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Palynostratigraphy of dinosaur footprint-bearing deposits from theTriassic–Jurassic boundary interval of Sweden

Vajda, Vivi (author)
Lund University,Lunds universitet,Naturhistoriska riksmuseet,Enheten för paleobiologi,Berggrundsgeologi,Geologiska institutionen,Naturvetenskapliga fakulteten,Lithosphere and Biosphere Science,Department of Geology,Faculty of Science
Calner, Mikael (author)
Lund University,Lunds universitet,Berggrundsgeologi,Geologiska institutionen,Naturvetenskapliga fakulteten,Lithosphere and Biosphere Science,Department of Geology,Faculty of Science
Ahlberg, Anders (author)
Lund University,Lunds universitet,Berggrundsgeologi,Geologiska institutionen,Naturvetenskapliga fakulteten,Lithosphere and Biosphere Science,Department of Geology,Faculty of Science
 (creator_code:org_t)
Informa UK Limited, 2013
2013
English.
In: GFF. - : Informa UK Limited. - 1103-5897 .- 2000-0863. ; 135, s. 120-130
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • The Triassic–Jurassic boundary (c. 200 Ma) marks one of the five largest Phanerozoic mass extinction events and is characterized by a major turnover in biotas. A palynological study of sedimentary rock slabs bearing dinosaur footprints from Rhaeto–Hettangian strata of Skåne, Sweden was carried out. The theropod dinosaur footprints (Kayentapus soltykovensis) derive from the southern part of the abandoned Vallåkra quarry (Höganäs Formation) and were originally dated as earliest Jurassic (Hettangian) based on lithostratigraphy. Our results reveal that two of the footprints are correlative with the latest Triassic (latest Rhaetian) disaster zone typified by a high abundance of the enigmatic gymnosperm pollen Ricciisporites tuberculatus and Perinopollenites elatoides together with the key taxon Limbosporites lundbladii and fern spores. Two footprints are dated to correlate with the Transitional Spore-spike Interval. One footprint is interpreted as Hettangian in age based on the relatively high abundance of Pinuspollenites spp. together with the presence of the key taxa Retitriletes semimuris and Zebrasporites intercriptus. Our new palynological study suggests that the Kayentapus ichnogenus already appeared in the end of Triassic, and our study highlights the use of palynology as a powerful tool to date historical collections of fossils in museums, universities and elsewhere. The Hettangian footprint reflects a marine influence while all other studied ichnofossil specimens occur in non-marine (floodplain and delta interdistributary) sediments. The sediments associated with the Hettangian footprint include a significant proportion of charcoal transported from land after wildfires. The Rhaeto–Hettangian vegetation was otherwise characterized by multi-storey gymnosperm–pteridophyte communities.

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geologi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geology (hsv//eng)
SAMHÄLLSVETENSKAP  -- Utbildningsvetenskap -- Pedagogik (hsv//swe)
SOCIAL SCIENCES  -- Educational Sciences -- Pedagogy (hsv//eng)

Keyword

Dinosaurs
Vallåkra
footprints
trackways
vegetation
mass extinction
Jurassic
Dinosaurier
Vallåkra
fotspår
vegetation
massutdöende
Jura
Ecosystems and species history
Ekosystem och arthistoria
Triassic-Jurassic
dinosaur footprints
ecological crisis
palynology
Sweden

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ref (subject category)
art (subject category)

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By the author/editor
Vajda, Vivi
Calner, Mikael
Ahlberg, Anders
About the subject
NATURAL SCIENCES
NATURAL SCIENCES
and Earth and Relate ...
and Geology
SOCIAL SCIENCES
SOCIAL SCIENCES
and Educational Scie ...
and Pedagogy
Articles in the publication
GFF
By the university
Swedish Museum of Natural History
Lund University

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