GC001
Advances and applications in Quaternary geochronology
Advances and applications in Quaternary geochronology
Session ID#: 79646
Session Description:
Reconstructing climate and environmental change throughout the Quaternary relies on precise and accurate chronologies to determine sequences of events. Inter-chronometer calibration is often critical, as no one dating approach can be applied to all geological archives. Although radiocarbon dating continues to be pivotal in providing chronological control over the last 50,000 years, other geochronological techniques (e.g., cosmogenic isotopes, tephrochronology, astronomical dating, luminescence dating, palaeomagnetism, Ar/Ar dating, U-series) have become increasingly essential for the accurate and precise reconstruction of Quaternary climatic evolution, both within and beyond the timescales accessed with radiocarbon. This session welcomes contributions that (1) aim to reduce and/or quantify uncertainties in any Quaternary dating method, including high-resolution radiocarbon, (2) improve geochronological methods to define and answer new questions about Quaternary climate evolution, and (3) combine different chronometric techniques to reconstruct the timescales of Earth system change during the Quaternary.
Index Terms:
1105 Quaternary geochronology [GEOCHRONOLOGY]
Primary Convener: Darren F Mark, Scottish Universities Environmental Research Center at the University of Glasgow, East Kilbride, United Kingdom
Conveners: Marissa M Tremblay, University of California Berkeley, Department of Earth and Planetary Science, Berkeley, CA, United States, Courtney Sprain, University of Liverpool, Department of Earth, Ocean and Ecological Sciences, Liverpool, United Kingdom and Noah McLean, University of Kansas, Kansas, United States
Primary Liaison: Darren F Mark, SUERC, East Kilbride, United Kingdom
See more of: Global Environmental Change
