Paleolimnology

Paleolimnology (Greek: paleon=old, limne=lake, logos=study) is a scientific subdiscipline closely related to both limnology and paleoecology. Palaeolimnological studies are concerned with reconstructing the paleoenvironments of inland waters (lakes and streams; freshwater, brackish, or saline) – and especially changes associated with such events as climatic change, human impacts (e.g., eutrophication, or acidification), and internal ontogenic processes.

Paleolimnological studies are commonly based on meticulous analyses of sediment cores, including the physical, chemical and mineralogical properties of sediments, and diverse biological records (e.g., fossil diatoms, cladocera, ostracodes, molluscs, pollen, pigments, or chironomids). One of the primary sources for recent paleolimnological research is the Journal of Paleolimnology.

Most early paleolimnological studies focused especially on the biological productivity of lakes, and the role of internal lake processes in directing lake development. Although Einar Naumann had speculated that the productivity of lakes should gradually decrease due to leaching of catchment soils, August Thienemann suggested that the reverse process likely occurred. Early midge records seemed to support Thienemann's view.

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