Fennoscandia is the key area for glacial isostatic adjustment (GIA) research. Owing to its
long settlement and excellent infrastructure, ongoing land uplift in the north as well as …

The warming at the Younger Dryas–Holocene transition (∼ 11,600 cal. BP) triggered the
rearrangement of vegetation across Europe. To better understand that response, we …

The seabed in southern Scandinavia contains numerous traces of a submerged landscape
that is thought to be the remnant of a once important habitat for Mesolithic hunter-gatherers …

THE BORDER BETWEEN THE Mesolithic and the Neolithic in Central Europe is traditionally
defined on the basis of subsistence strategy. It is the development from hunter-gatherer …

during the last one million years the land area of europe was at times 40% larger than at
present, and was usually 10-20% larger because of the global volumes of water locked up in …

According to a basic model, the formation of the coastal barriers in the southwestern Baltic
can be divided into four evolutionary stages which are characterized by different rates of sea …

Terrestrial surface waters and submarine ground water discharge (SGD) act as a source of
dissolved substances for coastal systems. Solute fluxes of SGD depend on the ground water …

The history of regional sea-level changes is critically important for building global
environmental reconstruction models and identifying major driving forces. The coastal …

The global warming at the end of the last glacial period led to a sea level rise, which induced
substantial long-term landscape changes in the southwestern Baltic Sea. During the …

Glacio-isostatic adjustment (GIA) corrected limiting non-marine and marine sea-level data
from the western Baltic Sea indicate a rapid relative sea-level (RSL) rise of 18 m for the first …