La subsistencia en el Magdaleniense Mediterráneo ibérico

2021 ◽  
Author(s):  
Cristina Real

Este libro aporta datos relevantes para el conocimiento de las poblaciones humanas modernas y sus actividades de subsistencia en el área central del Mediterráneo Ibérico durante el Paleolítico Superior Final (Magdaleniense). Para ello se aplica un estudio arqueozoológico y tafonómico a tres conjuntos de fauna de la Cova de les Cendres. This book provides data relevant to understanding modern human populations and their subsistence activities in the central area of the Iberian Mediterranean during the Final Upper Palaeolithic (Magdalenian). It includes an archaeozoological and taphonomic analysis of three faunal assemblages from Cova de les Cendres

1992 ◽  
Vol 337 (1280) ◽  
pp. 225-234 ◽  

The transition from anatomically ‘archaic’ to ‘modern’ populations would seem to have occurred in most regions of Europe broadly between ca.40 and 30 ka ago: much later than in most other areas of the world. The archaeological evidence supports the view that this transition was associated with the dispersal of new human populations into Europe, equipped with a new technology (‘Aurignacian’) and a range of radical behavioural and cultural innovations which collectively define the ‘Middle-Upper Palaeolithic transition'. In several regions of Europe there is archaeological evidence for a chronological overlap between these populations and the final Neanderthal populations and, apparently, for various forms of contact, interaction and, apparently, ‘acculturation’ between these two populations. The fundamental behavioural adaptations implicit in the ‘Upper Palaeolithic Revolution’ (possibly including language) are thought to have been responsible for this rapid dispersal of human populations over the ecologically demanding environments of last-glacial Europe.


PLoS ONE ◽  
2010 ◽  
Vol 5 (2) ◽  
pp. e9157 ◽  
Author(s):  
Anne-Laure Daniau ◽  
Francesco d'Errico ◽  
Maria Fernanda Sánchez Goñi

2021 ◽  
Author(s):  
Ekaterina Stansfield ◽  
Philipp Mitteroecker ◽  
Sergey Vasilyev ◽  
Sergey Vasilyev ◽  
Lauren Butaric

Abstract When our human ancestors migrated out of Africa, they faced a considerably harsher climate, but the extent to which human cranial morphology has adapted to climate is still debated. In particular, it remains unclear when such facial adaptations arose in human populations. Here, we explore climate-associated features of face shape in a worldwide modern human sample using 3D geometric morphometrics and a novel application of reduced rank regression. Based on these data, we assess climate adaptations in two crucial Upper Palaeolithic human fossils, Sungir and Mladeč, both of which have been archaeologically associated with a boreal-to-temperate climate. We found several aspects of face shape, especially the relative dimensions of the external and internal nose as well as of the maxillary sinuses, that are strongly associated with temperature and humidity, even after accounting for auto-correlation due to geographical proximity of populations. For these features, both fossils revealed adaptations to a dry environment, with Sungir being strongly associated with cold and Mladeč with warm-to-hot temperatures. As both fossils are dated among the earliest recent modern humans in Europe, our results suggest a relatively fast rate of climate adaptation in human respiratory morphology.


2021 ◽  
Vol 11 (1) ◽  
Author(s):  
Ekaterina Stansfield ◽  
Philipp Mitteroecker ◽  
Sergey Y. Vasilyev ◽  
Sergey Vasilyev ◽  
Lauren N. Butaric

AbstractAs our human ancestors migrated into Eurasia, they faced a considerably harsher climate, but the extent to which human cranial morphology has adapted to this climate is still debated. In particular, it remains unclear when such facial adaptations arose in human populations. Here, we explore climate-associated features of face shape in a worldwide modern human sample using 3D geometric morphometrics and a novel application of reduced rank regression. Based on these data, we assess climate adaptations in two crucial Upper Palaeolithic human fossils, Sungir and Mladeč, associated with a boreal-to-temperate climate. We found several aspects of facial shape, especially the relative dimensions of the external nose, internal nose and maxillary sinuses, that are strongly associated with temperature and humidity, even after accounting for autocorrelation due to geographical proximity of populations. For these features, both fossils revealed adaptations to a dry environment, with Sungir being strongly associated with cold temperatures and Mladeč with warm-to-hot temperatures. These results suggest relatively quick adaptative rates of facial morphology in Upper Palaeolithic Europe.


2021 ◽  
Vol 4 (1) ◽  
Author(s):  
R. Dinnis ◽  
A. Bessudnov ◽  
N. Reynolds ◽  
T. Devièse ◽  
A. Dudin ◽  
...  

