Quantification of paleotemperature changes during isotopic stage 2 in the La Draga continental sequence (NE Spain) based on the Mg/Ca ratio of freshwater ostracods
Past summer temperature changes are quantified from the La Draga sequence (Banyoles, NE Spain) during Stage 2 (24-10 ka BP), using trace-element content in lacustrine ostracod valves. The high resolution results from this new method are compared to summer paleotemperature reconstructions from sequen...
Published in: | Quaternary Science Reviews |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Pergamon-elsevier Science Ltd
1996
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Online Access: | http://hdl.handle.net/2078.1/47114 https://doi.org/10.1016/0277-3791(95)00044-5 |