Chemical and physical methods in dating human skeletal remains

Chemical and physical methods for dating skeletal remains were examined. Benzidine reaction, ultra-violet fluorescence, specific gravity and supersonic conductivity were carried out on 71 dated skeletal findings distributed over the span of the last 3,500 years. Results given by benzidine reaction and ultra-violet fluorescence basically coincide, and positive readings were obtained up to about 200–350 years. Values measured in specific gravity and supersonic conductivity testing show a parallel trend, pointing out a clear difference between samples of the three first centuries and the ones belonging to more ancient periods examined.     

The dead-arm evolution of river systems: A comparison between the information provided by living Copepoda and Cladocera populations and by Bosminidae and Chydroidae remains

Methodological investigations, using remains of Bosminidae and Chydoridae, were undertaken to study the development of ecosystems in former river channels. Four biotopes from two former channels of different ages were used in this work. The Copepoda and Cladocera populations characterized each of the 11 sampling stations in relation to ecological factors, which are linked to the development stage in each ecosystem. Analysis of only the Bosminidae and Chydoridae populations presented practically the same information as an analysis of the total populations of Copepoda and Cladocera. The distribution of Bosminidae and Chydoridae remains taken from the surficial sediments at the deepest point of each former channel strongly resembled the distribution of the living populations sampled at several stations during one full year. Therefore, Bosminidae and Chydoridae remains could provide us with pertinent information concerning each phase of ecological succession that occurs in abandoned river channels.     

Effects of recent acidification on Cladocera in small clear-water lakes studied by means of sedimentary remains

Cladoceran populations, as revealed by sedimentary remains, were studied in six lakes which by diatom evidence have become strongly acidified during the past 30 years. The accumulation rates of cladoceran remains and in two of the most strongly acidified lakes both relative and absolute numbers ofBosmina greatly increased during this period. Species numbers were not reduced, but there were shifts in relative abundances of cladoceran species.Bosmina longispina dominated all the lakes. Low pH (4.7) seemed not to be straight-forwardly harmful toDaphnia longispina, but the relative abundances of this taxon were reduced because ofBosmina.     

Zooplankton decline in the Černé Lake (Šumava Mountains,Bohemia) as reflected in the stratification of cladoceran remains in the sediment

Stratigraphy of cladoceran remains in the upper 18 cm of a sediment core from the Lake Černé was studied. The successive disappearance of Bosmina longispina, Daphnia longispina and Ceriodaphnia quadrangula from the upper layers of the sediment corresponds with our knowledge concerning the disappearance of these species from the open water.     

Cannibalism in prehistoric Europe

The key argument for the identification of prehistoric cannibalism is provided by analysis of close similarities in the treatment of human and animal remains. Such analysis requires precise data on depositional context, meticulous excavation records, detailed bone modification studies, a relatively large sample of human and animal postcranial bones, and data on local mortuary practices. With the exception of Fontbrégoua Cave, these necessary conditions are lacking at all Stone Age European sites where it has been hypothesized that cannibalism occurred. The alternative hypothesis of secondary burial practices has been proposed informally for some sites and, in a more formal and detailed way, for Krapina and Fontbrégoua. However, this hypothesis does not have a higher probability, is not justified by current data, and uses ethnographic analogies to prop up interpretations of materials for which contextual data are missing or have been neglected. At Fontbrégoua, cannibalism remains the simplest and most plausible explanation of the evidence; at Krapina and other sites the available evidence is insufficient to prove either secondary burial or cannibalism.     

A new method for assessing the sex of fragmentary skeletal remains: femoral shaft circumference

A simple discriminant function using midshaft femoral circumference for the determination of sex has been tested with 114 skeletons from the Libben Site, Ontario County, Ohio. The results have been shown to be 85% consistent with other, accepted means of determining sex. Femur circumference an be an aid to the sexual identification of poorly preserved and fragmentary skeletal remains.     

新疆米兰遗址吐蕃时期的植物遗存

米兰遗址位于新疆塔里木盆地东南缘的若羌县,是丝绸之路新疆段南道上的重要遗址之一,延续年代可从吐蕃占领时期上溯至汉朝。遗址群内包含佛寺、屯田、灌溉水利设施、烽燧、戍堡以及城址等15处单体遗迹。2012年,新疆文物考古研究所对米兰遗址再次发掘,其中戍堡内出土了一批植物遗存,年代在距今1200年左右,包括黍、粟、青稞、小麦、桃、稗子、小獐毛和苦豆子等8种。结合植物鉴定和前人研究成果,本文认为吐蕃占领时期的米兰地区微环境较今天更为湿润,米兰戍堡的守卫者有一定的屯垦行为。除栽培谷物外,此地还有一定规模的桃树栽培。     

Detection of DNA in Ancient Skeletal Remains Using DNA Flow Cytometry

Cortical bone samples were removed from individual burials from Tomb Dk31 in the Dakhleh Oasis, Egypt. The tissue was disaggregated, stained with the DNA specific fluorescent dye DAPI and analyzed using the flow cytom-eter. DNA flow cytometry measures the cellular DNA content and this is correlated with modal chromosome content. When DNA is present in skeletal remains further investigations such as extracting, amplifying and sequencing may then be carried out. The method offers a relatively rapid and inexpensive means of pinpointing samples of skeletal DNA that can be further analyzed.     

The Life Cycle of Lestes viridis (Odonata: Lestidae) in Two Seasonal Streams of the Sierra Morena Mountains (Southern Spain)

The life cycle of the zygopteran odonate Lestes viridis in two seasonal streams in the Sierra Morena Mountains is inferred from size-frequency analyses of handnet samples of larvae and records of presence and reproductive activity of adults during three consecutive years. The egg stage (duration 5–6 months) overwinters, larval development is brief (6–8 weeks) and adults undergo a protracted, prereproductive, summer diapause (up to 3 months) before mating and ovipositing in late September, about one week after the first appreciable fall of rain, but before surface water reappears in the streams after having been absent for about four months during the hot, dry summer. Comparison between this life cycle and those of more northerly populations reveals a latitude-correlated cline in phenology resembling that found in some other northern hemisphere odonates that, like L. viridis, maintain an obligatorily univoltine life cycle at different latitudes.     

Plant tempering of Predynastic pisé at Adaïma in Upper Egypt: building material and taphonomy

Macroscopic plant remains found in pisé material (clay or mud used in building), used as lining in pits at the Upper Egyptian Predynastic site of Adaïma were investigated. Comparison with assemblages from the sediment fills of these pits and with assemblages from other contexts in the same site demonstrated the taphonomical importance of pisé as a building material for the formation of the sites archaeological sediment. In particular, the influence of the pisé plant temper on the composition of plant assemblages in the sediment fills of the pits was brought to the fore. The choice of specific plant materials for their use as temper in pisé or mud bricks is shown, in particular that of barley (Hordeum vulgare) threshing remains. The importance of cereal processing by-products as construction material is also assessed in a wider economic context and compared with later Egyptian mud brick plant contents.