Archaeobotanical research at the medieval fortified site of ?g?l?z (Anti-Atlas, Morocco) with particular reference to the exploitation of the argan tree

The analysis of botanical macro-remains (seeds, fruits and wood) from the fortress site of ?g?l?z, situated in the Anti-Atlas mountain range of southern Morocco, provides a first glimpse of the plant economy of a medieval rural community in this part of North Africa. Considered as the original stronghold of the religious community led by Ibn T?mart, the founder of the Almohad dynasty, the site was occupied from the 10th to the 13th century a.d. The crop assemblage identified from ashy contexts in a central grouping of buildings (the qasba) comprises barley (Hordeum vulgare), sorghum (Sorghum sp., earliest occurrence known so far from Morocco), wheat (Triticum sp.) and a pulse (Lathyrus sativus/cicera). Several arboreal fruit species are also identified: fig (Ficus carica), almond (Prunus dulcis), date palm (Phoenix dactylifera), grapevine (Vitis vinifera) and argan (Argania spinosa). The latter, predominant in the archaeobotanical record in the form of both fruit and wood remains, is of particular interest as it is the first time that this species, endemic to south-western Morocco and of prime economic interest regionally, has been identified from an archaeological context. In the past, as today, the argan tree seems to have played a major role in village economies as a source of wood for fuel and construction, fodder for livestock and food in the form of an edible oil, extracted from the oleaginous seeds. This article focuses on present and past uses of Argania spinosa as well as on the ecology and morpho-anatomy of this emblematic species.     

Discovery of an Upper Miocene Vertebrate fauna near Tizi N’Tadderht,Skoura, Ouarzazate Basin (Central High Atlas,Morocco)

The discovery of Upper Miocene vertebrates at Tizi N’Tadderht in the Ouarzazate basin (Morocco) helps to fill a gap in our knowledge of Neogene faunas in North Africa. The new fauna includes an ostrich cf. Struthio sp, a turtle cf. Centrochelys sp., Crocodylus cf. niloticus, and a relatively diverse fauna of large mammals. The mammal assemblage probably includes three hipparion species, including a very small form not previously reported from Africa, aff. Cremohipparion periafricanum, two species of rhinoceros cf. Ceratotherium sp. and aff. Chilotherium sp., a Proboscidean cf. Tetralophodon sp., a large member of the Giraffidae similar to “Palaeotragus” germaini and two bovids of which one is likely related to Prostrepsiceros, while the other is a new medium-sized antelope with spiral horns, certainly a representative of the Caprinae, a group that is rare in Africa. A late Miocene age, corresponding to the European Turolian Mammal age, is most likely for this fauna.     

First selenosteid placoderms from the eastern Anti‐Atlas of Morocco; osteology,phylogeny and palaeogeographical implications

Abstract: A new placoderm assemblage is reported from the Kellwasser facies of the eastern Anti‐Atlas, Morocco. This is the first record of an abundant Frasnian placoderm assemblage from Africa. The following new selenosteid taxa are described: Draconichthys elegans gen. et sp. nov., Enseosteus marocanensis sp. nov. and Walterosteus lelievrei sp. nov. In addition, material of Rhinosteus cf. parvulus is figured and described for the first time from Gondwana. The genera Enseosteus, Rhinosteus and Walterosteus are reviewed. ‘Wildungenichthys’ is regarded as a junior subjective synonym of Walterosteus. The new material and a revision of the taxa from Bad Wildungen, Germany, are the basis for a new phylogenetic analysis of the selenosteid arthrodires. The monophyly of the selenosteids is confirmed. The North American selenosteids are a sister group of Moroccan and European selenosteids, excluding Pachyosteus. The Moroccan vertebrate assemblage resembles that of Bad Wildungen. This supports the close palaeogeographical positions of Gondwana and Laurussia during the Late Devonian and indicates that biogeographical barriers for placoderms that could have separated the two assemblages were absent.     

First and second millennium a.d. agriculture in Rwanda: archaeobotanical finds and radiocarbon dates from seven sites

This article presents the results from a programme of bulk soil sampling and flotation of first and second millennium a.d. early farming, ‘Iron Age’, archaeological sites in Rwanda conducted in 2006–2007 alongside a new set of associated radiocarbon dates, which contribute toward the development of a chronology of plant use for the region. This research has identified the earliest examples of pearl millet (Pennisetum glaucum), finger millet (Eleusine coracana) and sorghum (Sorghum bicolor) in Great Lakes Africa and thus this article also discusses the significance of these finds within the later archaeology of the region and presents a brief synthesis of the direct archaeological evidence for finger millet in sub-Saharan Africa.     

