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Title: Radiocarbon variability in the western equatorial Pacific inferred from a high-resolution coral record from Nauru Island

Journal Article · · Journal of Geophysical Research
DOI:https://doi.org/10.1029/98JC02271· OSTI ID:670200
;  [1]; ;  [2]
  1. Department of Earth and Planetary Sciences, Harvard University, Cambridge, Massachusetts (United States)
  2. Center for Accelerator Mass Spectrometry, Lawrence Livermore National Laboratory, Livermore, California (United States)

We have generated a high resolution coral {Delta}{sup 14}C record spanning the last 50 years to document the seasonal and interannual redistribution of surface waters in the western tropical Pacific. Prebomb (1947{endash}1956) {Delta}{sup 14}C values average {minus}63{per_thousand} and have a total range of 30{per_thousand}. Values begin to increase in 1957, reaching a maximum of 137{per_thousand} in mid-1983. Large interannual variability of up to 80{per_thousand} closely follows the El Ni{tilde n}o-Southern Oscillation (ENSO). During each ENSO warm phase, {Delta}{sup 14}C values begin to increase, reflecting the reduction of low-{sup 14}C water upwelling in the east and the invasion of subtropical water into the western equatorial tropical Pacific. Maximum {Delta}{sup 14}C values are in phase or lag the corresponding sea surface temperature maxima in the eastern tropical Pacific, whereas the rapid return to more negative {Delta}{sup 14}C is in phase with eastern Pacific ENSO indices. The highest-amplitude excursions occur during the 1965/1966 and 1972/1973 events, when the {sup 14}C contrast is highest between the eastern Pacific and subtropics. The 1982/1983 El Ni{tilde n}o, although a larger ENSO event, has a lower {Delta}{sup 14}C amplitude, reflecting the penetration of bomb radiocarbon into the equatorial undercurrent and the reduced contrast in {Delta}{sup 14}C between thermocline and subtropical surface waters at that time. This coral record demonstrates the potential for using similar radiocarbon time series for documenting variability in Pacific shallow circulation over interannual and decadal timescales. {copyright} 1998 American Geophysical Union

OSTI ID:
670200
Journal Information:
Journal of Geophysical Research, Vol. 103, Issue C11; Other Information: PBD: Oct 1998
Country of Publication:
United States
Language:
English