Tag Archives: Samartin et al (2017)

Chironomid vs pollen: Holocene climate change in southern Europe

Pollen-inferred summer temperature reconstruction from southern Europe show a cool early Holocene summers and a warmer late Holocene summer (Davis et al 2003, Mauri et al 2015). In contrast,  warm early Holocene summers are reconstructed elsewhere in Europe and most … Continue reading

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