Anthropogenic pollen indicators in pollen records are an established tool for reconstructing
the history of human impacts on vegetation and landscapes. They are also used to …

Northern peatlands store globally-important amounts of carbon in the form of partly
decomposed plant detritus. Drying associated with climate and land-use change may lead to …

Minerotrophic fens and ombrotrophic bogs differ in their nutrient status, hydrology,
vegetation and carbon dynamics, and their geographical distribution is linked to various …

In contrast to marked climate change across glacial-interglacial cycles, the Holocene epoch
represents a relatively warm, stable interval. However, on finer temporal scales, it too has …

Holocene peatland development and associated carbon (C) dynamics were reconstructed
for a southern boreal Finnish peatland complex with fen and bog areas. In order to assess …

Data on past peatland growth patterns, vegetation development, and carbon (C) dynamics
during the various Holocene climate phases may help us to understand possible future …

Fire is a critical component of many ecosystems and, as predicted by various climate
models, fire activity may increase significantly in the following years due to climate change …

The aim of this study is to assess the impact of biotic and abiotic factors on peatland
formation in the Central Sudetes (central Europe) during the late Holocene. The research …

The coastal ridge–swale systems in the west Estonian archipelago (Röögu, Lõimastu) and
on the northern coast (Juminda), where wave and wind-built ridges are separated from each …

Fires in forested raised bogs occur both as a result of natural processes and as a result of
human activity. Although there is a generally accepted opinion that their impact on …