The Phytolith 14 C Puzzle: A Tale of Background Determinations and Accuracy Tests
Over the past decades, analysis of occluded carbon in phytoliths (opaline silica mineral bodies that form in and between plant cells) has become a workhorse of paleoclimate and archaeological studies. Since different plant types exhibit distinctive phytolith morphologies, their assemblages are used...
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Veröffentlicht in: | Radiocarbon 2010, Vol.52 (1), p.113-128 |
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Format: | Artikel |
Sprache: | eng |
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Zusammenfassung: | Over the past decades, analysis of occluded carbon in phytoliths (opaline silica mineral bodies that form in and between plant cells) has become a workhorse of paleoclimate and archaeological studies. Since different plant types exhibit distinctive phytolith morphologies, their assemblages are used in identifying vegetation histories or food culture adaptations. A few direct radiocarbon AMS measurements of phytoliths have been carried out, but these measurements are difficult due to the low concentrations of phytoliths in some plant species, and the small amount of C per phytolith ( |
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ISSN: | 0033-8222 1945-5755 |
DOI: | 10.1017/S0033822200045070 |