Pollen and plant macrofossil analysis
Pollen analysis examines fossil sporomorphs. Pollen grains contain the male germ cells of plants. They are passively transmitted to the female flower by wind or insects. The protective outer exine is resistant to mechanical and chemical influences. In suitable deposits (e.g., in lake sediments or in bogs), they are embedded and do not decay due to the absence of atmospheric oxygen. Through drilling, samples are obtained and chemically processed in the laboratory. The pollen-enriched residue is analyzed under the microscope. Based on the shape of the fossil pollen grains, an identification to certain plants can be made (usually at genus level, more rarely up to the species level). Using pollen diagrams, quantitative changes in vegetation composition over time can be shown (Fig.2).
The analysis of plant macrofossil remains focuses on the identification of fruits and seeds as well as leaves and wood. Frequently, an identification up to the species level is possible. However, plant macrofossil remains are less common than pollen in corresponding deposits. Moreover, the environmental conditions in lakes and bogs often only detect residues of aquatic and marsh plants. In contrast to the pollen analysis, it is thus possible to gain an insight into the local vegetation. A combination of both methods is therefore useful for the paleoecological or paleoclimate interpretation.
Selected Literature:
https://doi.org/10.1016/j.quascirev.2018.03.029
https://doi.org/10.1016/j.quascirev.2009.03.002
https://doi.org/10.1016/j.quascirev.2012.06.012
https://doi.org/10.1016/j.quascirev.2014.03.017
https://doi.org/10.1111/j.1502-3885.2009.00096.x
https://doi.org/10.1016/j.quascirev.2016.11.013
https://doi.org/10.5194/cp-12-575-2016
https://doi.org/10.1016/j.quascirev.2019.04.033
https://doi.org/10.1016/j.palaeo.2015.06.015
https://doi.org/10.5194/cp-11-1491-2015
https://doi.org/10.5194/cp-13-689-2017
https://doi.org/10.1007/s00334-017-0658-3