| China Geological Survey Chinese Academy of Geological Sciences | Host |
| 科学出版社 | Publish |
| Citation: |
YE Guiqi, JI Wenbing, YANG Zhongfang, YU Tao, HOU Qingye, QIAN Kun. 2025. Research progress and prospect of oxygen isotope technique in soil−vegetation−ecology−environment studies[J]. Geology in China, 52(2): 527-573. doi: 10.12029/gc20240410003
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Research progress and prospect of oxygen isotope technique in soil−vegetation−ecology−environment studies
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Abstract
This paper is the result of environmental geological survey engineering.
Objective Oxygen is one of the basic elements that make up living matter, and the oxygen cycle in nature is the basic guarantee for life activities. Oxygen isotope technology is a powerful tracer that can effectively indicate biogeochemical cycling processes and has been widely used in ecological and environmental research.
Methods This paper reviewes the fractionation mechanism of oxygen isotopes and its application in soil−vegetation−ecological environment by reviewing a large number of literatures on oxygen isotopes.
Results Depending on the large isotope mass ratio difference, oxygen isotopes can undergo the greatest degree of isotope fractionation under natural conditions. The application of oxygen isotopes mainly includes three aspects: (1) Tracing the source of environmental pollutants; (2) Paleoenvironment and paleoclimate restoration; (3) Tracing the geographical origin of food (animals).
Conclusions In practice, oxygen isotopes are usually used together with other isotopes (hydrogen, carbon, nitrogen, etc.) to track multi-dimensional climate, vegetation development, and geographical location. In the future, oxygen stable isotopes can be combined with substitute models in the fields of global change, such as tree rings, foraminifera, loess, and salt lakes, and play a more important role in environmental ecology research.
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References
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YE Guiqi, JI Wenbing, YANG Zhongfang, YU Tao, HOU Qingye, QIAN Kun. 2025. Research progress and prospect of oxygen isotope technique in soil−vegetation−ecology−environment studies[J]. Geology in China, 52(2): 527-573. doi: 10.12029/gc20240410003
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Figure 1.
Relationship between isotope exchange half−life and pH between dissolved substances in hydrothermal systems(after Chiba and Sakai, 1985)
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Figure 2.
Isotopic fractionation of ozone formation（after Thiemens et al., 1983；Thiemens，2006）
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Figure 3.
Triple oxygen isotope compositions of atmospheric MIF component that have been measured to date（after Lin et al., 2024）
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Figure 4.
Oxygen isotope composition of phosphates in natural substances（a）and oxygen isotope composition of different parts of soil（b，after Tian et al., 2020）
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Figure 5.
δ18OP values in different P pools and potential sources in the sediment（after Yuan et al., 2019）
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Figure 6.
Nitrogen and oxygen isotopes signatures of nitrate from different sources（after Nestler et al., 2011）
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Figure 7.
Scatter plot of δ15N−NO3− and Δ17O−NO3− values in river water, rainwater and potential nitrate sources in the Wen-Rui Tang River watershed（after Ji et al., 2022）
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Figure 8.
The relationship between δD and
$\delta^{18} \mathrm{O}_{\mathrm{H}_2 \mathrm{O}} $ of river water and mine wastewater samples（after Li et al., 2022） -
Figure 9.
Modeling stable oxygen isotope fractionation in conifers（after McCarroll and Loader, 2004）
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Figure 10.
The 5-year moving average scatter diagram of δ18O of LGB69 ice core and temperature departure of Davis Station from 1968 to 2001（after Zhang Ziyang et al., 2021）
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Figure 11.
Latest Pleistocene to Holocene records of stalagmite δ18O from three caves in east Asia
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Figure 12.
Plot of average δ18O and δ13Cvalues of lacustrine carbonate rocks in different stratigraphic units in comparison with δ18O and δ13C domains of primary lacustrine carbonates in modern open and closed lakes（after Wang Chunlian et al., 2013）
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Figure 13.
The relationship of δD−δ18O of the different water samples in Yanhu Lake basin (after Fu Changchang and Liu Cong, 2022)
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Figure 14.
Scatterplots of meteoric water isotope values (after Aron et al., 2021)
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Figure 15.
Schematic showing the similarities between (a) dexcess and Δ′17O (b, after Aron et al., 2021)
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Figure 16.
Schematic representation of the effect of the hydrologic cycle on oxygen isotope ratios (after Rohling, 2013；Li Yue et al., 2016)
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Figure 17.
δ18OAr values of serial samples fromBellamya shell and the calculated temperature (black smooth line) variation along the direction of shell growth from Fuxian Lake（after Roy et al., 2019）
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Figure 18.
Global deep-sea oxygen and carbon isotope records（after Zachos et al., 2001）
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Figure 19.
Thermal modeling results of clumped isotope of drilling sample from Permian Maokou Formation in eastern Sichuan Basin on strata temperature（after Qiu Nansheng et al., 2023）
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Figure 20.
Variation of δ18O content in milk water (a) and (D/H)I of ethanol(b)of different European regions according to their latitude (from North to South)(after Perini et al., 2022)
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Figure 21.
Boxplots of the δ18OSMOWvalues in the bones of the thirteen marine mammal species considered（after Drago et al., 2020）
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Figure 22.
Boxplots of carbon (δ13C) and oxygen isotopes (δ18O) in octopus statoliths（after Martino et al., 2022）
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Figure 23.
CAP plot of chemical characteristics of octopus from different geographical origins（after Martino et al., 2022）