Comparative Skeletal Pathology and the Case for Conspecific Care in Middle Pleistocene Hominids

Lebel et al. (2001, Proc Natl Acad Sci98, 11097) claim that the pathological alterations to the Aubesier 11 partial mandible demonstrate that Middle Pleistocene hominid populations, “had achieved a level of sociocultural elaboration sufficient to maintain debilitated individuals and to provide the motivation to do so”. This hypothesis is tested here by comparing the pathological processes seen in the Aubesier 11 hominid specimen with those evident in wild non-human primate skeletal material. A variety of wild non-human primates have similar pathological processes of equal or greater severity than that seen in Aubesier 11. There is also no evidence of any condition in Aubesier 11 which would have prevented that individual from providing for himself/herself. Therefore the Aubesier 11 partial mandible cannot be taken as evidence for an increased level of conspecific care in Middle Pleistocene hominids, contra Lebel et al. (2001). This illustrates the importance of a comparative approach to palaeopathology.     

Middle Pleistocene bird consumption at Level XI of Bolomor Cave (Valencia, Spain)

The consumption of small prey dates back to the Plio-Pleistocene chronologies in some African sites. However, the systematic acquisition and consumption of small prey in the pre-Upper Palaeolithic times is still a highly debated topic in Europe. Although the utilization of leporids has been recorded in several pre-Late Pleistocene European sites, the evidence of bird consumption is not as common for these periods. Nevertheless, Level XI (MIS 6) of Bolomor Cave has clear diagnostic elements to document the acquisition and use of birds (Aythya sp.) for food in the form of: (1) cutmarks on bones of both the front and hind limb; (2) presence of burning patterns on the extremities of the bones (areas of the skeleton with less meat); and (3) human toothmarks on limb bones. The capture of birds is classified as quick-flying game in the archaeological sites. The acquiring of fast-running (mostly lagomorphs) and quick-flying small prey requires a sophisticated technology and involves obtaining and processing ways different from those used for large- and medium-sized animals. From this perspective, the aim of this paper is to examine possible patterns in the processing sequence of birds from Level XI of Bolomor Cave and to improve the data on their butchery and human consumption in the Middle Pleistocene of Iberian Peninsula.     

The first record of Galea Meyen, 1832 (Rodentia,Hystricognathi, Caviidae) in the late Pleistocene of southern Brazil and its palaeobiogeographic implications

The first caviine rodent referable to Galea Meyen, 1832 is described from the late Pleistocene of southern Brazil based on a left dentary with the p4–m3 series. The specimen derives from the Ponte Velha I locality in the Touro Passo Creek (Touro Passo Formation, upper Pleistocene), western Rio Grande do Sul State. The main characters used to assign this specimen to Galea are: anterior area of horizontal crest at the level of prism I of p4; deep anterior area of masseteric fossa; incisor alveolus on the medial face of the dentary extended up to the level of prism II of m2; and presence of cement in the hypoflexid. Currently, the genus has a disjunct distribution, with a group in Argentina, Bolivia and Peru, and another in northern and northeastern Brazil. The presence of this taxon in Pleistocene deposits of Rio Grande do Sul State, Uruguay and the Argentine Mesopotamian, where there are no extant representatives of the genus, indicates its wider distribution during the late Pleistocene.     

Tertiary gymnosperms from Tasmania: Araucariaceae

Three new species of the Araucariaceae are described from leaf remains, Araucaria readiae from the Early Eocene Regatta Point flora, A. hastiensis from the Middle-Late Eocene Hasties flora, and Agathis tasmanica from the Early Oligocene-Early Miocene Little Rapid River flora. Additionally, emended diagnoses are presented for Araucarioides linearis and A. annulata. A. readiae is the first organically preserved species in the section Eutacta described from Tasmania, A. hastiensis is the first record of a species not in section Eutacta in Tasmania, and A. tasmanica is the first record of Agathis in Tasmania. These species, along with other records from south-eastern Australia indicate the presence of a high diversity of araucarian species in the region in the Early-Middle Tertiary, although no species survive there today. Climatic change and competition from angiosperms may have led to their demise in that region.     