Phylogeography and demographic history of Shaw's Jird (Meriones shawii complex) in North Africa

Palaeoenvironmental data and climatic reconstructions show that the Mediterranean ecoregion of North Africa underwent drastic ecological changes during the Pleistocene. Given its rich palaeontological record, North Africa is a pertinent region for documenting the role of climate change and human mediated‐habitat changes on the demography and genetic structure of faunal species. In the present study, we collected data from this species in Morocco, Algeria, and Tunisia, and we combined molecular (mitochondrial and nuclear DNA sequences, microsatellites), fossil, palaeoenvironmental, and human context data to propose an explanation for the fluctuations of populations belonging to the Meriones shawii complex in the past. Genetic and fossil data both indicate a strong bottleneck in Moroccan populations at the Middle Holocene (last interglacial optimum) compared to the Late Pleistocene. Our mitochondrial DNA data suggest a diversification event within Morocco corresponding to the 130–125 kya interglacial optimum. Given that (1) major demographic changes in the M. shawii complex coincide with the interglacial optimums, and (2) the impact of human activities on the landscape and faunal communities was moderate during the Middle Holocene (beginnings of the Neolithic culture), our results demonstrate that climate, rather than anthropogenic influences, likely explains the M. shawii complex population decline in the Holocene.     

Taphonomy and palaeoecology of the late Pleistocene to middle Holocene small mammal succession of El Harhoura 2 cave (Rabat-Témara, Morocco)

The relationship between local and global climatic variations and the origin and dispersal of Homo sapiens in Africa is complex, and North Africa may have played a major role in these events. In Morocco, very few studies are specifically dedicated to small fossil vertebrates, and neither taphonomic nor palaeoecological studies have been undertaken on these taxa, particularly in archaeological contexts. The late Pleistocene to middle Holocene succession of El Harhoura 2 cave, situated in the region of Témara, yields an exceptionally rich small vertebrate assemblage. We present the results of a first systematic, taphonomic, and palaeoecological study of the small mammals from Levels 1 to 8 of El Harhoura 2. The absence of bone sorting and polishing, as well as the presence of significant traces of digestion indicate that the small mammal bones were accumulated in the cave by predators and that no water transport occurred. Other traces observed on the surface of bones consist mainly of root marks and black traces (micro-organisms or more probably manganese) which affected the majority of the material. The percentage of fragmentation is very high in all stratigraphic levels, and the post-depositional breakage (geologic and anthropogenic phenomena) obscure the original breakage patterns of bones by predators. According to the ecology of the different species present in the levels of El Harhoura 2, and by taking into account possible biases highlighted by the taphonomic analysis, we reconstruct the palaeoenvironmental evolution in the region. For quantitative reconstructions we used two indices: the Taxonomic Habitat Index (THI) and the Gerbillinae/Murinae ratio. Late Pleistocene accumulations were characterised by a succession of humid (Levels 3, 4a, 6, and 8) and arid (Levels 2?, 5, and 7) periods, with more or less open landscapes, ending in an ultimate humid and wooded period during the middle Holocene (Level 1). We discuss particular limits of our results and interpretations, due to an important lack of taxonomic, ecological, and taphonomic knowledge in North Africa.     

Taphonomy of Small Predators multi-taxa accumulations: palaeoecological implications

Abstract

Most small terrestrial vertebrate accumulations in archaeological and palaeontological sites result from predation but we are far from having an exhaustive knowledge of modern predators’ diet, ecological niches and bone modification patterns especially in North African sites. The few neotaphonomic referentials available result from taxon-specialized palaeontologists’ initiatives. A survey of the literature on North Africa predators shows that their prey diversity is high and not only include rodent and shrews but also amphibians, squamates, bats and insects. We performed here a pilot taphonomic study of a Moroccan Tyto alba nest pellets including the whole taxa consumed (birds, rodents, shrews, amphibians, insects). We analyzed bone representation, fragmentation and digestion for each taxa and then compared the results. We observe differences between the taxa but on the whole find higher modification levels for this assemblage compared to roost sites of barn owls from other sites. We used for the comparisons homologous bones like the femur and the humerus and also found differences between the taxa. For example, digestion was lower on amphibians and birds than on micromammals. We discuss here some methodological issues as well as archaeological and palaeoenviromental ones by comparison with the Pleisto-Holocene site of El Harhoura II (Morocco).     

