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Spatial and Temporal Robustness of Sr/Ca‐SST Calibrations in Red Sea Corals: Evidence for Influence of Mean Annual Temperature on Calibration Slopes

Authors :
Nathalie F. Goodkin
Konrad A Hughen
Justin E. Ossolinski
R. S. Davis
S. A. Murty
Whitney N. Bernstein
Asian School of the Environment
Interdisciplinary Graduate School (IGS)
Earth Observatory of Singapore
Source :
Paleoceanography and Paleoclimatology. 33:443-456
Publication Year :
2018
Publisher :
American Geophysical Union (AGU), 2018.

Abstract

Sr/Ca ratios recorded in the aragonite skeleton of massive coral colonies are commonly used to reconstruct seasonal‐ to centennial‐scale variability in sea surface temperature (SST). While the Sr/Ca paleothermometer is robust in individual colonies, Sr/Ca‐SST relationships between colonies vary, leading to questions regarding the utility of the proxy. We present biweekly‐resolution calibrations of Sr/Ca from five Porites spp. corals to satellite SST across 10° of latitude in the Red Sea to evaluate the Sr/Ca proxy across both spatial and temporal scales. SST is significantly correlated with coral Sr/Ca at each site, accounting for 69–84% of Sr/Ca variability (P ≪ 0.01). Intercolony variability in Sr/Ca‐SST sensitivities reveals a latitudinal trend, where calibration slopes become shallower with increasing mean annual temperature. Mean annual temperature is strongly correlated with the biweekly‐resolution calibration slopes across five Red Sea sites (r2 = 0.88, P = 0.05), while also correlating significantly to Sr/Ca‐SST slopes for 33 Porites corals from across the entire Indo‐Pacific region (r2 = 0.26, P < 0.01). Although interannual summer, winter, and mean annual calibrations for individual Red Sea colonies are inconsistently robust, combined multicoral calibrations are significant at summer (r2 = 0.53, P ≪ 0.01), winter (r2 = 0.62, P ≪ 0.01), and mean annual time scales (r2 = 0.79, P ≪ 0.01). Our multicoral, multisite study indicates that the Sr/Ca paleothermometer is accurate across both temporal and spatial scales in the Red Sea and also potentially explains for the first time variability in Sr/Ca‐SST calibration slopes across the Indo‐Pacific region. Our study provides strong evidence supporting the robustness of the coral Sr/Ca proxy for examining seasonal to multicentury variability in global climate phenomena. NRF (Natl Research Foundation, S’pore) MOE (Min. of Education, S’pore) Published version

Details

ISSN :
25724525 and 25724517
Volume :
33
Database :
OpenAIRE
Journal :
Paleoceanography and Paleoclimatology
Accession number :
edsair.doi.dedup.....94a316ac38a870a61af74c6fa6864bbe
Full Text :
https://doi.org/10.1029/2017pa003276