Development and Application of the Branched and Isoprenoid GDGT Machine Learning Classification Algorithm (BIGMaC) for Paleoenvironmental Reconstruction
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Final Published Version
Author
Martínez-Sosa, P.Tierney, J.E.
Pérez-Angel, L.C.
Stefanescu, I.C.
Guo, J.
Kirkels, F.
Sepúlveda, J.
Peterse, F.
Shuman, B.N.
Reyes, A.V.
Affiliation
Department of Geosciences, The University of ArizonaIssue Date
2023-07-06
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John Wiley and Sons IncCitation
Martínez-Sosa, P., Tierney, J. E., Pérez-Angel, L. C., Stefanescu, I. C., Guo, J., Kirkels, F., et al. (2023). Development and application of the branched and isoprenoid GDGT machine learning classification algorithm (BIGMaC) for paleoenvironmental reconstruction. Paleoceanography and Paleoclimatology, 38, e2023PA004611. https://doi.org/10.1029/2023PA004611Rights
© 2023. American Geophysical Union. All Rights Reserved.Collection Information
This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.Abstract
Glycerol dialkyl glycerol tetraethers (GDGTs), both archaeal isoprenoid GDGTs (isoGDGTs) and bacterial branched GDGTs (brGDGTs), have been used in paleoclimate studies to reconstruct environmental conditions. Since GDGTs are produced in many types of environments, their relative abundances also depend on the depositional setting. This suggests that the distribution of GDGTs also preserves useful information that can be used more broadly to infer these depositional environments in the geological past. Here, we combined existing iso- and brGDGT relative abundance data with newly analyzed samples to generate a database of 1,153 samples from several modern sedimentary settings. We observed a robust relationship between the depositional environment and the relative abundances of GDGTs in our samples. This data set was used to train and test the Branched and isoGDGT Machine learning Classification (BIGMaC) algorithm, which identifies the environment a sample comes from based on the distribution of GDGTs with high precision and recall (F1 = 0.95). We tested the model on the sedimentary record from the Giraffe kimberlite pipe, an Eocene maar in subantarctic Canada, and found that the BIGMaC reconstruction agrees with independent stratigraphic and palynological information, provides new information about the paleoenvironment of this site, and helps improve its paleotemperature reconstruction. In contrast, we also include an example from the PETM-aged Cobham lignite as a cautionary example that illustrates the limitations of the algorithm. We propose that in cases where paleoenvironments are unknown or are changing, BIGMaC can be applied in concert with other proxies to generate more refined paleoclimate records. © 2023. American Geophysical Union. All Rights Reserved.Note
6 month embargo; first published 06 July 2023ISSN
2572-4517Version
Final Published Versionae974a485f413a2113503eed53cd6c53
10.1029/2023PA004611
