129I/127I and Δ14C records in a modern coral from Rowley Shoals off northwestern Australia reflect the 20th-century human nuclear activities and ocean/atmosphere circulations

Highlights: • ¹²⁹I/¹²⁷I and Δ¹⁴C data of modern coral annual bands in Rowley Shoals are presented. • Natural (non-anthropogenic) ¹²⁹I/¹²⁷I and Δ¹⁴C levels in Rowley Shoals are evaluated. • ¹²⁹I from the US Pacific bomb tests was conveyed to Rowley Shoals by ocean currents. • ¹²⁹I is more conservative than ¹⁴C, as an anthropogenic tracer of ocean currents. • Airborne ¹²⁹I from nuclear-fuel reprocessing plants has an impact on Rowley Shoals. Radionuclides produced by 20th-century human nuclear activities from 1945 (e.g., atmospheric nuclear explosions and nuclear-fuel reprocessing) made significant impacts on earth's surface environments. Long-lived shallow-water corals living in tropical/subtropical seas incorporate the anthropogenically-produced radionuclides, including ¹²⁹I and ¹⁴C, into their skeletons, and provide time series records of the impacts of nuclear activities. Here, we present ¹²⁹I/¹²⁷I and Δ¹⁴C time series records of an annually-banded modern coral skeleton from Rowley Shoals, off the northwestern coast of Australia, in the far eastern Indian Ocean. The ¹²⁹I/¹²⁷I and Δ¹⁴C records, covering the period 1930s−1990s, exhibit distinct increases caused by the nuclear activities, and their increasing profiles are clearly different from each other. The first distinct ¹²⁹I/¹²⁷I increase occurs from 1955 to 1959, followed by a decrease in 1960–1963. The increase is probably due to US atmospheric nuclear explosions in Bikini and Eniwetok Atolls in 1954, 1956 and 1958. The ¹²⁹I produced in those nuclear tests would be transported by the North Equatorial Current, a portion of which passes through the Indonesian Throughflow and then reaches Rowley Shoals. This initial increase from 1955 is, however, absent in the Δ¹⁴C record, which shows a distinct increase from 1959 and its peak around the mid-1970s, followed by a gradual decrease. This absence and the 4-year-delayed Δ¹⁴C increase are likely due to dilution of explosion-produced ¹⁴C with natural carbon (by seawater mixing and air-sea gas exchange) being much more intense than that of explosion-produced ¹²⁹I with natural iodine (by the same processes), suggesting that the ¹²⁹I/¹²⁷I ratio is a more conservative anthropogenic tracer in surface ocean waters, as compared to Δ¹⁴C. The second ¹²⁹I/¹²⁷I increase is contemporaneous with a rapid Δ¹⁴C increase during 1964–1967, followed by a rapid ¹²⁹I/¹²⁷I decrease in 1968–1969; the increases can be ascribed to very large atmospheric nuclear explosions conducted in the former Soviet Union in 1961–1962. The third ¹²⁹I/¹²⁷I increase appears between 1969/1970 and 1992, which can be attributed to airborne ¹²⁹I released from nuclear-fuel reprocessing facilities in Europe, the former Soviet Union and the US. The coral ¹²⁹I/¹²⁷I and Δ¹⁴C time series records, combined with previous studies, enhance our understanding of the behavior of anthropogenic ¹²⁹I and ¹⁴C in the global ocean and atmosphere.