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WFRF:(Skovsted Christian B.)
 

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LIBRIS Formathandbok  (Information om MARC21)
FältnamnIndikatorerMetadata
00003802nam a2200493 4500
001oai:DiVA.org:uu-3910
003SwePub
008031215s2003 | |||||||||||000 ||eng|
020 a 9150617311q print
024a https://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-39102 URI
040 a (SwePub)uu
041 a engb eng
042 9 SwePub
072 7a vet2 swepub-contenttype
072 7a dok2 swepub-publicationtype
100a Skovsted, Christian B.,d 1974-u Uppsala universitet,Institutionen för geovetenskaper4 aut
2451 0a The Early Cambrian Fauna of North-East Greenland
246a Den tidigkambriska faunan från Nordöstgrönland
264 1a Uppsala :b Institutionen för geovetenskaper,c 2003
300 a 22 s.
338 a electronic2 rdacarrier
520 a Small shelly fossils are common in sediments of Early Cambrian age and include the earliest common representatives of metazoan animals with mineralized hard parts. The group includes fossils of very different morphology, composition and ultrastructure. They seem to represent skeletal remains of numerous animal groups, the biological affinities of which are largely unresolved. However, the wide geographic range of many forms has the potential to enhance biostratigraphic and palaeogeographic resolution in the Early Cambrian. The late Early Cambrian sequence of North-East Greenland has yielded an assemblage of more than 88 species of small shelly fossils, brachiopods and trilobites, indicative of a middle Dyeran age (Botoman equivalent). The recovered fossils include a number of species that are known from other Early Cambrian palaeocontinents, and particularly strong ties to late Early Cambrian faunas of Australia are documented. The many cosmopolitan taxa thus identified suggests a close juxtaposition of palaeocontinents at this time. The systematic affinity of many of these small shelly fossils is poorly understood, partly because of their fragmentary nature and poor preservation. However, new data from North-East Greenland improves our understanding of the function and biological affinity of certain taxa. Collections of the problematic fossil Mongolitubulus from North and North-East Greenland exhibit characters indicative of a defensive function as spines of bivalved arthropods, while species of the problematic genus Triplicatella represent the opercula of an unknown tubular shell, probably related to orthothecid hyoliths. The bivalved fossil Mickwitzia from North-East Greenland combines characters of linguliform brachiopods and sclerites of Micrina, a non-bivalved problematic form (halkieriid) from Australia. The combination suggests that Mickwitzia is a stem group brachiopod and strengthens arguments for a halkieriid ancestry of the brachiopod phylum.
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskap0 (SwePub)1052 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciences0 (SwePub)1052 hsv//eng
653 a Earth sciences
653 a Early Cambrian
653 a Dyeran
653 a Botoman
653 a Biostratigraphy
653 a Palaeogeography
653 a Small Shelly Fossils
653 a Brachiopoda
653 a Mollusca
653 a Hyolitha
653 a Trilobita
653 a Geovetenskap
653 a Earth sciences
653 a Geovetenskap
700a Peel, John S.4 ths
700a Holmer, Lars E.4 ths
700a Geyer, Gerd,c Professoru Institut für Paläontologie, Universität Würtzburg, Würtzburg4 opn
710a Uppsala universitetb Institutionen för geovetenskaper4 org
856u https://uu.diva-portal.org/smash/get/diva2:163880/FULLTEXT01.pdfx primaryx Raw objecty fulltext
8564 8u https://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-3910

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