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Climate variability and associated vegetation response throughout Central and Eastern Europe (CEE) between 60 and 8 ka
Records of past climate variability and associated vegetation response exist in various
regions throughout Central and Eastern Europe (CEE). To date, there has been no coherent …
regions throughout Central and Eastern Europe (CEE). To date, there has been no coherent …
12,000-Years of fire regime drivers in the lowlands of Transylvania (Central-Eastern Europe): a data-model approach
The usefulness of sedimentary charcoal records to document centennial to millennial scale
trends in aspects of fire regimes (frequency, severity) is widely acknowledged, yet the long …
trends in aspects of fire regimes (frequency, severity) is widely acknowledged, yet the long …
Late Pleniglacial vegetation in eastern-central Europe: are there modern analogues in Siberia?
Abstract To characterize Late Pleniglacial (LPG: 26.5–15 ka cal BP) and particularly Last
Glacial Maximum (LGM: 21±2 ka cal BP) vegetation and climate, fossil pollen assemblages …
Glacial Maximum (LGM: 21±2 ka cal BP) vegetation and climate, fossil pollen assemblages …
Chironomid-inferred Holocene temperature changes in the South Carpathians (Romania)
We present a Holocene summer air temperature reconstruction based on fossil chironomids
from Lake Brazi (1740 masl), a shallow mountain lake in the South Carpathians. Summer air …
from Lake Brazi (1740 masl), a shallow mountain lake in the South Carpathians. Summer air …
[HTML][HTML] Lipid biomarker (brGDGT)-and pollen-based reconstruction of temperature change during the Middle to Late Holocene transition in the Carpathians
To reconstruct changes in vegetation, temperature, and sediment geochemistry through the
last 6.5 cal ka BP, in the Subcarpathian belt of the Eastern Carpathians (Romania), pollen …
last 6.5 cal ka BP, in the Subcarpathian belt of the Eastern Carpathians (Romania), pollen …
[HTML][HTML] The transformation of the forest steppe in the lower Danube Plain of southeastern Europe: 6000 years of vegetation and land use dynamics
Forest steppes are dynamic ecosystems, highly susceptible to changes in climate,
disturbances and land use. Here we examine the Holocene history of the European forest …
disturbances and land use. Here we examine the Holocene history of the European forest …
Millennial scale climate oscillations recorded in the Lower Danube loess over the last glacial period
In this study we provide a correlative age model for last glacial loess at the Rasova-Valea cu
Pietre site in the Lower Danube region, based on the correlation of palaeoenvironmental …
Pietre site in the Lower Danube region, based on the correlation of palaeoenvironmental …
Vegetation and environmental responses to climate forcing during the Last Glacial Maximum and deglaciation in the East Carpathians: attenuated response to …
Abstract The Carpathian Mountains were one of the main mountain reserves of the boreal
and cool temperate flora during the Last Glacial Maximum (LGM) in East-Central Europe …
and cool temperate flora during the Last Glacial Maximum (LGM) in East-Central Europe …
Trends in biomass burning in the Carpathian region over the last 15,000 years
Fire is recognized as a critical process with significant impacts on biota and the atmosphere.
In this study, 11 micro-and macrocharcoal sedimentary records extracted from peat bogs …
In this study, 11 micro-and macrocharcoal sedimentary records extracted from peat bogs …
Late Glacial and Holocene paleoenvironmental records in the Tatra Mountains, East-Central Europe, based on lake, peat bog and colluvial sedimentary data: A …
Abstract The Tatra Mountains are the highest massif in the Carpathian mountain arc (2655
m) and represent a typical alpine landscape developed in the course of Pleistocene …
m) and represent a typical alpine landscape developed in the course of Pleistocene …