“…While arthropods, both soft-bodied and biomineralized, dominate the deposit, members of many modern phyla have also been reported; further, in many instances, these represent the first appearances of these phyla in the fossil record (Hou et al 2017). The composition of the Chengjiang biota is similar to the middle Cambrian (Miaolingian; Wuliuan) Burgess Shale Lagerstätte of Canada, and previous research has shown that there are ecological and taphonomic similarities between the two deposits (Conway Morris 1986;Gabbott et al 2004;Dornbos and Chen 2008;Caron et al 2013Caron et al , 2014Zhao et al 2014;Saleh et al 2020). While few, if any species, are shared between the deposits, as they are from distinct biogeographic regions and temporally differentiated, several genera are shared between the Chengjiang biota and the Burgess Shale, as well as other Laurentian BST deposits, including Anomalocaris, Cambroraster, Canadaspis, Choia, Eldonia, Isoxys, Leanchoilia, Sidneyia, Tuzoia, and various trilobites (see Hendricks and Lieberman 2007;Vannier et al 2007;Williams et al 2007;Hendricks et al 2008;Garcia-Bellído and Aceñolaza 2011;Caron et al 2013Caron et al , 2014Hendricks 2013;Kimmig and Pratt 2015;Paterson et al 2015a, b;Hou et al 2017;Lerosey-Aubril et al 2018Harper et al 2019;Kimmig et al 2019a;Pates et al 2019;and Liu et al 2020 for a discussion of Cambrian BST deposits).…”