| Citation: | Jingxun Zuo, Xuejian Zhu, Yonglin Chen, Wenjian Zhai. Carbon Isotope from Shallow Marine System in North China: Implications for Stratigraphical Correlation and Sea-Level Changes in Cambrian. Journal of Earth Science, 2023, 34(6): 1777-1792. doi: 10.1007/s12583-021-1463-6
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Cambrian System at the Shatan Section in northern Henan, North China, consists of sedimentary successions of tidal flat and shallow-water carbonate platform facies. Data of carbon isotope (δ13Ccarb) from this section reveals five positive δ13Ccarb (Pst-1–Pst-5) and five negative δ13Ccarb excursions (Nst-1–Nst-5). In the positive excursions, δ13Ccarb rises to 0.88‰, 1.05‰, 2.04‰, 1.00‰ and 2.97‰, respectively, while in the negative excursions δ13Ccarb drops to -8.00‰, -3.50‰, -1.00‰, -0.33‰ and around -2.00‰, respectively. On the basis of chronostratigraphy of Cambrian, the most remarkable carbon isotope excursions can be correlated regionally and globally. In addition, one second-order and ten third-order sequences have been recognized at this section. Correlating third-order sequences and chemostratigraphy indicates that carbonates from the basal part of the transgression system tract (TST) and the upper part of the high-water system (LHST) generally have lighter δ13Ccarb values, whereas massive carbonates with microbialite from the lower part of the high-water system tract (EHST) usually have heavier δ13Ccarb values. The association of δ13Ccarb values with sea-level fluctuations suggests that the positive carbon isotope excursions or high δ13Ccarb values may have been caused by an increase in the marine primary productivity in response to maximum seawater flooding during the transgression.
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