LIPOTHERM: A Calibration Framework for GDGT Paleothermometry Based on Machine Learning

IF 3.3 2区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Vikash Kumar, Manish Tiwari, Biswajit Roy
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引用次数: 0

Abstract

SST reconstruction from glycerol dialkyl glycerol tetraethers (GDGT) preserved in marine sediments is an important tool in quantitative paleoclimatology. These reconstructions require calibration frameworks that provide mapping between sediment GDGT data and temperature values. Improvements in modeling and data coverage can reduce bias in existing calibrations, such as those based on the univariate TEX86 index and other multivariate frameworks. GDGT cyclization is also known to be affected by nutrient stress as a non-thermal control. In this study, we present LIPOTHERM (Lipid Paleothermometry), a new GDGT-SST calibration trained on an extensive collection of globally distributed core-top GDGT data using supervised machine learning. LIPOTHERM features substantially lower calibration root mean square error than existing forms. Inclusion of core-top nutrient conditions as auxiliary predictors further lowers the calibration error. LIPOTHERM demonstrates that robust paleothermometry frameworks can be constructed by accumulating incremental improvements over different methodological refinements involving algorithm selection, feature space representation, expanding data coverage, and adding auxiliary non-thermal covariates.

LIPOTHERM:一种基于机器学习的GDGT古温度计校准框架
从海洋沉积物中保存的甘油二烷基甘油四醚(GDGT)重建海温是定量古气候学的重要工具。这些重建需要提供沉积物GDGT数据和温度值之间映射的校准框架。建模和数据覆盖方面的改进可以减少现有校准中的偏差,例如基于单变量TEX86指数和其他多变量框架的校准。作为一种非热控制,GDGT环化也受到营养胁迫的影响。在这项研究中,我们提出了LIPOTHERM(脂质古温度计),这是一种新的GDGT- sst校准方法,使用监督式机器学习对广泛收集的全球分布的核心顶部GDGT数据进行了训练。LIPOTHERM具有比现有形式低得多的校准均方根误差。纳入核心顶部营养条件作为辅助预测因子进一步降低了校准误差。LIPOTHERM表明,通过累积不同方法的改进,包括算法选择、特征空间表示、扩大数据覆盖范围和添加辅助非热协变量,可以构建稳健的古温学框架。
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来源期刊
Geochemistry Geophysics Geosystems
Geochemistry Geophysics Geosystems 地学-地球化学与地球物理
CiteScore
5.90
自引率
11.40%
发文量
252
审稿时长
1 months
期刊介绍: Geochemistry, Geophysics, Geosystems (G3) publishes research papers on Earth and planetary processes with a focus on understanding the Earth as a system. Observational, experimental, and theoretical investigations of the solid Earth, hydrosphere, atmosphere, biosphere, and solar system at all spatial and temporal scales are welcome. Articles should be of broad interest, and interdisciplinary approaches are encouraged. Areas of interest for this peer-reviewed journal include, but are not limited to: The physics and chemistry of the Earth, including its structure, composition, physical properties, dynamics, and evolution Principles and applications of geochemical proxies to studies of Earth history The physical properties, composition, and temporal evolution of the Earth''s major reservoirs and the coupling between them The dynamics of geochemical and biogeochemical cycles at all spatial and temporal scales Physical and cosmochemical constraints on the composition, origin, and evolution of the Earth and other terrestrial planets The chemistry and physics of solar system materials that are relevant to the formation, evolution, and current state of the Earth and the planets Advances in modeling, observation, and experimentation that are of widespread interest in the geosciences.
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