scholarly journals Das Mittelwürm in den Lössen Südmährens und seine paläolithischen Kulturen

1996 ◽  
Vol 46 (1) ◽  
pp. 54-64
Author(s):  
Karel Valoch
Keyword(s):  
Upper Palaeolithic ◽  
Radiocarbon Dates ◽  
Southern Moravia ◽  
Vegetation And Climate ◽  
Archaeological Excavations ◽  
Micromorphological Analysis

Abstract. Archaeological excavations at several sites in the loesses of Southern Moravia have revealed an Middle Würm Interstadial soil, classed by micromorphological analysis as between pararendzinas and chernozems. This soil has been named Bohunice after the locality where it was first defined and in accordance with the works of Haesaerts. Anthraconistic and palynologic analysis enabled a reconstruction of the vegetation and climate. The dominant landscape was open, with scattered groups of trees; the climate was cool and moderately wet. A number of radiocarbon dates relate to the period between 40 000 and 30 000 years B.P. At the time transitional cultures developed between the Middle and Upper Palaeolithic (Bohunician, Szeletian) and also the earliest Upper Palaeolithic culture (Aurignacian).

scholarly journals Eastern Europe’s “Transitional Industry”?: Deconstructing the Early Streletskian

2021 ◽  
Vol 4 (1) ◽  
Author(s):  
R. Dinnis ◽  
A. Bessudnov ◽  
N. Reynolds ◽  
T. Devièse ◽  
A. Dudin ◽  
...  
Keyword(s):  
Modern Human ◽  
East European Plain ◽  
Upper Palaeolithic ◽  
Radiocarbon Dates ◽  
East European ◽  
Archaeological Material ◽  
Younger Age ◽  
Layer V ◽  
Precise Relationship ◽  
Early Upper

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.

scholarly journals The earliest evidence for dwelling construction in the Upper Palaeolithic of Eastern Europe: a 30,000-year-old surface structure from Mira layer I

Vita Antiqua ◽  
2021 ◽  
pp. 43-54
Author(s):  
V.N. Stepanchuk ◽  
Keyword(s):  
Eastern Europe ◽  
Surface Structure ◽  
Steppe Zone ◽  
East European Plain ◽  
Upper Palaeolithic ◽  
Interior Space ◽  
Radiocarbon Dates ◽  
East European ◽  
Surface Dwelling ◽  
Layer I

The purpose of this article is to present data on the surface structure identified in the upper layer of the Mira site in the Dnieper valley. The occupation of layer I, based on a set of consistent data, constitutes the remains of a seasonal winter camp of Pleistocene horse hunters. Ten available radiocarbon dates place the calibrated age of layer I between 31,000 to 28,000 cal BP. The rapid albeit gentle overlapping of the settlement remains with alluvial sediments ensured that the original settlement and dwelling patterns and their elements survived well. Thanks to this, it is possible to reconstruct some significant aspects of the construction process, as well as details of the arrangement of the dwelling’s interior space. A 30,000-year-old, permanent skeleton cylindrical yaranga type surface construction from Mira layer I is currently representing the oldest dwelling known in the Upper Palaeolithic of Ukraine and a broader context of the steppe zone of the East European plain. Keywords: Upper Palaeolithic, surface dwelling, Eastern Europe

Direct radiocarbon dates of mid Upper Palaeolithic human remains from Dolní Věstonice II and Pavlov I, Czech Republic

2019 ◽  
Vol 27 ◽  
pp. 102000 ◽  
Author(s):  
Helen Fewlass ◽  
Sahra Talamo ◽  
Bernd Kromer ◽  
Edouard Bard ◽  
Thibaut Tuna ◽  
...  
Keyword(s):  
Czech Republic ◽  
Human Remains ◽  
Upper Palaeolithic ◽  
Radiocarbon Dates

scholarly journals Radiocarbon Dates and the Earliest Colonization of East Polynesia: More than a Case Study

Radiocarbon ◽  
2009 ◽  
Vol 51 (2) ◽  
pp. 681-693 ◽  
Author(s):  
Philippe Della Casa
Keyword(s):  
Vegetation History ◽  
French Polynesia ◽  
Easter Island ◽  
Sample Material ◽  
Ongoing Debate ◽  
Radiocarbon Dates ◽  
Almost All ◽  
Early Human ◽  
Archaeological Excavations

