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carbonaceous fossils of Charnia and Hiemalora[edit]
Charnia and Hiemalora not preserved as carbonaceous films, these fossils from Siberia are deformations (phantoms) on microbial-algal mats what preserved as carbonaceous films. D. V. Grazhdankin (October 2008). "Carbonate-hosted Avalon-type fossils in arctic Siberia". Geology. 36 (10): 803–806. {{cite journal}}: Unknown parameter |coauthor= ignored (|author= suggested) (help) Aleksey (Alnagov (talk) 09:59, 29 July 2009 (UTC))[reply]
there are two biotas of multicellular organisms and these biotas not having general members, as was considered until recently: It's not just the impenetrable grammar: Would "general members" signify fossils appearing in both biota?--Wetman (talk) 03:37, 7 October 2009 (UTC)[reply]