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World Ocean 14C plateau tuning
On the basis of minor time scale adjustments including the synchronization on IntCal20 the Suigetsu-based atmospheric 14C plateau structures are shown to be authentic. Their global significance is demonstrated by the coherence with the tree ring record 10 to 15 cal. ka. The suite of atmospheric structures can be recognized in high-resolution ocean sediment records independent of various processes leading to partial distortion of a sediment record. This provides a unique tool for global stratigraphic correlation and paleoceanographic studies as shown by supplementary figures and tables from 19 cores obtained from key locations in the world ocean
Age determination results from site Voorthuizen
Age determination results from site Voorthuize
Age determination results from site Pessey-Sonnaz
Age determination results from site Pessey-Sonna
Age determination results from site Samerberg
Age determination results from site Samerber
Age determination results from site Amersfoort
Age determination results from site Amersfoor
Age determination results from site La_Croix_Rouge
Age determination results from site La_Croix_Roug
Age determination results from site Beaverdam_Creek
Age determination results from site Beaverdam_Cree
Age determination results from site Aschersleben
Age determination results from site Ascherslebe
Age determination results from site La_Flachere
Age determination results from site La_Flacher
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