Microstructural characteristics of hair of pleistocene mummy of “Bilibino horse” <Emphasis Type="Italic">Equus</Emphasis> sp.

The microstructure of hair of all mummified horses found in Northeastern Siberia has been studied for the first time in a comparative aspect by means of light optical and electron microscopy techniques. The possibility of using hair of horse mummies of different geological ages for a comparative analysis has been demonstrated. No fundamental differences were found in hair microstructure between the mummy of the “Bilibino” horse Equus sp. (geological age 58500 years) and mummified remains of the Lena horse Equus lenesis Russanov, 1968 (geological age 38 5000–29 500 years), which suggests their close relationship. It has been shown that morphological adaptations in the structure of the equine hair coat formed during the Pleistocene and Holocene under the specific climate conditions of Northeastern Siberia.     

Immunospecificity of albumin detected in 1.6 million-year-old fossils from Venta Micena in Orce,Granada, Spain

The Orce skull fragment from southern Spain, dated at 1.6 Myr, has been a subject of heated controversy since it was first discovered in 1982. If it is hominid, as its discoverers contend, it is by far the oldest fossil hominid yet found in western Europe and implies that human populations settled this region much earlier than was previously realized. Numerous stone artifacts found at the Orce sites provide evidence that hominids were indeed present there in the Lower Pleistocene. Some paleontologists maintain that the 8 cm diameter occipital fragment is from a horse, not a hominid. Two independent investigations of the residual proteins in the skull were undertaken, one at the University of Granada in Spain, the other at the University of California, San Francisco. Two immunological methods of comparable sensitivity were employed for detection and species attribution of protein extracted from fossil bone: the Granada team used an enzyme-linked-immunosorbent assay (ELISA), and the UCSF team used a radioimmunoassay (RIA). Both teams obtained reactions characteristic of human albumin in the Orce skull and horse albumin in some of the horse fossils. These results support the lithic evidence that hominids were living in Andalusia 1.6 million years ago. Am J Phys Anthropol 103:433–441, 1997. © 1997 Wiley-Liss, Inc.     

Unicorn “holotype” skeleton from the Late Pleistocene spotted hyena den site Sewecken-Berge (Germany)

Late Pleistocene Ice Age spotted hyena remains are described from the “Unicorn holotype skeleton” gypsum karst site Quedlinburg-Sewecken-Berge, Germany (Central Europe). The hyena population consists of adolescent to late adult individuals (96% of hyena NISP; 15% of megafauna NISP) indicating a commuting den site type. The comparisons to other European bone assemblages support hunting specialization on woolly rhinoceros (19% of NISP) and horses (27% of NISP). Specialization on bovids (Bison/Bos) can be added for this site. The megafauna contain few Eemian warm period remains of a large horse Equus ferus fossilis. Most (95%) of the megafauna is attributed to the Late Pleistocene glacial (Weichselian/Wuermian). Horse bones are dominated by distal leg elements from the smaller Przewalski horses Equus ferus przewalskii (26% of NISP). The Unicorn “holotype” skeleton originates from a composed horse skull, vertebrae and front legs, whereas the elephant remains added to this biologically not valid species must have been a straight-tusked elephant tusk.     

福建漳平奇和洞发现的新石器时代早期人类头骨

2011年在福建漳平奇和洞发现的距今1万年左右的新石器时代早期人类遗骸"奇和洞III号",是迄今在福建地区发现的最早、最完整的古人类头骨,为探讨华南更新世晚期向全新世过渡阶段人类的体质特征及现代人群的形成与分化提供了重要的研究材料。本文对这件头骨进行了研究,奇和洞III号为35岁左右的男性个体,牙齿龋病严重,推测当时人类的经济模式主要以农耕为主。通过与更新世晚期柳江、山顶洞101号及14组新石器时代人类头骨的比较,发现奇和洞III号头骨兼有更新世晚期人类及新石器南、北方居民的混合体质特征:奇和洞III号头骨长而脑量大,似更新世晚期人类;其高而狭窄的面部、宽阔而低矮的鼻部,呈现出不同于南、北方人群的特殊体质特征。主成分分析显示,奇和洞III号与对比的新石器时代各组在头骨的测量数据上没有表现为明显的南、北地区间差异,但在头骨的测量指数或形状上存在时代和地区间的不同。本文研究为新旧石器过渡阶段人类体质特征的变异提供了进一步证据。     