Mammal distributions in the western Mediterranean: the role of human intervention

The natural distribution of the 17 non-flying mammal species occurring wild in both the Maghreb (north-west Africa) and Iberia (south-west Europe) is considered. It is concluded that only four species – Red Fox Vulpes vulpes, Wild Boar Sus scrofa, Wild Cat Felis silvestris and Otter Lutra lutra – are native to both regions, while another three – Red Deer Cervus elaphus, Brown Bear Ursus arctos and Aurochs Bos primigenius – were native to North Africa until the mid-Holocene but have probably died out naturally. Algerian Hedgehog Atelerix algirus, Barbary Ape Macaca sylvanus, Genet Genetta genetta and Egyptian Mongoose Herpestes ichneumon are widely accepted as introductions to Europe from North Africa. The remaining six species, and Red Deer now found in Africa, were also probably introduced – Rabbit Oryctolagus cuniculus, Weasel Mustela nivalis, Wood Mouse Apodemus sylvaticus and Lesser White-toothed Shrew Crocidura russula from Europe to Africa; Algerian Mouse Mus spretus from Africa to Europe; Savi’s Pygmy Shrew Suncus etruscus perhaps from the eastern Mediterranean to both Iberia and the Maghreb. There are two Maghrebi species which, although not found in Europe, are more closely related to Palaearctic than to Afrotropical species: Garden Dormouse Eliomys melanurus, probably native to north-west Africa, although possible augmentation of the natural population cannot be ruled out, and Whitaker’s Shrew Crocidura whitakeri, a North African endemic. Removal of so many species of European provenance from the list of mammals native to north-west Africa should not be considered to weaken its position as part of the Palaearctic zoogeographical region. Bats and other, non-mammalian, taxa illustrate the clear faunal relationship between the Maghreb and south-west Europe, whilst emphasizing its distinction from subsaharan Africa.     

Palaeoenvironmental and palaeoclimatic reconstruction of the Middle to Late Pleistocene sequence of Scladina Cave (Namur,Belgium) using the small-mammal assemblages

The habitat weighting, the bioclimatic model methods and the Simpson diversity index are applied to the small-mammals assemblage of Scladina Cave (border between High and Middle Belgium) in order to reconstruct the environmental and climatic fluctuations that are reflected on the Middle to Late Pleistocene sequence of the cave. The small-mammal data analyzed come from two surveys carried out at the entrance of the cave and allow us to identify within the section one cold episode: a dry, cool phase in the upper part of the sequence (probably associated with the MIS 3). The environmental and climatic data show an alternation of open meadows and woodland formations through both sequences, punctuated by peaks in local watery environments together with lower temperatures and higher precipitations rates than at present. Finally, a comparison of the small-mammal fossil assemblage from the studied surveys with the small-mammals assemblage from the Holocene deposits of Scladina Cave shows that layers related with MIS 5 temperate sub-stages (MIS 5c and MIS 5a) present environmental characteristics similar to those prevailing nowadays (a landscape dominated by woodland formations and water streams) in the area surrounding the cave. This is coherent with the available chronostratigraphic datasets on this part of the sequence, suggesting the record of the humid and temperate phases at the beginning of the Late Pleistocene.     

Protonemura berberica,a New Species of Nemouridaefrom North Africa (Plecoptera)

Protonemura berberica sp. n. is described from the Rif mountains (Morocco, North Africa). This species belongs to the Protonemura corsicana group, which has a circum-mediterranean distribution. The male is clearly distinguished by the shape of the epiproct, with its very short terminal filament which is directed upwards, and by the shape of the paraprocts.     

Mus in Morocco: a Quaternary sequence of intraspecific evolution

North Africa is an intricate biogeographical region at the crossroads of immigration waves from tropical Africa and Asia. Species confined between various barriers (Atlas Mountains, arid environments such as the Sahara in the south, water masses such as the Mediterranean Sea in the north, and the Atlantic Ocean in the west) were generally forced to adapt locally to environmental changes instead of tracking their habitat by shifting their distribution area. The present study aims at providing first insight into the evolution of the genus Mus, and more specifically of the western Mediterranean species Mus spretus in this area. The study relies on the abundant Late Pleistocene and Middle Holocene fossil assemblage from the El Harhoura 2 cave (Rabat‐Témara, Morocco). This exceptional record was studied using geometric morphometrics applied to first upper and lower molars, constituting the most informative and best preserved fossil remains for such small rodents. Two main issues were addressed. (1) Geometric morphometrics was used to clarify taxonomic status and phylogenetic relationships among fossil and modern species in this area. Morphometric analysis revealed good discrimination of most modern and fossil species but failed to document intermediate forms tracing anagenetic evolution. Not mutually exclusive, the occurrence of complex processes of morphological evolution in this genus such as parallel evolution and the action of stabilizing selection may make it difficult to translate patterns of morphological evolution into phylogenetic conclusions. (2) The record was shown to document a sequence of intraspecific evolution of M. spretus. The morphology of the molars through the fossil record of El Harhoura 2 was surprisingly stable despite extensive modern variation. The limited temporal variation largely failed to correlate to palaeoenvironmental proxies. The mouse fossil record at El Harhoura 2 thus presents an intriguing case of morphological stasis despite extensive environmental changes. This long‐term stability may have been recently perturbed by anthropogenic factors including landscape changes and introduction of various competitors and predators, leading to a size reduction. © 2013 The Linnean Society of London, Biological Journal of the Linnean Society, 2013, 109 , 599–621.     

