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        <gco:CharacterString>STUDY NOTES: Rarotonga coral radiocarbon (14C) timeseries. Coral radiocarbon (Delta-14C) on untreated, low-speed drilled samples. Precision is Â±4 per mil as documented by an in-house homogenized coral standard, and presented as AGE CORRECTED DELTA-14C [see Stuiver &amp; Polach, 1977]. The sample cores were made on a Porites lutea coral located in openmarine conditions off Rarotonga. Cores were split and cleaned with distilled water. After identifying the major vertical growth axis, the coral was sequentially sampled at 1 mm increments with a low-speed drill. Splits (~1 mg) were reacted in vacuo in a modified autocarbonate device at 90Â°C and the purified CO2 analyzed on a gas source stable isotope ratio mass spectrometer. Additional splits were analyzedby ICP-AES for Sr, and Ca. The delta-18O and [Sr/Ca] results wereindividually mapped to the Kaplan OI and IGOSS sea surface temperaturetime-series for the grid box containing Rarotonga. The resulting age modelindicates an average linear extension rate on the order of 16mm/yr withan estimated age-model error of Â±1 month. For the interval 1959-1997,approximately every other sample was analyzed for 14C (~8samples/yr), andfor the interval 1950-1959 every sample was analyzed. Splits (~10mg) were placed in individual reaction chambers, evacuated, heated, and then acidified with orthophosphoric acid at 90Â°C. The evolved CO2 was purified, trapped, and converted to graphite in the presence of cobalt catalyst in individual reactors [Vogel et al., 1987].Graphite targets were measured at the Center for Accelerator Mass Spectrometry, Lawrence Livermore National Laboratory [Davis et al., 1990]. Radiocarbon results are reported as Delta-14C (per mil) as defined by Stuiver and Polach [1977] and include the d13C correction obtained from the stable isotope results and are "age corrected". Analytical precision and accuracy of the radiocarbon measurements is Â±4 per mil (1s) based on repeated analyses of an in-house homogenized near-modern coral and accepted secondary and tertiary radiocarbon standards. WATER DEPTH: Top of coral water depth 18m. CORE LENGTH: 3.7m. DATE OF COLLECTION: 03/97 (J. Wellington et al.) 
ABSTRACT SUPPLIED BY ORIGINATOR: We have generated a high-resolution coral Î14C record from the southwest subtropical Pacific spanning the last 50 yr. Prebomb (1950â1956) Î14C values average â52%. Values begin to increase in 1957, reaching a maximum in the early 1970s, about 10 yr after the atmospheric peak. There is a consistent 10â15% seasonal cycle whose relationship with vertical mixing evolves as a consequence of the penetration of the bomb transient into subsurface waters. Comparison of this record with that simulated in an ocean general circulation model highlights the difficulty in modeling vertical exchange processes.</gco:CharacterString>
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