Dry-bone manifestations of rickets in infancy and early childhood

Rickets and osteomalacia are the subadult and adult expressions of a disease in which the underlying problem is a failure to mineralize bone protein (osteoid). The most common cause of this disease is a physiological deficiency in vitamin D. The associated problems include deformed bones and this condition is well known in pre-modern medical texts and documents as a fairly common cause of morbidity. Given these facts, it is surprising that the literature on palaeopathology provides very little evidence of this disease in archaeological human skeletal samples. The medieval sample (N=687) of human remains from Wharram Percy, North Yorkshire, England contains a remarkable subsample of eight burials in which a spectrum of pathological features is expressed. The subsample includes infants ranging in age from 3 to 18 months at the time of death. Ten abnormal bone features were identified in the subsample, including: (i) cranial vault porosity; (ii) orbital roof porosity; (iii) deformation of the mandibular ramus; (iv) deformation of arm bones; (v) deformation of leg bones; (vi) flared costo-chondral ends of ribs; (vii) irregular and porous cortex of the costo-chondral ends of the ribs; (viii) abnormality of the growth plates of long bones; (ix) irregular and porous surfaces of the metaphyseal cortex; (x) thickening of the long bones, particularly in the metaphyseal areas. Not all of these features were found in all of the cases. Nevertheless, the overall pattern of skeletal abnormality fits well with the anatomical and radiological conditions associated with rickets. © 1998 John Wiley & Sons, Ltd.     

Bennett’s wallaby (Macropus rufogriseus) marrow quality vs quantity: evaluating human decision-making and seasonal occupation in late Pleistocene Tasmania

A pilot study on the fatty acid composition of the bone marrow, brain tissue and muscle (flesh) of the medium-sized marsupial the Bennett’s wallaby (Macropus rufogriseus), aimed to explore the mechanisms behind the dominance of this human prey species in late Pleistocene southwest Tasmania. In particular it was designed to investigate why humans frequently selected and transported the wallaby hindquarters, breaking open their longbones and metatarsals to expose the marrow cavity, when these animals could easily have been transported whole. Initial results indicated that the percentage of unsaturated fatty acids particularly palmitoleic acid (C_16:1) and oleic acid (C_18:1) in the bone marrow increased distally away from the body core temperature or the heart, towards the hands and feet. There is a corresponding decrease in the percentage of the saturated fatty acids, particularly palmitic acid (C_16:0) and stearic acid (C_18:0). This is similar to the pattern identified in placental artiodactyls (even-toed ungulates) and rodents. The preliminary study was then expanded to a year-long seasonal experiment involving wallabies from different Tasmanian environmental and climatic zones to see if this can better help explain the apparent seasonal occupation of caves indicated from recent Bennett’s wallaby teeth annuli (Skeletochronological studies). It was found that the Bennett’s wallaby remained a relatively stable and dependable resource throughout the year, with environmental, altitudinal and seasonal variability having only a minor effect on the fatty acid composition or nutritional quality of their bone marrow, muscle and brain tissue. Interestingly, the animals had increased desirable unsaturated fatty acids in their marrow, muscle and brain during the winter and spring with decreased amounts during the summer and autumn. This lends support to an earlier Kidney Fat Index (KFI) analysis for the Bennett’s wallaby which recorded significant seasonal differences within and between regions, indicating an environmental effect on overall body condition. Fatty acid analysis of the Common wombat Vombatus ursinus, the Tasmanian pademelon Thylogale billardierii, and the Forester or Eastern Grey kangaroo Macropus giganteus were also included to ascertain why these animals remained constant, although minor, prey species throughout the late Pleistocene. While the results from these animals were similar to the Bennett’s wallaby, there were some unexpected and surprising patterns that require further investigation. All of these fatty acid analyses have important implications for understanding human decision-making and occupation of southwest Tasmania during the Last Glacial Maximum, for modern dietary and palaeodietary benefits, and for understanding the physiology of these unique Australian marsupials.     

