Matches in SemOpenAlex for { <https://semopenalex.org/work/W2543443338> ?p ?o ?g. }
Showing items 1 to 93 of
93
with 100 items per page.
- W2543443338 abstract "The succession of the Digermulen Peninsula in Finnmark, northern Norway, is the only fossiliferous site inScandinavia with sedimentation across the Ediacaran–Cambrian transition without a significant hiatus. Geologicalinvestigations started in the 1930’s, but the Peninsula was first mapped in the 60’s. Ediacara-type fossils werefirst discovered in the late 80’s but recent discoveries will establish the Digermulen Peninsula as one of the mostsignificant Ediacaran sites in northern Europe. The parautochthonous strata are exposed in the Tanafjord areaalong the coast and in valleys on the east side of the Peninsula. The beds dip slightly to the west with the strikefollowing the coastline (ca. 045°). The Ediacaran succession is close to 1000 m thick and dominantly siliciclastic.It starts with interglacial sediments of the Nyborg Formation (tentatively the earliest Ediacaran), overlying astacked succession of diamictites of the Cryogenian Smalfjord Formation. After a hiatus follows the glaciogenicdiamictites of the Mortensnes Formation (~60 m thick), which is commonly seen to represent the ~582 Ma-oldGaskiers glaciation. Upwards, the contact to the overlying Stahpogiedde Formation is not exposed locally, but hasbeen shown to represent a hiatus followed by transitional fluvial to marine sediments of the Lillevannet Member.Ediacaran-type fossils appear in the succeeding Innerelva Member. This is a two-cycle deepening upwardssuccession of laminated mudstone with intercalated sand bodies showing load structures. Preliminary microfossilssamples of the Member have so far proven almost barren, making dating more challenging. The basal part of thesucceeding Manndraperelva Member consists of three cycles; first a succession of reddish sandstone followed bytwo coarsening-upward cycles. Each starts with mudstone and fine sandstone and terminates in cross-beddedsandstone. The Ediacaran–Cambrian boundary is located within the third cycle, identified by the trace fossilTreptichnus pedum and associated trilobed trace fossils.The Digermulen Early Life Research Group has since2011 made significant new finds, and focused fieldwork aims to resolve tighter age constraints, provenance of thesediments and the range and diversity of the extended Ediacaran biota." @default.
- W2543443338 created "2016-11-04" @default.
- W2543443338 creator A5008893290 @default.
- W2543443338 creator A5011314398 @default.
- W2543443338 creator A5028193259 @default.
- W2543443338 creator A5032731539 @default.
- W2543443338 creator A5046303265 @default.
- W2543443338 creator A5059118728 @default.
- W2543443338 creator A5069381791 @default.
- W2543443338 creator A5070823788 @default.
- W2543443338 creator A5076888037 @default.
- W2543443338 date "2015-01-01" @default.
- W2543443338 modified "2023-10-17" @default.
- W2543443338 title "Stratigraphy of the Ediacaran and basal Cambrian of the Digermulen Peninsula, Northern Norway" @default.
- W2543443338 hasPublicationYear "2015" @default.
- W2543443338 type Work @default.
- W2543443338 sameAs 2543443338 @default.
- W2543443338 citedByCount "1" @default.
- W2543443338 countsByYear W25434433382020 @default.
- W2543443338 crossrefType "journal-article" @default.
- W2543443338 hasAuthorship W2543443338A5008893290 @default.
- W2543443338 hasAuthorship W2543443338A5011314398 @default.
- W2543443338 hasAuthorship W2543443338A5028193259 @default.
- W2543443338 hasAuthorship W2543443338A5032731539 @default.
- W2543443338 hasAuthorship W2543443338A5046303265 @default.
- W2543443338 hasAuthorship W2543443338A5059118728 @default.
- W2543443338 hasAuthorship W2543443338A5069381791 @default.
- W2543443338 hasAuthorship W2543443338A5070823788 @default.
