Glaciomarine deposition around the Irish Sea basin: some problems and solutions
Abstract Reconstructing the depositional processes and setting (marine or terrestrial depositional environment) of late Devensian age glacigenic sediments around the Irish Sea basin (ISB) is critical for developing an all‐embracing and consistent glacial model that can account for all observed field...
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crwiley:10.1002/jqs.630 2024-06-02T08:08:18+00:00 Glaciomarine deposition around the Irish Sea basin: some problems and solutions Knight, Jasper 2001 http://dx.doi.org/10.1002/jqs.630 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.630 https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.630 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Journal of Quaternary Science volume 16, issue 5, page 405-418 ISSN 0267-8179 1099-1417 journal-article 2001 crwiley https://doi.org/10.1002/jqs.630 2024-05-03T10:59:11Z Abstract Reconstructing the depositional processes and setting (marine or terrestrial depositional environment) of late Devensian age glacigenic sediments around the Irish Sea basin (ISB) is critical for developing an all‐embracing and consistent glacial model that can account for all observed field evidence. Identifying episodes of marine and terrestrial glacial deposition from field data is considered the first step in achieving this goal. Criteria for distinguishing marine and terrestrial glacial environments in the ISB include the geomorphology, sedimentology and faunal content (biofacies) of the associated deposits. Exposures of glacigenic sediments around the ISB are very diverse in terms of their morphosedimentary characteristics and associated biofacies, and thus inferred depositional processes and setting. Possible reasons for the diverse geological record include the differing geometry of eastern and western ISB coasts, time‐transgressive ice retreat, and differential land rebound effects as a result of forebulge collapse and neotectonics. Poor geochronometric control on ice sheet events has not helped the correlation of ISB events with glacial and climatic events elsewhere. Future investigations of glacial sites around the ISB should use an integrated methodological approach involving a range of geomorphological, sedimentary and biofacies data, and dating control where possible. This will help in developing a more precise and holistic late Devensian glacial model that is constrained rigorously by field geological evidence. Copyright © 2001 John Wiley & Sons, Ltd. Article in Journal/Newspaper Ice Sheet Wiley Online Library Journal of Quaternary Science 16 5 405 418 |
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English |
description |
Abstract Reconstructing the depositional processes and setting (marine or terrestrial depositional environment) of late Devensian age glacigenic sediments around the Irish Sea basin (ISB) is critical for developing an all‐embracing and consistent glacial model that can account for all observed field evidence. Identifying episodes of marine and terrestrial glacial deposition from field data is considered the first step in achieving this goal. Criteria for distinguishing marine and terrestrial glacial environments in the ISB include the geomorphology, sedimentology and faunal content (biofacies) of the associated deposits. Exposures of glacigenic sediments around the ISB are very diverse in terms of their morphosedimentary characteristics and associated biofacies, and thus inferred depositional processes and setting. Possible reasons for the diverse geological record include the differing geometry of eastern and western ISB coasts, time‐transgressive ice retreat, and differential land rebound effects as a result of forebulge collapse and neotectonics. Poor geochronometric control on ice sheet events has not helped the correlation of ISB events with glacial and climatic events elsewhere. Future investigations of glacial sites around the ISB should use an integrated methodological approach involving a range of geomorphological, sedimentary and biofacies data, and dating control where possible. This will help in developing a more precise and holistic late Devensian glacial model that is constrained rigorously by field geological evidence. Copyright © 2001 John Wiley & Sons, Ltd. |
format |
Article in Journal/Newspaper |
author |
Knight, Jasper |
spellingShingle |
Knight, Jasper Glaciomarine deposition around the Irish Sea basin: some problems and solutions |
author_facet |
Knight, Jasper |
author_sort |
Knight, Jasper |
title |
Glaciomarine deposition around the Irish Sea basin: some problems and solutions |
title_short |
Glaciomarine deposition around the Irish Sea basin: some problems and solutions |
title_full |
Glaciomarine deposition around the Irish Sea basin: some problems and solutions |
title_fullStr |
Glaciomarine deposition around the Irish Sea basin: some problems and solutions |
title_full_unstemmed |
Glaciomarine deposition around the Irish Sea basin: some problems and solutions |
title_sort |
glaciomarine deposition around the irish sea basin: some problems and solutions |
publisher |
Wiley |
publishDate |
2001 |
url |
http://dx.doi.org/10.1002/jqs.630 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.630 https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.630 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Journal of Quaternary Science volume 16, issue 5, page 405-418 ISSN 0267-8179 1099-1417 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/jqs.630 |
container_title |
Journal of Quaternary Science |
container_volume |
16 |
container_issue |
5 |
container_start_page |
405 |
op_container_end_page |
418 |
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1800753521713217536 |