Extended Data Fig. 9: T. miraclensis in open platform and bank facies of the Lianglitag Formation, Tarim Basin. | Nature Plants

Extended Data Fig. 9: T. miraclensis in open platform and bank facies of the Lianglitag Formation, Tarim Basin.

From: Ordovician marine Charophyceae and insights into land plant derivations

Extended Data Fig. 9

a, Bioclastic grainstone containing T. miraclensis (T), corals (cor.), and the dasycladalean Dasyporella (Das.), TZ161-25-55-28. b, Bioclastic grainstone containing T. miraclensis, TZ822-9-5727.55. c, Open platform packstone containing T. miraclensis and abundant dasycladaleans: Vermiporella (Ver.) and Arthroporella (Art.), TZ70-6-66-21. d, Bioclastic grainstone, containing T. miraclensis, echinoderms (ech.), and bryozoans (bry.), TZ822-5727.55. e, Open platform packstone, containing T. miraclensis and unidentified bioclasts, TZ24-7-48-44. f, TZ70-9-58-48, Open platform packstone, containing T. miraclensis. g, Open platform packstone, containing dasycladaleans (das.) T. miraclensis, TZ161-32-52-19. For recognition of open platform and bank facies see ref. 40.

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