onr:"swepub:oai:DiVA.org:uu-241122"
Sökning: onr:"swepub:oai:DiVA.org:uu-241122" > Storm origin of bon...
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| Fältnamn | Indikatorer | Metadata |
|---|---|---|
| 000 | 03153naa a2200421 4500 | |
| 001 | oai:DiVA.org:uu-241122 | |
| 003 | SwePub | |
| 008 | 150108s2014 | |||||||||||000 ||eng| | |
| 024 | 7 | a https://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-2411222 URI |
| 024 | 7 | a https://doi.org/10.7306/gq.11912 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 Szrek, Piotr4 aut |
| 245 | 1 0 | a Storm origin of bone-bearing beds in the Lower Devonian placoderm sandstone from Podlazie Hill (Holy Cross Mountains, central Poland) |
| 264 | c 2014-09-15 | |
| 264 | 1 | b Polish Geological Institute - National Research Institute (PGI-NRI),c 2014 |
| 338 | a print2 rdacarrier | |
| 520 | a The placoderm sandstone (Emsian, Holy Cross Mountains) exposed in the abandoned quarry at Podlazie Hill was revisited and excavated during fieldwork conducted in 2011–2013. Bone-bearing breccias were studied in details for the first time at this site and subjected to taphonomic analysis. Vertebrate remains are dominated by heterostracans, while true placoderm compose less than 20% of the total vertebrate assemblage. The high degree of fragmentation of the bones and low degree of abrasion indicate that the remains were reworked and transported be fore final burial. This is consistent with the mixed character of the bone accumulations, which comprise both open-shelf forms (acanthodians, chondrichthyans) as well as those related to marginal-marine environments (placoderms and sarcopterygians). The bone-bearing succession has been subdivided into five depositional facies attributed to a coastal lagoon influenced by stormy, possibly tidal conditions. The occurrence of the invertebrate trace fossil Ilmenichnus sp. accompanied by Lockeia and Monomorphichnus supports this interpretation. | |
| 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 |
| 650 | 7 | a NATURVETENSKAPx Geovetenskap och miljövetenskapx Geologi0 (SwePub)105042 hsv//swe |
| 650 | 7 | a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Geology0 (SwePub)105042 hsv//eng |
| 653 | a placoderm sandstone | |
| 653 | a Lower Devonian | |
| 653 | a Emsian | |
| 653 | a Holy Cross Mountains | |
| 653 | a Earth Science with specialization in Historical Geology and Palaeontology | |
| 653 | a Geovetenskap med inriktning mot historisk geologi och paleontologi | |
| 700 | 1 | a Niedzwiedzki, Grzegorz,d 1980-u Uppsala universitet,Evolution och utvecklingsbiologi4 aut0 (Swepub:uu)grzni333 |
| 700 | 1 | a Dec, Marek4 aut |
| 710 | 2 | a Uppsala universitetb Evolution och utvecklingsbiologi4 org |
| 773 | 0 | t Geological Quarterlyd : Polish Geological Institute - National Research Institute (PGI-NRI)g 58:4, s. 795-806q 58:4<795-806x 1641-7291x 2082-5099 |
| 856 | 4 | u https://gq.pgi.gov.pl/article/download/9323/pdf_1183 |
| 856 | 4 8 | u https://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-241122 |
| 856 | 4 8 | u https://doi.org/10.7306/gq.1191 |
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