Our knowledge of past sea-level change is largely relying on high-precision uranium/thorium disequilibrium dating on fossil corals.
Isotope Geochemistry - Wang Xianfeng
This research team uses istotope geochemistry as a tool to solve the mysteries of paleoclimate. Xianfeng Wang and his group seek to understand how hydro-climates change in the tropics during late Pleistocene and Holocene, how the changes relate to those in other parts of the world, if they are connected at all, and how tropical climate changes influence human society or vice versa.
To achieve these, the team works with both terrestrial and marine sediment samples from the tropics, including speleothems and corals. Sample ages are typically determined by high precision radiometric dating techniques, while their stable isotopic compositions and elemental ratios are often applied for semi-quantitative climate assessments and correlations.
The main areas of research involve the study of hydrology of climate through speleothem records and the study of corals as indicators of sea level changes.
Characterizing coral open-system behavior by high-precision U/Th dating: a case study in Sumba Island, Indonesia
Mercury Isotopes for Source Apportionment Study of Atmospheric Particle Bound Mercury in an Urban Setting
By studying mercury isotopes in particle bound mercury, Wang and team are trying to understand whether the isotopic composition is representative of anthropogenic pollution sources or is modified by atmospheric phenomenon.
In a joint effort involving tectonics, geomorphology, carbonate sedimentology, and geochronology, this project will revisit corals along Sumatra's northern coast to refine seisimic hazard estimates.
Any dramatic climate change in the tropical Indo-Pacific may threaten the livelihoods of more than half of the world’s population. The Isotope Geochemistry team is reconstructing past climate patterns to learn the ultimate mechanisms that drive...
Wang and his team are reconstructing the monsoon system dynamics for the past million years with cave deposits in China to determine the monsoon's predictability.
Coral-based Climate Variability in the Eastern Bay of Bengal during the Medieval Climate Anomaly and Little Ice Age
Wang and his team are analysing corals to reconstruct climate data from the last 500 years to understand the Indian Summer Monsoon and its influence on climate.