Apollen core is a core sample of a medium containing a stratigraphic sequence of pollen. Analysis of the type and frequency of the pollen in each layer is used to study changes in climate or land use using regional vegetation as a proxy.[1][2] This analysis is conceptually comparable to the study of ice cores.
Cores are obtained from deposits where pollen is likely to have been trapped. Cores are generally obtained from lacustrine sediments and peat bogs although soil sediments may also be obtained. Degradation of the pollen exine and bioturbation may reduce the quality of the pollen grains and stratigraphy of the core so researchers frequently select locations where the sediments are under anaerobic conditions.
The cores are then subjected to pollen analysisbypalynologists who are able to infer the proportions of major plant types from the concentrations of different pollen types found in the cores.
There are a number of tools used for coring, often with specialized uses:
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