Upcoming Expedition to the southwest Pacific
SUMMER 2019 Next summer a team of researchers from UT Austin (including myself!) are headed to Vanuatu in the southwest Pacific to collect corals that were alive ~21,000 years during the Last Glacial Maximum (LGM). This is an NSF-sponsored expedition entitled “Fossil Coral Records of ENSO during the Last Glacial Period” (award). We are building a customized drill designed to core a series of holes up to 30 m deep along the southern coast of Espiritu Santo, Vanuatu. The rapid uplift of 6-7 mm/yr raised corals from 120 m depth to ~20-30 m below present day sea level. High-precision uranium-thorium dating will confirm the ages of the collected coral material.
The study will investigate ENSO variability during the LGM. Reconstructing ENSO variability during the LGM will help us understand the nature of ENSO activity during a very different background state compared to today. The reconstructed climate data from this study will help validate climate models that simulate past ENSO variability, many of which are also also used forecast future changes in ENSO with climate change.
UT AUstin MARINE GEOLOGY & GEOPHYSICS FIELD COURSE
MAY-JUNE 2017 This summer course teaches University of Texas students valuable field skills about the collection, processing, and analysis of shipboard measurements, including seismic, CHIRP, and side-scan sonar data. We also collected a marine sediment core. This year’s study site was offshore of Galveston, TX to study the sedimentary evolution of the Trinity River during the late Quaternary.
GULF OF MEXICO SEDIMENT TRAP DEPLOYMENT
NOVEMBER 2015 I participated in a short research cruise aboard the R/V Point Sur to deploy a new sediment trap in the Gulf of Mexico. The scientific team consisted of graduate and undergraduate students and researchers from the USGS, UT Austin, and the University of South Carolina. This fieldwork was conducted as part of the long-term USGS Paleoclimate Proxy Calibration project that uses the collected sediment trap data to establish the relationship between the shell chemistry of marine microfossils and modern ocean conditions. The relationship is used to calibrate paleoclimate reconstructions for the Gulf of Mexico.