Published November 10, 2016
| Version v1
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Figure 1 in A silicified Early Triassic marine assemblage from Svalbard
- 1. Jackson School of Geosciences, University of Texas, Austin, TX 78712, USA; & Earth Sciences, Plymouth University, Plymouth, PL4 8AA, UK; & Department of Earth Sciences, Natural History Museum, London, SW7 5BD, UK;
- 2. Earth Sciences, Plymouth University, Plymouth, PL4 8AA, UK; & Department of Geology, University of Georgia, Athens, GA 30602, USA
- 3. Department of Earth Sciences, Natural History Museum, London, SW7 5BD, UK;
Description
Figure 1. Locality and stratigraphy of the studied section in Lusitaniadalen. A, locality map of the Lusitaniadalen section; B, palaeogeographical position; C, stratigraphical column indicating the position of the sampled concretionary levels (LD-04 and LD-05) and disappearance of bioturbation associated with marine ecosystem collapse and the Late Permian mass extinction (LPE; modified from Nabbefeld et al. 2010). Abbreviations: KSF, Kapp Starostin Formation; ii, ichnofabric index. Palaeogeography after Blakey (2012).
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Related works
- Is part of
- Journal article: 10.1080/14772019.2016.1245680 (DOI)
- Journal article: urn:lsid:plazi.org:pub:390273358050E82B6D0FFFE98D67263C (LSID)
- Journal article: http://publication.plazi.org/id/390273358050E82B6D0FFFE98D67263C (URL)
- Journal article: https://zenodo.org/record/10883052 (URL)