Solar forcing of climatic change during the mid-Holocene:indications from raised bogs in The Netherlands
Two cores of mid-Holocene raised-bog deposits from the Netherlands were C-14 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 Delta(14)C archive (probably caused by major declines in solar activity). The use of Delta(14)C 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 Holo... Mehr ...
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| Dokumenttyp: | Artikel |
| Erscheinungsdatum: | 2004 |
| Reihe/Periodikum: | Blaauw , M , Geel , B V & Plicht , J V D 2004 , ' Solar forcing of climatic change during the mid-Holocene : indications from raised bogs in The Netherlands ' , The Holocene , vol. 14 , no. 1 , pp. 35-44 . https://doi.org/10.1191/0959683604h1687rp |
| Schlagwörter: | climatic change / solar forcing / raised bogs / C-14 wiggle-match dating / mid-Holocene / wet-shifts / The Netherlands / COSMOGENIC NUCLIDE PRODUCTION / WEST EUROPEAN MIRES / HOLOCENE CLIMATE / YOUNGER DRYAS / BRITISH-ISLES / ATMOSPHERIC RADIOCARBON / ECOLOGICAL GRADIENTS / OCEAN CIRCULATION / CALLUNA-VULGARIS / BIOLOGICAL FLORA |
| Sprache: | Englisch |
| Permalink: | https://search.fid-benelux.de/Record/base-26825383 |
| Datenquelle: | BASE; Originalkatalog |
| Powered By: | BASE |
| Link(s) : | https://hdl.handle.net/11370/5f2e5352-2bd3-4d7d-a8dd-89417028a67a |
Two cores of mid-Holocene raised-bog deposits from the Netherlands were C-14 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 Delta(14)C archive (probably caused by major declines in solar activity). The use of Delta(14)C 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.