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Using peatland archives to test paleoclimate hypotheses
Author(s) -
Robert K. Booth,
ST Jackson,
Michael Notaro
Publication year - 2010
Publication title -
pages news
Language(s) - English
Resource type - Journals
eISSN - 1811-1610
pISSN - 1811-1602
DOI - 10.22498/pages.18.1.6
Subject(s) - peat , paleoclimatology , test (biology) , geology , physical geography , archaeology , geography , paleontology , climate change , oceanography
Figure 2: Focus Interval III (cal a AD 800–1800) of the ACCROTELM project, showing proxy-climate data from the Danish bog site: Blue line = normalized testate amoebae water table reconstruction (inverted); Green dashed line = plant macrofossil Dupont wetness index; Gray line = normalized C relative production rate (q). Arrows indicate start of significant rises in water table. Historical solar minima are indicated. Figure adapted from Mauquoy et al., 2008. For further discussion of solar-climate relationships in peat records, see van Geel and Mauquoy, this issue.

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