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000490157 1001_ $$0P:(DE-HGF)0$$aOsés, Gabriel Ladeira$$b0
000490157 245__ $$aEdiacaran Corumbella has a cataphract calcareous skeleton with controlled biomineralization
000490157 260__ $$aSt. Louis$$bElsevier$$c2022
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000490157 520__ $$aSummary:Corumbella is a terminal Ediacaran tubular, benthic fossil of debated morphology, composition, and biological affinity. Here, we show that Corumbella had a biomineralized skeleton, with a bilayered construction of imbricated calcareous plates and rings (sclerites) yielding a cataphract organization, that enhanced flexibility. Each sclerite likely possessed a laminar microfabric with consistent crystallographic orientation, within an organic matrix. Original aragonitic mineralogy is supported by relict aragonite and elevated Sr (mean = ca. 11,800 ppm in central parts of sclerites). In sum, the presence of a polarisation axis, sclerites with a laminar microfabric, and a cataphract skeletal organization reminiscent of early Cambrian taxa, are all consistent with, but not necessarily indicative of, a bilaterian affinity. A cataphract skeleton with an inferred complex microstructure confirms the presence of controlled biomineralization in metazoans by the terminal Ediacaran, and offers insights into the evolution of development and ecology at the root of the ‘Cambrian radiation’.
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000490157 7001_ $$0P:(DE-HGF)0$$aWood, Rachel$$b1
000490157 7001_ $$0P:(DE-HGF)0$$aRomero, Guilherme Raffaeli$$b2
000490157 7001_ $$0P:(DE-HGF)0$$aEvangelista Martins Prado, Gustavo Marcondes$$b3
000490157 7001_ $$0P:(DE-H253)PIP1017023$$aBidola, Pidassa Malimda$$b4
000490157 7001_ $$0P:(DE-H253)PIP1005953$$aHerzen, Julia$$b5
000490157 7001_ $$0P:(DE-H253)PIP1009227$$aPfeiffer, Franz$$b6
000490157 7001_ $$0P:(DE-HGF)0$$aStampar, Sérgio Nascimento$$b7
000490157 7001_ $$0P:(DE-H253)PIP1016032$$aAlves Forancelli Pacheco, Mírian Liza$$b8$$eCorresponding author
000490157 773__ $$0PERI:(DE-600)2927064-9$$a10.1016/j.isci.2022.105676$$gVol. 25, no. 12, p. 105676 -$$n12$$p105676$$tiScience$$v25$$x2589-0042$$y2022
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