The limits of biomolecular palaeopathology: ancient DNA cannot be used to study venereal syphilis

To determine whether ancient DNA (aDNA) can be used to study the palaeopathology of venereal syphilis, we carried out a comprehensive analysis of the preservation of human and pathogen DNA in a set of 46 bones of various ages, most of which displayed osteological indications of the disease. Bones came from seven English cemetery sites that were in use during the 9th–19th centuries. Twelve of the 46 bones consistently yielded mitochondrial DNA (mtDNA) sequences after replicate polymerase chain reactions (PCRs), and a further 13 bones yielded mtDNA sequences with less reproducibility. The sequence data enabled tentative mitochondrial haplogroups to be assigned to nine of the bones, and the identities and frequencies of these haplogroups were compatible with the geographical origins of the bones. Twenty-one bones consistently gave negative results with all mtDNA PCRs, indicating that at least these bones were not contaminated with modern human DNA, and those bones that gave positive results only yielded one sequence each, again suggesting that widespread modern contamination had not occurred. Mycobacterium tuberculosis sequences were obtained from seven bones, including three of five bones with tuberculous lesions. The cloned and direct sequences obtained from both the mtDNA and M. tuberculosis PCR products showed features typical of degraded aDNA. All of these results suggest that at least some of the 46 bones that we studied were suitable for aDNA analysis. All 46 bones were tested with nine different treponemal PCRs, each optimised to give a detection limit of ≤5 genomes. Although various bones gave PCR products of the expected size with one or more of these PCRs, sequencing showed that none of these products were authentic treponemal amplicons. Our failure to detect treponemal DNA in bones that were suitable for aDNA analysis, using highly sensitive PCRs, suggests that treponemal DNA is not preserved in human bone and that it is therefore not possible to use aDNA analysis to study venereal syphilis. Any past or future paper claiming detection of treponemal aDNA should therefore be accompanied by a detailed justification of the results.     

The Temperature Response in the Ring Widths of Phyllocladus Aspleniifolius (Celery–top Pine) Along an Altitudinal Gradient in the Warra LTER Area,Tasmania

The temperature response of four Phyllocladus aspleniifolius (Celery–top Pine) sites along an altitudinal gradient within a cool temperate broad leaf forest environment in the southwest of Tasmania, Australia was examined. Although strong evidence of a systematically changing response with elevation could not be found, there was evidence that minimum temperature in particular may be important in determining the altitudinal extent of the species. Climatic responses of the Warra LTER (Long Term Ecological Research) area sites were representative of other known sites in southwestern Tasmania. A link between event years in P. aspleniifolius and warm/dry conditions indicates that these event years may provide a guide to the historical frequency of fire weather in Tasmania’s southwest.     

Acaste (Trilobita: Phacopina) from the Early Devonian of Tasmania

Edgecombe, G.D. March 2007. Acaste (Trilobita: Phacopina) from the Early Devonian of Tasmania. Alcheringa 31, 59-66. ISSN 0311-5518.

The widespread Siluro-Devonian acastid trilobites Acaste and Acastella are known from few occurrences in Australasia, these being confined to Lochkovian strata in Victoria and New Zealand. A new species, Acaste andersoni, is described from a correlative of the Bell Shale near St Valentines Peak in north-western Tasmania. Acaste supplements the biogeographic links between the Early Devonian faunas of New Zealand, Victoria and Tasmania.

Gregory D. Edgecombe [greged@austmus.gov.au], Australian Museum, 6 College Street, Sydney, NSW 2010, Australia; received 2.3.2005, revised 6.4.2005.     

Akhalkalaki: The Taphonomy of An Early Pleistocene Locality in the Republic of Georgia

