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 …

Peatlands are ecosystems of exceptional conservation value because of their beauty,
biodiversity, importance in global geochemical cycles, and the paleoenvironmental records …

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 …

Testate amoebae are an abundant and diverse polyphyletic group of shelled protozoa living
in aquatic to moist habitats ranging from estuaries to lakes, rivers, wetlands, soils, litter, and …

Salt-marsh foraminifera have been used to reconstruct Holocene sea-level changes from
coastlines around the world. In this work, we compile the results of surface foraminiferal …

The use of testate amoebae in studies of peatland hydrology and palaeohydrology has been
increasing, and considerable efforts have been made over the past decade to standardise …

Late Quaternary Environmental Change addresses the interaction between human agency
and other environmental factors in the landscapes, particularly of the temperate zone …

Proxies such as plant macrofossils, humification indices and testate amoebae have been
developed to reconstruct past hydrological variability in ombrotrophic peatlands …

We studied the relationship between testate amoebae (Protozoa) communities and the
depth to the water table (DWT), pH, conductivity, and microhabitat type in Sphagnum …

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 …