“…The lithostratigraphy and biostratigraphy of the Zhangjiagou section were studied by Li (1984) and Steiner et al (2004a), Steiner et al (2007). The same locality and horizon have previously yielded abundant and beautifully preserved microfossils, such as specimens of Olivooides (Liu et al, 2014a;Steiner et al, 2014;Liu et al, 2017;Shao et al, 2018b;Shao et al, 2019a), Pseudooides, the oldest known priapulid-like cycloneuralians as well as other scalidophorans (Liu et al, 2014b;Shao et al, 2016;Shao et al, 2018b;Shao et al, 2019b;Wang et al, 2019;Wang D et al, 2020) and possibe Saccorhytus (Han et al, 2017;Liu et al, 2022). The fossil-bearing horizon correlates with the Anabarites trisulcatus-Protohertzina anabarica assemblage zone (Steiner et al, 2007;Steiner et al, 2014), which has an estimated age of 531.8-536.4 Ma and falls within the Fortunian Stage (Peng et al, 2020).…”