AbstractThe Streletskian is central to understanding the onset of the Upper Palaeolithic on the East European Plain. Early Streletskian assemblages are frequently seen as marking the Neanderthal-anatomically modern human (AMH) anthropological transition, as well as the Middle-to-Upper Palaeolithic archaeological transition. The age of key Streletskian assemblages, however, remains unclear, and there are outstanding questions over how they relate to Middle and Early Upper Palaeolithic facies. The three oldest Streletskian layers—Kostenki 1 Layer V, Kostenki 6 and Kostenki 12 Layer III—were excavated by A. N. Rogachev in the mid-20th century. Here, we re-examine these layers in light of problems noted during Rogachev’s campaigns and later excavations. Layer V in the northern part of Kostenki 1 is the most likely assemblage to be unmixed. A new radiocarbon date of 35,100 ± 500 BP (OxA- X-2717-21) for this assemblage agrees with Rogachev’s stratigraphic interpretation and contradicts later claims of a younger age. More ancient radiocarbon dates for Kostenki 1 Layer V are from areas lacking diagnostic Streletskian points. The Kostenki 6 assemblage’s stratigraphic context is extremely poor, but new radiocarbon dates are consistent with Rogachev’s view that the archaeological material was deposited prior to the CI tephra (i.e. >34.3 ka BP). Multiple lines of evidence indicate that Kostenki 12 Layer III contains material of different ages. Despite some uncertainty over the precise relationship between the dated sample and diagnostic lithic material, Kostenki 1 Layer V (North) therefore currently provides the best age estimate for an early Streletskian context. This age is younger than fully Upper Palaeolithic assemblages elsewhere at Kostenki. Other “Streletskian” assemblages and Streletskian points from younger contexts at Kostenki are briefly reviewed, with possible explanations for their chronostratigraphic distribution considered. We caution that the cultural taxon Streletskian should not be applied to assemblages based simply on the presence of bifacially worked artefacts.


Nature ◽  
2021 ◽  
Vol 592 (7853) ◽  
pp. 253-257 ◽  
Author(s):  
Mateja Hajdinjak ◽  
Fabrizio Mafessoni ◽  
Laurits Skov ◽  
Benjamin Vernot ◽  
Alexander Hübner ◽  
...  

AbstractModern humans appeared in Europe by at least 45,000 years ago1–5, but the extent of their interactions with Neanderthals, who disappeared by about 40,000 years ago6, and their relationship to the broader expansion of modern humans outside Africa are poorly understood. Here we present genome-wide data from three individuals dated to between 45,930 and 42,580 years ago from Bacho Kiro Cave, Bulgaria1,2. They are the earliest Late Pleistocene modern humans known to have been recovered in Europe so far, and were found in association with an Initial Upper Palaeolithic artefact assemblage. Unlike two previously studied individuals of similar ages from Romania7 and Siberia8 who did not contribute detectably to later populations, these individuals are more closely related to present-day and ancient populations in East Asia and the Americas than to later west Eurasian populations. This indicates that they belonged to a modern human migration into Europe that was not previously known from the genetic record, and provides evidence that there was at least some continuity between the earliest modern humans in Europe and later people in Eurasia. Moreover, we find that all three individuals had Neanderthal ancestors a few generations back in their family history, confirming that the first European modern humans mixed with Neanderthals and suggesting that such mixing could have been common.


Nature ◽  
2021 ◽  
Author(s):  
Elena I. Zavala ◽  
Zenobia Jacobs ◽  
Benjamin Vernot ◽  
Michael V. Shunkov ◽  
Maxim B. Kozlikin ◽  
...  

AbstractDenisova Cave in southern Siberia is the type locality of the Denisovans, an archaic hominin group who were related to Neanderthals1–4. The dozen hominin remains recovered from the deposits also include Neanderthals5,6 and the child of a Neanderthal and a Denisovan7, which suggests that Denisova Cave was a contact zone between these archaic hominins. However, uncertainties persist about the order in which these groups appeared at the site, the timing and environmental context of hominin occupation, and the association of particular hominin groups with archaeological assemblages5,8–11. Here we report the analysis of DNA from 728 sediment samples that were collected in a grid-like manner from layers dating to the Pleistocene epoch. We retrieved ancient faunal and hominin mitochondrial (mt)DNA from 685 and 175 samples, respectively. The earliest evidence for hominin mtDNA is of Denisovans, and is associated with early Middle Palaeolithic stone tools that were deposited approximately 250,000 to 170,000 years ago; Neanderthal mtDNA first appears towards the end of this period. We detect a turnover in the mtDNA of Denisovans that coincides with changes in the composition of faunal mtDNA, and evidence that Denisovans and Neanderthals occupied the site repeatedly—possibly until, or after, the onset of the Initial Upper Palaeolithic at least 45,000 years ago, when modern human mtDNA is first recorded in the sediments.


1992 ◽  
Vol 87 ◽  
pp. 1-28 ◽  
Author(s):  
Geoff Bailey

Klithi is a rockshelter in the lower reaches of the Voidomatis gorge, near the village of Klithonia in Epirus. Excavations in progress since 1983 have revealed evidence of a late Upper Palaeolithic occupation dated between 16,000 BP and 10,000 BP, with rich microlithic stone tool industries and faunal assemblages dominated by chamois and ibex. The excavations have been accompanied by wider investigations of the local and regional palaeoenvironment and reexamination of the Middle and Upper Palaeolithic sites excavated by Eric Higgs in the 1960s, notably Kokkinopilos, Asprochaliko, and Kastritsa. This paper presents some of the detailed results of the Klithi excavations and sets the results within the wider context of the global issues which inform the study of Palaeolithic archaeology, the Palaeolithic of Greece as a whole, and the regional picture of Palaeolithic settlement in Epirus.


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