A probable case of Hand-Schueller-Christian's disease in an Egyptian mummy revealed by CT and MR investigation of a dry mummy

The challenging mission of paleopathologists is to be capable to diagnose a disease just on the basis of limited information gained by means of one or more paleodiagnostic techniques. In this study a radiologic, anthropologic and paleopathologic analysis of an ancient Egyptian mummy through X-rays, CT and MR was conducted. An Ancient Egyptian mummy ("Mistress of the house", Archeological Museum, Zagreb, Croatia) underwent digital radiography, computed tomography and magnetic resonance imaging employing 3-dimensional ultra-short-echo time (UTE) sequence, that allows to image ancient dry tissue. Morphological observations on the skull and pelvis, the stages of epiphyseal union and dental wear indicated that the remains are those of a young adult male. Multiple osseous lytic lesions were observed throughout the spine as well as on the frontal, parietal, and occipital bone, orbital wall and the sella turcica of the sphenoid. Considering the sex and age of the individual and the features of the lesions, the authors propose the diagnosis of Hand-Schueller-Christian's disease. This is the first study to have effectively used MR images in the differential diagnosis of a disease. It also confirmed the CT value in revealing central nervous system involvement just by detecting skeletal lesions. Although the mummy was previously dated to 3rd century B.C. based on the properties of the sarcophagi, the sex of the mummy suggests that it was most probably transferred into these sarcophagi in later times. The mummification techniques used and radiometric data (C14) dated it to 900-790. B.C.     

Oldest known pantherine skull and evolution of the tiger

The tiger is one of the most iconic extant animals, and its origin and evolution have been intensely debated. Fossils attributable to extant pantherine species-lineages are less than 2 MYA and the earliest tiger fossils are from the Calabrian, Lower Pleistocene. Molecular studies predict a much younger age for the divergence of modern tiger subspecies at <100 KYA, although their cranial morphology is readily distinguishable, indicating that early Pleistocene tigers would likely have differed markedly anatomically from extant tigers. Such inferences are hampered by the fact that well-known fossil tiger material is middle to late Pleistocene in age. Here we describe a new species of pantherine cat from Longdan, Gansu Province, China, Panthera zdanskyi sp. nov. With an estimated age of 2.55-2.16 MYA it represents the oldest complete skull of a pantherine cat hitherto found. Although smaller, it appears morphologically to be surprisingly similar to modern tigers considering its age. Morphological, morphometric, and cladistic analyses are congruent in confirming its very close affinity to the tiger, and it may be regarded as the most primitive species of the tiger lineage, demonstrating the first unequivocal presence of a modern pantherine species-lineage in the basal stage of the Pleistocene (Gelasian; traditionally considered to be Late Pliocene). This find supports a north-central Chinese origin of the tiger lineage, and demonstrates that various parts of the cranium, mandible, and dentition evolved at different rates. An increase in size and a reduction in the relative size of parts of the dentition appear to have been prominent features of tiger evolution, whereas the distinctive cranial morphology of modern tigers was established very early in their evolutionary history. The evolutionary trend of increasing size in the tiger lineage is likely coupled to the evolution of its primary prey species.     

