformia, Musteloidea, Mustelidae, and Felidae. There was a significant correlation between phylogeny and morphological integration only within the higher-level clade Feliformia (cats, civets, mongooses, and hyaenas) when a branch-length-based phylogenetic distance matrix was analyzed, with and without size. In contrast, diet was significantly correlated with similarity in morphological integration in arctoid carnivorans (bears, raccoons, and weasels), but had no significant relationship with integration in feliforms or canids. These results support the proposition that evolutionary history is correlated with cranial integration across large clades, although in some smaller clades diet also exerts significant influence on the correlated evolution of traits.     

红树植物木榄幼树斑块形状的分形分析

应用分形理论分析了山口国家级红树林自然保护区木榄幼树斑块形状的分形特征。木榄幼树斑块在整体水平上的分形维数为 1 .1 2 ,而单个斑块的分形维数介于 1 .1 7～ 1 .3 7之间。分形维数的大小与斑块形状的复杂程度密切相关。频谱法和周长 -面积法都适用于分析幼树斑块形状的分形特征。     

A note on the KNM-ER 999 hominid femur

The KNM-ER 999 hominid femur, in light of improved knowledge of later Pleistocene human postcranial morphology and ongoing reassessments of the emergence of modern humans in Africa, appears morphologically aligned with early modern humans rather than with late archaic humans. This is reflected especially in its having a clear pilaster, a proximally positioned minimum diaphyseal breadth (thereby lacking a proximo-medial diaphyseal buttress) and an exceptionally high neck-shaft angle. In these features, and especially the fast, it shows affinities to the Levantine Qafzeh-Skhul early modern human sample. However, the uncertainty regarding its stratigraphic provenience (early Late Pleistocene versus early Holocene) makes its relevance to the emergence of modern humans in Africa tenuous.     

Tissue origins and interactions in the mammalian skull vault.

During mammalian evolution, expansion of the cerebral hemispheres was accompanied by expansion of the frontal and parietal bones of the skull vault and deployment of the coronal (fronto-parietal) and sagittal (parietal-parietal) sutures as major growth centres. Using a transgenic mouse with a permanent neural crest cell lineage marker, Wnt1-Cre/R26R, we show that both sutures are formed at a neural crest-mesoderm interface: the frontal bones are neural crest-derived and the parietal bones mesodermal, with a tongue of neural crest between the two parietal bones. By detailed analysis of neural crest migration pathways using X-gal staining, and mesodermal tracing by DiI labelling, we show that the neural crest-mesodermal tissue juxtaposition that later forms the coronal suture is established at E9.5 as the caudal boundary of the frontonasal mesenchyme. As the cerebral hemispheres expand, they extend caudally, passing beneath the neural crest-mesodermal interface within the dermis, carrying with them a layer of neural crest cells that forms their meningeal covering. Exposure of embryos to retinoic acid at E10.0 reduces this meningeal neural crest and inhibits parietal ossification, suggesting that intramembranous ossification of this mesodermal bone requires interaction with neural crest-derived meninges, whereas ossification of the neural crest-derived frontal bone is autonomous. These observations provide new perspectives on skull evolution and on human genetic abnormalities of skull growth and ossification.     

Formation,evolution and demise of a tectonically controlled volcanic lake: A case study from the lower Pleistocene Sousaki succession

The complex interaction of local tectonics and volcanism usually produces palaeoenvironments that require to be studied in detail in order to define the role of each factor in the local palaeoenvironmental evolution. This is the case for the Sousaki Basin lying at the eastern part of the Gulf of Corinth. It presents a complex Pliocene and Pleistocene stratigraphy, affected by deformational processes due to the local tectonic regime. The Sousaki volcano is a low standing volcano that constitutes the western endpoint of the South Aegean Volcanic Arc and may also contribute to the palaeoenvironmental evolution of the basin. The studied section, in the Sousaki Basin, consists of marly and conglomeratic layers with intercalations of organic rich sediments. The base of the section consists of impermeable volcanic products. A micropalaeontological analysis based on 29 samples has been conducted in order to reconstruct the palaeoenvironment after the termination of the activity of the last volcanic period. A diversified fauna has been retrieved, consisting of Gelasian (early Pleistocene) ostracods, gastropods, diatoms, charophyte gyrogonites, thecamoebians, fish otoliths and teeth. Count-based statistical treatments performed on ostracod species revealed that a volcano-tectonic lake evolved after the emplacement of the volcanic products in the basin. Afterwards, a braided river environment dominated the landscape. Due to the lateral migration of the riverbed, several laterally evolving sub-environments were established, ranging from marginal lakes to marshes. Ultimately, the palaeoenvironmental reconstruction of the study area revealed the formation, evolution and demise of a tectonically controlled volcanic lake.