T89 Advances in Ocean and Climate Reconstructions from Environmental Proxies

Monday, 23 September 2019
8:00 AM - 12:00 PM
Room 228AB, North Building

OPTIMAL: A NEW MACHINE LEARNING APPROACH FOR GDGT-BASED PALAEOTHERMOMETRY

Paper number: T89-7
Program: Technical Sessions
Time: 9:35 AM – 9:50 AM

Authors

Abstract

The relative abundances of Glycerol dialkyl glycerol tetraether (GDGT) compounds produced by modern marine archaeal communities show a significant dependence on the local sea surface temperature at the site of formation. When preserved in ancient marine sediments, the measured abundances of these fossil lipid biomarkers thus have the potential to provide a geological record of long-term variability in sea surface temperatures. Several empirical calibrations have been made between observed GDGT relative abundances in late Holocene core top sediments, forming the basis of the widely used TEX86 palaeothermometer. There are, however, two outstanding problems with this approach, first the appropriate assignment of uncertainty to estimates of ancient sea surface temperatures based on the relationship of the ancient GDGT assemblage to the modern calibration data set; and second, the problem of making temperature estimates beyond the range of the modern empirical calibrations (>30 ºC). Here we apply modern machine-learning tools, including Gaussian Process Emulators and forward modelling, to develop a new mathematical approach we call OPTiMAL (Optimised Palaeothermometry from Tetraethers via MAchine Learning) to improve temperature estimation and the representation of uncertainty based on the relationship between ancient GDGT assemblage data and the structure of the modern calibration data set. We provide a new quantitative measure of the distance between an ancient GDGT assemblage and the nearest neighbour within the modern calibration dataset, as a test for significant non-analogue behaviour. We further reduce the root mean square uncertainty on temperature predictions (validated using the modern data set) from ~± 6 ºC using TEX86 based estimators to ± 3.6 ºC using Gaussian Process estimators for temperatures below 30 ºC.

Geological Society of America Abstracts with Programs. Vol. 51, No. 5

doi: 10.1130/abs/2019AM-338267

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