Review of the genus Hippidion Owen, 1869 (Mammalia: Perissodactyla) from the Pleistocene of South America

This review of Hippidion is based on a multivariate analysis of the foot, and some morphological characteristics of the skull and dentition. We recognize only one genus ( Hippidion ) including all the hippidiform horses, with three different species: H. principale, H. devillei and H. saldiasi. The latter species is stratigraphically and geographically restricted to the period from 13000 to 8000 years BP in the southern part of South America. Hippidion principale and H. devillei have a large geographical distribution (Argentina, Bolivia, Chile, Perú, Uruguay, Brazil) through the Upper Pliocene-Upper Pleistocene. Both species show some morphometric variations across their geographic range; these features may result from the environmental characteristics.     

A new hominid parietal from Bodo, Middle Awash Valley, Ethiopia

A piece of left parietal of a Middle Pleistocene hominid, recovered from the Upper Bodo Sand Unit, in the Middle Awash, Ethiopia, is described anatomically and compared to Middle Pleistocene hominids and modern Homo sapiens. It bears several primitive features and has important implications for the original Bodo skull, found at the same stratigraphic level in the same area. The new fossil skull represents a different individual from the original Bodo skull.     

Endocranial capacity of the bodo cranium determined from three-dimensional computed tomography

The 600,000-year-old cranium from Bodo, Ethiopia, is the oldest and most complete early Middle Pleistocene hominid skull from Africa. "Virtual endocast" models created by three-dimensional computed tomography (CT) techniques indicate an endocranial capacity of about 1,250 cc for this cranium (with a reasonable range between approximately 1,200-1,325 cc, depending on how missing portions of the basicranial region are reconstructed). From these determinations, several important implications emerge concerning current interpretations of "tempo and mode" in early hominid brain evolution: 1) already by the early Middle Pleistocene, at least one African hominid species, Homo heidelbergensis, had reached an endocranial capacity within the normal range of modern humans; 2) in spite of its large endocranial capacity, estimates of Bodo's encephalization quotient fall below those found in a large sample of Homo sapiens (both fossil and recent) and Neandertals; and 3) the greatest burst of brain expansion in the Homo lineage may not have been in the last several hundred thousand years, but rather much earlier in the Lower to early Middle Pleistocene.     

A comparative study of ancient sedimentary DNA, pollen and macrofossils from permafrost sediments of northern Siberia reveals long-term vegetational stability

Although ancient DNA from sediments (sedaDNA) has been used to investigate past ecosystems, the approach has never been directly compared with the traditional methods of pollen and macrofossil analysis. We conducted a comparative survey of 18 ancient permafrost samples spanning the Late Pleistocene (46-12.5 thousand years ago), from the Taymyr Peninsula in northern Siberia. The results show that pollen, macrofossils and sedaDNA are complementary rather than overlapping and, in combination, reveal more detailed information on plant palaeocommunities than can be achieved by each individual approach. SedaDNA and macrofossils share greater overlap in plant identifications than with pollen, suggesting that sedaDNA is local in origin. These two proxies also permit identification to lower taxonomic levels than pollen, enabling investigation into temporal changes in species composition and the determination of indicator species to describe environmental changes. Combining data from all three proxies reveals an area continually dominated by a mosaic vegetation of tundra-steppe, pioneer and wet-indicator plants. Such vegetational stability is unexpected, given the severe climate changes taking place in the Northern Hemisphere during this time, with changes in average annual temperatures of >22 °C. This may explain the abundance of ice-age mammals such as horse and bison in Taymyr Peninsula during the Pleistocene and why it acted as a refugium for the last mainland woolly mammoth. Our finding reveals the benefits of combining sedaDNA, pollen and macrofossil for palaeovegetational reconstruction and adds to the increasing evidence suggesting large areas of the Northern Hemisphere remained ecologically stable during the Late Pleistocene.     

<Emphasis Type="Italic">Equus (Hemionus) nalaikhaensis</Emphasis> from the Pleistocene of Mongolia,the earliest kulan of Central Asia

The type series of the earliest kulan Equus (Hemionus) nalaikhaensis Kuznetsova et Zhegallo, 1996 from the Pleistocene of Mongolia is described in detail. The lectotype (an almost complete skull without a lower jaw) is designated. The assignment of this species to the subgenus Hemionus is validated.     

