The “Missing Glaciations” of the Middle Pleistocene
Global glaciations have varied in size and magnitude since the Early-Middle Pleistocene transition (~773 ka), despite the apparent regular and high-amplitude 100 kyr pacing of glacial-interglacial cycles recorded in marine isotopic records. The evidence on land indicates that patterns of glaciation...
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Online Access: | https://research.manchester.ac.uk/en/publications/d36eb014-1242-4ec6-9ae1-fb674fd4394a https://doi.org/10.1017/qua.2019.76 https://pure.manchester.ac.uk/ws/files/144687057/Hughesetal_MissingGlaciations_FINAL_withFigs.pdf |
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ftumanchesterpub:oai:pure.atira.dk:publications/d36eb014-1242-4ec6-9ae1-fb674fd4394a 2024-06-23T07:45:58+00:00 The “Missing Glaciations” of the Middle Pleistocene Hughes, Philip Gibbard, Philip Ehlers, Jürgen 2020-02-04 application/pdf https://research.manchester.ac.uk/en/publications/d36eb014-1242-4ec6-9ae1-fb674fd4394a https://doi.org/10.1017/qua.2019.76 https://pure.manchester.ac.uk/ws/files/144687057/Hughesetal_MissingGlaciations_FINAL_withFigs.pdf eng eng https://research.manchester.ac.uk/en/publications/d36eb014-1242-4ec6-9ae1-fb674fd4394a info:eu-repo/semantics/openAccess Hughes , P , Gibbard , P & Ehlers , J 2020 , ' The “Missing Glaciations” of the Middle Pleistocene ' , Quaternary Research , vol. 96 , pp. 161-183 . https://doi.org/10.1017/qua.2019.76 Illinoian Quaternary stratigraphy Saalian Wolstonian glacial cycles ice ages orbital forcing article 2020 ftumanchesterpub https://doi.org/10.1017/qua.2019.76 2024-06-04T00:56:17Z Global glaciations have varied in size and magnitude since the Early-Middle Pleistocene transition (~773 ka), despite the apparent regular and high-amplitude 100 kyr pacing of glacial-interglacial cycles recorded in marine isotopic records. The evidence on land indicates that patterns of glaciation varied dramatically between different glacial-interglacial cycles. For example, MIS (Marine Isotope Stages) 8, 10 and 14 are all noticeably absent from many terrestrial glacial records in North America and Europe. However, globally, the patterns are more complicated with major glaciations recorded in MIS 8 in Asia and in parts of the Southern Hemisphere, such as Patagonia for example. This spatial variability in glaciation between glacial-interglacial cycles is likely to be driven by ice volume changes in the West Antarctic Ice Sheet and associated interhemispheric connections through ocean-atmosphere circulatory changes. The weak global glacial imprint in some glacial-interglacial cycles is related to the pattern of global ice build-up. This is caused by feedback mechanisms within glacier systems themselves which partly result from long-term orbital changes driven by eccentricity. Article in Journal/Newspaper Antarc* Antarctic Ice Sheet The University of Manchester: Research Explorer Antarctic Patagonia West Antarctic Ice Sheet Quaternary Research 96 161 183 |
institution |
Open Polar |
collection |
The University of Manchester: Research Explorer |
op_collection_id |
ftumanchesterpub |
language |
English |
topic |
Illinoian Quaternary stratigraphy Saalian Wolstonian glacial cycles ice ages orbital forcing |
spellingShingle |
Illinoian Quaternary stratigraphy Saalian Wolstonian glacial cycles ice ages orbital forcing Hughes, Philip Gibbard, Philip Ehlers, Jürgen The “Missing Glaciations” of the Middle Pleistocene |
topic_facet |
Illinoian Quaternary stratigraphy Saalian Wolstonian glacial cycles ice ages orbital forcing |
description |
Global glaciations have varied in size and magnitude since the Early-Middle Pleistocene transition (~773 ka), despite the apparent regular and high-amplitude 100 kyr pacing of glacial-interglacial cycles recorded in marine isotopic records. The evidence on land indicates that patterns of glaciation varied dramatically between different glacial-interglacial cycles. For example, MIS (Marine Isotope Stages) 8, 10 and 14 are all noticeably absent from many terrestrial glacial records in North America and Europe. However, globally, the patterns are more complicated with major glaciations recorded in MIS 8 in Asia and in parts of the Southern Hemisphere, such as Patagonia for example. This spatial variability in glaciation between glacial-interglacial cycles is likely to be driven by ice volume changes in the West Antarctic Ice Sheet and associated interhemispheric connections through ocean-atmosphere circulatory changes. The weak global glacial imprint in some glacial-interglacial cycles is related to the pattern of global ice build-up. This is caused by feedback mechanisms within glacier systems themselves which partly result from long-term orbital changes driven by eccentricity. |
format |
Article in Journal/Newspaper |
author |
Hughes, Philip Gibbard, Philip Ehlers, Jürgen |
author_facet |
Hughes, Philip Gibbard, Philip Ehlers, Jürgen |
author_sort |
Hughes, Philip |
title |
The “Missing Glaciations” of the Middle Pleistocene |
title_short |
The “Missing Glaciations” of the Middle Pleistocene |
title_full |
The “Missing Glaciations” of the Middle Pleistocene |
title_fullStr |
The “Missing Glaciations” of the Middle Pleistocene |
title_full_unstemmed |
The “Missing Glaciations” of the Middle Pleistocene |
title_sort |
“missing glaciations” of the middle pleistocene |
publishDate |
2020 |
url |
https://research.manchester.ac.uk/en/publications/d36eb014-1242-4ec6-9ae1-fb674fd4394a https://doi.org/10.1017/qua.2019.76 https://pure.manchester.ac.uk/ws/files/144687057/Hughesetal_MissingGlaciations_FINAL_withFigs.pdf |
geographic |
Antarctic Patagonia West Antarctic Ice Sheet |
geographic_facet |
Antarctic Patagonia West Antarctic Ice Sheet |
genre |
Antarc* Antarctic Ice Sheet |
genre_facet |
Antarc* Antarctic Ice Sheet |
op_source |
Hughes , P , Gibbard , P & Ehlers , J 2020 , ' The “Missing Glaciations” of the Middle Pleistocene ' , Quaternary Research , vol. 96 , pp. 161-183 . https://doi.org/10.1017/qua.2019.76 |
op_relation |
https://research.manchester.ac.uk/en/publications/d36eb014-1242-4ec6-9ae1-fb674fd4394a |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1017/qua.2019.76 |
container_title |
Quaternary Research |
container_volume |
96 |
container_start_page |
161 |
op_container_end_page |
183 |
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1802643263406997504 |