Fundamental insight into the long-term 'geoecohydrological'dynamics of rivers and
floodplains is required for their sustainable management. To study these dynamics, a multi …

Numerous palaeoecological studies have used testate amoeba analysis to reconstruct
Holocene hydrological change in peatlands, and thereby past climatic change. Current …

Proxies that use changes in the composition of ecological communities to reconstruct
temporal changes in an environmental covariate are commonly used in paleoclimatology …

This thesis represents the first attempt to use quantitative testate amoebae (Protozoa:
Rhizopoda) analysis to measure hydrological fluctuations in British peatbogs over the …

Testate amoebae (Protozoa: Rhizopoda) are particularly abundant in peatlands. Previous
studies have used testate amoebae in palaeoenvironmental studies, but have used …

In the decade since the first pan-European testate amoeba-based transfer function for
peatland palaeohydrological reconstruction was published, a vast amount of additional data …

Peatlands offer the potential for high resolution records of water balance over Holocene
timescales, yet this potential is under-exploited in many areas of the world. Within Europe …

Testate amoebae-based transfer functions are commonly used in peatland palaeoclimate
studies. These models have been developed in several regions of the world and are …

Testate amoebae are a frequently used palaeoecological proxy for reconstructing changes
in palaeohydrological conditions, particularly in studies of Sphagnum-dominated peatlands …

Testate amoebae are common proxy for water table depth in peatlands and are commonly
used to reconstruct past hydroclimatic conditions. In northeastern America, previous transfer …