Testate amoebae as paleoindicators of surface-moisture changes on Michigan peatlands: modern ecology and hydrological calibration

By R. Booth. 2002

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Diversity and biogeography of testate amoebae (2008, methodology): “…are considerable records of testates from the Quaternary sediments where they have been used as hydrological and acidity indicators (Charman 1997; Booth 2002; Mitchell et al. 2007), thus providing valuable evidence of Quaternary palaeoenvironmental changes and also of the ecology of extant…”
Potential implications of differential preservation of testate amoeba shells for paleoenvironmental reconstruction in peatlands (2008, background): “The existence of vertical micro-distribution of testate amoebae in the upper part of Sphagnum peatlands in response to micro-environmental gradients has long been established (Bonnet 1958; Booth 2002; Chacharonis 1954, 1956; Meisterfeld 1977; Mitchell and Gilbert 2004).”
The Variation of Testacean Assemblages (Rhizopoda) Along the Complete Base-Richness Gradient in Fens: A Case Study from the Western Carpathians (2006, background): “(Hendon et al. 2001, Booth 2002, Schnitchen et al. 2003, Davis and Wilkinson 2004, Caseldine and Gearey 2005) and also as recent indicators of hydrological changes during restoration or ongoing climate change (Jauhiainen 2002, Kishaba and Mitchell 2005, Schoning et al. 2005).”