Ouyang, QingZhou, ChuanmingXiao, ShuhaiWu, ChengxiChen, ZheLang, XianguoShi, HongyiSun, Yunpeng2025-02-182025-02-182025https://hdl.handle.net/10919/124634Silicified microfossils are reported from nine stratigraphic sections of the Ediacaran Doushantuo Formation deposited in shelf margin, slope, and basin environments in Hunan Province of South China. These microfossils include sphaeromorphic and acanthomorphic acritarchs (15 genera and 29 species, including three new acanthomorph species, Bullatosphaera? colliformis n. sp., Eotylotopalla inflata n. sp., and Verrucosphaera? undulata n. sp.), multicellular algae, tubular microfossils, and other problematic forms, representing major fossil groups similar to those from the Doushantuo Formation in more proximal facies, e.g., inner shelf and shelf lagoon. A database of the abundance and occurrences of Doushantuo acanthomorphs is assembled and analyzed using quantitative and data visualization methods (i.e., rarefaction analysis, non-parametric multidimensional scaling, and network analysis). The results show that, at the genus- and species-level, taxonomic richness of Doushantuo acanthomorphs exhibits remarkable variation among facies, but this variation is largely due to sampling and taphonomic biases. The results also show that numerous acanthomorph taxa have broad facies distribution, affirming their biostratigraphic value. The analysis confirms that acanthomorphs in the Weng'an biota of shelf margin facies is transitional between Member II and Member III assemblages of shelf lagoon facies in the Yangtze Gorges area. The study shows the biostratigraphic potential of acanthomorphs in the establishment of regional biozones using the first appearance datum of widely distributed taxa, highlighting the importance of continuing exploration of undersampled Doushantuo sections in slope and basinal facies.79 page(s)application/pdfenIn CopyrightArticle - Refereedhttps://doi.org/10.1017/jpa.2023.92Xiao, Shuhai [0000-0003-4655-2663]