Hydrological and ecological changes in western Europe between 3200 and 2000 years BP derived from lipid biomarker delta D values in lake Meerfelder Maar sediments
JournalArticle (Originalarbeit in einer wissenschaftlichen Zeitschrift)
 
ID 4189739
Author(s) Rach, O.; Engels, S.; Kahmen, A.; Brauer, A.; Martin-Puertas, C.; van Geel, B.; Sachse, D.
Author(s) at UniBasel Kahmen, Ansgar
Year 2017
Title Hydrological and ecological changes in western Europe between 3200 and 2000 years BP derived from lipid biomarker delta D values in lake Meerfelder Maar sediments
Journal Quaternary Science Reviews
Volume 172
Pages / Article-Number 44-54
Keywords Holocene; Climate dynamics; Paleoclimatology; Western Europe; Continental biomarkers; Organic geochemistry; Stable isotopes; Vegetation dynamics
Abstract One of the most significant Late Holocene climate shifts occurred around 2800 years ago, when cooler and wetter climate conditions established in western Europe. This shift coincided with an abrupt change in regional atmospheric circulation between 2760 and 2560 cal years BP, which has been linked to a grand solar minimum with the same duration (the Homeric Minimum). We investigated the temporal sequence of hydroclimatic and vegetation changes across this interval of climatic change (Homeric climate oscillation) by using lipid biomarker stable hydrogen isotope ratios (ED values) and pollen assemblages from the annually-laminated sediment record from lake Meerfelder Maar (Germany).Over the investigated interval (3200-2000 varve years BP), terrestrial lipid biomarker ED showed a gradual trend to more negative values, consistent with the western Europe long-term climate trend of the Late Holocene. At ca. 2640 varve years BP we identified a strong increase in aquatic plants and algal remains, indicating a rapid change in the aquatic ecosystem superimposed on this long-term trend. Interestingly, this aquatic ecosystem change was accompanied by large changes in ED values of aquatic lipid biomarkers, such as nC(21) and nC(23) (by between 22 and 30%(0)). As these variations cannot solely be explained by hydroclimate changes, we suggest that these changes in the Wag value were influenced by changes in n-alkane source organisms. Our results illustrate that if ubiquitous aquatic lipid biomarkers are derived from a limited pool of organisms, changes in lake ecology can be a driving factor for variations on sedimentary lipid MN values, which then could be easily misinterpreted in terms of hydro climatic changes. (C) 2017 Elsevier Ltd. All rights reserved.
Publisher Elsevier
ISSN/ISBN 0277-3791
edoc-URL http://edoc.unibas.ch/58686/
Full Text on edoc No
Digital Object Identifier DOI 10.1016/j.quascirev.2017.07.019
ISI-Number 000411774700004
Document type (ISI) Article
 
   

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