Modern analog technique, often abbreviated as MAT, is a popular type of transfer function used in paleoceanography to reconstruct past ocean properties from the composition of fossil assemblages extracted from deep-sea sediments. In the vast majority of cases, MAT is applied to reconstruct past sea-surface temperature from remains of marine unicellular microplankton such as planktonic foraminifera, radiolaria, diatoms, and dinoflagellates.
The method has been introduced to paleoceanography by Hutson (1980). Mathematically, it is akin to k-nearest neighbor regression. Its procedure is computationally and conceptually very simple. First, a similarity coefficient is calculated between the composition of a fossil assemblage in a geological sample and the compositions of corresponding assemblages in a “calibration dataset” of surface-sediment samples. Then, the surface-sediment samples are sorted by their similarity coefficient, and a subset of those with most similar assemblages, termed...
Bibliography
Hutson, W. H., 1980. The Agulhas current during the late Pleistocene: analysis of modern faunal analogs. Science, 207, 64–66.
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Kucera, M. (2015). Modern Analog Techniques. In: Harff, J., Meschede, M., Petersen, S., Thiede, J. (eds) Encyclopedia of Marine Geosciences. Springer, Dordrecht. https://doi.org/10.1007/978-94-007-6644-0_77-3
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DOI: https://doi.org/10.1007/978-94-007-6644-0_77-3
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Modern Analog Techniques- Published:
- 09 February 2015
DOI: https://doi.org/10.1007/978-94-007-6644-0_77-3
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Modern Analog Techniques- Published:
- 12 February 2014
DOI: https://doi.org/10.1007/978-94-007-6644-0_77-2