A Late-glacial chironomid record from Hawes Water, northwest England
This paper presents the results of a high-resolution Late-glacial chironomid stratigraphy from Hawes Water, a small carbonate lake in northern Lancashire. The samples were from a core taken from the terrestrialised margin of the present lake, which represents an intermediate depth between the true l...
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John Wiley & Sons
2004
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ftedgehilluniv:oai:repository.edgehill.ac.uk:1457 2023-05-15T18:29:50+02:00 A Late-glacial chironomid record from Hawes Water, northwest England Bedford, A. Jones, R. Lang, B. Brooks, S. Marshall, J. 2004 http://repository.edgehill.ac.uk/1457/ unknown John Wiley & Sons Bedford, A., Jones, R., Lang, B., Brooks, S. and Marshall, J. (2004) A Late-glacial chironomid record from Hawes Water, northwest England. Journal of Quaternary Science, 19 (3). pp. 281-290. ISSN 0267-8179 DOI https://doi.org/10.1002/jqs.836 <https://doi.org/10.1002/jqs.836> G Geography (General) SF Animal culture Article PeerReviewed 2004 ftedgehilluniv https://doi.org/10.1002/jqs.836 2018-02-03T16:53:02Z This paper presents the results of a high-resolution Late-glacial chironomid stratigraphy from Hawes Water, a small carbonate lake in northern Lancashire. The samples were from a core taken from the terrestrialised margin of the present lake, which represents an intermediate depth between the true littoral and the profundal. The chironomid assemblage showed a high degree of sensitivity to both broad-scale and short-term temperature changes. Comparison with an existing proxy temperature record (δ18O) for the site confirmed the presence of four temperature inversions within the Late-glacial Interstadial. A mean July air temperature inference model, derived from acid, soft-water lakes in Norway and Svalbard, was applied to the data. Despite the absence of carbonate lakes within the Norwegian training set, there was a close similarity between trends in estimated July air temperature and the δ18O trace, with a particularly strong correspondence in the periods of clay deposition. This suggests that this model is highly robust. The inferred maximum Interstadial temperature was 13.4°C, dropping initially to 7.5°C in the Loch Lomond Stadial. Temperatures reach a maximum of nearly 10°C in this period, cool for a short period before rising rapidly to 13.2°C at the start of the Holocene. These temperatures are similar to but slightly higher than those estimated for Whitrig Bog, southeast Scotland, and lower than those inferred from coleopteran-based models for sites in South Wales. Article in Journal/Newspaper Svalbard Edge Hill University: Edge Hill Research Archive Svalbard Norway Loch Lomond ENVELOPE(-125.746,-125.746,54.239,54.239) Journal of Quaternary Science 19 3 281 290 |
institution |
Open Polar |
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Edge Hill University: Edge Hill Research Archive |
op_collection_id |
ftedgehilluniv |
language |
unknown |
topic |
G Geography (General) SF Animal culture |
spellingShingle |
G Geography (General) SF Animal culture Bedford, A. Jones, R. Lang, B. Brooks, S. Marshall, J. A Late-glacial chironomid record from Hawes Water, northwest England |
topic_facet |
G Geography (General) SF Animal culture |
description |
This paper presents the results of a high-resolution Late-glacial chironomid stratigraphy from Hawes Water, a small carbonate lake in northern Lancashire. The samples were from a core taken from the terrestrialised margin of the present lake, which represents an intermediate depth between the true littoral and the profundal. The chironomid assemblage showed a high degree of sensitivity to both broad-scale and short-term temperature changes. Comparison with an existing proxy temperature record (δ18O) for the site confirmed the presence of four temperature inversions within the Late-glacial Interstadial. A mean July air temperature inference model, derived from acid, soft-water lakes in Norway and Svalbard, was applied to the data. Despite the absence of carbonate lakes within the Norwegian training set, there was a close similarity between trends in estimated July air temperature and the δ18O trace, with a particularly strong correspondence in the periods of clay deposition. This suggests that this model is highly robust. The inferred maximum Interstadial temperature was 13.4°C, dropping initially to 7.5°C in the Loch Lomond Stadial. Temperatures reach a maximum of nearly 10°C in this period, cool for a short period before rising rapidly to 13.2°C at the start of the Holocene. These temperatures are similar to but slightly higher than those estimated for Whitrig Bog, southeast Scotland, and lower than those inferred from coleopteran-based models for sites in South Wales. |
format |
Article in Journal/Newspaper |
author |
Bedford, A. Jones, R. Lang, B. Brooks, S. Marshall, J. |
author_facet |
Bedford, A. Jones, R. Lang, B. Brooks, S. Marshall, J. |
author_sort |
Bedford, A. |
title |
A Late-glacial chironomid record from Hawes Water, northwest England |
title_short |
A Late-glacial chironomid record from Hawes Water, northwest England |
title_full |
A Late-glacial chironomid record from Hawes Water, northwest England |
title_fullStr |
A Late-glacial chironomid record from Hawes Water, northwest England |
title_full_unstemmed |
A Late-glacial chironomid record from Hawes Water, northwest England |
title_sort |
late-glacial chironomid record from hawes water, northwest england |
publisher |
John Wiley & Sons |
publishDate |
2004 |
url |
http://repository.edgehill.ac.uk/1457/ |
long_lat |
ENVELOPE(-125.746,-125.746,54.239,54.239) |
geographic |
Svalbard Norway Loch Lomond |
geographic_facet |
Svalbard Norway Loch Lomond |
genre |
Svalbard |
genre_facet |
Svalbard |
op_relation |
Bedford, A., Jones, R., Lang, B., Brooks, S. and Marshall, J. (2004) A Late-glacial chironomid record from Hawes Water, northwest England. Journal of Quaternary Science, 19 (3). pp. 281-290. ISSN 0267-8179 DOI https://doi.org/10.1002/jqs.836 <https://doi.org/10.1002/jqs.836> |
op_doi |
https://doi.org/10.1002/jqs.836 |
container_title |
Journal of Quaternary Science |
container_volume |
19 |
container_issue |
3 |
container_start_page |
281 |
op_container_end_page |
290 |
_version_ |
1766213246668242944 |