Peat cores from boreal bog and fen sites in the Hudson Bay Lowlands of Northern Ontario,
Canada, were analysed to calculate Holocene carbon accumulation rates, and to show how …

Abstract The Hudson Bay Lowlands (HBL) stores a significant proportion of the northern
peatland carbon pool, and constraints on the factors controlling local‐scale variation are …

Testate amoebae are abundant in the surface layers of northern peatlands. Analysis of their
fossilized shell (test) assemblages allows for reconstructions of local water‐table depths …

Testate amoebae have been used widely as a proxy of hydrological change in ombrotrophic
peatlands, although their response to abiotic controls in other types of mire and fenland …

Peatlands in northern Ontario, Canada, archive multiple biological indicators, including
macrofossils, algae, testate amoebae, and pollen. These proxies can provide insights …

Testate amoeba-derived transfer functions are frequently used in peatland
palaeohydrological studies and involve the development of training sets from surficial peats …

An environmental proxy routinely used in paleoecological studies of peatlands is testate
amoebae, which are used to infer successional and hydrological shifts through time …

Testate amoebae that inhabit peat are sensitive indicators of water table position. In this
study, we used testate amoebae in sediments from a mire in the western Alps (Lac du Thyl) …

Peatland testate amoebae are sensitive indicators of local hydrology and have been used
as proxies for surface moisture conditions in fossil studies. However, few regional calibration …

Subfossil remains of various groups of organisms preserved in peat and sediment archives
are commonly used to infer past environmental changes using transfer functions based on …