Applications of ESR dating and18O Paleotemperature data for studies on Quaternary sea-level changes

Huang Peihua; Peng Zicheng; Jin Sizhao; Liang Renyou; Quan Yucai; Wang Zhaorong

doi:10.1007/BF02842660

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Applications of ESR dating and18O Paleotemperature data for studies on Quaternary sea-level changes

OriginalPaper | Updated：2023-05-16

- Applications of ESR dating and18O Paleotemperature data for studies on Quaternary sea-level changes
- Applications of ESR dating and18O Paleotemperature data for studies on Quaternary sea-level changes
- 海洋湖沼学报（英文） 1989年7卷第1期页码：79-88
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- DOI：10.1007/BF02842660
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- 纸质出版：1989
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Applications of ESR dating and18O Paleotemperature data for studies on Quaternary sea-level changes[J]. 海洋湖沼学报（英文）, 1989,7(1):79-88.

Peihua, H., Zicheng, P., Sizhao, J. et al. Applications of ESR dating and18O Paleotemperature data for studies on Quaternary sea-level changes., Chin. J. Ocean. Limnol. 7, 79–88 (1989). https://doi.org/10.1007/BF02842660
Applications of ESR dating and18O Paleotemperature data for studies on Quaternary sea-level changes[J]. 海洋湖沼学报（英文）, 1989,7(1):79-88. DOI： 10.1007/BF02842660.

Peihua, H., Zicheng, P., Sizhao, J. et al. Applications of ESR dating and18O Paleotemperature data for studies on Quaternary sea-level changes., Chin. J. Ocean. Limnol. 7, 79–88 (1989). https://doi.org/10.1007/BF02842660 DOI：

摘要

Abstract

Electron Spin Resonance (ESR) dating is a relatively new technique applicable also to the dating of materials from littoral zones and shallow sea regions

such as shells

corals

bones and teeth

foraminifera

diatoms

etc. ESR dating can span the time interval between the older limit of14C dating and the younger limit of the K−Ar dating

an interval of 103–106 years. Therefore

ESR technique is very suitatie for the measurement of the age of Quaternary sea—level changes. This paper gives some samples’ results by ESR dating from Early Pleistoncene to Holocene. The Quaternary sea—level changes in China were mainly eustatisms that corresponded to the paleotemperature variation. We have just begun study on the18O Paleotemperature in our continental area. Preliminary results show the temperature curve of the stalagmitic growth in caves corresponds well to the sea—level changes in 76–55×103 years B. P. ESR dating and studies of the18O Paleotemperature in East China will raise studies on Quaternary sea—level changes to a higher scientific basis.

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references

Huang Peihua, et al., 1986. Study on ESR dating of Quaternary materials.Chinese Science Bulletin 31 (15): 1061–1064.

Huang Peihua, et al., 1988. ESR dating and trapped electrons life—time of quartz grains in China loess.Quatern. Sci. Rev. (in Press).

Huning, G.J. and R. Grun, 1983. ESR dating in Quaternary Geology.Quatern. Sci. Rev. 2: 159–238.

Ikeya, M., et al., 1981. Dating of fossil shells with electron spin resonance.J. Geol. 89: 249–250.

Jin Sizhao, et al., 1987. Determination of ESR age of Early quaternary Lampro tula and the age of the Nihewan Fauna.Journal of China University of Science and Technology 17 (4): 501–507. (in Chinese)

Koba, M., et al., 1985. ESR ages of the Pleistocene coral reef Limestones in the Ryukyu Islands, Japan, ESR dating and Dosimetry, IONICS, Tokyo, 93–104.

Liang Renyou, et al., 1987, ESR preliminary research on age of geological samples.Chinese Journal of Microwave and Radio-frequency Spectroscopy 4 (3): 265–273. (in Chinese)

Peng Zicheng, et al., The studies of age determinations by ESR method.Geographical Research (in press). (in Chinese)

Shackleton, N. J. and N.D. Opdyke, 1973. Oxygen isotope and paleomagnetic stratigraphy of equatorial Pacific core V-28-238: oxygen isotope temperatures and ice volumes on a 105 and 106 year scale.Quaternary Research 3: 39–55.

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