SEA LEVELS, SEA SURFACE TEMPERATURES AND EL NINO VARIABILITY DURING WARM INTERGLACIATIONS. Sea levels, sea surface temperatures and the variability of El Niño will be determined for previous warm interglacial periods using well dated, stratigraphically controlled fossil corals preserved in uplifted reefs. Relationships between past changes in sea level and warmer ocean temperatures will provide insights into the response of sea level to global warming. Knowledge of the frequency and amplitude o ....SEA LEVELS, SEA SURFACE TEMPERATURES AND EL NINO VARIABILITY DURING WARM INTERGLACIATIONS. Sea levels, sea surface temperatures and the variability of El Niño will be determined for previous warm interglacial periods using well dated, stratigraphically controlled fossil corals preserved in uplifted reefs. Relationships between past changes in sea level and warmer ocean temperatures will provide insights into the response of sea level to global warming. Knowledge of the frequency and amplitude of El Nino events that occurred during previous interglacial warm periods will provide a better understanding of processes controlling extreme events in the climate system.Read moreRead less
UPTAKE OF ATMOSPHERIC CO2 IN THE OCEANS AND IMPLICATIONS FOR GLOBAL CHANGE: NEW PROXY DEVELOPMENTS. This project aims to quantify the response of the oceans to increasing atmospheric CO2 from anthropogenic production. This will be achieved by using newly developed paleoceanographic indicators in deep sea sediments, corals and coralline sponges. These will be used to evaluate changes in seawater acidity and the response of the oceans to past variations in atmospheric CO2. The capacity and role o ....UPTAKE OF ATMOSPHERIC CO2 IN THE OCEANS AND IMPLICATIONS FOR GLOBAL CHANGE: NEW PROXY DEVELOPMENTS. This project aims to quantify the response of the oceans to increasing atmospheric CO2 from anthropogenic production. This will be achieved by using newly developed paleoceanographic indicators in deep sea sediments, corals and coralline sponges. These will be used to evaluate changes in seawater acidity and the response of the oceans to past variations in atmospheric CO2. The capacity and role of the oceans to buffer the rise of atmospheric of CO2 will be ascertained. This will provide constraints on the impact of increased seawater acidity on coral reefs such as the Great Barrier Reef.Read moreRead less
The key role of the Southern Ocean in atmospheric CO2 sequestration. The integrated approach proposed in this study aims to quantify past changes in marine productivity and its role in controlling past atmospheric CO2 variations. This will be achieved by studying deep sea sediments from the Southern Ocean, a key area with a fundamental importance in the global ocean biological pump. This research will enhance our understanding of the linkages connecting marine biota, the ocean carbon cycle and g ....The key role of the Southern Ocean in atmospheric CO2 sequestration. The integrated approach proposed in this study aims to quantify past changes in marine productivity and its role in controlling past atmospheric CO2 variations. This will be achieved by studying deep sea sediments from the Southern Ocean, a key area with a fundamental importance in the global ocean biological pump. This research will enhance our understanding of the linkages connecting marine biota, the ocean carbon cycle and global climate, providing the basis for more reliable predictions about the impacts of the recent rapid atmospheric CO2 increase. Possible remediation solutions involving marine phytoplankton to this CO2 excess will be thoroughly assessed.Read moreRead less