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  • 1. Brooks, Claire
    et al.
    Seow, Tricia
    Örbring, David
    Arenas, Adoni
    Salinas, Victor
    Einarsson, Elisabeth
    Lund University.
    Geographical knowledge disparities: regional variation in conceptions of school and academic geography and the influence on teachers and curriculum2017Conference paper (Other academic)
  • 2.
    Einarsson, Elisabeth
    Lund University.
    A mid-campanian marine extinction event: evidence from Kristianstad Basin, Southern Sweden2011Conference paper (Other academic)
  • 3.
    Einarsson, Elisabeth
    Lund University.
    Bland havssköldpaddor, hajar och havsmonster: en faunabeskrivning över Kristianstadstrakten för 80 miljoner år sedan2011Conference paper (Other academic)
  • 4.
    Einarsson, Elisabeth
    Lund University.
    Den nya lärarfortbildningen: med klimatet i fokus2014In: LMNT-nytt, Riksföreningen för lärarna i matematik, naturvetenskap och teknik, p. 24-25Article in journal (Other academic)
  • 5.
    Einarsson, Elisabeth
    Lund University.
    Dinosaurier och andra fossil2010In: Bladet, Vol. 10, no 1Article in journal (Other academic)
  • 6.
    Einarsson, Elisabeth
    Lund University.
    Dinosaurier på schemat!2008In: Bladet, Vol. 08, no 4Article in journal (Other academic)
  • 7.
    Einarsson, Elisabeth
    Lund University.
    Dinosaurier på schemat: från förskola till gymnasieskola2011In: Bi-lagan, no 3Article in journal (Other academic)
  • 8.
    Einarsson, Elisabeth
    Lund University.
    Geologi för alla: från förskola till gymnasium!2011In: Geologiskt forum, Vol. 18, no 71Article in journal (Other academic)
  • 9.
    Einarsson, Elisabeth
    Lund University.
    Geologi i skolan: en framtida verklighet?2014Conference paper (Other academic)
  • 10.
    Einarsson, Elisabeth
    Lund University.
    Geologi i skolan: en samlingspunkt i inlärningen2012In: Geologiska föreningen, Vol. 19, no 74, p. 31-31Article in journal (Other (popular science, discussion, etc.))
  • 11.
    Einarsson, Elisabeth
    Lund University.
    Geology in school2011Conference paper (Other academic)
  • 12.
    Einarsson, Elisabeth
    Lund University.
    Geology in school: interdisciplinary teaching based on Lgr11 with geology as the theme2014In: Geology in school: interdisciplinary teaching based on Lgr11 with geology as the theme, 2014Conference paper (Other academic)
  • 13.
    Einarsson, Elisabeth
    Lund University.
    I dinosauriernas fotspår: förhistorisk utgrävning på Åsen2011In: Näsums hembygds- och fornminnesförenings årsbok, ISSN 1104-1498, p. 60-66Article in journal (Other academic)
  • 14.
    Einarsson, Elisabeth
    Lund University.
    Mosasaur bite marks on a plesiosaur propodial from the Kristianstad basin, southern Sweden (Campanian, Late Cretaceous)2009Conference paper (Other academic)
  • 15.
    Einarsson, Elisabeth
    Lund University.
    Paleoenvironments, palaeoecology and palaeobiogeography of late cretaceous (campanian) faunas from the Kristianstad basin, southern Sweden, with applications for science education2018Doctoral thesis, comprehensive summary (Other academic)
    Abstract [en]