As part of our investigations into the potential of the Republic of Georgia for providing information on early hominin occupation of Eurasia, we report here on Akhalkalaki, a large late Early Pleistocene locality located along the lower slopes of a Miocene andesitic cone. Originally excavated in the 1950s as a palaeontological site, it was re-opened in the 1990s and stone tools were found associated with the fauna, suggesting that it is also an archaeological occurrence. Excavations in the 1950s and 1990s uncovered thousands of bones of an early Galerian fauna, including the remains of new species of Hippopotamus,Equus , and Canis (Vekua, 1962, 1987) and dominated by the remains of Equus süssenbornensis. We present the stratigraphy of the site, which together with faunal correlations and reversed paleomagnetics indicates an age most likely in the late Matuyama Chron, probably between 980,000 and 780,000 years ago. Taphonomic analysis suggests that the fauna was deposited and buried over a short time period, and was heavily modified by carnivores, but we cannot demonstrate involvement by hominins. Based on evidence of abundant krotovina (animal burrows filled with sediment) and the lack of definitive evidence for hominin modification to the bones, the stone tools at the site may have been mixed in with the older fauna. The taphonomic characteristics of the Akhalkalaki bone assemblage are not readily explained with reference to assemblage formation processes developed with actualistic studies that have been mostly conducted in Africa, including carnivore dens, predator arenas, human hunting and scavenging, mass deaths, or attritional bone deposition. Because of extreme anthropogenic modification of the present environments, the temperate setting, and the presence of mainly extinct taxa, local models based on actualistic studies cannot approximate the mammalian ecology reflected in the Akhalkalaki bone assemblage. A few comparisons are made with preliminary taphonomic observations from Dmanisi, an Early Pleistocene Homo ergaster site not far away.     

Human consumption of tortoises at Level IV of Bolomor Cave (Valencia, Spain)

The acquisition and consumption of small prey in the pre-Upper Palaeolithic is a highly debated topic at present. For some authors, the systematic obtaining of these animals is only part of the subsistence strategies used by anatomically modern Humans. However, the consumption of small prey dates back to the Plio-Pleistocene chronologies in some sites. Although the utilization of leporids has been recorded in several pre-Late Pleistocene European sites, the evidence of tortoise consumption is documented not as common for these periods. However, Level IV of Bolomor Cave has clear diagnostic elements to document the acquisition and use of tortoises (Testudo hermanni) for food in the form of: (1) cutmarks on limb bones and ventral surface of the carapace and plastron; (2) presence of burning on tortoise skeleton and shell; (3) elements of anthropogenic breakage on carapace and plastron: percussion pits, percussion notches and impact flakes; and (4) human toothmarks on limb bones. This paper tries to examine the possible patterns in the tortoise consumption sequence from Level IV of Bolomor Cave and improves data on the butchery process and tortoise consumption in the Late Middle Pleistocene.     

Sexual dimorphism in limb bones of ibex (Capra ibex L.): mixture analysis applied to modern and fossil data

Estimating sex ratios of fossil bone assemblages is an important step in the determination of demographic profiles, which are essential for understanding the palaeobiology and palaeoethology of any particular species, as well as its exploitation patterns by humans. This is especially true for ibex (Capra ibex), which was a main source of food for hominids during Pleistocene times. Classical methods for determining sexual dimorphism and sex ratio, such as analyses using uni‐ and bivariate plots, are based on an arbitrary fixing of limits between sexes. Here we use a more robust statistical method termed mixture analysis (MA) to determine the sex of postcranial remains (long bones, metapodials and tarsals) from ibex. For the first time, we apply MA to both a modern and a fossil sample of one species, by using metric data taken from (i) a collection of present‐day ibex skeletons and (ii) a Palaeolithic sample of the same species. Our results clearly show that the forelimb (humerus and radius) is more dimorphic than the hindlimb (femur and tibia) and is therefore better suited for sexing ibex. It also appears that metapodials should be used carefully for estimating sex ratios. On the basis of these results, we propose a classification of bone measurements that are more or less reliable for sexing ibex. The results of MA applied to the ibex fossil bones from the Upper Palaeolithic site of the Observatoire (Monaco) lead us to the conclusion that this assemblage consists of a majority of males. The quantitative estimations calculated by the MA make it possible to compare the size of Pleistocene and modern ibex for the whole set of variables used in this study. Copyright © 2006 John Wiley & Sons, Ltd.     

Camelus from the upper pleistocene of Mount Carmel,Israel

A Camelus metapodial, found among the animal bones excavated by Garrod from the Levalloiso-Mousterian of the Tabun Cave (Mount Carmel, Israel), adds to the relatively small number of Camelus finds reported from the Pleistocene of the Near East. The mammal faunas associated with these finds suggest relatively dry open conditions, but not desert conditions. The Tabun specimen is of moderate size, in contrast to the very large Camelus from Far'ah II; two species of camel may thus have been present in the Near East during the Upper Pleistocene.     

