TY - JOUR
T1 - Influences of paleoclimatic changes on organic matter enrichment mechanisms in freshwater and saline lacustrine oil shales in China
T2 - A machine learning approach
AU - Lu, Man
AU - Duan, Guoqiang
AU - Zhang, Tongxi
AU - Liu, Naihao
AU - Song, Yuxuan
AU - Zhang, Zezhou
AU - Qiao, Jinqi
AU - Wang, Zhaoyang
AU - Fang, Zilong
AU - Luo, Qingyong
N1 - Publisher Copyright:
© 2025 Elsevier B.V.
PY - 2025/3
Y1 - 2025/3
N2 - Lacustrine oil shales are valuable unconventional resources, with their organic matter (OM) enrichment closely linked to paleoclimatic conditions. However, the mechanisms controlling OM enrichment in freshwater and saline lacustrine environments remain underexplored. This study represents the first application of the random forest (RF) classifier to investigate how paleoclimatic changes influence OM enrichment mechanisms in lacustrine oil shales in China. By analyzing the bulk geochemical (total organic carbon (TOC), trace and major elements) and molecular biomarker data from seven representative lacustrine oil shales, we demonstrate that the RF classifier can effectively discriminate between freshwater and saline lacustrine oil shales. The results indicate that the TOC content is the most significant parameter, with freshwater shales having higher TOC values than their saline counterparts. Further analyses suggest that OM enrichment in these two types of lacustrine settings was driven by a combination of factors, including paleoproductivity, paleowater conditions, and terrigenous inputs, all modulated by paleoclimatic changes. Freshwater lacustrine shales were generally deposited during humid and warm periods with higher atmospheric CO2 levels and greater precipitation, which led to higher paleoproductivity, reduced terrigenous influx, rising lake levels, and improved OM production and preservation. In contrast, saline lacustrine shales were deposited during dry and cold periods, when increased water salinity and diminished paleoproductivity resulted in lower OM production, reduced preservation, and decreased TOC content. These findings provide key insights into the role of paleoclimate in shaping OM-rich lacustrine shales and establish a framework for evaluating organic-rich shale deposits. The study also underscores the potential for future geochemical datasets to enhance classification models and broaden applications of machine learning in the exploration of hydrocarbon resources.
AB - Lacustrine oil shales are valuable unconventional resources, with their organic matter (OM) enrichment closely linked to paleoclimatic conditions. However, the mechanisms controlling OM enrichment in freshwater and saline lacustrine environments remain underexplored. This study represents the first application of the random forest (RF) classifier to investigate how paleoclimatic changes influence OM enrichment mechanisms in lacustrine oil shales in China. By analyzing the bulk geochemical (total organic carbon (TOC), trace and major elements) and molecular biomarker data from seven representative lacustrine oil shales, we demonstrate that the RF classifier can effectively discriminate between freshwater and saline lacustrine oil shales. The results indicate that the TOC content is the most significant parameter, with freshwater shales having higher TOC values than their saline counterparts. Further analyses suggest that OM enrichment in these two types of lacustrine settings was driven by a combination of factors, including paleoproductivity, paleowater conditions, and terrigenous inputs, all modulated by paleoclimatic changes. Freshwater lacustrine shales were generally deposited during humid and warm periods with higher atmospheric CO2 levels and greater precipitation, which led to higher paleoproductivity, reduced terrigenous influx, rising lake levels, and improved OM production and preservation. In contrast, saline lacustrine shales were deposited during dry and cold periods, when increased water salinity and diminished paleoproductivity resulted in lower OM production, reduced preservation, and decreased TOC content. These findings provide key insights into the role of paleoclimate in shaping OM-rich lacustrine shales and establish a framework for evaluating organic-rich shale deposits. The study also underscores the potential for future geochemical datasets to enhance classification models and broaden applications of machine learning in the exploration of hydrocarbon resources.
KW - Depositional environments
KW - Geochemical characteristics
KW - Lacustrine oil shales
KW - Machine learning
KW - Organic matter
KW - Paleoclimate
UR - https://www.scopus.com/pages/publications/85217376929
U2 - 10.1016/j.earscirev.2025.105061
DO - 10.1016/j.earscirev.2025.105061
M3 - 文献综述
AN - SCOPUS:85217376929
SN - 0012-8252
VL - 262
JO - Earth-Science Reviews
JF - Earth-Science Reviews
M1 - 105061
ER -