    This thesis is thematically divided into two sections: Part1 presents studies related to the palaeoenvironments,palaeoecology and palaeobiogeography of the LateCretaceous (Campanian) faunas from the KristianstadBasin of southern Sweden; Part 2 reports on applicationsof palaeontological research for science education inschools.Part 1 was based on personally conducted fieldworkand biostratigraphical analysis at various Santonian-Campanian localities throughout Skåne. However, themost complete section at Åsen provided the primary datasource and was systematically excavated with a team ofvolunteers, who employed wet-sieving methods to extractbulk fossil material from each bed within the sequence. Aseries of globally correlated temperature-induced changeswas detected in the stepwise declining abundanceand disappearance of rudists, sclerorhynchids and therajiforms Rhinobatos and Squatirhina, as well as marinecrocodilians, various mosasaurid lizard taxa. A rangeof local palaeoenvironments were also reconstructed,including estuaries, rocky coastlines, sandy beaches,drowned river valleys, shallow neritic settings, anddeeper offshore conditions. An archipelago bordering theFennoscandian landmasses also supported continentalecosystems comprising ferns, conifers and early floweringplants, with dinosaurs, pterosaurs and non-marine turtles.Trophic levels within the marine system incorporatedred algae and dinoflagellates as primary producers, withcorals, brachiopods, bivalves, echinoids, barnacles anddecapod crustaceans as benthos, and belemnites withinthe water column. Actinopterygian fish, sharks, rays andchimaeroids, chelonioid sea turtles, marine crocodilians,polycotylid and elasmosaurid plesiosaurians, variousmosasaurids and aquatic hesperornithiform birdscollectively represented middle level and apex predators.Herbivorous and carnivorous dinosaurs, lizards and softshelledtryonichid turtles evidence elements of terrestrialisland communities. The palaeobiogeographicalrelationships and dispersal of these local assemblageswas probably influenced by marine transgressions andregressions. These would have affected habitat availabilityand connectivity via changing water depths.Part 2 presents three school education projects aimed atincreasing awareness of geoscience and natural history inschools. The better integration of geological time conceptsand geosciences into the Swedish school curriculum isalso discussed. The first study described a project wherebyfossils were found in the sandboxes in preschools, andtheir use as a tool for learning about dinosaurs, fossilsand natural history. A survey of teachers and childrenfound that both increased their knowledge base throughthis approach, and that the local context of the fossilsin particular generated interest about the subject. Theconcepts of geological time was similarly addressed in thesecond study, which utilized timescale projects and otherhands-on activities to create memory triggers for childrenand students, and to demonstrate how the perspective of‘deep time’ is relevant for understanding large-scale Earthprocesses, such as evolution and environmental change.The integration of geosciences into the Swedish schoolcurriculum is currently inadequate. Therefore, the finalpaper in this sequence discusses how geosciences forman interdisciplinary bridge between school subjects andcan be used to teach geography and biology at all schoollevels.

  • 16.
    Einarsson, Elisabeth
    Lund University.
    The Cretaceous world: fauna, flora and climate2013In: LUCCI Annual Report 2013/2014, 2013Conference paper (Other academic)
  • 17.
    Einarsson, Elisabeth
    Lund University.
    Vilken är din favoritplats på skolgården?2010In: Bladet, Vol. 10, no 3Article in journal (Other academic)
  • 18.
    Einarsson, Elisabeth
    et al.
    Lund University.
    Lindgren, Johan
    Lund University.
    Kear, Benjamin P.
    Uppsala University.
    Siverson, Mikael
    Australia.
    Mosasaur bite marks on a plesiosaur propodial from the Campanian (Late Cretaceous) of southern Sweden2010In: GFF, ISSN 1103-5897, E-ISSN 2000-0863, Vol. 132, no 2, p. 123-128Article in journal (Refereed)
    Abstract [en]

    Although plesiosaurs and mosasaurs co-existed for about 35 million years at the end of the Cretaceous, the fossil record documenting interactions between these two groups of marine reptiles is meagre. The discovery of deeply incised scars on a limb bone of an immature polycotylid plesiosaur from the latest early Campanian (in the European two-fold division of the Campanian Stage) of the Kristianstad Basin, southern Sweden, is thus significant because it represents a rare example of predation or scavenging on an immature polycotylid plesiosaur by a large mosasaur.

  • 19.
    Einarsson, Elisabeth
    et al.
    Lund University.
    Praszkier, Aron
    Vajda, Vivi
    First evidence of the Cretaceous decapod crustacean Protocallianassa from Sweden2016In: Geological Society, London, Special Publications, Vol. 434, p. 241-250Article in journal (Refereed)
    Abstract [en]

    An assemblage of the burrowing ghost shrimp, Protocallianassa faujasi, is described, providing the first evidence of this decapod species from Sweden. The fossils occur in successions of the informal earliest late Campanian Belemnellocamax balsvikensis zone at Åsen and the latest early Campanian B. mammillatus zone at Ivö Klack, both in the Kristianstad Basin of NE Skåne. Numerous, heavily calcified chelipeds were found within a restricted bed at Å sen that was rich in carbonate-cemented nodules. Based on the burrowing lifestyle of modern mud shrimps, we interpret these nodules as infilled burrow chambers. The low abundance of molluscs within the Protocallianassa beds is also consistent with analogous extant communities, indicating that a similar ecologically exclusive relationship ruled within the Late Cretaceous shallowmarine ecosystems.

