Last Deglacial Environmental Change in the Tropical South Pacific From Tahiti Corals

On glacial‐interglacial time scales, changes in the Earth's orbital configuration control climate seasonality and mean conditions. Tropical coral skeletons can be sampled at a sufficient resolution to reconstruct past seasonality. Here, last deglacial Porites skeletons from Integrated Ocean Drilling Program Expedition 310 to Tahiti are investigated and, supported by a modern calibration, monthly resolved time series in geochemical proxies (Sr/Ca, δ 18 O, δ 13 C) are constructed. For most of the deglaciation, Sr/Ca seasonality was similar to modern (0.139 ± 0.010 mmol mol −1 ; 2.8 ± 0.2°C) reflecting the small change in insolation seasonality. However, during the Younger Dryas, high values in Sr/Ca seasonality (0.171 ± 0.017 mmol mol −1 ; 3.4 ± 0.3°C) suggest a reduced mixed layer depth and enhanced influence of the South Pacific Subtropical Gyre due to South Pacific Convergence Zone (SPCZ) inactivity. Furthermore, high amplitudes in Younger Dryas skeletal δ 18 O (0.40 ± 0.22 ‰) and δ 13 C (0.86 ± 0.22 ‰) seasonality compared to modern (δ 18 O = 0.29 ± 0.08 ‰; δ 13 C = 0.27 ± 0.08 ‰) point to elevated winter‐summer discrepancies in rainfall and runoff. Mean coral Sr/Ca variability suggests an influence of Northern Hemisphere climate events, such as the Younger Dryas cooling (+0.134 ± 0.012 mmol mol −1 ;−2.6 ± 0.2°C), or the Bølling–Allerød warming (+0.032 ± 0.040 mmol mol −1 ; −0.6 ± 0.4°C). Deglacial mean coral Δδ 18 O (δ 18 O seawater contribution to skeletal δ 18 O), corrected for the ice volume effect, was elevated pointing to more saline, thus dryer conditions, likely due to a northward migration of the SPCZ. Seasonal cycles in coral δ 13 C were likely caused by variations in linear extension rates that were reduced during the last deglaciation (1.00 ± 0.6 cm year −1 ) compared to today (1.6 ± 0.3 cm year −1 ).