Abstract:HOOGENRAAD (1935) has given a survey of the rhizopad associations of several Sphagnetae of the Netherlands and a comparison with some populations from diverse localities in Europe, He based his analysis upon the three types distinguished by HARNISCH (1929) 3. Nebela carinata proved not to be restricted to one of HARNISCH's types but can be found in all three types; the absence in many associations is probably connected with its dependence of the humidity of the medium; it can be expected only in constantly we… Show more
“…It is notable that the most extreme deviant sample came from a site affected by A surprising feature of the species data is the number of species in common with peatland faunas in the Northern Hemisphere. This cosmopolitanism has been commented on before but the proportion of the fauna which is found in both New Zealand and northern peatlands is still more than would have been expected (Hoogenraad & de Groot 1979). As a result the individual species optima can be compared with those reported from similar studies on northern peatlands.…”
Research in the Northern Hemisphere shows the principal control on species distribution and abundance of testate amoebae to be local hydrology, which in ombrotrophic mires is linked directly to climate Fossil faunas can therefore be used to infer past hydrological and climatic conditions This study investigates whether a similar relationship can be found for New Zealand peatlands, as a first step towards developing a method for palaeomoisture reconstructions Fifty-seven samples from 13 peatlands were analysed for testate amoebae and related to site hydrology, pH and conductivity of mire waters, climate, and vegetation type using canonical correspondence analysis (CCA) Water table and soil moisture were the dominant factors, and their relationship with species assemblage was modelled using four transfer functions weighted averaging (WA), tolerance downweighted weighted averaging (WA-Tol), partial least squares (PLS), and weighted average partial least squares (WA-PLS) PLS and WA-PLS performed best, and suggest that palaeohydrology could be accurately inferred from fossil faunas Results are contrasted with those found in the northern peatlands
“…It is notable that the most extreme deviant sample came from a site affected by A surprising feature of the species data is the number of species in common with peatland faunas in the Northern Hemisphere. This cosmopolitanism has been commented on before but the proportion of the fauna which is found in both New Zealand and northern peatlands is still more than would have been expected (Hoogenraad & de Groot 1979). As a result the individual species optima can be compared with those reported from similar studies on northern peatlands.…”
Research in the Northern Hemisphere shows the principal control on species distribution and abundance of testate amoebae to be local hydrology, which in ombrotrophic mires is linked directly to climate Fossil faunas can therefore be used to infer past hydrological and climatic conditions This study investigates whether a similar relationship can be found for New Zealand peatlands, as a first step towards developing a method for palaeomoisture reconstructions Fifty-seven samples from 13 peatlands were analysed for testate amoebae and related to site hydrology, pH and conductivity of mire waters, climate, and vegetation type using canonical correspondence analysis (CCA) Water table and soil moisture were the dominant factors, and their relationship with species assemblage was modelled using four transfer functions weighted averaging (WA), tolerance downweighted weighted averaging (WA-Tol), partial least squares (PLS), and weighted average partial least squares (WA-PLS) PLS and WA-PLS performed best, and suggest that palaeohydrology could be accurately inferred from fossil faunas Results are contrasted with those found in the northern peatlands
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