“…The response of radiolarians mainly included structural adaptations, such as development of a pylome that was initiated by Darriwilian time in Triplococcus, Westernbrookia, and Protopylentonema n. gen., and successfully passed on to Late Ordovician Kalimnasphaera, Borisella, and Sandbian members of Protopylentonema n. gen. By Late Ordovician time, bandage- Perera and Aitchison-Late Sandbian radiolarians from Pingliang Formation, China type shell wall-bearing antygoporids and aspiculids of the Middle Ordovician were mostly replaced by solid, thick skeleton-bearing inaniguttids (Kalimnasphaera, Geminusphaera n. gen., Inanibigutta, Inanigutta, and Oriundogutta), increasing the robustness of the skeleton and adapting to both shallow-and deep-water facies. Although radiolarian discoveries are usually subjected to strong preservation and collection biases, which shadows true relative species abundances, many studies conducted for Ordovician radiolarians confirm the dominating occurrence of inaniguttids Wang, 1993;Danelian and Clarkson, 1998;Danelian and Floyd, 2001;Maletz and Bruton, 2008;Maletz et al, 2009;Noble and Webby, 2009;Kachovich and Aitchison, 2020;Perera et al, 2020). This indicates that the Inaniguttidae were the most successful family to diversify during the GOBE.…”