Forest Bed elks and giant deer revisited

Cervids of the Forest Bed Formation were studied by the present author in a paper now 40 years old. Some identifications and generic attributions are here revised. The fossils fall into one, or possibly two, distinct levels of the late Villefranchian (Early Pleistocene) and in the earlier Middle Pleistocene (Galerian, =Cromerian). In the earlier paper four elk species were recognized; these are now reduced to two: Cewalces gallicus , from the younger Late Villefranchian, and Cewalces latifrons , from the Galerian. A skull from Mundesley is proposed as the neotype of the latter, to replace a poorly diagnostic original holotype. These species are not closely related to the living Alces alces but are forerunners of the North American Cewalces scotti. The phylogeny of Pleistocene elks is discussed in this context. Giant deer are represented by two genera, with three species: Megaceroides verticomis, Megaceroides dawkinsi and Megaloceros savini. Some fossils misinterpreted in the former paper are revised. Megaceroides dawkinsi seems to be endemic to Great Britain, raising an intriguing problem of palaeogeography.     

New analysis of the Pleistocene carnivores from Petralona Cave (Macedonia, Greece) based on the Collection of the Thessaloniki Aristotle University

New taxonomic study of the “old collection” of Carnivora from Petralona Cave, associated to the well-known hominid skull, housed in the Geology School of the Thessaloniki Aristotle University since 1960, revealed 11 species (Canis arnensis, Lycaon lycaonoides, Vulpes praeglacialis, Ursus deningeri, U. spelaeus, U. arctos, Pliocrocuta perrieri, Pachycrocuta brevirostris, Crocuta crocuta, Panthera leo spelaea, and Felis silvestris), which are described in detail. The species composition is typical of the eastern part of the European Mediterranean and may be divided into three biostratigraphic assemblages: early Middle Pleistocene, late Middle Pleistocene and Late Pleistocene.     

A NEW SPECIES OF DICERORHINUS (RHINOCEROTIDAE) FROM THE PLIO‐PLEISTOCENE OF MYANMAR

Abstract: A skull and mandible of the new species Dicerorhinus gwebinensis sp. nov. of Rhinocerotidae (Mammalia, Perissodactyla) is described. The material is collected from the upper part of the Irrawaddy sediments (Plio‐Pleistocene) in central Myanmar. D. gwebinensis sp. nov. is morphologically more similar to the extant species D. sumatrensis (Sumatran rhinoceros) than to other species of the genus but differs from D. sumatrensis in having the comparatively shorter nasal, the more concave dorsal profile of the skull, the more elevated occiput and presence of molar crista in M3/. This is the first discovery of Dicerorhinus in the upper Miocene to lower Pleistocene of the Indian subcontinent and Mainland Southeast Asia, and fills the chronological and geographical gap of this lineage in Asia. The Dicerorhinus clade probably migrated into Southeast Asia from East Asia by the Pliocene or early Pleistocene. This hypothesis is supported by the scarcity or absence of this clade in the Neogene mammalian fauna of the Indian Subcontinent.     

The response of aphid secondary parasitoids to different patch densities of their host

Aphids are attacked by a large guild of natural enemies including many primary parasitoids which mummify their hosts. These mummies are themselves attacked by a guild of mummy parasitoids which are potentially important in regulating primary parasitoids at densities below which they can exert biological control. The response of mummy parasitoids to mummy densities was investigated in an experiment in which mummy densities of the pea aphid (Acyrthosiphon pisum) attacked by the parasitoid Aphidius ervi were manipulated across host plant patches. Overall, the risk of parasitism was density independent, though with very high inter-patch variability which may allow probabilistic refuges from secondary parasitism. Six species of four genera of mummy parasitoids were recorded. Of the responses of the individual genera, Coruna were reared most frequently from patches of high host density while amongst patches from which Syrphophagus was reared parasitism was inversely density dependent.     

