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Development and Application of the Branched and Isoprenoid GDGT Machine Learning Classification Algorithm (BIGMaC) for Paleoenvironmental Reconstruction

沉积沉积环境 古气候学 地质学 古生物学 相对物种丰度 沉积岩 丰度(生态学) 海洋学 生态学 气候变化 生物 构造盆地
作者
Pablo Martínez‐Sosa,Jessica E. Tierney,Lina C. Pérez‐Angel,Ioana C. Stefanescu,Jingjing Guo,Frédérique Kirkels,Julio Sepúlveda,Francien Peterse,Bryan N. Shuman,Alberto V. Reyes
出处
期刊:Paleoceanography and paleoclimatology [Wiley]
卷期号:38 (7) 被引量:1
标识
DOI:10.1029/2023pa004611
摘要

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 B ranched and isoGDGT Ma chine learning C lassification (BIGMaC) algorithm, which identifies the environment a sample comes from based on the distribution of GDGTs with high precision and recall ( F 1 = 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.

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