Ediacaran survivors in the Cambrian: suspicions, denials and a smoking gun

• Published in: Geological magazine 2022-07, Vol.159 (7), p.1210-1219
• Main Author: Hoyal Cuthill, Jennifer F
• Format: Article
• Language: English
• Subjects: adaptive radiation; biodiversity; biologic evolution; Biota; Burgess Shale; Cambrian; cladistics; Dynamics; Ediacaran; Evolution; extinction; Extreme values; Fossils; ichnofossils; Mass extinctions; Middle Cambrian; Morphology; Museums; Neoproterozoic; Original Article; paleobiology; Paleontology; Paleozoic; Petalonamae; Phylogeny; Precambrian; preservation; Proterozoic; Rangea; Sedimentary rocks; Shale; soft parts; species diversity; Species extinction; Stratigraphy; Stromatoveris psygmoglena; Survival; Taxonomy; Thaumaptilon; Twain, Mark (Samuel Langhorne Clemens) (1835-1910); upper Precambrian
• ISSN: 0016-7568; 1469-5081
• DOI: 10.1017/S0016756821001333

The relative timing of extinctions and originations is a foundation for reconstructing evolutionary causes. However, there has been a tendency to dismiss reported Ediacaran holdovers in favour of effective extinction around the Cambrian boundary. Here, focusing on the classically Ediacaran frondose biota (Petalonamae), I suggest four main reasons why proposed Ediacaran survivors have previously been denied the acceptance they deserve: denials based on mistaken identity, doppelgängers, a last gasp or dead clades walking. I then point to the lower Cambrian species Stromatoveris psygmoglena as a key example which simultaneously meets these objections. Collectively, Cambrian survivors are a ‘smoking gun’ showing that extinction of the classically Ediacaran frondose biota did not occur until at least 30 Ma after the end of the Ediacaran period, registered by phylogenetic petalonamid Thaumaptilon from the Burgess Shale. Therefore, to paraphrase Mark Twain, reports of their earlier demise have been greatly exaggerated. Causes of their ultimate extinction should instead be sought in their total range and diversity dynamics. Overall, the Ediacaran–Cambrian transition shows extremely low numbers of recorded survivors, but diversity dynamics are dominated by the Cambrian explosion. In this context, recorded occurrences for the classically Ediacaran frondose biota are compatible with at least two extinction events, one within a possible mass extinction near the Cambrian boundary, and later, their ultimate extinction in, or after, the middle Cambrian (Miaolingian Series, Wuliuan Stage). There is, however, no correlative basis for a causal link between the Cambrian transition and the effective or final demise of the classically Ediacaran soft-bodied biota.