THE NEW DICKINSONID FROM THE UPPER VENDIAN OF THE WHITE SEA WINTER COAST (RUSSIA, ARAKHANGELSK REGION)

dc.contributor.author	Ivantsov A.Yu.
dc.date.accessioned	2021-01-13T07:34:53Z
dc.date.available	2021-01-13T07:34:53Z
dc.date.issued	1999
dc.identifier	https://elibrary.ru/item.asp?id=14995356
dc.identifier.citation	Paleontologicheskii zhurnal, 1999, , 3, 10-11
dc.identifier.issn	0031-031X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/22832
dc.description.abstract	A description and reconstruction of the new fossil are based on the rounded isometric imprints which are composed of two rows of transverse elements. The elements are arranged in the manner of glide reflection symmetry. The lateral flanks of the elements are pointed and curved in identical directions. It is suggested tha this fossil was preserved as imprints of different appearances (positive and negative) including «trilobite-like» forms. The relief of the imprints could be positive or negative. The fossils occur as isolate imprints or in accumulations.
dc.subject	Vendian	en
dc.title	THE NEW DICKINSONID FROM THE UPPER VENDIAN OF THE WHITE SEA WINTER COAST (RUSSIA, ARAKHANGELSK REGION)
dc.type	Статья
dc.subject.age	Precambrian::Proterozoic::Neoproterozoic::Vendian	en
dc.subject.age	Докембрий::Протерозой::Неопротерозойская::Вендский	ru

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