  • 20.
    Einarsson, Elisabeth
    et al.
    Lund University.
    Vajda, Vivi
    How improve teachers’ motivation to educate in geology within the Swedish school system2012Conference paper (Other academic)
  • 21.
    Einarsson, Elisabeth
    et al.
    Lund University.
    Örbring, David
    Lund University.
    Ämnesdidaktiska hörnet: skolämnet geografi i relation till geologi2016In: Geografiska notiser, Vol. 74, no 2, p. 61-63Article in journal (Other academic)
  • 22.
    McLoughlin, Stephen
    et al.
    Swedish Museum of Natural History.
    Haig, David W.
    Australia.
    Siversson, Mikael
    Australia.
    Einarsson, Elisabeth
    Lund University.
    Did mangrove communities exist in the late cretaceous of the Kristianstad Basin, Sweden?2018In: Palaeogeography, Palaeoclimatology, Palaeoecology, ISSN 0031-0182, E-ISSN 1872-616X, Vol. 498, p. 99-114Article in journal (Refereed)
    Abstract [en]

    Previous inferences of oyster-dominated communities occupying mangrove-like depositional settings in the Kristianstad Basin, Sweden, during the late early Campanian are reassessed. A significant percentage of oysters (Acutostrea incurva) from the Belemnellocamax mammillatus zone in Bed 3 at Asen bear indentations on their left valves indicating attachment to plant axes. Many of these axes bear morphological features characteristic of the distal subaerial portions of woody plant branches and appear to have been rafted into the marine environment rather than representing in situ mangrove stems and roots. Foraminiferal assemblages recovered from sediment within the oyster body cavities differ from modern mangrove-community associations by the absence of siliceous agglutinated Foraminifera, the presence of diverse and relatively abundant Lagenida, relatively common triserial Buliminida, and a notable percentage of planktonic taxa. Chondrichthyan teeth assemblages from the same beds are similarly incompatible with the interpretation of a mangrove depositional environment based on comparisons with the distribution of related extant taxa. Apart from oyster shells and belemnite rostra, these beds are notably depauperate in diversity and abundance of macroinvertebrate remains compared with coeval carbonate shoal and rocky shoreline assemblages from the same basin. The collective palaeontological and sedimentological evidence favours an inner neritic sandy-substrate setting, but not nearshore or mangrove-like depositional environment for the oyster-rich Bed 3 at Asen. The absence of mangrove-like assemblages at Asen is consistent with the development of modern mangrove ecosystems much later (during the Maastrichtian and Cenozoic) based on the global palynological record.

  • 23.
    Mellgren, Johanna
    et al.
    Lund University.
    Einarsson, ElisabethLund University.
    Lundadagarna i historisk geologi och paleontologi XI, Abstracts2009Conference proceedings (editor) (Other academic)
  • 24. Proporat, Stephen F
    et al.
    Einarsson, Elisabeth
    Lund University.
    Lindgren, Johan
    Bazzi, Mohamad
    Lagerstam, Clarence
    Kear, Benjamin P
    Late Cretaceous dinosaurian remains from the Kristianstad Basin of southern Sweden2016In: Geological Society Special Publication, Vol. 434, p. 231-239Article in journal (Refereed)
    Abstract [en]

    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

  • 25.
    Scheyer, Torsten M.
    et al.
    Switzerland.
    Mors, Thomas
    Swedish Museum of Natural History.
    Einarsson, Elisabeth
    Lund University.
    First record of soft-shelled turtles (cryptodira, trionychidae) from the late cretaceous of Europe2012In: Journal of Vertebrate Paleontology, ISSN 0272-4634, E-ISSN 1937-2809, Vol. 32, no 5, p. 1027-1032Article in journal (Refereed)
    Abstract [en]

    Fossil soft-shelled turtles (Trionychidae) have so far been recognized in all continents except Antarctica, based largely on remains preserving their diagnostic sculptured shell bones. The origin of the group is generally assumed to be in the Early Cretaceous of Asia, whereas they first appear in North America and Europe during the Late Cretaceous and Paleocene, respectively. Here we describe the first record of an indeterminate trionychid from the late early Campanian from southern Sweden, a part of the paleobiogeographically isolated Fenno-Scandian Shield, thus extending the stratigraphic record of the group in Europe back about 15 Ma into the Late Cretaceous. Our finding provides evidence against the currently favored dispersal scenario in which trionychid turtles are interpreted to have come to Europe first during the Paleocene either directly from North America or via Asia. The described indeterminate trionychid possibly represents a relic of a pre-Cretaceous endemic radiation of North European trionychids living mainly on the Fenno-Skandian Shield or it may indicate a potential lower latitude dispersal route of trionychids from Asia to North America via Europe during the Late Cretaceous.

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