Results 171 to 180 of about 3,951 (214)
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Vendian strata in their type area

Geological Magazine, 1987
AbstractIn the Eastern European region Vendian strata are divisible into two complexes: the lower one, only locally developed, is composed of alternating tillites, volcanics, sandy–clay rocks and dolomites; and the upper one, of alternating sandstone, siltstone, and mudstone strata with medusoid fauna, resting transgressively on the lower complex and ...
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New Vendian Metazoa with Colonial Organization

Paleontological Journal
A new organism with colonial organization, Olgunia bondarenkoae gen. et sp. nov., of sponge or coelenterate grade, is described from the Vendian deposits of the South-Eastern White Sea region. The new genus is characterized by a modular pattern and coordinated growth of neighboring individuals arranged in a fan-shape. The new genus has a combination of
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The Eocambrian (Vendian sensu stricto)

1983
Different geologic formations that originated after the Katangan orogeny are here attributed to the Eocambrian, the time of their formation being after 680–650 m.y. and prior to the beginning of the Cambrian period, that is earlier than 570 m.y. The duration of the Eocambrian is thus 100–80 m.y., which is much shorter than that of other principal units
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Discussion on was Scotland a Vendian RRR junction?

Journal of the Geological Society, 1995
B. J. Bluck, T. J. Dempster & G. Rogers write: In a recent Special paper, Soper (1994) contends that Dalradian deposition continued after the emplacement of the Ben Vuirich granite at 590 Ma (Rogers et al. 1989). The granite, however, contains metasedimentary xenoliths with an
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Feeding traces of proarticulata—the Vendian metazoa

Paleontological Journal, 2011
Three types of low-topography impressions are described from the Late Vendian, which are interpreted as the feeding traces of representatives of the phylum Proarticulata Fedonkin, 1985, which became extinct in the Precambrian. The producers of two types of trace were found.
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Vendian Faunas and the Early Evolution of Metazoa

1992
Until recently, paleontological data were almost completely ignored by zoologists studying the origin of major groups of invertebrates and the early phylogeny of the Metazoa, chiefly because Charles Lyell had long ago emphasized the incompleteness of the geological and paleontological record.
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Vendian Polychaeta

1990
Boris S. Sokolov, Andrew B. Iwanowski
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Vendian Microfossils

1990
Boris S. Sokolov, Andrew B. Iwanowski
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Vendian of the Urals

1990
Boris S. Sokolov, M. A. Fedonkin
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