Merging chironomid training sets: Implications for palaeoclimate reconstructions

Icelandic and Norwegian chironomid calibration or training sets were merged to investigate whether a larger combined training set would be useful to apply to subfossil chironomid data from Iceland for periods such as the early Holocene, the Holocene Thermal Maximum and the Little Ice Age, when tempe...

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Published in:Quaternary Science Reviews
Main Authors: Holmes, Naomi, Langdon, Peter G., Caseldine, Chris, Brooks, Stephen J., Birks, H. John B.
Format: Article in Journal/Newspaper
Language:English
Published: 2011
Subjects:
Online Access:https://eprints.soton.ac.uk/194501/
https://eprints.soton.ac.uk/194501/1/Holmes_et_al_QSR_2011_in_press.pdf
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spelling ftsouthampton:oai:eprints.soton.ac.uk:194501 2023-07-30T04:04:21+02:00 Merging chironomid training sets: Implications for palaeoclimate reconstructions Holmes, Naomi Langdon, Peter G. Caseldine, Chris Brooks, Stephen J. Birks, H. John B. 2011-07-14 text https://eprints.soton.ac.uk/194501/ https://eprints.soton.ac.uk/194501/1/Holmes_et_al_QSR_2011_in_press.pdf en eng https://eprints.soton.ac.uk/194501/1/Holmes_et_al_QSR_2011_in_press.pdf Holmes, Naomi, Langdon, Peter G., Caseldine, Chris, Brooks, Stephen J. and Birks, H. John B. (2011) Merging chironomid training sets: Implications for palaeoclimate reconstructions. Quaternary Science Reviews, 30 (19-20), 2793-2804. (doi:10.1016/j.quascirev.2011.06.013 <http://dx.doi.org/10.1016/j.quascirev.2011.06.013>). Article PeerReviewed 2011 ftsouthampton https://doi.org/10.1016/j.quascirev.2011.06.013 2023-07-09T21:23:16Z Icelandic and Norwegian chironomid calibration or training sets were merged to investigate whether a larger combined training set would be useful to apply to subfossil chironomid data from Iceland for periods such as the early Holocene, the Holocene Thermal Maximum and the Little Ice Age, when temperatures can be expected to be outside the current temperature range of the Icelandic training set. Following taxonomic harmonisation, the Icelandic and Norwegian data sets were compared before being merged to form a combined Norwegian-Icelandic training set. Analyses showed that it was biologically and statistically valid to merge the two data sets. The resulting combined inference model for mean July air temperature had improved performance statistics (r2jack = 0.87; RMSEPjack = 1.13) when compared to the best performing Icelandic model (r2jack = 0.61; RMSEPjack = 0.83), due to the longer environmental gradient covered (Icelandic 6–11 °C; combined 3.5–16 °C), and to the increased number of samples (Icelandic = 53 lakes; combined = 207 lakes) and taxa (Icelandic = 47 taxa; combined = 133 taxa) present within the combined training set. The inference models were applied to an early Holocene chironomid sequence from Vatnamýri, north Iceland, and a 450-year recent record from Myfluguvatn, north-west Iceland, to compare the reconstructions produced. The various inference models produced similar trends and patterns of temperature reconstruction, but the inference model based on the combined training set produced a larger range of reconstructed temperatures than the Icelandic model. It was found that different inference models produced more variation in the reconstruction than when different training sets were used. A comparison of the Myfluguvatn reconstructions with meteorological observations showed that the combined Norwegian–Icelandic inference model produced more reliable results than the Icelandic or Norwegian inference models alone. Article in Journal/Newspaper Iceland University of Southampton: e-Prints Soton Quaternary Science Reviews 30 19-20 2793 2804
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collection University of Southampton: e-Prints Soton
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language English
description Icelandic and Norwegian chironomid calibration or training sets were merged to investigate whether a larger combined training set would be useful to apply to subfossil chironomid data from Iceland for periods such as the early Holocene, the Holocene Thermal Maximum and the Little Ice Age, when temperatures can be expected to be outside the current temperature range of the Icelandic training set. Following taxonomic harmonisation, the Icelandic and Norwegian data sets were compared before being merged to form a combined Norwegian-Icelandic training set. Analyses showed that it was biologically and statistically valid to merge the two data sets. The resulting combined inference model for mean July air temperature had improved performance statistics (r2jack = 0.87; RMSEPjack = 1.13) when compared to the best performing Icelandic model (r2jack = 0.61; RMSEPjack = 0.83), due to the longer environmental gradient covered (Icelandic 6–11 °C; combined 3.5–16 °C), and to the increased number of samples (Icelandic = 53 lakes; combined = 207 lakes) and taxa (Icelandic = 47 taxa; combined = 133 taxa) present within the combined training set. The inference models were applied to an early Holocene chironomid sequence from Vatnamýri, north Iceland, and a 450-year recent record from Myfluguvatn, north-west Iceland, to compare the reconstructions produced. The various inference models produced similar trends and patterns of temperature reconstruction, but the inference model based on the combined training set produced a larger range of reconstructed temperatures than the Icelandic model. It was found that different inference models produced more variation in the reconstruction than when different training sets were used. A comparison of the Myfluguvatn reconstructions with meteorological observations showed that the combined Norwegian–Icelandic inference model produced more reliable results than the Icelandic or Norwegian inference models alone.
format Article in Journal/Newspaper
author Holmes, Naomi
Langdon, Peter G.
Caseldine, Chris
Brooks, Stephen J.
Birks, H. John B.
spellingShingle Holmes, Naomi
Langdon, Peter G.
Caseldine, Chris
Brooks, Stephen J.
Birks, H. John B.
Merging chironomid training sets: Implications for palaeoclimate reconstructions
author_facet Holmes, Naomi
Langdon, Peter G.
Caseldine, Chris
Brooks, Stephen J.
Birks, H. John B.
author_sort Holmes, Naomi
title Merging chironomid training sets: Implications for palaeoclimate reconstructions
title_short Merging chironomid training sets: Implications for palaeoclimate reconstructions
title_full Merging chironomid training sets: Implications for palaeoclimate reconstructions
title_fullStr Merging chironomid training sets: Implications for palaeoclimate reconstructions
title_full_unstemmed Merging chironomid training sets: Implications for palaeoclimate reconstructions
title_sort merging chironomid training sets: implications for palaeoclimate reconstructions
publishDate 2011
url https://eprints.soton.ac.uk/194501/
https://eprints.soton.ac.uk/194501/1/Holmes_et_al_QSR_2011_in_press.pdf
genre Iceland
genre_facet Iceland
op_relation https://eprints.soton.ac.uk/194501/1/Holmes_et_al_QSR_2011_in_press.pdf
Holmes, Naomi, Langdon, Peter G., Caseldine, Chris, Brooks, Stephen J. and Birks, H. John B. (2011) Merging chironomid training sets: Implications for palaeoclimate reconstructions. Quaternary Science Reviews, 30 (19-20), 2793-2804. (doi:10.1016/j.quascirev.2011.06.013 <http://dx.doi.org/10.1016/j.quascirev.2011.06.013>).
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container_title Quaternary Science Reviews
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container_issue 19-20
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