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Porter, Susannah M., Meisterfeld, Ralf, Knoll, Andrew H. (2003) Vase-shaped microfossils from the Neoproterozoic Chuar Group, Grand Canyon: A classification guided by modern testate amoebae. Journal of Paleontology, 77 (3) 409-429 doi:10.1017/s0022336000044140

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Reference TypeJournal (article/letter/editorial)
TitleVase-shaped microfossils from the Neoproterozoic Chuar Group, Grand Canyon: A classification guided by modern testate amoebae
JournalJournal of Paleontology
AuthorsPorter, Susannah M.Author
Meisterfeld, RalfAuthor
Knoll, Andrew H.Author
Year2003 (May)Volume77
Issue3
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0022336000044140Search in ResearchGate
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Mindat Ref. ID419725Long-form Identifiermindat:1:5:419725:0
GUID0
Full ReferencePorter, Susannah M., Meisterfeld, Ralf, Knoll, Andrew H. (2003) Vase-shaped microfossils from the Neoproterozoic Chuar Group, Grand Canyon: A classification guided by modern testate amoebae. Journal of Paleontology, 77 (3) 409-429 doi:10.1017/s0022336000044140
Plain TextPorter, Susannah M., Meisterfeld, Ralf, Knoll, Andrew H. (2003) Vase-shaped microfossils from the Neoproterozoic Chuar Group, Grand Canyon: A classification guided by modern testate amoebae. Journal of Paleontology, 77 (3) 409-429 doi:10.1017/s0022336000044140
In(2003, May) Journal of Paleontology Vol. 77 (3) Cambridge University Press (CUP)
Abstract/NotesVase-shaped microfossil (VSM) assemblages from early diagenetic carbonate nodules in >742 ± 6 Ma black shales of the Chuar Group, Grand Canyon, provide evidence for affinities with testate amoebae. Not only are VSMs exceptionally preserved in Chuar rocks, they exhibit a much higher degree of morphological diversity than was previously known. Using the taxonomy of modern testate amoebae as a guide, nine new species and eight new genera of VSMs are described, augmenting the eight species and two genera already recognized. Taxa described here areMelanocyrillium hexodiademaBloeser, 1985,Trigonocyrillium horodyskii(Bloeser, 1985) n. comb.,T. fimbriatum(Bloeser, 1985) n. comb.,Cycliocyrillium simplexn. sp.,C. torquatan. sp.,Bonniea dacrucharesn. sp.,B. pytinaian. sp.,Trachycyrillium pudensn. sp.,Palaeoarcella athanatan. sp.,Hemisphaeriella ornatan. sp.,Bombycion micronn. sp., andMelicerion poikilonn. sp. All of the test characters observed in VSM taxa (e.g., collars; indentations; hexagonal symmetry; lobed, triangular or invaginated apertures; curved necks) occur in modern testate amoeban taxa, though not always in the same combinations. Some VSM species have characters found today in diverse extant taxa, making it difficult to assess their relationships. A few species, however, have character combinations that closely approximate those found in specific genera of both lobose and filose testate amoebae, suggesting that at least stem group, and possibly crown group, representatives of these taxa were present ∼742 Ma.These fossils indicate that ecosystems were diverse and complex, that eukaryotic biomineralization had already evolved, and that the last common ancestor of animals+fungi had already appeared by ∼750 Ma.


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