WFRF:(Bonde Niels)
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| Fältnamn | Indikatorer | Metadata |
|---|---|---|
| 000 | 03707naa a2200493 4500 | |
| 001 | oai:DiVA.org:uu-241113 | |
| 003 | SwePub | |
| 008 | 150108s2014 | |||||||||||000 ||eng| | |
| 024 | 7 | a https://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-2411132 URI |
| 024 | 7 | a https://doi.org/10.2478/popore-2014-00302 DOI |
| 040 | a (SwePub)uu | |
| 041 | a engb eng | |
| 042 | 9 SwePub | |
| 072 | 7 | a ref2 swepub-contenttype |
| 072 | 7 | a art2 swepub-publicationtype |
| 100 | 1 | a Sulej, Tomasz4 aut |
| 245 | 1 0 | a New perspectives on the Late Triassic vertebrates of East Greenland :b preliminary results of a Polish−Danish palaeontological expedition |
| 264 | 1 | b Polish Academy of Sciences Chancellery,c 2014 |
| 338 | a print2 rdacarrier | |
| 520 | a The Fleming Fjord Formation (Jameson Land, East Greenland) documents a diverse assemblage of terrestrial vertebrates of Late Triassic age. Expeditions from the turn of the 21st century have discovered many important fossils that form the basis of our current knowledge of Late Triassic Greenlandic faunas. However, due to the scarcity and incompleteness of the fossils and their insufficient study, our understanding of the taxonomic diversity of the Fleming Fjord Formation is hindered. Here, we report the preliminary findings of a Polish−Danish expedition to the Fleming Fjord Formation that took place in 2014. Three areas were visited – the fairly well known MacKnight Bjerg and Wood Bjerg and the virtually unexplored Liasryggen. MacKnigth Bjerg and Liasryggen yielded fossils which promise to significantly broaden our knowledge of vertebrate evolution in the Late Triassic. Stem−mammal remains were discovered at Liasryggen. Other fossils found at both sites include remains of actinopterygians, sarcopterygians, temnospondyl amphibians and various archosaurs (including early dinosaurs). Numerous vertebrate trace fossils, including coprolites, pseudosuchian footprints, theropod and sauropodomorph dinosaur tracks, were also discovered. Newly discovered skeletal remains as well as abundant trace fossils indicate higher tetrapod diversity in the Late Triassic of Greenland than previously thought. Trace fossils also allow inferences of early theropod and sauropodomorph dinosaur behaviour. | |
| 650 | 7 | a NATURVETENSKAPx Geovetenskap och miljövetenskap0 (SwePub)1052 hsv//swe |
| 650 | 7 | a NATURAL SCIENCESx Earth and Related Environmental Sciences0 (SwePub)1052 hsv//eng |
| 653 | a Arctic | |
| 653 | a Greenland | |
| 653 | a stem−mammals | |
| 653 | a dinosaurs | |
| 653 | a footprints | |
| 653 | a Fleming Fjord Formation | |
| 653 | a Late Triassic | |
| 653 | a Earth Science with specialization in Historical Geology and Palaeontology | |
| 653 | a Geovetenskap med inriktning mot historisk geologi och paleontologi | |
| 653 | a Biologi med inriktning mot evolutionär organismbiologi | |
| 653 | a Biology with specialization in Evolutionary Organismal Biology | |
| 700 | 1 | a Wolniewicz, Andrzej4 aut |
| 700 | 1 | a Bonde, Niels4 aut |
| 700 | 1 | a Błażejowski, Blazej4 aut |
| 700 | 1 | a Niedźwiedzki, Grzegorz,d 1980-u Uppsala universitet,Institutionen för organismbiologi4 aut0 (Swepub:uu)grzni333 |
| 700 | 1 | a Tałanda, Mateusz4 aut |
| 710 | 2 | a Uppsala universitetb Institutionen för organismbiologi4 org |
| 773 | 0 | t Polish Polar Researchd : Polish Academy of Sciences Chancelleryg 35:4, s. 541-552q 35:4<541-552x 0138-0338x 2081-8262 |
| 856 | 4 | u https://doi.org/10.2478/popore-2014-0030y Fulltext |
| 856 | 4 | u https://doi.org/10.2478/popore-2014-0030 |
| 856 | 4 8 | u https://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-241113 |
| 856 | 4 8 | u https://doi.org/10.2478/popore-2014-0030 |
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