Floral evidence for high summer temperatures in southern Scandinavia during 15-11 cal ka BP

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Schenk , F , Bennike , O , Valiranta , M , Avery , R , Björck , S & Wohlfarth , B 2020 , ' Floral evidence for high summer temperatures in southern Scandinavia during 15-11 cal ka BP ' , Quaternary Science Reviews , vol. 233 , 106243 . https://doi.org/10.1016/j.quascirev.2020.106243

Title: Floral evidence for high summer temperatures in southern Scandinavia during 15-11 cal ka BP
Author: Schenk, Frederik; Bennike, Ole; Valiranta, Minna; Avery, Rachael; Björck, Svante; Wohlfarth, Barbara
Contributor: University of Helsinki, Helsinki Institute of Sustainability Science (HELSUS)
Date: 2020-04-01
Language: eng
Number of pages: 12
Belongs to series: Quaternary Science Reviews
ISSN: 0277-3791
URI: http://hdl.handle.net/10138/320058
Abstract: The global climate transition from the Lateglacial to the Early Holocene is dominated by a rapid warming trend driven by an increase in orbital summer insolation over high northern latitudes and related feedbacks. The warming trend was interrupted by several abrupt shifts between colder (stadial) and warmer (interstadial) climate states following instabilities of the Atlantic Meridional Overturning Circulation (AMOC) in response to rapidly melting ice sheets. The sequence of abrupt shifts between extreme climate states had profound impacts on ecosystems which make it challenging to reliably quantify state variables like July temperatures within a non-analogue climate envelope. For Europe, there is increasing albeit inconclusive evidence for higher stadial summer temperatures than initially thought. Here we present a comprehensive floral compilation of plant macrofossils from lake sediment cores of 15 sites from S-Scandinavia covering the period similar to 15 to 11 ka BP. We find evidence for a continued presence of plant species indicating high July temperatures throughout the last deglaciation. The presence of hemiboreal plants in close vicinity to the southern margin of the Fennoscandian Ice Sheet implies a strong thermal summer forcing for the rapid ice sheet melt. Consistent with some recent studies, we do not find evidence for a general stadial summer cooling, which indicates that other reasons than summer temperatures caused drastic setbacks in proxy signals possibly driven by extreme winter cooling and/or shorter warm seasons. (C) 2020 The Authors. Published by Elsevier Ltd.
Subject: Deglaciation
Paleoclimatology
Scandinavia
Plant macrofossils
Summer temperatures
YOUNGER DRYAS
ENVIRONMENTAL-CHANGE
CLIMATIC CHANGES
NORTHERN EUROPE
BALTIC SEA
ICE-SHEET
KYR BP
HOLOCENE
LAKE
RECONSTRUCTION
1172 Environmental sciences
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