Fission track dating of ancient man site in Baise, China, and its significances in space research, paleomagnetism and stratigraphy

• Published in: Radiation measurements Vol. 28; no. 1; pp. 565 - 570
• Main Authors: Guo, S.-L., Huang, W., Hao, X.-H., Chen, B.-L.
• Format: Journal Article Conference Proceeding
• Language: English
• Published: Oxford Elsevier Ltd 1997; Elsevier
• Subjects: ancient man site; Earth sciences; Earth, ocean, space; Exact sciences and technology; Fission track dating; Geochronology; Isotope geochemistry. Geochronology; Marine and continental quaternary; paleomagnetism; space research; stratigraphy; Surficial geology; tektite; Far East; Guangxi China; China; ancient man site; Fission track dating; tektite; stratigraphy; space research; paleomagnetism; reversals; magnetic polarity; upper Cenozoic; Prehistoric artefacts; magnetostratigraphy; fission tracks; Quaternary; Matuyama Epoch; upper Quaternary; annealing; impactite; Brunhes Epoch; corrections; Asia; dating; tektites; Cenozoic; Phanerozoic; Pleistocene
• ISSN: 1350-4487; 1879-0925
• DOI: 10.1016/S1350-4487(97)00140-6

A large number of artifacts (stone tools) have been discovered in Baise (Bose), Guangxi, China in recent years. They show that ancient man were living in the south of China during very ancient times. During excavation, tektites were discovered in the same layer of deposits as the stone tools. The structure of the layers of deposits in this site was never disturbed, which is the evidence that the stone tools were left behind by the ancient man at the time when the tektites fell on the earth, which were slowly covered over by layers of deposits. Fission track dating has been carried out on tektites. The age of the tektites is 0.732 ± 0.039 Ma, which is also the age of the ancient man in Baise, Guangxi, China. The annealing degree of spontaneous fission tracks in the tektite was investigated by measuring track diameters. A correction of age for track fading has been made by track diameter technique. According to current understanding, tektites were formed by the impact of falling asteroids or comets on the earth's surface. The dating shows that a big impact occurred on the earth 0.732 Ma ago. The coincidence of the age of the tektites with the age of geomagnetic polarity reversal (∼ 0.73 Ma) from the Matuyama Epoch to the Brunhes Epoch proposes a plausible explanation that the possible cause of the geomagnetic polarity reversal is due to the big impact of space objects falling onto the earth. The result of the dating also set up a standard for inferring the ages of the deposits in South China as well as in South-East Asia where laterite (red soil) deposits exist in the entire region.