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A 7500-year peat-based palaeoclimatic reconstruction and evidence for an 1100-year cyclicity in bog surface wetness from Temple Hill Moss, Pentland Hills, southeast Scotland

✍ Scribed by P.G. Langdon; K.E. Barber; P.D.M. Hughes


Book ID
117446413
Publisher
Elsevier Science
Year
2003
Tongue
English
Weight
347 KB
Volume
22
Category
Article
ISSN
0277-3791

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