Botanical-climatological transfer function for the reconstruction of the paleoclimate
The climate indicator-species method is based on observations of current geobotany, according to which recent distribution areas or area limits of selected plant species may depend on specific climate parameters. These relationships are transferred to the past by using fossil pollen and plant macroremains. In the meantime, classical methods have been substantially extended and modified by computer-aided statistical methods.
The so-called pdf method (pdf – probability density function) uses reconstruction-related probability density functions, whereby a high-resolution global climatology with distribution areas of the plant species are linked. The statistical approach provides a most probable climate by combining (multiplying) the pdfs of several species occurring together in a fossil pollen and/or macro sample.
![Abb. 1_Carpinus_pdf_aglitt_aglitt_.jpg](https://www.paleontology.uni-bonn.de/de/medien-inhalte/arbeitsgruppen/palaeobotanik/palaeobotanik_tlitt/abb-1_carpinus_pdf.jpg/@@images/image)
![Abb. 2 Transfer function_aglitt_aglitt_.jpg](https://www.paleontology.uni-bonn.de/de/medien-inhalte/arbeitsgruppen/palaeobotanik/palaeobotanik_tlitt/abb-2-transfer-function.jpg/@@images/image)
Literature:
https://doi.org/10.1007/s00382-007-0299-9
https://doi.org/10.1016/j.quascirev.2007.10.004
https://doi.org/10.1006/qres.2002.2380
https://doi.org/10.1111/j.1502-3885.2009.00096.x
https://doi.org/10.1016/j.quascirev.2019.04.033
https://doi.org/10.1007/s00334-006-0046-x