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. 2021 Nov 26;12:6935. doi: 10.1038/s41467-021-27054-5

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© The Author(s) 2021

Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.

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Fig. 5 — a Al flux at the Bajiazui section¹⁷. b SiO₂/Al₂O₃ from the Xifeng section²⁰. c Zr/Rb from the Jiaxian red clay section²⁶. d Median grain size from the Xifeng section²⁰. e, f Fine (5–16 μm) and coarse (>20 μm) particle concentration from the Shilou section⁵⁶. Red smooth curves are fitted using the MatLab LOWESS function. g, h Cold-aridiphilous (CA) and thermo-humidiphilous (TH) terrestrial mollusk changes in the Dongwan red clay⁵⁷.