Collaborative Research: Extracting multi-century low-latitude sea surface temperatures from coral skeletons using replicated records of annual growth: method refinement & application

Lead PI: Dr. Braddock K. Linsley , Anne Cohen, Delia Oppo

Unit Affiliation: Biology and Paleo Environment, Lamont-Doherty Earth Observatory (LDEO)

September 2011 - August 2013
Pacific Ocean ; Fiji ; Tonga ; Lamont Doherty Earth Observatory ; Woods Hole Oceanographic Institution
Project Type: Research

DESCRIPTION: Proxy reconstructions of global temperatures over the past 1000 years provide a context for understanding recent warming trends and allow better estimates of the contribution of anthropogenic (greenhouse gas) forcing to global climate change. Data compiled mostly from high latitude tree ring records suggest that the late 20th century was the warmest period of the last millennium. Nevertheless, the uncertainties associated with these estimates are significant, especially during the period known as the Medieval Warming which ended ~700 years ago. Temperature changes at the earth?s surface follow most closely those of the global tropics, which are 75% ocean; yet few datasets that span the last 1000 years exist from the low latitude oceans. In order to improve global temperature reconstructions and to reduce uncertainties, well-replicated records of sea surface temperature (SST) from the low-latitude oceans are urgently needed.

Massive long-lived corals, which accrete calcium carbonate skeleton in annual bands like growth rings on a tree, have the potential to provide this information. The PIs have recently applied a method of reconstructing annual SST that takes advantage of the demonstrated relationship between the skeletal growth of corals and water temperature. In multiple records generated from 3 coral species, coral growth captures between 50-60% of the SST variability in the instrumental record, on interannual and longer timescales. Applying the method to a ~440-year long slow-growing coral collected from the Bahamas suggests that SSTs were within error of modern ~ AD1550, that Little Ice Age SSTs were about 1ÂșC cooler than today and that there is a strong anthropogenic signal in the SSTs of the last 50 years. The PIs will build on this initial work, focusing on refining the method of extracting SST from coral growth records and applying it to generate multi-century long proxy SST records for the low-latitude Atlantic and Pacific Oceans. Data acquisition by 3-D CAT scanning of intact coral cores is relatively rapid and inexpensive, enabling generation of many records of varying lengths from multiple colonies at each site, and, using techniques applied in dendrochronology, provide enough data to provide realistic error estimates on reconstructed SSTs. Funding will support 3 PIs, a post-doctoral research scientist, a PhD student, and research experience for an undergraduate.

OUTCOMES: No relationship between skeletal extension rate and SST was found. A decreasing trend in skeletal growth was found which has been linked to anthropogenic changes in the atmospheric CO2 reservoir. Three journal publications, four abstracts, and two student symposia completed.


National Science Foundation (NSF)




Woods Hole Oceanographic Institution



Dassie, E.P. G. M. Lemely, B. K. Linsley. "The Suess Effect in Fiji coral d13C and its potential as a tracer of anthropogenic CO2 uptake," Palaeography, Palaeoclimatology, Palaeoecology, v.370, 2013, p. 30. doi:vol 370, 30-40, 2013

Wu, H. B. K. Linsley, E. Dassie, B. Schiraldi, P. deMenocal. "Oceanographic variability in the South Paci?c Convergence Zone region over the last 210 years from multi-site coral Sr/Ca records," Geophys. Geochem., Geosys (G^3), v.May 17, 2013. doi:doi:10.1029/2012GC004293


sea surface temperature ocean and climate physics coral growth rates fossil corals paleoclimate