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Neolithic woodland management and land-use in south-eastern Europe: The anthracological evidence from Northern Greece and Bulgaria
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Wood charcoal (anthracological) remains accumulated in archaeological deposits provide a valuable tool for reconstruction of past local vegetation and its use. They can offer evidence complementary to pollen analysis or be the main source on past vegetation change in areas where no pollen preservation is available. The current study assembles the anthracological evidence from 18 Neolithic sites situated in the zone spanning between the Lower Danube plain and the Aegean coast. This evidence is presented within the broader archaeological and paleoecological context of the region and in cal. years BC and/or BP. The data is interpreted in terms of land-use related to woodland management and exploitation of woodland resources during three chronological phases which could be distinguished within the Neolithic of south-eastern Europe: a) 6500-5800 cal. BC, b) 5800-5500 cal. BC, and c) 5500-4900 cal BC). The main vegetation type targeted by the Neolithic population were the thermophilous, mixed deciduous oak communities, which contained a rich and diverse undergrowth of light-demanding and fruit/nut bearing trees, shrubs and herbs. Those plant communities were the major source of fuel wood, forest pasture, fodder, gathered fruits, etc. The analyses indicate stability and sustainability of the firewood procurement and woodland management practices for the whole considered period and further suggest that the Neolithic land-use strategies favoured the rich and often fruit-bearing undergrowth of the oak forests and woodland.
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RBINS Staff Publications 2018
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Neotype of Pseudagrion approximans Selys, 1876 designated to resolve a nomenclatorial confusion in the genus Aciagion Selys, 1891 (Odonata: Coenagrionidae)
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Nest relocation and high mortality rate in a Neotropical social wasp: impact of an exceptionally rainy La Niña year / Migration et fort taux de mortalité chez une guêpe Néotropicale: conséquence de pluies exceptionnelles durant une année La Niña.
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Nestedness in sessile and periphytic rotifer communities: A meta-analysis.
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Net ecosystem production and carbon dioxide fluxes in the Scheldt estuarine plume
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Neurogenomic Profiling Reveals Distinct Gene Expression Profiles between Brain Parts that are Consistent in Ophthalmotilapia Cichlids
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RBINS Staff Publications 2018
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New amphisbaenian lizards from the Early Paleogene of Europe and their implications for the early evolution of modern amphisbaenians
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Three new amphisbaenian lizard taxa are described from the Early Paleogene of Western Europe. Two new basal forms, Polyodontobaena belgica gen. et sp. nov. from the Early Paleocene of Hainin (Belgium) and Camptognathosaurus parisiensis gen. et sp. nov. from the Late Paleocene of Rivecourt-Patit Pâtis and Cernay-lès-Reims (France), are characterised by a dentary lacking a strong angle at the symphysis and bearing 10 to 12 massively built and conical teeth. These two taxa form the new family Polyodontobaenidae. A third new amphisbaenian, Blanosaurus primeocaenus gen. et sp. nov., is also described from the Early Eocene of Dormaal (Belgium), Condé-en-Brie and Prémontré (France) and represents the oldest modern amphisbaenian lizard of Europe, tentatively assigned to Blanidae. It is characterised by a reduction of tooth number and by the presence of a strong angle at the symphysis. Palaeobiogeographic considerations suggest a first hypothesis that the Eocene forms would have evolved from the Paleocene species.The second hypothesis would be that as for the lizard Scincoideus haininensis, primitive amphisbaenians were present in Europe from the Paleocene,whereasbeginning in the Early Eocene only modern forms with typical reduced dentition (fewer than 10 teeth) are present. The origin of these modern forms is very likely related with the dispersal of the first modern mammals.
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New and revised cyrtospiriferid (Spiriferida) brachiopods from the lower Famennian (Upper Devonian) of Armenia
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RBINS Staff Publications 2022
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New archaeozoological analysis of baboons buried at Hierakonpolis (Upper Egypt) shows two species were imported in the Predynastic period
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Excavations, on-going since 1979, in the elite Predynastic cemetery HK6 at Hierakonpolis, Upper Egypt, have revealed the burials of more than 150 domestic and wild animals. These animals, buried whole, were interred in subsidiary graves surrounding the elaborate tombs of the highest elite, who were local or possibly regional rulers in the Naqada IC-IIB period (c. 3700-3500 BC). Among the wild fauna are elephants and baboons, species that were not part of Egypt’s native fauna during the Holocene and must have been obtained from elsewhere. Here we discuss all the finds of baboons made so far. These include 20 individuals, constituting the earliest evidence for the occurrence of these primates in Egypt. Conflicting species identification in previous publications (first as Papio hamadryas and later as Papio anubis) led us to re-evaluate the diagnostic features described to differentiate them by examining a large series of modern skulls from natural history collections. Using the criteria that we found to be valid, we show that both P. hamadryas and P. anubis were present at Hierakonpolis. At least six graves contained baboons, which were buried either in groups of up to 8 individuals or as single interments. These graves can be associated with five of the mortuary complexes identified so far, covering a time span of several generations. Rachitis, observed in one very young animal is the only evidence so far for metabolic disorders that might be related to local breeding. This suggests that the baboons were not routinely bred on site and may have been imported on several occasions into Hierakonpolis, indicating more complex trade interactions with the lands to the far south than previously assumed.
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RBINS Staff Publications 2026
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New Archaeozoological Data from the Fayum ‘‘Neolithic’’ with a Critical Assessment of the Evidence for Early Stock Keeping in Egypt
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Faunal evidence from the Fayum Neolithic is often cited in the framework of early stock keeping in Egypt. However, the data suffer from a number of problems. In the present paper, large faunal datasets from new excavations at Kom K and Kom W (4850–4250 BC) are presented. They clearly show that, despite the presence of domesticates, fish predominate in the animal bone assemblages. In this sense, there is continuity with the earlier Holocene occupation from the Fayum, starting ca. 7350 BC. Domesticated plants and animals appear first from approximately 5400 BC. The earliest possible evidence for domesticates in Egypt are the very controversial domesticated cattle from the 9th/8th millennium BC in the Nabta Playa-Bir Kiseiba area. The earliest domesticates found elsewhere in Egypt date to the 6th millennium BC. The numbers of bones are generally extremely low at this point in time and only caprines are present. From the 5th millennium BC, the numbers of sites with domesticates dramatically increase, more species are also involved and they are usually represented by significant quantities of bones. The data from the Fayum reflect this two phase development, with very limited evidence for domesticates in the 6th millennium BC and more abundant and clearer indications in the 5th millennium BC. Any modelling of early food production in Egypt suffers from poor amounts of data, bias due to differential preservation and visibility of sites and archaeological remains, and a lack of direct dates for domesticates. In general, however, the evidence for early stock keeping and accompanying archaeological features shows large regional variation and seems to be mainly dependent on local environmental conditions. The large numbers of fish at Kom K and Kom W reflect the proximity of Lake Qarun.
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