Three pollen diagrams from the Peel peatlands, a raised bog area in the southern part of The Netherlands reveal the post-Boreal vegetation history of that region. There are two or three land-occupation phases in the Neolithic and Bronze ages, that show but low values of terrestrial herbs. They are negatively correlated with Ulmus. The Fagus curve starts slightly below the first occupation phase at around 2500 B.C. In the Subatlantic there is an Iron age and a Medieval occupation phase with higher values of terrestrial herbs. Fagus shows two maxima, one at the beginning of our era and another at around 700 A.D. The trend of the pollen curves for bog species is discussed in relation to bog development
AbstractThe infill of an abandoned branch of the small river Vlootbeek, a tributary of the Meuse, re...
A Late Glacial - Holocene sequence from the Bisoca peat bog (Buzăului Subcarpathians) was studied fr...
Pollen data are well established for quantitative climate reconstructions over long timescales, incl...
In the Monnikenberg estate, built in the mid-19th century in a Pleistocene coversand area to the sou...
We studied twelve late Holocene organic deposits in West-Frisia, The Netherlands. Pollen, spores, no...
ABSTRACT: It is concluded from the uneven distribution of megalith graves (hunebedden) and the prese...
The evolution of heathlands during the Holocene has been registered in various soil records. Paleoec...
The Noordoostpolder is an archaeologically rich area in the central Netherlands. A sediment profile,...
We studied a Holocene peat fill of a small depression in Pleistocene coversand, in the western borde...
Understanding the ecohydrological responses of peatlands to climate change is particularly challengi...
A pollen diagram from the Ahlequellmoor in the Solling area shows the history of vegetation and sett...
Quantified analyses of plant macrofossil remains have been made from three profiles of peat from rai...
Plant macrofossil remains have been analysed from two raised peat bogs in northern Germany and Denma...
We determined the effects of climate change and human activities on the species composition of ombro...
Interdisciplinary, landscape-oriented studies from an archaeological viewpoint in the Low Countries ...
AbstractThe infill of an abandoned branch of the small river Vlootbeek, a tributary of the Meuse, re...
A Late Glacial - Holocene sequence from the Bisoca peat bog (Buzăului Subcarpathians) was studied fr...
Pollen data are well established for quantitative climate reconstructions over long timescales, incl...
In the Monnikenberg estate, built in the mid-19th century in a Pleistocene coversand area to the sou...
We studied twelve late Holocene organic deposits in West-Frisia, The Netherlands. Pollen, spores, no...
ABSTRACT: It is concluded from the uneven distribution of megalith graves (hunebedden) and the prese...
The evolution of heathlands during the Holocene has been registered in various soil records. Paleoec...
The Noordoostpolder is an archaeologically rich area in the central Netherlands. A sediment profile,...
We studied a Holocene peat fill of a small depression in Pleistocene coversand, in the western borde...
Understanding the ecohydrological responses of peatlands to climate change is particularly challengi...
A pollen diagram from the Ahlequellmoor in the Solling area shows the history of vegetation and sett...
Quantified analyses of plant macrofossil remains have been made from three profiles of peat from rai...
Plant macrofossil remains have been analysed from two raised peat bogs in northern Germany and Denma...
We determined the effects of climate change and human activities on the species composition of ombro...
Interdisciplinary, landscape-oriented studies from an archaeological viewpoint in the Low Countries ...
AbstractThe infill of an abandoned branch of the small river Vlootbeek, a tributary of the Meuse, re...
A Late Glacial - Holocene sequence from the Bisoca peat bog (Buzăului Subcarpathians) was studied fr...
Pollen data are well established for quantitative climate reconstructions over long timescales, incl...