Dr. Mimi Chen from PKU gave us a talk entitled "When atmospheric S met hydrothermal S in Archean deep ocean".
ICIER is a cross-college and cross-discipline research hub. All of our faculty members are affiliated with different colleges in Nanjing University.Both Chinese and English are primary means of scientific communication at ICIER.
Peng, Y., H. Bao, G. Jiang, P. Crockford, D. Feng, S. Xiao, A. J. Kaufman and J. Wang (2022). A transient peak in marine sulfate after the 635-Ma snowball Earth. Proc Natl Acad Sci U S A, 119(19): e2117341119.
Chihiro, M., Yoshinori, L., Sumito, M., Shohei, H., Yoshio, T. Gypsum formation from calcite in the atmosphere recorded in aerosol particles transported and trapped in Greenland ice core sample is a signature of secular change of SO2 emission in East Asia. Atmospheric Environment, 119061.
Yan, H., Peng, YB., Bao, HM. Isotope fractionation during capillary leaking in an isotope ratio mass spectrometer. Rapid Communications in Mass Spectrometry, v. 36, no. 11, e9290.
Ma, HR., Shen, B., Lang, XG., Peng, YB. et al. Active biogeochemical cycles during the Marinoan global glaciation. Geochimica et Cosmochimica Acta 321: 155-169.
Han, T., Peng, YB., Bao, HM. Sulfate-limited euxinic seawater facilitated Paleozoic massively bedded barite deposition. Earth and Planetary Science Letters 582: 117419.