Ecosystem dynamics through the past 2000 years as revealed by fossil mammals from Lamar cave in Yellowstone National Park,USA

Lamar Cave, a late Holocene paleontological site in Yellowstone National Park, USA, has yielded 36 fossil mammal species from 10 stratigraphic units representing about 2000 years. The fossil fauna is similar to the mammals in the park today and affords a unique opportunity to investigate paleocommunity and ecosystem dynamics through time.

Remains of an extralimital species in Yellowstone today, Microtus ochrogaster are found only in the oldest cave deposits, dated at 1695 ± 60 yr B.P. Disappearance of this species by about 1550 years ago marks evolution into the ecosystem that has persisted into the present and is recognizable by a fossil mammal assemblage that is virtually identical to the modern one. Relative abundance fluctuations in the mammal populations imply community resilience through the past 2000 years. Trends in relative abundances of small mammals, particularly the inverse relationship between Microtus and Spermophilus are interpreted as evidence of declining grass cover near Lamar Cave between approximately 1500 and 1000 years ago. The initiation of this environmental change may well have stimulated the ecosystem change marked by Microtus ochrogaster extirpation. Support for this hypothesis is found in a pollen record from a nearby lake.     

House mouse dispersal in Iron Age Spain: a geometric morphometrics appraisal

During the Iron Age, sea trade in the Mediterranean increased, particularly with the expansion of Phoenician and Greek colonies in the Western Mediterranean. A side effect of these human movements was the involuntary dispersion of commensal species, such as the house mouse (Mus musculus domesticus). One archaeological layer dated from the 4th Century BC, coming from an Iberian village located in the Mediterranean coast of Spain, contained a large and reliable accumulation of small mammals. The presence of the house mouse was highly suspected within this layer. To assess its abundance quantitatively, we used a geometric morphometrics approach of the first lower molar contour using elliptical Fourier analysis. We also increased the power of the discrimination between the Algerian mouse (Mus spretus) and the house mouse by combining a dimension reduction approach together with different validation procedures. The relative importance of age, sex, and geographical origin onto the shape and form of the lower molar contour was also investigated. The results obtained demonstrate the presence and the dominance of the house mouse in the landscape surrounding the Iberian village in the 1st Millennium BC, only a few centuries after its arrival in the Western Mediterranean Basin. A cross‐validated linear discriminant function considering different Mediterranean populations suggest Morocco and France as the most probable geographical origins for the Algerian mouse, and Tunisia for the origin of house mice in North‐Eastern Spain. © 2011 The Linnean Society of London, Biological Journal of the Linnean Society, 2011, 102 , 483–497.     

四川炉霍县虾拉沱晚更新世哺乳类化石

本文简记了在四川省炉霍县虾拉沱附近鲜水河左岸发现的十三种哺乳动物化石.根据动物群的性质和 C~(14) 年代的测定,初步确定含化石层的时代为晚更新世最晚期.     

Plant economy of hunter-gatherer groups at the end of the last Ice Age: plant macroremains from the cave of Santa Maira (Alacant, Spain) ca. 12000–9000 b.p.

Up till now, plant macroremains of hunter-gatherer groups at the end of the last Ice Age and the very early Holocene have very rarely been investigated on the Iberian Peninsula and elsewhere. The use of systematic recovery techniques at the archaeological cave site of Santa Maira has allowed the recovery of a large amount of plant remains (fruits, seeds and wood) from Upper Palaeolithic and Epipalaeolithic levels (12000–9000 b.p.) Charcoal analysis has allowed us to reconstruct the surrounding vegetation of the site. In the valley bottoms mesophilous woodland with Quercus was present even in the lowest layers (Upper Magdalenian) During the Late-glacial Juniperus was very important, in the early Holocene Quercus (both evergreen and deciduous) took over. Large numbers of macroremains of fruits (Quercus sp., Sorbus sp., Olea sp. and Vitis sp.) were found, but a significant quantity of legumes together with a few grass seeds have also been identified. This assemblage most probably represents the gathering of wild plant resources by the inhabitants of the cave, and allows us to reconstruct some of the food gathered from plant resources.     