First fossil pollen record of Auriculiidites Elsik, 1964 in Australia

Macphail, M.K. & Partridge, A.D., June 2012. First fossil pollen record of Auriculiidites Elsik, 1964 Elsik, W. C. 1964. A new sporomorph genus from eastern Peru. Pollen et Spores, 6: 601–604.  [Google Scholar] in Australia. Alcheringa 36, 283–286. ISSN 0311-5518.

Fossil auriculate pollen assigned to Auriculiidites Elsik is preserved in middle early Eocene estuarine facies near Strahan, on the west coast of Tasmania. This is the first record of this otherwise Late Cretaceous–Paleocene morphogenus in Australia and possibly the Southern Hemisphere. Auriculiidites is one of several, now tropical, taxa found at Strahan and underscores the area's importance in understanding the impact of early Eocene global warming at high latitudes.

Mike Macphail [mike.macphail@anu.edu.au], Department of Archaeology & Natural History, College of Asia and the Pacific, Australian National University, ACT 0200, Australia; Alan D. Partridge, Biostrata Pty. Ltd. 302 Waiora Rd., Macleod, Victoria 3085, Australia. Received 28.8.2011, revised 5.2.2012, accepted 16.2.2012.     

First record of Procariama simplex Rovereto, 1914 (Phorusrhacidae,Psilopterinae) in the Cerro Azul Formation (upper Miocene) of La Pampa Province; remarks on its anatomy,palaeogeography and chronological range

Vezzosi, R.I., June 2012. First record of Procariama simplex Rovereto, 1914 (Phorusrhacidae, Psilopterinae) in the Cerro Azul Formation (upper Miocene) of La Pampa Province; remarks on its anatomy, palaeogeography and chronological range. Alcheringa, 157–169. ISSN 0311-5518.

New records of Procariama simplex in central and northwestern Argentina are reported. The fossil material includes mandibular bones, cervical vertebrae and several elements of the fore and hindlimbs. After an exhaustive comparison of anatomical characters and morphometric analysis, the fossil specimens are assigned to the psilopterine Procariama simplex. The specimen from La Pampa Province represents the first record of a psilopterine in this central region of Argentina and derives from upper Miocene sediments of the Cerro Azul Formation. Lithological features and biostratigraphical data allow the host bed to be assigned to the Huayquerian faunal stage (late Miocene). The La Pampa record broadens the geographical distribution of Procariama simplex, which was previously restricted to northwestern Argentina.

Raúl Ignacio Vezzosi [vezzosiraul@gmail.com], Centro de Investigaciones Científicas y Transferencia de Tecnología a la Producción CICYTTP-CONICET, Materi y España s/n (3105), Diamante, Entre Ríos, Argentina. Received 1.4.2011, revised 28.5.2011, accepted 14.6.2011.     

The hunted hunter: the capture of a lion (Panthera leo fossilis) at the Gran Dolina site,Sierra de Atapuerca,Spain

Many Pleistocene caves and rock shelters contain evidence of carnivore and human activities. For this reason, it is common to recover at these sites faunal remains left by both biological agents. In order to explain the role that carnivores play at the archaeological sites it is necessary to analyse several elements, such as the taxonomical and skeletal representation, the age profiles, the ratio of NISP to MNI, the anthropogenic processing marks on the carcasses (location and purpose of cutmarks and burning and bone breakage patterns), carnivore damage (digested bones, location and frequencies of toothmarks and bone breakage), length of the long bones, frequencies of coprolites and vertical distribution of the faunal remains, inter alia. From this, the documentation of carnivores in a faunal assemblage with a clear anthropogenic component can be understood from three main phenomena: (1) the carnivores as accumulators and the use of the site as a den; (2) carnivores as scavengers of hominid refuse and; (3) carnivores as hominids’ prey. Of these three phenomena, the last one is the least documented at the Middle Pleistocene sites. From this perspective, here we present the case of the anthropogenic use of a lion (Panthera leo fossilis) from level TD10-1 of Gran Dolina (MIS 9, Sierra de Atapuerca, Burgos, Spain). The lion bone remains show signs of direct interaction between this big cat and human groups that occupied Gran Dolina in these chronologies. From this perspective, the aim of this paper is to contribute to the knowledge of the role developed by large carnivores in the anthropogenic contexts and to provide data on human use of these predators at the European Middle Pleistocene sites.     

