The Lateglacial and Early Holocene are key periods with respect to the understanding of the present-day vegetation and environment. An interdisciplinary approach is important for the study of these changes. Only by interlinking biological and geoscience evidence can we obtain a more comprehensive picture of this key period. It is not possible to interpret any pollen spectrum in the sedimentary record without knowledge of the history of the locality and its vicinity. Rapid climate changes had a crucial effect on the environment and vegetation. Continentality of the climate and a deficit of precipitation amplify the effect of local conditions. Vegetation, as in the case of vertebrates and molluscs, comprises a combination of species of a cont...
Palaeopalynological analysis of two organic Quaternary deposits revealed that plant community of tai...
Quaternary climate variability strongly affected ecosystems and vegetation. Climatic oscillations be...
The remains from a sub-fossil pine forest burried in layers of peat deposits at the northern edge of...
The Hercynian mountain ranges were islands of mountain glaciation and alpine tundra in a Central Eur...
Conclusions The main conclusions, specific to each research topic, have been mentioned in appropriat...
The Danubian Plain is nothern part of the Pannonian Plain and in terms of palaeobotanical research i...
In the sense of postglacial vegetation development, western Bohemia represents one of the least stud...
Basics and principles of vegetation history reconstruction since the Last Glacial Maximum During th...
While general trends in Central European postglacial recolonisation dynamics are relatively well kno...
<p>Alarming predictions and contrasting results regarding species loss consequence of climate change...
Palaeoecological, palaeohydrological, and paleoenvironmental reconstruction of the Late Glacial and ...
Some examples of postglacial and modern European vegetation are presented as starting points for a d...
The Carpathian Mountains are great range in Europe. This rewiew is target to identify main evolution...
The study of past environments, their ecology, and detailed changes through time has become an impor...
This paper combines complex archaeological records from excavations of sandstone rockshelters with p...
Palaeopalynological analysis of two organic Quaternary deposits revealed that plant community of tai...
Quaternary climate variability strongly affected ecosystems and vegetation. Climatic oscillations be...
The remains from a sub-fossil pine forest burried in layers of peat deposits at the northern edge of...
The Hercynian mountain ranges were islands of mountain glaciation and alpine tundra in a Central Eur...
Conclusions The main conclusions, specific to each research topic, have been mentioned in appropriat...
The Danubian Plain is nothern part of the Pannonian Plain and in terms of palaeobotanical research i...
In the sense of postglacial vegetation development, western Bohemia represents one of the least stud...
Basics and principles of vegetation history reconstruction since the Last Glacial Maximum During th...
While general trends in Central European postglacial recolonisation dynamics are relatively well kno...
<p>Alarming predictions and contrasting results regarding species loss consequence of climate change...
Palaeoecological, palaeohydrological, and paleoenvironmental reconstruction of the Late Glacial and ...
Some examples of postglacial and modern European vegetation are presented as starting points for a d...
The Carpathian Mountains are great range in Europe. This rewiew is target to identify main evolution...
The study of past environments, their ecology, and detailed changes through time has become an impor...
This paper combines complex archaeological records from excavations of sandstone rockshelters with p...
Palaeopalynological analysis of two organic Quaternary deposits revealed that plant community of tai...
Quaternary climate variability strongly affected ecosystems and vegetation. Climatic oscillations be...
The remains from a sub-fossil pine forest burried in layers of peat deposits at the northern edge of...