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The Quaternary covers the last 2.5 million years in Earth's
history. This unique period is well known for a record of
oscillating climatic parameters. Fluctuating climates are reflected
in peatbog profiles. Paleoecological studies using plant
macrofossils, like bryophyte remains, have an important role in the
reconstruction of past hydrological changes in lakes and peatbogs.
Plant macrofossil analysis has been used most frequently in the
oceanic regions of Europe, where the moisture gradient is reflected
clearly in different Sphagnum taxa. This book discusses research in
regard to the paleoecology of peatlands, with a particular emphasis
placed on Hungary.
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