Radiocarbon calibration beyond 20,000 C-14 yr BP by means of planktonic foraminifera of the Iberian Margin

摘要

We present a new set of C-14 ages obtained by accelerator mass spectrometry (AMS) on planktonic foraminifera from a deep-sea core collected off the Iberian Margin (MD952042). This site, at 37 degreesN, is distant from the high-latitude zones where C-14 reservoir age is large and variable. Many independent proxies - alkenones, magnetic susceptibility, ice-rafted debris, foraminifera stable isotopes, abundances of foraminifera, pollen, and dinoflagellates - show abrupt changes correlative with Dansgaard-Oeschger and Heinrich events of the last glacial period. The good stratigraphic agreement of all proxies - from the fine to the coarse-size fractions - indicates that the foraminifera C-14 ages are representative of the different sediment fractions. To obtain reliable C-14 ages of foraminifera beyond 20,000 C-14 yr B.P., we leached the shells prior to carbonate hydrolysis and subsequent analysis. For a calendar age scale, we matched the Iberian Margin U-37'(K) profile with that of Greenland Summit delta(18)O. Both are proxies for temperature, which in models varies synchronously in the two areas. The match creates no spurious jumps in sedimentation rate and requires only a limited number of tie points. Except for ages older than 40,000 C-14 yr B.P., Greenland's GISP2 and GRIP records yield similar calendars. The C-14 and imported calendar ages of the Iberian Margin record are then compared to data - from lacustrine annual varves and from corals and speleothems dated by U-Th - previously used to extend the calibration beyond 20,000 14C yr B.P. The new record follows a smooth pattern between 23,000 and 50,000 cat yr B.P. We find good agreement with the previous data sets between 23,000 and 31,000 cal yrB.P. In the interval between 33,000 and 41,000 Cal yrB.P., for which previous records disagree by up to 5000 cat yr, the Iberian Margin record closely follows the polynomial curve that was previously defined by an interpolation of the coral ages and runs between the Lake Suigetsu and the Bahamian speleothem data sets. (C) 2004 University of Washington. All rights reserved.