Over the last 30 yr, there has been an ongoing debate on the dates and modes of the earliest colonization of East Polynesia, namely the Cook Islands, the 5 archipelagos of French Polynesia, the Hawai'i Islands, Easter Island, and New Zealand. At least 3 alternative models were proposed by Sinoto, Anderson, Kirch, and Conte, but interestingly all these models basically relied on the same set of roughly 200 radiocarbon dates on various organic materials from archaeological excavations as far back as the 1950s. Some of the models differed by 500–1000 yr—for a proposed initial colonization around the turn of the BC/AD eras, if not considerably later. By comparing the different approaches to this chronological issue, it becomes evident that almost all known problems in dealing with 14C dates from archaeological excavations are involved: stratigraphy and exact location of samples, sample material and quality, inbuilt ages and reservoir effects, lab errors in ancient dates, etc. More recently, research into landscape and vegetation history has produced alternative 14C dating for early human impact, adding to the confusion about the initial stages of island colonization, while archaeological 14C dates, becoming increasingly “young” as compared to former investigations, now advocate a rapid and late (post-AD 900) colonization of the archipelagos. As it appears, the Polynesian case is more than just another case study, it's a lesson on 14C-based archaeological chronology. The present paper does not pretend to solve the problems of early Polynesian colonization, but intends to contribute to the debate on how 14C specialists and archaeologists might cooperate in the future.

Climate change and human disturbance of fynbos vegetation during the late Holocene at Princess Vlei, Western Cape, South Africa

The Holocene ◽  
2011 ◽  
Vol 21 (7) ◽  
pp. 1137-1149 ◽  
Author(s):  
F.H. Neumann ◽  
L. Scott ◽  
M.K. Bamford
Keyword(s):  
Anthropogenic Disturbance ◽  
Late Holocene ◽  
Climate Changes ◽  
Western Cape ◽  
Radiocarbon Dates ◽  
The Core ◽  
Pollen Types ◽  
Hydrological System ◽  
Vegetation And Climate ◽  
Floating Mat

Pollen analysis of a core in Princess Vlei in the Fynbos Biome near Cape Town gives a 4150 year record of vegetation and climate changes followed by disturbance by colonial settlers since c. 300 years ago. Their impact replaced climate as a major factor in changing the vegetation. The chronology is based on eight radiocarbon dates. Pollen types such as Restionaceae, Ericaceae, and Proteaceae reflect changes in fynbos. Pollen indicators at the bottom of the core suggest drier conditions followed by an increase in Morella, Cyperaceae and Carpacoce pollen, which might indicate moist conditions c. 3400–2600 cal. yr BP. Drier conditions prevail c. 2600–1900 cal. yr BP. Apparent light disturbance after c. 2000 cal. yr BP might be attributed to Khoi herders. Deeper water and damp surroundings are indicated c. 1900–1000 cal. yr BP. The top of the core shows an increase of Poaceae while Restionaceae decrease with anthropogenic disturbance, including the introduction of neophytes such as Pinus ( c. 300 years ago) and Zea mays. Charcoal percentages point to intense fires after the arrival of the Europeans. Water between 105 and 75 cm indicates the development of a floating mat resulting from changes in the hydrological system possibly connected to disturbances by settlers.

Late Quaternary Vegetation and Climate of Southern Tierra del Fuego

1989 ◽  
Vol 31 (3) ◽  
pp. 396-406 ◽  
Author(s):  
Calvin J. Heusser
Keyword(s):  
Late Quaternary ◽  
Pollen Dispersal ◽  
Late Glacial ◽  
Tierra Del Fuego ◽  
Fossil Pollen ◽  
Radiocarbon Dates ◽  
Modern Pollen ◽  
Open Woodland ◽  
Glacial Time ◽  
Vegetation And Climate

