Abstract
Two cores of mid-Holocene raised-bog deposits from the Netherlands were 14C wiggle-match dated at high precision. Changes in local moisture conditions were inferred from the changing species composition of consecutive series of macrofossil samples. Several wet-shifts were inferred, and these were often coeval with major rises in the D14C archive (probably caused by major declines in solar activity). The use of D14C as a proxy for changes in solar activity is validated. This paper adds to the increasing body of evidence that solar variability forced climatic changes during the Holocene.
Original language | English |
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Pages (from-to) | 35-44 |
Number of pages | 10 |
Journal | The Holocene |
Volume | 14(1) |
Issue number | 1 |
DOIs | |
Publication status | Published - Jan 2004 |
ASJC Scopus subject areas
- Earth and Planetary Sciences (miscellaneous)