Exploring Holocene continentality changes in Fennoscandia using present and past tree distributions

With global warming, the distribution of warmth through the year is likely to change in the future and comparable changes may have occurred over the course of the Holocene. Its effect on vegetation composition and species distribution can be compared to that of a continental versus an oceanic climat...

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Main Authors: Giesecke, T, Bjune, AE, Chiverrell, RC, Seppa, H, Ojala, AEK, Birks, HJB
Format: Article in Journal/Newspaper
Language:unknown
Published: PERGAMON-ELSEVIER SCIENCE LTD 2008
Subjects:
Online Access:http://discovery.ucl.ac.uk/166197/
id ftucl:oai:eprints.ucl.ac.uk.OAI2:166197
record_format openpolar
spelling ftucl:oai:eprints.ucl.ac.uk.OAI2:166197 2023-05-15T16:11:31+02:00 Exploring Holocene continentality changes in Fennoscandia using present and past tree distributions Giesecke, T Bjune, AE Chiverrell, RC Seppa, H Ojala, AEK Birks, HJB 2008-07 http://discovery.ucl.ac.uk/166197/ unknown PERGAMON-ELSEVIER SCIENCE LTD QUATERNARY SCI REV , 27 (13-14) 1296 - 1308. (2008) CORYLUS-AVELLANA L. NORTHERN SWEDEN ENVIRONMENTAL HISTORY CLIMATIC-CHANGE SEED STERILITY TILIA-CORDATA ALPINE LAKE EUROPE POLLEN TEMPERATURE Article 2008 ftucl 2017-03-09T23:11:01Z With global warming, the distribution of warmth through the year is likely to change in the future and comparable changes may have occurred over the course of the Holocene. Its effect on vegetation composition and species distribution can be compared to that of a continental versus an oceanic climate. The distribution of five major tree species along a continentality gradient was studied in Fennoscandia based on distribution maps and on their proportions of pollen in surface-sediment samples. Both analyses indicate that the five arboreal species show similar patterns of response to a continentality index in the order Ulmus glabra, Corylus avellana, Quercus robur, Tilia cordata, and Picea abies from the most oceanic to most continental. Continentality, growing degree days above 5 degrees C, and January temperature were reconstructed quantitatively from four pollen diagrams using transfer functions based on a combined Fennoscandian pollen surface-sample data-set. Quantitative reconstructions indicate that the climate in Fennoscandia has become increasingly more continental over the last 7000 years, and this is largely an effect of winter cooling. Early Holocene vegetation composition has poor analogues to the present vegetation in Fennoscandia, which hampers quantitative reconstructions. Qualitative reconstructions suggest that the early Holocene in Fennoscandia was the most oceanic period, but probably with a high variability in temperature. (C) 2008 Elsevier Ltd. All rights reserved. Article in Journal/Newspaper Fennoscandia Fennoscandian Northern Sweden University College London: UCL Discovery Alpine Lake ENVELOPE(-129.182,-129.182,55.529,55.529)
institution Open Polar
collection University College London: UCL Discovery
op_collection_id ftucl
language unknown
topic CORYLUS-AVELLANA L.
NORTHERN SWEDEN
ENVIRONMENTAL HISTORY
CLIMATIC-CHANGE
SEED STERILITY
TILIA-CORDATA
ALPINE LAKE
EUROPE
POLLEN
TEMPERATURE
spellingShingle CORYLUS-AVELLANA L.
NORTHERN SWEDEN
ENVIRONMENTAL HISTORY
CLIMATIC-CHANGE
SEED STERILITY
TILIA-CORDATA
ALPINE LAKE
EUROPE
POLLEN
TEMPERATURE
Giesecke, T
Bjune, AE
Chiverrell, RC
Seppa, H
Ojala, AEK
Birks, HJB
Exploring Holocene continentality changes in Fennoscandia using present and past tree distributions
topic_facet CORYLUS-AVELLANA L.
NORTHERN SWEDEN
ENVIRONMENTAL HISTORY
CLIMATIC-CHANGE
SEED STERILITY
TILIA-CORDATA
ALPINE LAKE
EUROPE
POLLEN
TEMPERATURE
description With global warming, the distribution of warmth through the year is likely to change in the future and comparable changes may have occurred over the course of the Holocene. Its effect on vegetation composition and species distribution can be compared to that of a continental versus an oceanic climate. The distribution of five major tree species along a continentality gradient was studied in Fennoscandia based on distribution maps and on their proportions of pollen in surface-sediment samples. Both analyses indicate that the five arboreal species show similar patterns of response to a continentality index in the order Ulmus glabra, Corylus avellana, Quercus robur, Tilia cordata, and Picea abies from the most oceanic to most continental. Continentality, growing degree days above 5 degrees C, and January temperature were reconstructed quantitatively from four pollen diagrams using transfer functions based on a combined Fennoscandian pollen surface-sample data-set. Quantitative reconstructions indicate that the climate in Fennoscandia has become increasingly more continental over the last 7000 years, and this is largely an effect of winter cooling. Early Holocene vegetation composition has poor analogues to the present vegetation in Fennoscandia, which hampers quantitative reconstructions. Qualitative reconstructions suggest that the early Holocene in Fennoscandia was the most oceanic period, but probably with a high variability in temperature. (C) 2008 Elsevier Ltd. All rights reserved.
format Article in Journal/Newspaper
author Giesecke, T
Bjune, AE
Chiverrell, RC
Seppa, H
Ojala, AEK
Birks, HJB
author_facet Giesecke, T
Bjune, AE
Chiverrell, RC
Seppa, H
Ojala, AEK
Birks, HJB
author_sort Giesecke, T
title Exploring Holocene continentality changes in Fennoscandia using present and past tree distributions
title_short Exploring Holocene continentality changes in Fennoscandia using present and past tree distributions
title_full Exploring Holocene continentality changes in Fennoscandia using present and past tree distributions
title_fullStr Exploring Holocene continentality changes in Fennoscandia using present and past tree distributions
title_full_unstemmed Exploring Holocene continentality changes in Fennoscandia using present and past tree distributions
title_sort exploring holocene continentality changes in fennoscandia using present and past tree distributions
publisher PERGAMON-ELSEVIER SCIENCE LTD
publishDate 2008
url http://discovery.ucl.ac.uk/166197/
long_lat ENVELOPE(-129.182,-129.182,55.529,55.529)
geographic Alpine Lake
geographic_facet Alpine Lake
genre Fennoscandia
Fennoscandian
Northern Sweden
genre_facet Fennoscandia
Fennoscandian
Northern Sweden
op_source QUATERNARY SCI REV , 27 (13-14) 1296 - 1308. (2008)
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