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Sökning: id:"swepub:oai:DiVA.org:umu-161654" > Mid-Devensian clima...

Mid-Devensian climate and landscape in England : new data from Finningley, South Yorkshire

Buckland, Philip I., Dr. 1973- (författare)
Umeå universitet,Miljöarkeologiska laboratoriet
Bateman, Mark D. (författare)
Department of Geography, University of Sheffield, Sheffield S10 2TN, UK
Bennike, Ole (författare)
GEUS Geological Survey of Denmark and Greenland, ØsterVoldgade 10, Copenhagen 1350, Denmark
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Buckland, Paul C. (författare)
Bugs
Chase, Brian M. (författare)
Institut des Sciences de l’Evolution-Montpellier (ISEM), Universite´ de Montpellier, CNRS, EPHE, IRD, Bat 22, CC061, Place Euge`ne Bataillon, 34095 Montpellier cedex 5, France
Frederick, Charles (författare)
6Department of Geography and the Environment, The University of Texas at Austin, Austin, TX, USA
Greenwood, Malcolm (författare)
Department of Geography, Loughborough University, Leics LE11 3TU, UK
Murton, Julian (författare)
Department of Geography, University of Sussex, Brighton BN1 9RH, UK
Murton, Della (författare)
Department of Zoology, University of Cambridge, Downing Street, Cambridge CB2 3EJ, UK
Panagiotakopulu, Eva (författare)
Institute of Geography, University of Edinburgh, Drummond Street, Edinburgh EH8 9XP, UK
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 (creator_code:org_t)
2019-07-10
2019
Engelska.
Ingår i: Royal Society Open Science. - : Royal Society Publishing. - 2054-5703. ; 6:7
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • While there is extensive evidence for the Late Devensian, less is known about Early and Middle Devensian (approx. 110-30 ka) climates and environments in the UK. The Greenland ice-core record suggests the UK should have endured multiple changes, but the terrestrial palaeo-record lacks sufficient detail for confirmation from sites in the British Isles. Data from deposits at Finningley, South Yorkshire, can help redress this. A channel with organic silts, dated 40 314-39 552 cal a BP, contained plant macrofossil and insect remains showing tundra with dwarf-shrub heath and bare ground. Soil moisture conditions varied from free draining to riparian, with ponds and wetter vegetated areas. The climate was probably low arctic with snow cover during the winter. Mutual climatic range (MCR), based on Coleoptera, shows the mean monthly winter temperatures of -22 to -2 degrees C and summer ones of 8-14 degrees C. Periglacial structures within the basal gravel deposits and beyond the glacial limits indicate cold-climate conditions, including permafrost. A compilation of MCR reconstructions for other Middle Devensian English sites shows that marine isotope stage 3-between 59 and 28 ka-experienced substantial variation in climate consistent with the Greenland ice-core record. The exact correlation is hampered by temporal resolution, but the Finningley site stadial at approximately 40 ka may correlate with the one of the Greenland stadials 7-11.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geologi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geology (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences (hsv//eng)
NATURVETENSKAP  -- Biologi -- Ekologi (hsv//swe)
NATURAL SCIENCES  -- Biological Sciences -- Ecology (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Klimatforskning (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Climate Research (hsv//eng)

Nyckelord

mid-Devensian
Vale of York
plant macrofossils
Trichoptera
Coleoptera
periglaciation
environmental archaeology
miljöarkeologi
Entomology
entomologi
environmental science
miljövetenskap
bantuistik
bantu languages

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