Forgotten Times and Spaces: New Perspectives in Paleoanthropological, Paleoetnological and Archeological Studies. 2015
DOI: 10.5817/cz.muni.m210-7781-2015-27
|View full text |Cite
|
Sign up to set email alerts
|

Darkness under candlestick: glacial refugia on mountain glaciers

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
1
1

Citation Types

0
6
0

Year Published

2017
2017
2022
2022

Publication Types

Select...
6

Relationship

1
5

Authors

Journals

citations
Cited by 7 publications
(6 citation statements)
references
References 10 publications
0
6
0
Order By: Relevance
“…In the mountains of north‐western Slovakia, Picea (<13.3%), Corylus (<5.6%), Alnus (<15%), Fagus (<1.9%) and Tilia (<1.6%) were more abundant in comparison with the south, but Quercus (<6.3%) and Ulmus (<3%) occurred as well. Although in view of the records from the more southern parts of the Pannonian lowlands (Sümegi, Magyari, Dániel, Molnár, & Törőcsik, ), the Late Glacial occurrence of temperate trees in south‐western Slovakia was anticipated, reports from colder mountains in north‐western Slovakia may seem surprising (but see Horáček et al., ). This mountain region, however, showed rather high precipitation distributed equally throughout the year during the LGM, without temperature extremes that would have suppressed temperate species (Bhagwat & Willis, ).…”
Section: Discussionmentioning
confidence: 99%
See 1 more Smart Citation
“…In the mountains of north‐western Slovakia, Picea (<13.3%), Corylus (<5.6%), Alnus (<15%), Fagus (<1.9%) and Tilia (<1.6%) were more abundant in comparison with the south, but Quercus (<6.3%) and Ulmus (<3%) occurred as well. Although in view of the records from the more southern parts of the Pannonian lowlands (Sümegi, Magyari, Dániel, Molnár, & Törőcsik, ), the Late Glacial occurrence of temperate trees in south‐western Slovakia was anticipated, reports from colder mountains in north‐western Slovakia may seem surprising (but see Horáček et al., ). This mountain region, however, showed rather high precipitation distributed equally throughout the year during the LGM, without temperature extremes that would have suppressed temperate species (Bhagwat & Willis, ).…”
Section: Discussionmentioning
confidence: 99%
“…The co‐occurrence of contrasting biogeographical elements in the region may be explained by the presence of different types of glacial and post‐glacial refugia. Northernmost populations of warm‐temperate forest species may reflect glacial northern micro‐refugia (Horáček, Ložek, Knitlová, & Juřičková, ; Juřičková, Horáčková, & Ložek, ; Willner et al., ). Isolated southern and western populations of arctic, boreal and/or continental species may reflect post‐glacial refugia of glacial tundra (Kliment, Šibíková, & Šibík, ), steppe‐tundra (Horsák et al., ) or forest‐steppe (Feurdean et al., ; Kuneš et al., ).…”
Section: Introductionmentioning
confidence: 99%
“…The LGM is known to have had a profound effect on the biogeography of many animal and plant species [ 111 , 112 ] as well as on human populations in the Upper Palaeolithic, which resulted in population movements across the continent [ 3 ]. Traditionally, the environmental deterioration during the LGM has been linked to an abandonment of Central and Northern Europe.…”
Section: Discussionmentioning
confidence: 99%
“…It obviously represents a paleoendemite element of minute dispersal capacity, closely adapted to the specific conditions characterizing its Recent range, which most probably were locally available in the Alps throughout glacial times similarly as it was obviously the case of the High Tatra Mts. [ 85 ]. The remaing clade of European Apodemus (A .…”
Section: Discussionmentioning
confidence: 99%