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Magnetostratigraphic dating of mammalian fossils in Junggar Basin, northwest China

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  • Geology
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Chinese Science Bulletin

Abstract

The first detailed chronology for the late Oligocene to early Miocene continental record in northern Junggar Basin is presented, based on rock magnetic experiments and magnetostratigraphic investigations of a 192 m thick mammal-bearing section in the Ulungur River area. Magnetites and hematites were identified as the main carriers for the characteristic remanent magnetization, and the resulting polarity sequence allows an unambiguous correlation to the geomagnetic polarity time scale (GPTS). Furthermore, the Tieersihabahe fauna layer occurs below the Paleocene/Neocene boundary, and the Suosuoquan fauna layer is just above the Neocene onset. Therefore, the age of the Tieersihabahe fauna and Suosuoquan fauna layers can be definitely estimated to be about 25.2 Ma and 22.5 Ma, respectively.

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Correspondence to Yue LePing.

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Supported by the National Natural Science Foundation of China (Grant Nos. 40372202 and 40172610) and National Important Basic Research Project of China (Grant No. G2003CB214607)

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Zhang, R., Yue, L. & Wang, J. Magnetostratigraphic dating of mammalian fossils in Junggar Basin, northwest China. CHINESE SCI BULL 52, 1526–1531 (2007). https://doi.org/10.1007/s11434-007-0205-1

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  • DOI: https://doi.org/10.1007/s11434-007-0205-1

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