- W2543443338 hasAuthorship W2543443338A5076888037 @default.
- W2543443338 hasConcept C109007969 @default.
- W2543443338 hasConcept C109281948 @default.
- W2543443338 hasConcept C112959462 @default.
- W2543443338 hasConcept C123588078 @default.
- W2543443338 hasConcept C127313418 @default.
- W2543443338 hasConcept C146588470 @default.
- W2543443338 hasConcept C150117547 @default.
- W2543443338 hasConcept C151730666 @default.
- W2543443338 hasConcept C15739521 @default.
- W2543443338 hasConcept C166957645 @default.
- W2543443338 hasConcept C186240526 @default.
- W2543443338 hasConcept C18903297 @default.
- W2543443338 hasConcept C205649164 @default.
- W2543443338 hasConcept C2778648423 @default.
- W2543443338 hasConcept C2780142684 @default.
- W2543443338 hasConcept C77928131 @default.
- W2543443338 hasConcept C86803240 @default.
- W2543443338 hasConcept C93257316 @default.
- W2543443338 hasConceptScore W2543443338C109007969 @default.
- W2543443338 hasConceptScore W2543443338C109281948 @default.
- W2543443338 hasConceptScore W2543443338C112959462 @default.
- W2543443338 hasConceptScore W2543443338C123588078 @default.
- W2543443338 hasConceptScore W2543443338C127313418 @default.
- W2543443338 hasConceptScore W2543443338C146588470 @default.
- W2543443338 hasConceptScore W2543443338C150117547 @default.
- W2543443338 hasConceptScore W2543443338C151730666 @default.
- W2543443338 hasConceptScore W2543443338C15739521 @default.
- W2543443338 hasConceptScore W2543443338C166957645 @default.
- W2543443338 hasConceptScore W2543443338C186240526 @default.
- W2543443338 hasConceptScore W2543443338C18903297 @default.
- W2543443338 hasConceptScore W2543443338C205649164 @default.
- W2543443338 hasConceptScore W2543443338C2778648423 @default.
- W2543443338 hasConceptScore W2543443338C2780142684 @default.
- W2543443338 hasConceptScore W2543443338C77928131 @default.
- W2543443338 hasConceptScore W2543443338C86803240 @default.
- W2543443338 hasConceptScore W2543443338C93257316 @default.
- W2543443338 hasLocation W25434433381 @default.
- W2543443338 hasOpenAccess W2543443338 @default.
- W2543443338 hasPrimaryLocation W25434433381 @default.
- W2543443338 hasRelatedWork W1513291151 @default.
- W2543443338 hasRelatedWork W1542845244 @default.
- W2543443338 hasRelatedWork W1577153269 @default.
- W2543443338 hasRelatedWork W1977763156 @default.
- W2543443338 hasRelatedWork W2039544921 @default.
- W2543443338 hasRelatedWork W2063492707 @default.
- W2543443338 hasRelatedWork W2076820956 @default.
- W2543443338 hasRelatedWork W2080677939 @default.
- W2543443338 hasRelatedWork W2096384323 @default.
- W2543443338 hasRelatedWork W2098147009 @default.
- W2543443338 hasRelatedWork W2123323322 @default.
- W2543443338 hasRelatedWork W2127983420 @default.
- W2543443338 hasRelatedWork W2153805427 @default.
- W2543443338 hasRelatedWork W2198102060 @default.
- W2543443338 hasRelatedWork W2199767425 @default.
- W2543443338 hasRelatedWork W2279722816 @default.
- W2543443338 hasRelatedWork W2314781636 @default.
- W2543443338 hasRelatedWork W2319542789 @default.
- W2543443338 hasRelatedWork W2802662489 @default.
- W2543443338 hasRelatedWork W3183022925 @default.
- W2543443338 hasVolume "47" @default.
- W2543443338 isParatext "false" @default.
- W2543443338 isRetracted "false" @default.
- W2543443338 magId "2543443338" @default.
- W2543443338 workType "article" @default.