Solar forcing of climate change during the mid-Holocene: indications from raised bogs in the Netherlands.

Maarten Blaauw, B. Van Geel, J. Van Der Plicht

Research output: Contribution to journalArticlepeer-review

97 Citations (Scopus)

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 languageEnglish
Pages (from-to)35-44
Number of pages10
JournalThe Holocene
Volume14(1)
Issue number1
DOIs
Publication statusPublished - Jan 2004

ASJC Scopus subject areas

  • Earth and Planetary Sciences (miscellaneous)

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