Coral oxygen isotope records of interdecadal climate variations in the South Pacific Convergence Zone region

The South Pacific Convergence Zone (SPCZ), a region of high rainfall, is a major feature of subtropical Southern Hemisphere climate and contributes to and interacts with circulation features across the Pacific, yet its past temporal variability and forcing remain only partially understood. Here we compare coral oxygen isotopic (δ 18 O) series (spanning A.D. 1997–1780 and A.D. 2001–1776) from two genera of hermatypic corals in Fiji, located within the SPCZ, to examine the fidelity of these corals in recording climate change and SPCZ interdecadal dynamics. One of these coral records is a new 225‐year subannually resolved δ 18 O series from the massive coral Diploastrea heliopora . Diploastrea 's use in climate reconstructions is still relatively new, but this coral has shown encouragingly similar interannual variability to Porites , the coral genus most commonly used in Pacific paleoclimate studies. In Fiji we observe that interdecadal δ 18 O variance is also similar in these two coral genera, and Diploastrea contains a larger‐amplitude interdecadal signal that more closely tracks instrumental‐based indices of Pacific interdecadal climate change and the SPCZ than Porites . Both coral δ 18 O series record greater interdecadal variability from ∼1880 to 1950, which is consistent with the observations of Folland et al. (2002), who reported higher variability in SPCZ position before 1945. These observations indicate that Diploastrea will likely provide a significant new source of long‐term climate information from the SPCZ region.