江苏丹徒莲花洞动物群

1981年3月和5月中至6月初,先后从丹徒县西南白龙岗山的莲花洞中采集到一颗智人牙齿及15种哺乳动物化石。人类牙齿为—M_2,可能属于一青少年个体;哺乳动物组合性质表明莲花洞堆积物的时代为晚更新世,早于溧水神仙洞,晚于江苏句容洞穴堆积物的时代。     

Mammals in Last 30 to 7 ka Interval (Late Pleistocene-Early Holocene) in Southern Uruguay (Santa Lucía River Basin): Last Occurrences,Climate, and Biogeography

Fossiliferous Quaternary sedimentary beds in the Santa Lucía Basin (southern Uruguay) are potentially useful for the study of the last occurrences of extinct taxa, as well as the environmental and climatic patterns in the late Pleistocene to the early Holocene. They have provided a chronological framework (AMS ¹⁴C and Optically Stimulated Luminescence dates), a mammalian diversity and interpretations of last occurrence, the climatic-environmental setting, and some associated biogeographic processes. The ages produced encompass the last 30 to 7 ka interval (latest Pleistocene-early Holocene). The mammalian assemblage (36 genera, 24 species) includes typical South American late Pleistocene mammals, extinct species of extant genera, and some extant species that still exist elsewhere on the continent. The preservation pattern includes articulated and semi-articulated skeletons of large and small mammals. The presence in the southern Uruguayan Pampean area of some mammals currently inhabiting Patagonia, northwest and central Argentina (Dolichotis, Galea, Microcavia, Chaetophractus, Lagostomus, and Vicugna) is explained by the predominance of open areas and cold climates associated with the Last Glacial Maximum. The mammalian record depicts local extinctions or shifting ranges occurring in latest Pleistocene or early Holocene. The sedimentary chronological framework and taphonomic features suggest the persistence into the early Holocene of Eutatus seguini, Morenelaphus brachyceros, Equus neogeus, Hemiauchenia sp., Lama sp., and Vicugna sp. Glyptodon and Glossotherium seem to persist at least to the latest Pleistocene. This pattern can substantiate the hypothesis that some megafauna and large mammals persisted for some millennia alongside people with extinction occurring before, during, and after human colonization.     

Les Anoures (Amphibiens) du pléistocène inférieur (« Villafranchien å) du Jebel Irhoud (carrir̀e « Ocre å), Maroc

Anurans (Amphibians) from the Late Pleistocene (“Villafranchian”) of Jebel Irhoud (“Ocre” quarry), Morocco. The Villafranchian anurans of Jebel Irhoud (“Ocre” quarry) Morocco, belong to the Discoglossidae (Baleaphryne), Bufonidae (Bufo cf. B. viridis, Bufo cf. B. regularis) and Ranidae (Rana sp.). The presence of Pelodytidae (Pelodytes) in this site is possible but not ascertained. The genus Baleaphryne is reported for the first time in Africa. Likewise, Pelodytes, if this identification proves correct, would be the first one ever found in Africa.     

The long‐term history of dispersal among lizards in the early Eocene: new evidence from a microvertebrate assemblage in the Bighorn Basin of Wyoming,USA

Abstract: Early Eocene mammal faunas of North America were transformed by intercontinental dispersal at the Paleocene–Eocene boundary, but lizard faunas from the earliest Eocene of the same area were dominated by immigrants from within the continent. A new lizard assemblage from the middle early Eocene of Wyoming sheds light on the longer‐term history of dispersal in relation to climate change. The assemblage consists of three iguanid species (including two new species possibly closely related to living Anolis), Scincoideus, ‘Palaeoxantusia’, four anguids, two species of an undescribed new anguimorph clade, Provaranosaurus and a varanoid (cf. Saniwa). Most North American glyptosaurin glyptosaurines are now referred to Glyptosaurus, and Glyptosaurus hillsi is given a new diagnosis. Scincoideus is otherwise known only from the mid‐Paleocene of Belgium, and the specimens described here are the first to document intercontinental dispersal to North America among lizards in the early Eocene. Like in mammals, some immigrant lizard lineages first appearing in the Bighorn Basin in the earliest Eocene persisted in the area long after the Paleocene–Eocene thermal maximum, but other immigrants appear to have been restricted to the Paleocene–Eocene thermal maximum.