Late Cretaceous dinosaurian remains from the Kristianstad Basin of southern Sweden

Mesozoic dinosaur fossils are exceptionally rare in Scandinavia. The Swedish record is typically depauperate, with the Kristianstad Basin of SkÅne (Scania) yielding all of the known fossils from Swedish Cretaceous strata. Although highly fragmentary, these body remnants are important because they pr...

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Published in:Geological Society, London, Special Publications
Main Authors: Poropat, Stephen F., Einarsson, Elisabeth, Lindgren, Johan, Bazzi, Mohamad, Lagerstam, Clarence, Kear, Benjamin P.
Format: Article in Journal/Newspaper
Language:English
Published: Geological Society of London 2016
Subjects:
Online Access:https://lup.lub.lu.se/record/7661dec0-3cae-42d3-a477-51aa8b60c300
https://doi.org/10.1144/SP434.8
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spelling ftulundlup:oai:lup.lub.lu.se:7661dec0-3cae-42d3-a477-51aa8b60c300 2023-09-05T13:19:24+02:00 Late Cretaceous dinosaurian remains from the Kristianstad Basin of southern Sweden Poropat, Stephen F. Einarsson, Elisabeth Lindgren, Johan Bazzi, Mohamad Lagerstam, Clarence Kear, Benjamin P. 2016 https://lup.lub.lu.se/record/7661dec0-3cae-42d3-a477-51aa8b60c300 https://doi.org/10.1144/SP434.8 eng eng Geological Society of London https://lup.lub.lu.se/record/7661dec0-3cae-42d3-a477-51aa8b60c300 http://dx.doi.org/10.1144/SP434.8 scopus:84970021313 Geological Society Special Publication; 434, pp 231-239 (2016) ISSN: 0305-8719 Geology contributiontojournal/article info:eu-repo/semantics/article text 2016 ftulundlup https://doi.org/10.1144/SP434.8 2023-08-16T22:28:39Z Mesozoic dinosaur fossils are exceptionally rare in Scandinavia. The Swedish record is typically depauperate, with the Kristianstad Basin of SkÅne (Scania) yielding all of the known fossils from Swedish Cretaceous strata. Although highly fragmentary, these body remnants are important because they provide evidence of a relatively diverse fauna, including previously recognized hesperornithiform birds and leptoceratopsid ceratopsians, as well as indeterminate ornithopods that are confirmed here for the first time. In this paper, we describe three phalanges (from Åsen) and an incomplete right tibia (from Ugnsmunnarna) from the Kristianstad Basin. One of the phalanges appears to pertain to a leptoceratopsid ceratopsian, providing further evidence of these small ornithischians in the Cretaceous sediments of Sweden. The other two phalanges are interpreted as deriving from small ornithopods similar to Thescelosaurus and Parksosaurus. The tibia appears to represent the first evidence of a non-avian theropod dinosaur in the Cretaceous of Sweden, with a previous report of theropod remains based on fish teeth having been corrected by other authors. The remains described herein provide important additions to the enigmatic dinosaurian fauna that inhabited the Fennoscandian archipelago during the latest Cretaceous. Article in Journal/Newspaper Fennoscandian Lund University Publications (LUP) Geological Society, London, Special Publications 434 1 231 239
institution Open Polar
collection Lund University Publications (LUP)
op_collection_id ftulundlup
language English
topic Geology
spellingShingle Geology
Poropat, Stephen F.
Einarsson, Elisabeth
Lindgren, Johan
Bazzi, Mohamad
Lagerstam, Clarence
Kear, Benjamin P.
Late Cretaceous dinosaurian remains from the Kristianstad Basin of southern Sweden
topic_facet Geology
description Mesozoic dinosaur fossils are exceptionally rare in Scandinavia. The Swedish record is typically depauperate, with the Kristianstad Basin of SkÅne (Scania) yielding all of the known fossils from Swedish Cretaceous strata. Although highly fragmentary, these body remnants are important because they provide evidence of a relatively diverse fauna, including previously recognized hesperornithiform birds and leptoceratopsid ceratopsians, as well as indeterminate ornithopods that are confirmed here for the first time. In this paper, we describe three phalanges (from Åsen) and an incomplete right tibia (from Ugnsmunnarna) from the Kristianstad Basin. One of the phalanges appears to pertain to a leptoceratopsid ceratopsian, providing further evidence of these small ornithischians in the Cretaceous sediments of Sweden. The other two phalanges are interpreted as deriving from small ornithopods similar to Thescelosaurus and Parksosaurus. The tibia appears to represent the first evidence of a non-avian theropod dinosaur in the Cretaceous of Sweden, with a previous report of theropod remains based on fish teeth having been corrected by other authors. The remains described herein provide important additions to the enigmatic dinosaurian fauna that inhabited the Fennoscandian archipelago during the latest Cretaceous.
format Article in Journal/Newspaper
author Poropat, Stephen F.
Einarsson, Elisabeth
Lindgren, Johan
Bazzi, Mohamad
Lagerstam, Clarence
Kear, Benjamin P.
author_facet Poropat, Stephen F.
Einarsson, Elisabeth
Lindgren, Johan
Bazzi, Mohamad
Lagerstam, Clarence
Kear, Benjamin P.
author_sort Poropat, Stephen F.
title Late Cretaceous dinosaurian remains from the Kristianstad Basin of southern Sweden
title_short Late Cretaceous dinosaurian remains from the Kristianstad Basin of southern Sweden
title_full Late Cretaceous dinosaurian remains from the Kristianstad Basin of southern Sweden
title_fullStr Late Cretaceous dinosaurian remains from the Kristianstad Basin of southern Sweden
title_full_unstemmed Late Cretaceous dinosaurian remains from the Kristianstad Basin of southern Sweden
title_sort late cretaceous dinosaurian remains from the kristianstad basin of southern sweden
publisher Geological Society of London
publishDate 2016
url https://lup.lub.lu.se/record/7661dec0-3cae-42d3-a477-51aa8b60c300
https://doi.org/10.1144/SP434.8
genre Fennoscandian
genre_facet Fennoscandian
op_source Geological Society Special Publication; 434, pp 231-239 (2016)
ISSN: 0305-8719
op_relation https://lup.lub.lu.se/record/7661dec0-3cae-42d3-a477-51aa8b60c300
http://dx.doi.org/10.1144/SP434.8
scopus:84970021313
op_doi https://doi.org/10.1144/SP434.8
container_title Geological Society, London, Special Publications
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