Food availability and temperature optima shaped functional composition of chironomid assemblages during the Late Glacial–Holocene transition in Northern Europe

2021 ◽  
Vol 266 ◽  
pp. 107083
Author(s):  
Normunds Stivrins ◽  
Simon Belle ◽  
Liva Trasune ◽  
Ansis Blaus ◽  
Sakari Salonen
Human Ecology ◽  
2018 ◽  
Vol 46 (5) ◽  
pp. 621-632 ◽  
Author(s):  
Felix Riede ◽  
Jesper B. Pedersen

1987 ◽  
Vol 27 (1) ◽  
pp. 89-102 ◽  
Author(s):  
Ian R. Walker ◽  
Rolf W. Mathewes

AbstractChironomid (midge) remains analyzed from an 8.95-m-long sediment core from Marion Lake reveal successional changes over the last 12,000 yr since deglaciation. A late-glacial Heterotrissocladius-dominated association characterizes the earliest sediments. Succeeding this community, at the onset of the Holocene, is a Tanytarsini-dominated assemblage. The transition between these communities occurs during a time of rapid climatic amelioration, preceding an early Holocene xerothermic interval. The late-glacial fossil fauna is suggestive of more northerly affinities. Similar sequences have been reported in late-glacial lake sediments elsewhere in North America and in Europe. The composite picture of these chironomid assemblages suggests the gradual retreat of a formerly widely distributed, cold stenothermous fauna. The response of the chironomid community accords well with paleoclimatic inferences based on pollen data at the lake. Subsequent postglacial changes are less pronounced and most are probably attributable to the gradual shallowing of the basin. Chironomid remains from shallow, weakly stratified lakes may yield valuable paleoclimatological data.


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.


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