Massive scleractinian corals growing in our tropical oceans are ideal environmental and climate archives because of their ability to record changes in ocean-atmosphere interactions in its calcium carbonate skeletons. The skeletons of these corals are continuously deposited for up to hundreds of years at a single location and Dr. Wu’s research is focused on using the geochemical signatures locked inside these skeletal materials to understand climate change of the past two thousand years.
Dr. Wu and his research team have investigated the behavior of tropical climate in the Common Era over multiple timescales from the sub-seasonal to the decadal-interdecadal and centennial using corals. His research group’s use of paleoclimate and paleoceanographic proxies (physical characteristics of the past represented as direct measurements) such as stable isotopes (e.g. δ13C, δ18O, δ11B) and trace elements (e.g. Sr, Li, Mg) are common in marine biogeochemistry and enables the reconstruction of past climate from coral skeletons. Coral core samples as recorders of the environment can be of modern age existing in the anthropogenic era or fossilized specimens from the deeper geological past.
Many of the research questions central to Dr. Wu's investigations involve the large-scale changes of tropical ocean sea surface temperature (SST), salinity (SSS), evaporation-precipitation, seawater pH and carbonate chemistry, and ocean circulations. The ocean and climate change interpretations are only as accurate as the proxy and Dr. Wu also aims to improve the reproducibility and reliability of proxies’ analyses and reconstructions. Finally, understanding the changes and interactions of the ocean-atmosphere and climate systems in the past will be critical to predicting climate under future climate change scenarios.
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- OASIS Project Webpage
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- Ocean Acidification
- Coral-based climate reconstructions
- Climate and the collapse of the Maya Civilization
- Study sites of the Coral Climatology Research Group
- Research approaches and methods
Current Research Topics
Make Our Planet Great Again!
The pumping of CO2 into our Earth's atmosphere since the Industrial Revolution not only warms our planet due to the Greenhouse Effect but the absorption of anthropogenic atmospheric CO2 by our oceans is also severely impacting calcifying animals living in our tropical oceans.
Using corals as archives to document climate change: X-radiograph of coral growth revealing the density layers deposited every year similar to tree rings or ice cores.
Reconstructing sub-seasonal climate and surface ocean conditions or variations (e.g. sea surface temperature, salinity) in the tropical Indo-Pacific using coral geochemical records, also known as proxy records (e.g. stable isotopes, trace elements).
We use the proxy records from coral skeletal materials to interpret long-term deviations or changes in the Pacific Ocean such as the significant spatial and temporal evolution of the El Niño/Southern Oscillation (ENSO) seen here based on SST variations.
We use precisely dated fossil coral skeleton records to interpret the changes in climate (e.g. sea surface temperature, salinity, precipitation) on the Yucatán Peninsula, which led to the prolonged droughts that possibly brought on the demise of the Maya Civilization during the Termical Classic Period (Year 750–1050 Common Era).
- Previous and Current locations: Palau, Clipperton Atoll, Fiji, Tonga, Rarotonga, Bonaire, Indonesia, China, New Caledonia, Costa Rica, Cuba, Puerto Rico, Fanning Island, Wallis and Futuna, Tuvalu, Tokelau, Rotuma.
- Coming Soon: Caribbean Sea.
When not out in the field observing and collecting coral samples for science, our research team spends a lot of time in the chemistry laboratory preparing and analyzing the tropical coral samples for stable isotopes and trace elements as climate and environmental proxies.
We utilize the high precision Isotope Ratio Mass Spectrometer (IRMS; Thermo Fischer Scientific MAT 253) for the analysis of the proxies, δ13C and δ18O.
For trace elements analyses, we utilize the Inductively Coupled Plasma – Mass Spectrometer (ICP-MS; Analytik Jena Q-ICP-MS) and Optical Emissions Spectrometer (ICP-OES; Spectro Cirro ICP-OES) to understand the changes of Sr/Ca, Li/Mg, B/Ca, U/Ca, Ba/Ca, and other ratios.
For coral skeletal δ11B signature analysis, we require the Multi-Collector ICP-MS (Thermo Fischer Scientific Neptune Plus MC-ICP-MS).
The Scanning Electron Microscopy (SEM) is also often utilized to examine the fine and detailed skeletal microstructures of the coral samples for chemical and biological alterations and preservation state.