AbstractVegetation and climate over approximately the past 13,000 yr are reconstructed from fossil pollen in a 9.4-m mire section at Caleta Róbalo on Beagle Channel, Isla Navarino (54°56′S, 67°38′W), southern Tierra del Fuego. Fifty surface samples reflecting modern pollen dispersal serve to interpret the record. Chronologically controlled by nine radiocarbon dates, fossil pollen assemblages are: Empetrum-Gramineae-Gunnera-Tubuliflorae (zone 3b, 13,000–11,850 yr B.P.), Gramineae-Empetrum-assorted minor taxa (zone 3a, 11,850-10,000 yr B.P.), Nothofagus-Gramineae-Tubuliflorae-Polypodiaceae (zone 2, 10,000–5000 yr B.P.), Nothofagus-Empetrum (zone 1b, 5000-3000 yr B.P.), and Empetrum-Nothofagus (zone 1a, 3000-0 yr B.P.). Assemblages show tundra under a cold, dry climate (zone 3), followed by open woodland (zone 2), as conditions became warmer and less dry, and later, with greater humidity and lower temperatures, by closed forest and the spread of mires (zone 1). Comparisons drawn with records from Antarctica, New Zealand, Tasmania, and the subantarctic islands demonstrate broadly uniform conditions in the circumpolar Southern Hemisphere. The influences of continental and maritime antarctic air masses were apparently considerable in Tierra del Fuego during cold late-glacial time, whereas Holocene climate was largely regulated by interplay between maritime polar and maritime tropical air.

scholarly journals Between two worlds: Cova Eirós and the Middle-Upper Palaeolithic transition in NW Iberia

2021 ◽  
Author(s):  
Arturo de LOMBERA-HERMIDA ◽  
Xose-Pedro RODRÍGUEZ-ÁLVAREZ ◽  
Alicia AMEIJENDA IGLESIAS ◽  
Mikel DÍAZ RODRÍGUEZ ◽  
undefined Iván REY-RODRÍGUEZ ◽  
...  
Keyword(s):  
Upper Paleolithic ◽  
Raw Material ◽  
Upper Palaeolithic ◽  
Subsistence Strategies ◽  
Radiocarbon Dates ◽  
Nw Iberia ◽  
Early Upper Paleolithic ◽  
Anatomically Modern Humans ◽  
Late Survival ◽  
Early Upper

Iberia, a natural cul-de-sac peninsula, plays a major role in the study of the Neanderthals demise and its eventual relationship with the spread of Anatomically Modern Humans (AMH) in Europe. The site of Cova Eirós (Galicia, Spain), located in NW Iberia, contains Middle and Upper Palaeolithic levels, based on the cultural remains recovered at the site. No human remains directly associated with those levels were discovered yet. The available radiocarbon dates from the levels 2 (c. 35 ka cal BP, Early Upper Paleolithic) and 3 (c. 41 ka cal BP, Late Middle Paleolithic), point to a late survival of Neanderthal groups in North Iberia and to a relative quick arrival of the AMH, c. 35-36 ka cal BP, with respect to other territories of the Iberian Peninsula. The archaeological record shows clear differences between the Middle and the Upper Palaeolithic occupations, regarding raw-material acquisition, lithic technology and subsistence strategies. The location of Cova Eirós in the westernmost margin of the Cantabrian Rim and in the Atlantic Façade, makes this site a key place to understand the spread of the first AMH and the progressive demise of Neanderthal populations.

scholarly journals Pieces of people in the Pavlovian

2019 ◽  
Vol 5 (1) ◽  
pp. 70-87 ◽  
Author(s):  
Erik Trinkaus ◽  
Sandra Sázelová ◽  
Jiří Svoboda
Keyword(s):  
Czech Republic ◽  
Social Dynamics ◽  
Human Remains ◽  
Upper Palaeolithic ◽  
Faunal Remains ◽  
Site Structure ◽  
Abundant Evidence ◽  
Southern Moravia ◽  
The Rich ◽  
Human Burials

The rich earlier Mid Upper Palaeolithic (Pavlovian) sites of Dolní Vĕstonice I and II and Pavlov I (∼32,000–∼30,000 cal BP) in southern Moravia (Czech Republic) have yielded a series of human burials, isolated pairs of extremities and isolated bones and teeth. The burials occurred within and adjacent to the remains of structures (‘huts’), among domestic debris. Two of them were adjacent to mammoth bone dumps, but none of them was directly associated with areas of apparent discard (or garbage). The isolated pairs and bones/teeth were haphazardly scattered through the occupation areas, many of them mixed with the small to medium-sized faunal remains, from which many were identified post-excavation. It is therefore difficult to establish a pattern of disposal of the human remains with respect to the abundant evidence for site structure at these Upper Palaeolithic sites. At the same time, each form of human preservation raises questions about the differential mortuary behaviours, and hence social dynamics, of these foraging populations and how we interpret them through an archaeological lens.

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