Reconstructing North Atlantic marine climate variability using an absolutely-dated sclerochronological network

This is the final version of the article. Available from Elsevier via the DOI in this record. Reconstructing regional to hemispheric-scale climate variability requires the application of spatially representative and climatically sensitive proxy archives. Large spatial networks of dendrochronologies...

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Published in:Palaeogeography, Palaeoclimatology, Palaeoecology
Main Authors: Reynolds, DJ, Richardson, CA, Scourse, JD, Butler, PG, Hollyman, P, Román-González, A, Hall, IR
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2016
Subjects:
Online Access:http://hdl.handle.net/10871/26357
https://doi.org/10.1016/j.palaeo.2016.08.006
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author Reynolds, DJ
Richardson, CA
Scourse, JD
Butler, PG
Hollyman, P
Román-González, A
Hall, IR
author_facet Reynolds, DJ
Richardson, CA
Scourse, JD
Butler, PG
Hollyman, P
Román-González, A
Hall, IR
author_sort Reynolds, DJ
collection University of Exeter: Open Research Exeter (ORE)
container_start_page 333
container_title Palaeogeography, Palaeoclimatology, Palaeoecology
container_volume 465
description This is the final version of the article. Available from Elsevier via the DOI in this record. Reconstructing regional to hemispheric-scale climate variability requires the application of spatially representative and climatically sensitive proxy archives. Large spatial networks of dendrochronologies have facilitated the reconstruction of atmospheric variability and inferred variability in the Atlantic Ocean system. However, the marine environment has hitherto lacked the direct application of the spatial network approach because of the small number of individual absolutely-dated marine archives. In this study we present the first analyses of a network of absolutely-dated annually-resolved growth increment width chronologies from the marine bivalves Glycymeris glycymeris and Arctica islandica. The network contains eight chronologies spanning > 500 km along the western British continental shelf from the southern Irish Sea to North West Scotland. Correlation analysis of the individual chronologies and a suite of climate indices, including the Atlantic Multidecadal Oscillation (AMO), Central England surface air temperature (CET), northeast Atlantic sea surface temperatures (SST's) and the winter North Atlantic Oscillation (wNAO), demonstrates that, despite the large geographical distances been sites and the heterogeneous nature of the marine environment, the increment width variability in these series contains an element of coherence likely driven by a common response to changing environmental forcing. A nested Principal component analysis (PCA) was used to construct five composite series which explain between 31% and 74% of the variance across the individual chronologies. Linear regression analyses indicate that the composite series explain up to 41% of the variance in Northeast Atlantic SSTs over the calibration period (1975–2000). Calibration verification (reduction of error [RE] and coefficient of efficiency [CE]) statistics indicate that the composite series contains significant skill at reconstructing ...
format Article in Journal/Newspaper
genre Arctica islandica
North Atlantic
North Atlantic oscillation
Northeast Atlantic
genre_facet Arctica islandica
North Atlantic
North Atlantic oscillation
Northeast Atlantic
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op_doi https://doi.org/10.1016/j.palaeo.2016.08.006
op_relation doi:10.1016/j.palaeo.2016.08.006
http://hdl.handle.net/10871/26357
Palaeogeography, Palaeoclimatology, Palaeoecology
op_rights Open Access funded by Natural Environment Research Council. Under a Creative Commons license: https://creativecommons.org/licenses/by/4.0/
publishDate 2016
publisher Elsevier
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spelling ftunivexeter:oai:ore.exeter.ac.uk:10871/26357 2025-04-06T14:46:53+00:00 Reconstructing North Atlantic marine climate variability using an absolutely-dated sclerochronological network Reynolds, DJ Richardson, CA Scourse, JD Butler, PG Hollyman, P Román-González, A Hall, IR 2016 http://hdl.handle.net/10871/26357 https://doi.org/10.1016/j.palaeo.2016.08.006 en eng Elsevier doi:10.1016/j.palaeo.2016.08.006 http://hdl.handle.net/10871/26357 Palaeogeography, Palaeoclimatology, Palaeoecology Open Access funded by Natural Environment Research Council. Under a Creative Commons license: https://creativecommons.org/licenses/by/4.0/ Sclerochronology Spatial network Arctica islandica Glycymeris glycymeris North Atlantic Article 2016 ftunivexeter https://doi.org/10.1016/j.palaeo.2016.08.006 2025-03-11T01:39:59Z This is the final version of the article. Available from Elsevier via the DOI in this record. Reconstructing regional to hemispheric-scale climate variability requires the application of spatially representative and climatically sensitive proxy archives. Large spatial networks of dendrochronologies have facilitated the reconstruction of atmospheric variability and inferred variability in the Atlantic Ocean system. However, the marine environment has hitherto lacked the direct application of the spatial network approach because of the small number of individual absolutely-dated marine archives. In this study we present the first analyses of a network of absolutely-dated annually-resolved growth increment width chronologies from the marine bivalves Glycymeris glycymeris and Arctica islandica. The network contains eight chronologies spanning > 500 km along the western British continental shelf from the southern Irish Sea to North West Scotland. Correlation analysis of the individual chronologies and a suite of climate indices, including the Atlantic Multidecadal Oscillation (AMO), Central England surface air temperature (CET), northeast Atlantic sea surface temperatures (SST's) and the winter North Atlantic Oscillation (wNAO), demonstrates that, despite the large geographical distances been sites and the heterogeneous nature of the marine environment, the increment width variability in these series contains an element of coherence likely driven by a common response to changing environmental forcing. A nested Principal component analysis (PCA) was used to construct five composite series which explain between 31% and 74% of the variance across the individual chronologies. Linear regression analyses indicate that the composite series explain up to 41% of the variance in Northeast Atlantic SSTs over the calibration period (1975–2000). Calibration verification (reduction of error [RE] and coefficient of efficiency [CE]) statistics indicate that the composite series contains significant skill at reconstructing ... Article in Journal/Newspaper Arctica islandica North Atlantic North Atlantic oscillation Northeast Atlantic University of Exeter: Open Research Exeter (ORE) Palaeogeography, Palaeoclimatology, Palaeoecology 465 333 346
spellingShingle Sclerochronology
Spatial network
Arctica islandica
Glycymeris glycymeris
North Atlantic
Reynolds, DJ
Richardson, CA
Scourse, JD
Butler, PG
Hollyman, P
Román-González, A
Hall, IR
Reconstructing North Atlantic marine climate variability using an absolutely-dated sclerochronological network
title Reconstructing North Atlantic marine climate variability using an absolutely-dated sclerochronological network
title_full Reconstructing North Atlantic marine climate variability using an absolutely-dated sclerochronological network
title_fullStr Reconstructing North Atlantic marine climate variability using an absolutely-dated sclerochronological network
title_full_unstemmed Reconstructing North Atlantic marine climate variability using an absolutely-dated sclerochronological network
title_short Reconstructing North Atlantic marine climate variability using an absolutely-dated sclerochronological network
title_sort reconstructing north atlantic marine climate variability using an absolutely-dated sclerochronological network
topic Sclerochronology
Spatial network
Arctica islandica
Glycymeris glycymeris
North Atlantic
topic_facet Sclerochronology
Spatial network
Arctica islandica
Glycymeris glycymeris
North Atlantic
url http://hdl.handle.net/10871/26357
https://doi.org/10.1016/j.palaeo.2016.08.006