The first evidence of trace fossils and pseudo-fossils in the continental interlava volcaniclastic sediments on the Faroe Islands
Interlava volcaniclastic sediments, mostly sandstones, from the Palaeogene Faroe Islands Basalt Group (Malinstindur and Sneis Formations) contain rare ichnofauna and well-preserved pseudofossils in the form of linear structures. Five specimens of two ichnogenera have been identified, which include H...
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ftczacademyscien:oai:asep.lib.cas.cz:CavUnEpca/0453417 2024-09-15T18:05:30+00:00 The first evidence of trace fossils and pseudo-fossils in the continental interlava volcaniclastic sediments on the Faroe Islands Pokorný, R. Krmíček, L. (Lukáš) Árting, U. E. 2015 http://hdl.handle.net/11104/0254240 eng eng urn:pissn: 2245-7070 urn:eissn: 2245-7070 http://hdl.handle.net/11104/0254240 Faroe Islands trace fossils pseudo-fossils volcaniclastic sediments info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2015 ftczacademyscien 2024-08-19T05:33:00Z Interlava volcaniclastic sediments, mostly sandstones, from the Palaeogene Faroe Islands Basalt Group (Malinstindur and Sneis Formations) contain rare ichnofauna and well-preserved pseudofossils in the form of linear structures. Five specimens of two ichnogenera have been identified, which include Helminthoidichnites isp. and ?Palaeophycus isp. The linear structures are interpreted to be desiccation cracks. This association indicates an environment with low to moderate hydrodynamic energy, which confirms a mosaic landscape of floodplains with rivers and shallow lakes. Article in Journal/Newspaper Faroe Islands The Czech Academy of Sciences: Publication Activity (ASEP) |
institution |
Open Polar |
collection |
The Czech Academy of Sciences: Publication Activity (ASEP) |
op_collection_id |
ftczacademyscien |
language |
English |
topic |
Faroe Islands trace fossils pseudo-fossils volcaniclastic sediments |
spellingShingle |
Faroe Islands trace fossils pseudo-fossils volcaniclastic sediments Pokorný, R. Krmíček, L. (Lukáš) Árting, U. E. The first evidence of trace fossils and pseudo-fossils in the continental interlava volcaniclastic sediments on the Faroe Islands |
topic_facet |
Faroe Islands trace fossils pseudo-fossils volcaniclastic sediments |
description |
Interlava volcaniclastic sediments, mostly sandstones, from the Palaeogene Faroe Islands Basalt Group (Malinstindur and Sneis Formations) contain rare ichnofauna and well-preserved pseudofossils in the form of linear structures. Five specimens of two ichnogenera have been identified, which include Helminthoidichnites isp. and ?Palaeophycus isp. The linear structures are interpreted to be desiccation cracks. This association indicates an environment with low to moderate hydrodynamic energy, which confirms a mosaic landscape of floodplains with rivers and shallow lakes. |
format |
Article in Journal/Newspaper |
author |
Pokorný, R. Krmíček, L. (Lukáš) Árting, U. E. |
author_facet |
Pokorný, R. Krmíček, L. (Lukáš) Árting, U. E. |
author_sort |
Pokorný, R. |
title |
The first evidence of trace fossils and pseudo-fossils in the continental interlava volcaniclastic sediments on the Faroe Islands |
title_short |
The first evidence of trace fossils and pseudo-fossils in the continental interlava volcaniclastic sediments on the Faroe Islands |
title_full |
The first evidence of trace fossils and pseudo-fossils in the continental interlava volcaniclastic sediments on the Faroe Islands |
title_fullStr |
The first evidence of trace fossils and pseudo-fossils in the continental interlava volcaniclastic sediments on the Faroe Islands |
title_full_unstemmed |
The first evidence of trace fossils and pseudo-fossils in the continental interlava volcaniclastic sediments on the Faroe Islands |
title_sort |
first evidence of trace fossils and pseudo-fossils in the continental interlava volcaniclastic sediments on the faroe islands |
publishDate |
2015 |
url |
http://hdl.handle.net/11104/0254240 |
genre |
Faroe Islands |
genre_facet |
Faroe Islands |
op_relation |
urn:pissn: 2245-7070 urn:eissn: 2245-7070 http://hdl.handle.net/11104/0254240 |
_version_ |
1810443050735894528 |