Chironomid-inferred summer temperatures for the Last Glacial-Interglacial Transition from a lake sediment sequence in Muir Park Reservoir, west-central Scotland

Author:

Brooks Stephen J.1,Davies Kimberley L.2,Mather Karen A.3,Matthews Ian P.3,Lowe J. John3

Affiliation:

1. Department of Life Sciences; Natural History Museum, Cromwell Road; London SW7 4UB UK

2. School of Geography, Earth and Environmental Sciences; Plymouth University; Plymouth UK

3. Centre for Quaternary Research, Department of Geography; Royal Holloway, University of London; Egham UK

Publisher

Wiley

Subject

Paleontology,Earth and Planetary Sciences (miscellaneous),Arts and Humanities (miscellaneous)

Reference56 articles.

1. Rapid oceanic and atmospheric changes during the Younger Dryas cold period;Bakke;Nature Geoscience,2009

2. Interhemispheric Atlantic seesaw response during the last deglaciation;Barker;Nature,2009

3. Determination of the number of zones in a biostratigraphical sequence;Bennett;New Phytologist,1996

4. BGS 2013 KML - Onshore geology 1: 625 000 scale (DiGMap GB - 625) www.bgs.ac.uk/data/services/digmapgb625kml.html

5. Biological responses to rapid climate change at the Younger Dryas-Holocene transition at Kråkenes, western Norway;Birks;Holocene,2008

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