2008
DOI: 10.1016/j.palaeo.2008.09.008
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Late quaternary vegetation and hydrological change at Ljubljansko barje (Slovenia)

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Cited by 24 publications
(21 citation statements)
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“…GI-1e presents a rapid rise in temperature, observed regionally in Slovenia and Romania, whilst GI-1d is seen as relatively stable with a warmer and drier environment at Lake Bled from 13.8ka cal BP onwards (Feurdean et al, 2014). At Lake Ljubljana in Slovenia, groundcover was composed of open mixed pine and birch (Betula) woodland (Andrič et al, 2008). In and around the Great Adriatic Plain, multiple proxies including plant pollen and macrofossils, sedimentology, and molluscs from Lake Vrana and Valun Bay on the isle of Cres suggest open grassland vegetation in the late glacial (Schmidt et al, 2000).…”
Section: Gi-1 (Bølling-allerød; 14642±186 To 12846±138 Cal Bp)mentioning
confidence: 98%
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“…GI-1e presents a rapid rise in temperature, observed regionally in Slovenia and Romania, whilst GI-1d is seen as relatively stable with a warmer and drier environment at Lake Bled from 13.8ka cal BP onwards (Feurdean et al, 2014). At Lake Ljubljana in Slovenia, groundcover was composed of open mixed pine and birch (Betula) woodland (Andrič et al, 2008). In and around the Great Adriatic Plain, multiple proxies including plant pollen and macrofossils, sedimentology, and molluscs from Lake Vrana and Valun Bay on the isle of Cres suggest open grassland vegetation in the late glacial (Schmidt et al, 2000).…”
Section: Gi-1 (Bølling-allerød; 14642±186 To 12846±138 Cal Bp)mentioning
confidence: 98%
“…The climate of the eastern Adriatic was mild and wet, near present-day conditions, by around 9,000 cal BP (Rossignol-Strick, 1999), with evidence for an increase in local humidity at the end of the Boreal (Andrič et al, 2008). Conditions were still warm-temperate and perhaps less variable, with winter temperatures only ranging from -2°C to 5°C (Peyron et al, 1998).…”
Section: Earlymentioning
confidence: 99%
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“…The Istrian Peninsula of Croatia has a diverse topography and coastline, unique environmental history, and is a “crossroads” location between Europe and Southwest Asia. Based on regional records, the terminal Pleistocene Bølling-Allerød interstadial (14,600–12,900 BP) was characterized by a sustained rise in temperatures and increased water availability, leading to the spread of forest into upland areas from refugial populations located on lower slopes in Istria and the surrounding area [ 14 , 39 42 ]. The Younger Dryas (12,900–11,500) was cool and dry, and grassland and open shrubland were the dominant groundcover [ 42 45 ].…”
Section: Introductionmentioning
confidence: 99%