Transfer functions are widely used in palaeoecology to infer past environmental conditions from fossil remains of many groups of organisms. In contrast to traditional training-set design with one observation per site, some training-sets, including those for peatland testate amoeba-hydrology transfer functions, have a clustered structure with many observations from each site. Here we show that this clustered design causes standard performance statistics to be overly optimistic. Model performance when applied to independent data sets is considerably weaker than suggested by statistical cross-validation. We discuss the reasons for these problems and describe leave-one-site-out cross-validation and the cluster bootstrap as appropriate methods f...
Proxy climate data can be obtained from reconstructions of hydrological changes on ombrotrophic (rai...
This is the author accepted manuscript. The final version is available from Wiley via the DOI in thi...
Fossil testate amoeba assemblages have been used to reconstruct peatland palaeohydrology for more th...
Transfer functions are widely used in palaeoecology to infer past environmental conditions from foss...
Transfer functions are widely used in palaeoecology to infer past environmental conditions from foss...
Transfer functions are valuable tools in palaeoecology, but their output may not always be meaningfu...
Transfer functions are now widely available to infer past environmental conditions from biotic assem...
We present a testate amoebae training set for building a paleohydrology transfer function. Ninety-on...
This is the final version of the article. Available from Elsevier via the DOI in this record.Transfe...
Testate amoebae-based transfer functions are commonly used in peatland palaeoclimate studies. These ...
Abstract: Testate amoebae are unicellular micro-organisms whose hydrological sensitivity and good pr...
In the decade since the first pan-European testate amoeba-based transfer function for peatland palae...
The melting of high-latitude permafrost peatlands is a major concern due to a potential positive fee...
Peatlands are widely exploited archives of paleoenvironmental change. We developed and compared mult...
Proxy climate data can be obtained from reconstructions of hydrological changes on ombrotrophic (rai...
This is the author accepted manuscript. The final version is available from Wiley via the DOI in thi...
Fossil testate amoeba assemblages have been used to reconstruct peatland palaeohydrology for more th...
Transfer functions are widely used in palaeoecology to infer past environmental conditions from foss...
Transfer functions are widely used in palaeoecology to infer past environmental conditions from foss...
Transfer functions are valuable tools in palaeoecology, but their output may not always be meaningfu...
Transfer functions are now widely available to infer past environmental conditions from biotic assem...
We present a testate amoebae training set for building a paleohydrology transfer function. Ninety-on...
This is the final version of the article. Available from Elsevier via the DOI in this record.Transfe...
Testate amoebae-based transfer functions are commonly used in peatland palaeoclimate studies. These ...
Abstract: Testate amoebae are unicellular micro-organisms whose hydrological sensitivity and good pr...
In the decade since the first pan-European testate amoeba-based transfer function for peatland palae...
The melting of high-latitude permafrost peatlands is a major concern due to a potential positive fee...
Peatlands are widely exploited archives of paleoenvironmental change. We developed and compared mult...
Proxy climate data can be obtained from reconstructions of hydrological changes on ombrotrophic (rai...
This is the author accepted manuscript. The final version is available from Wiley via the DOI in thi...
Fossil testate amoeba assemblages have been used to reconstruct peatland palaeohydrology for more th...