Land-ocean changes on orbital and millennial time scales and the penultimate glaciation

Past glacials can be thought of as natural experiments in which variations in boundary conditions influenced the character of climate change. However, beyond the last glacial, an integrated view of orbital- and millennial-scale changes and their relation to the record of glaciation has been lacking....

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Published in:Geology
Main Authors: argari, Vasiliki, Skinner, Luke C., Hodell, David A., Martrat, Belen, Toucanne, Samuel, Grimalt, Joan O., Gibbard, Philip L., Lunkka, Juha Pekka, Tzedakis, Polychronis Chronis
Format: Article in Journal/Newspaper
Language:English
Published: 2015
Subjects:
Online Access:http://hdl.handle.net/10261/117716
https://doi.org/10.1130/G35070.1
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spelling ftcsic:oai:digital.csic.es:10261/117716 2024-02-11T10:04:52+01:00 Land-ocean changes on orbital and millennial time scales and the penultimate glaciation argari, Vasiliki Skinner, Luke C. Hodell, David A. Martrat, Belen Toucanne, Samuel Grimalt, Joan O. Gibbard, Philip L. Lunkka, Juha Pekka Tzedakis, Polychronis Chronis 2015-07-08 http://hdl.handle.net/10261/117716 https://doi.org/10.1130/G35070.1 en eng Preprint 10.1130/G35070.1 Sí Geology 42 (3): 183-186 (2014) http://hdl.handle.net/10261/117716 doi:10.1130/G35070.1 open Bipolar seesaw Climate oscillation European ice sheets Extreme events Freshwater discharge Heat transport Meridional overturning circulations Natural experiment artículo http://purl.org/coar/resource_type/c_6501 2015 ftcsic https://doi.org/10.1130/G35070.1 2024-01-16T10:08:28Z Past glacials can be thought of as natural experiments in which variations in boundary conditions influenced the character of climate change. However, beyond the last glacial, an integrated view of orbital- and millennial-scale changes and their relation to the record of glaciation has been lacking. Here, we present a detailed record of variations in the land-ocean system from the Portuguese margin during the penultimate glacial and place it within the framework of ice-volume changes, with particular reference to European ice-sheet dynamics. The interaction of orbital- and millennial-scale variability divides the glacial into an early part with warmer and wetter overall conditions and prominent climate oscillations, a transitional mid-part, and a late part with more subdued changes as the system entered a maximum glacial state. The most extreme event occurred in the mid-part and was associated with melting of the extensive European ice sheet and maximum discharge from the Fleuve Manche river. This led to disruption of the meridional overturning circulation, but not a major activation of the bipolar seesaw. In addition to stadial duration, magnitude of freshwater forcing, and background climate, the evidence also points to the influence of the location of freshwater discharges on the extent of interhemispheric heat transport. a Environmental Change Research Centre, Department of Geography, University College London, London WC1E 6BT, United Kingdom b Department of Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, United Kingdom c Institute of Environmental Assessment and Water Research (IDAEA), Spanish Council for Scientific Research (CSIC), 08034 Barcelona, Spain d IFREMER, Laboratoire Environnements Sédimentaires, F-29280 Plouzané, France e Department of Geography, University of Cambridge, Cambridge CB2 3EN, United Kingdom f Institute of Geosciences, University of Oulu, Oulu, FIN-90014, Finland No Article in Journal/Newspaper Ice Sheet Digital.CSIC (Spanish National Research Council) Geology 42 3 183 186
institution Open Polar
collection Digital.CSIC (Spanish National Research Council)
op_collection_id ftcsic
language English
topic Bipolar seesaw
Climate oscillation
European ice sheets
Extreme events
Freshwater discharge
Heat transport
Meridional overturning circulations
Natural experiment
spellingShingle Bipolar seesaw
Climate oscillation
European ice sheets
Extreme events
Freshwater discharge
Heat transport
Meridional overturning circulations
Natural experiment
argari, Vasiliki
Skinner, Luke C.
Hodell, David A.
Martrat, Belen
Toucanne, Samuel
Grimalt, Joan O.
Gibbard, Philip L.
Lunkka, Juha Pekka
Tzedakis, Polychronis Chronis
Land-ocean changes on orbital and millennial time scales and the penultimate glaciation
topic_facet Bipolar seesaw
Climate oscillation
European ice sheets
Extreme events
Freshwater discharge
Heat transport
Meridional overturning circulations
Natural experiment
description Past glacials can be thought of as natural experiments in which variations in boundary conditions influenced the character of climate change. However, beyond the last glacial, an integrated view of orbital- and millennial-scale changes and their relation to the record of glaciation has been lacking. Here, we present a detailed record of variations in the land-ocean system from the Portuguese margin during the penultimate glacial and place it within the framework of ice-volume changes, with particular reference to European ice-sheet dynamics. The interaction of orbital- and millennial-scale variability divides the glacial into an early part with warmer and wetter overall conditions and prominent climate oscillations, a transitional mid-part, and a late part with more subdued changes as the system entered a maximum glacial state. The most extreme event occurred in the mid-part and was associated with melting of the extensive European ice sheet and maximum discharge from the Fleuve Manche river. This led to disruption of the meridional overturning circulation, but not a major activation of the bipolar seesaw. In addition to stadial duration, magnitude of freshwater forcing, and background climate, the evidence also points to the influence of the location of freshwater discharges on the extent of interhemispheric heat transport. a Environmental Change Research Centre, Department of Geography, University College London, London WC1E 6BT, United Kingdom b Department of Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, United Kingdom c Institute of Environmental Assessment and Water Research (IDAEA), Spanish Council for Scientific Research (CSIC), 08034 Barcelona, Spain d IFREMER, Laboratoire Environnements Sédimentaires, F-29280 Plouzané, France e Department of Geography, University of Cambridge, Cambridge CB2 3EN, United Kingdom f Institute of Geosciences, University of Oulu, Oulu, FIN-90014, Finland No
format Article in Journal/Newspaper
author argari, Vasiliki
Skinner, Luke C.
Hodell, David A.
Martrat, Belen
Toucanne, Samuel
Grimalt, Joan O.
Gibbard, Philip L.
Lunkka, Juha Pekka
Tzedakis, Polychronis Chronis
author_facet argari, Vasiliki
Skinner, Luke C.
Hodell, David A.
Martrat, Belen
Toucanne, Samuel
Grimalt, Joan O.
Gibbard, Philip L.
Lunkka, Juha Pekka
Tzedakis, Polychronis Chronis
author_sort argari, Vasiliki
title Land-ocean changes on orbital and millennial time scales and the penultimate glaciation
title_short Land-ocean changes on orbital and millennial time scales and the penultimate glaciation
title_full Land-ocean changes on orbital and millennial time scales and the penultimate glaciation
title_fullStr Land-ocean changes on orbital and millennial time scales and the penultimate glaciation
title_full_unstemmed Land-ocean changes on orbital and millennial time scales and the penultimate glaciation
title_sort land-ocean changes on orbital and millennial time scales and the penultimate glaciation
publishDate 2015
url http://hdl.handle.net/10261/117716
https://doi.org/10.1130/G35070.1
genre Ice Sheet
genre_facet Ice Sheet
op_relation Preprint
10.1130/G35070.1

Geology 42 (3): 183-186 (2014)
http://hdl.handle.net/10261/117716
doi:10.1130/G35070.1
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container_title Geology
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