Climate warming and vegetation response after Heinrich event 1 (16 700–16 000 cal yr BP) in Europe south of the Alps

Chironomids preserved in a sediment core from Lago di Origlio (416 m a.s.l.), a lake in the foreland of the Southern Swiss Alps, allowed quantitative reconstruction of Late Glacial and Early Holocene summer temperatures using a combined Swiss–Norwegian temperature inference model based on chironomid...

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Bibliographic Details
Main Authors: W. Tinner, A. F. Lotter, O. Heiri, S. Samartin
Format: Article
Language:English
Published: Copernicus Publications 2012-11-01
Series:Climate of the Past
Online Access:http://www.clim-past.net/8/1913/2012/cp-8-1913-2012.pdf

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