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Conference Paper

Late-Glacial/Holocene changes of the climatic and trophic conditions in three Eifel maar lakes, as indicated by faunal remains. 2. Chironomidae (Diptera)

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http://pubman.mpdl.mpg.de/cone/persons/resource/persons56734

Hofmann,  Wolfgang
Department Ecophysiology, Max Planck Institute for Limnology, Max Planck Institute for Evolutionary Biology, Max Planck Society;

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Citation

Hofmann, W. (1993). Late-Glacial/Holocene changes of the climatic and trophic conditions in three Eifel maar lakes, as indicated by faunal remains. 2. Chironomidae (Diptera). In J. F. W. Negendank, & B. Zolitschka (Eds.), Paleolimnology of European Maar Lakes (pp. 421-433). Berlin: Springer.


Cite as: http://hdl.handle.net/11858/00-001M-0000-000F-E42E-A
Abstract
Differences in the structure of the chironomid faunas between the oligotrophic Weinfelder Maar and the eutrophic Schalkenmehrener Maar and Holzmaar existed since the beginning of the Holocene. The eutrophic maar lakes passed through a period of strong eutrophication in the Atlantic period. In the Weinfelder Maar, a decrease of Micropsectra indicated a higher trophic state in the early Subatlantic