Dietary traits and habitats of the reindeer (Rangifer tarandus) during the Late Glacial of Northern Europe

2020 ◽  
Vol 12 (5) ◽  
Author(s):  
Florent Rivals ◽  
Dorothée G. Drucker ◽  
Mara-Julia Weber ◽  
Françoise Audouze ◽  
James G. Enloe
Human Ecology ◽  
2018 ◽  
Vol 46 (5) ◽  
pp. 621-632 ◽  
Author(s):  
Felix Riede ◽  
Jesper B. Pedersen

2011 ◽  
Vol 366 (1566) ◽  
pp. 793-808 ◽  
Author(s):  
Felix Riede

The niche construction model postulates that human bio-social evolution is composed of three inheritance domains, genetic, cultural and ecological, linked by feedback selection. This paper argues that many kinds of archaeological data can serve as proxies for human niche construction processes, and presents a method for investigating specific niche construction hypotheses. To illustrate this method, the repeated emergence of specialized reindeer ( Rangifer tarandus ) hunting/herding economies during the Late Palaeolithic ( ca 14.7–11.5 kyr BP) in southern Scandinavia is analysed from a niche construction/triple-inheritance perspective. This economic relationship resulted in the eventual domestication of Rangifer . The hypothesis of whether domestication was achieved as early as the Late Palaeolithic, and whether this required the use of domesticated dogs ( Canis familiaris ) as hunting, herding or transport aids, is tested via a comparative analysis using material culture-based phylogenies and ecological datasets in relation to demographic/genetic proxies. Only weak evidence for sustained niche construction behaviours by prehistoric hunter–gatherer in southern Scandinavia is found, but this study nonetheless provides interesting insights into the likely processes of dog and reindeer domestication, and into processes of adaptation in Late Glacial foragers.


Rangifer ◽  
1986 ◽  
Vol 6 (2) ◽  
pp. 235 ◽  
Author(s):  
E. Pulliainen ◽  
P. I. Danilov ◽  
K. Heikura ◽  
E. Erkinaro ◽  
S. Sulkava ◽  
...  

The relevance of the familiar area hypothesis to the behaviour of the wild forest reindeer (Rangifer tarandus fennicus Lönnb.) was studied in a Fenno-Soviet project by radio and field tracking of these ungulates in Karelia, Northern Europe, in 1978 - 1985. This subpopulation (500 - 600 exx.) has a tradition of overwintering in a restricted area around Lake Lentua (ca. 1000 km2). The spring migration period is shorter in length than the autumn migration. The migration routes are generally the same in autumn and spring, although exceptions occur, indicating exploratory behaviour. The large winter herds disband into small groups or lone individuals for the summertime, when this subpopulation is spread over a much wider area (ca. 5400 km2). It is concluded that the observations made support the familiar area hypothesis in all essential points.


Antiquity ◽  
2003 ◽  
Vol 77 (296) ◽  
pp. 232-240 ◽  
Author(s):  
Paul G. Blackwell ◽  
Caitlin E. Buck

How and when was northern Europe reoccupied at the end of the last Ice Age? Radiocarbon dates from the earliest post-glacial contexts provide one answer: they offer a sequence in which the regions of Europe, from the Upper Rhine to Britain, saw the return of humans. The authors use Bayesian methods to model a chronology and thus arrive at a sequence with clear assessments of uncertainty.


1994 ◽  
Vol 60 (1) ◽  
pp. 75-84 ◽  
Author(s):  
Jill Cook ◽  
Roger Jacobi
Keyword(s):  

A reindeer antler object found in Northamptonshire possesses the characteristic traits of a Lyngby axe. Such implements are themselves characteristic of the Late Glacial of northern Europe but hitherto unknown in Britain. A direct radiocarbon accelerator date of 10, 320±150 BP (OxA–803) confirms the typological dating and places it amongst a small number of finds which link Britain with the Ahrensburgian phase in Europe. The function of the axe cannot be determined, but consideration of its features throws some light on this problem.


2019 ◽  
Vol 23 (2) ◽  
pp. 162-185 ◽  
Author(s):  
Livija Ivanovaitė ◽  
Kamil Serwatka ◽  
Christian Steven Hoggard ◽  
Florian Sauer ◽  
Felix Riede

The Late Glacial, that is the period from the first pronounced warming after the Last Glacial Maximum to the beginning of the Holocene (c. 16,000–11,700 cal bp), is traditionally viewed as a time when northern Europe was being recolonized and Late Palaeolithic cultures diversified. These cultures are characterized by particular artefact types, or the co-occurrence or specific relative frequencies of these. In north-eastern Europe, numerous cultures have been proposed on the basis of supposedly different tanged points. This practice of naming new cultural units based on these perceived differences has been repeatedly critiqued, but robust alternatives have rarely been offered. Here, we review the taxonomic landscape of Late Palaeolithic large tanged point cultures in eastern Europe as currently envisaged, which leads us to be cautious about the epistemological validity of many of the constituent groups. This, in turn, motivates us to investigate the key artefact class, the large tanged point, using geometric morphometric methods. Using these methods, we show that distinct groups are difficult to recognize, with major implications for our understanding of patterns and processes of culture change in this period in north-eastern Europe and perhaps elsewhere.


Antiquity ◽  
2019 ◽  
Vol 93 (367) ◽  
pp. 260-263
Author(s):  
Harry K. Robson

This three-volume publication presents an up-to-date overview on the human colonisation of Northern Europe across the Pleistocene–Holocene transition in Scandinavia, the Eastern Baltic and Great Britain. Volume 1, Ecology of early settlement in Northern Europe, is a collection of 17 articles focusing on subsistence strategies and technologies, ecology and resource availability and demography in relation to different ecological niches. It is structured according to three geographic regions, the Skagerrak-Kattegat, the Baltic Region and the North Sea/Norwegian Sea, while its temporal focus is Late Glacial and Postglacial archaeology, c. 11000–5000 cal BC. These regions are particularly interesting given the long research history, which goes back as far as the nineteenth century (see Gron & Rowley-Conwy 2018), and the numerous environmental changes that have taken place throughout the Holocene: the presence of ice until c. 7500 cal BC, isostatic rebound alongside sea-level rise and the formation of the Baltic Sea, all of which have contributed to the preservation of outstanding archaeology.


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