Hemiptelea mikii sp. nov. (Ulmaceae), fossil fruits and woods from the pleistocene of central Japan

A new fossil species,Hemiptelea mikii, is described on the basis of fruits from the Pleistocene of central Japan. It is distinguished fromH. davidii, the only extant species of the genus restricted to Korea and China, in having shorter fruits. Fossil woods discovered from the same horizon differ from the extant one in some anatomical characteristics, and are assigned to the new fossil species. Taken together with earlier records of fossil fruit occurrence in the early and the middle Pleistocene of central Japan, the latest finding of fossil fruits and woods from the last glacial sediments (ca. 50,000 years ago) at Kita-egota site of Tokyo suggests thatH. mikii was widespread in central Japan throughout the Pleistocene and survived until as late as the Last Glacial age.     

On a skull of a fossil macaque from the shikimizu limestone quarry in the Shikoku district,Japan

An almost complete calvaria of an adult macaque was found among remain from the Shikimizu limestone quarry at Hijikawa-cho, Kita-gun, Ehime Pref., Shikoku, Japan. Its exact age is unknown, but probably Pleistocene because mammalian bones from this quarry include not only recent but some Pleistocene elements. The Shikimizu skull has a somewhat different feature as compared with the skull of livingMacaca fuscata, mainly in that its facial region is much broader. In this feature, the Shikimizu skull seems to somewhat resembleMacaca robustus from China, suggesting that the older the lineage offuscata is traced back in the Pleistocene, the more its ancestral type would becomerobustus-like in the morphology.     

Megafaunal extinctions and the disappearance of a specialized wolf ecomorph

The gray wolf (Canis lupus) is one of the few large predators to survive the Late Pleistocene megafaunal extinctions [1]. Nevertheless, wolves disappeared from northern North America in the Late Pleistocene, suggesting they were affected by factors that eliminated other species. Using skeletal material collected from Pleistocene permafrost deposits of eastern Beringia, we present a comprehensive analysis of an extinct vertebrate by exploring genetic (mtDNA), morphologic, and isotopic (delta(13)C, delta(15)N) data to reveal the evolutionary relationships, as well as diet and feeding behavior, of ancient wolves. Remarkably, the Late Pleistocene wolves are genetically unique and morphologically distinct. None of the 16 mtDNA haplotypes recovered from a sample of 20 Pleistocene eastern-Beringian wolves was shared with any modern wolf, and instead they appear most closely related to Late Pleistocene wolves of Eurasia. Moreover, skull shape, tooth wear, and isotopic data suggest that eastern-Beringian wolves were specialized hunters and scavengers of extinct megafauna. Thus, a previously unrecognized, uniquely adapted, and genetically distinct wolf ecomorph suffered extinction in the Late Pleistocene, along with other megafauna. Consequently, the survival of the species in North America depended on the presence of more generalized forms elsewhere.     

American Association of Physical Anthropologists. Abstracts of papers to be presented at the Forty-Ninth Annual Meeting,April 17–19, 1980, Niagara Falls,New York

An interdisciplinary team performed autopsies on an adult male and an infant male mummy from the American Southwest. Cause of death has not been determined for the infant. The presence of an unhealed skull fracture associated with an apparent hematoma in the adult male is suggestive of trauma as the cause of death in the adult. Evidence of disease is minimal. Analysis of powder thought to be dried blood from the thoracic cavity of the adult suggests the presence of human IgG. The instability of this protein may indicate the presence of proteolytic activity by enzymes that degrade immunoglobulins upon rehydration. The possibility of enzymatic degradation of proteins will be an important factor in future studies of such immunoglobulins in mummy remains and also indicates the importance of maintaining the desiccated condition of mummy tissues.