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River response to high-frequency climate oscillations in southern Europe over the past 200 k.y.
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1998
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EngineeringGeomorphologySouthern EuropePhysical GeographyFluvial ProcessEarth ScienceSocial SciencesHigh-frequency Climate OscillationsRegional Climate ResponseHydroclimate ModelingClimate ChangeClimate VariabilityHydrometeorologyClimate SciencesGeographyClimate IssueRiver ResponseHydrologyClimate SystemClimate DynamicsClimatologyEarth Sciences
Research Article| March 01, 1998 River response to high-frequency climate oscillations in southern Europe over the past 200 k.y. Ian C. Fuller; Ian C. Fuller 1Division of Geography and Environmental Management, University of Northumbria, Newcastle-upon-Tyne NE1 8ST, United Kingdom Search for other works by this author on: GSW Google Scholar Mark G. Macklin; Mark G. Macklin 2School of Geography, University of Leeds, Leeds LS2 9JT, United Kingdom Search for other works by this author on: GSW Google Scholar John Lewin; John Lewin 3Institute of Geography and Earth Sciences, University of Wales, Aberystwyth SY23 3DB, United Kingdom Search for other works by this author on: GSW Google Scholar David G. Passmore; David G. Passmore 4Department of Geography, University of Newcastle, Newcastle-upon-Tyne NE1 7RU, United Kingdom Search for other works by this author on: GSW Google Scholar Ann G. Wintle Ann G. Wintle 3Institute of Geography and Earth Sciences, University of Wales, Aberystwyth SY23 3DB, United Kingdom Search for other works by this author on: GSW Google Scholar Author and Article Information Ian C. Fuller 1Division of Geography and Environmental Management, University of Northumbria, Newcastle-upon-Tyne NE1 8ST, United Kingdom Mark G. Macklin 2School of Geography, University of Leeds, Leeds LS2 9JT, United Kingdom John Lewin 3Institute of Geography and Earth Sciences, University of Wales, Aberystwyth SY23 3DB, United Kingdom David G. Passmore 4Department of Geography, University of Newcastle, Newcastle-upon-Tyne NE1 7RU, United Kingdom Ann G. Wintle 3Institute of Geography and Earth Sciences, University of Wales, Aberystwyth SY23 3DB, United Kingdom Publisher: Geological Society of America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1998) 26 (3): 275–278. https://doi.org/10.1130/0091-7613(1998)026<0275:RRTHFC>2.3.CO;2 Article history First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Ian C. Fuller, Mark G. Macklin, John Lewin, David G. Passmore, Ann G. Wintle; River response to high-frequency climate oscillations in southern Europe over the past 200 k.y.. Geology 1998;; 26 (3): 275–278. doi: https://doi.org/10.1130/0091-7613(1998)026<0275:RRTHFC>2.3.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract A 200 k.y. chronology of river response to climate-related environmental change has been established for northeast Spain using newly developed luminescence dating techniques. This constitutes the best-documented record of late Quaternary river behavior currently available for the North Atlantic region and enables fluvial stratigraphies to be compared with high-resolution ice core and marine oxygen isotope climate series. Pleistocene and Holocene river aggradational episodes coincide with stadial or neoglacial events, while phases of river incision occur during interstadial or interglacial periods. Alluviation and erosion cycles would appear to track variations in sediment supply controlled by vegetation cover and winter storm frequency. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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