Peat, especially from acidic mires (bogs), is a natural archive of past environmental change.
Reconstructions of past climate from bogs commenced in the 19th Century through …

Reconstruction of hydroclimate variability is an important part of understanding natural
climate change on decadal to millennial timescales. Peatland records reconstruct 'bog …

This third edition of Reconstructing Quaternary Environments has been completely revised
and updated to provide a new account of the history and scale of environmental changes …

Peat humification or decomposition is a frequently used proxy to extract past time changes in
hydrology and climate from peat bogs. During the past century several methods to determine …

The peat sequence at Hani in northeastern China accumulated over the past 16calkyr in a
percolation mire in which rain water and ground water seeped through the peat system. The …

Testate amoebae are increasingly used in ecological and palaeoecological studies of
wetlands. To characterise the amoeba community a certain number of individuals need to be …

Calibration data sets give a unique opportunity to establish patterns of biological existence
and their statistical associations with environmental variables. By use of calibration data …

Based on paleoclimatic reconstructions using various proxies, the Holocene Climate
Optimum (10.5–6ka) has been characterized as a warmer and wetter period in most of East …

We assessed the vulnerability of blanket peat to climate change in Great Britain using an
ensemble of 8 bioclimatic envelope models. We used 4 published models that ranged from …

Mid-to-late Holocene high-resolution testate amoebae-derived water table reconstructions
from two peatlands in the North of Ireland are presented. The proxy climate records are …