Presence of the African Saber-toothed FelidMegantereon whitei(Broom, 1937) (Mammalia, Carnivora, Machairodontinae) in Apollonia-1 (Mygdonia Basin, Macedonia, Greece)

We have made a multivariate morphometric study of the fossils ofMegantereonfrom the Apollonia-1 site at the Mygdonia Basin (Macedonia, Greece), using discriminant functions. Results obtained indicate that these specimens belong to the African speciesMegantereon whiteiBroom, which is also found in the Lower Pleistocene of Dmanisi (East Georgia, Caucasus) and Orce (Southern Spain). Morphofunctional studies ofM. whiteisuggest that this saber-toothed felid was an ambush predator with great killing capability in relation to its food requirements, thus leaving enough meat to be scavenged by both hyaenas and hominids.M. whiteimay have played an important ecological role making the first dispersal ofHomoto Eurasia the Lower Pleistocene possible.     

Cut marks on the Middle Pleistocene elephant carcass of Áridos 2 (Madrid,Spain)

Áridos 1 and Áridos 2 (Madrid, Spain) are two Middle Pleistocene sites belonging to the isotopic stages 9–11. Both places contain partial carcasses of Elephas (Paleoxodon) antiquus associated to Acheulian stone tools. In this work, the taphonomic study of the elephant remains of Áridos 2 is presented. This study has documented several cut marks on different bones, which indicate bulk flesh and viscerae extraction by Middle Pleistocene hominins. Several arguments are provided to support that at least some of the cut marks were made with handaxes, further suggesting that some of these artifacts were butchering tools in this stage of human evolution. Although cut marks on elephant carcasses have been documented at some Middle Pleistocene sites, very few have been published in detail to allow consideration of their status as hominin-imparted marks. By doing so, the present study provides more evidence of large carcass exploitation by hominins during this period.     

The Middle Pleistocene argali (Ovis ammon antiqua) assemblages at the Caune de l'Arago (Tautavel,Pyrénées‐Orientales,France): were prehistoric hunters or carnivores responsible for their accumulation?

The argali (Ovis ammon antiqua) assemblages from the Middle Pleistocene site of the Caune de l'Arago (Tautavel, southern France) were studied in terms of zooarchaeology and taphonomy. It is possible to discern palaeobiological information lost during fossilisation, as well as the palaeoethology of the bone collector, by the observation of taphonomic details preserved on the bone assemblages. The observations leave no doubt that both humans and carnivores were involved in the accumulation of argali carcasses in the cave. In some assemblages, the type of bones found in articulation and the gnawing marks observed are characteristic of carnivores. In other levels, the intense fracturing of the major limb bones in relation to their marrow content and mineral density, and butchering marks found on specimens in the earlier levels, are in favour of human accumulation, the modalities of which are discussed. The results suggest that the degree of carnivore activity seems to have been higher in levels M, N and O than in level F. Copyright © 2006 John Wiley & Sons, Ltd.     

Two new camerate crinoid species from the Permian of eastern Australia

The habitat and habit of Australia's first recorded Tertiary marsupial species, Wynyardia bassiana, found some 130 years ago at Wynyard on the northwestern coast of Tasmania, remain enigmatic (Aplin 1987, Aplin &; Rich 1990). Fossil pollen and spores preserved in a rafted clast of estuarine silts from the same sequence of earliest Miocene marine sandstones as the skeletal remains indicate the local vegetation was Nothofagus-gymnosperm evergreen rainforest, probably with a cryptogam-rich rather than woody subcanopy stratum. Comparisons with present-day Nothofagus rainforests suggest that, although the subcanopy would have been sufficiently open to allow the passage of a large ground-dwelling herbivorous marsupial, limited food resources are more consistent with Wynyardia being a generalist arboreal herbivore.