Published May 22, 2018
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Fig. 7 in Arthropod trace fossils from Eocene cold climate continental strata of King George Island, West Antarctica
Description
Fig. 7. Arthropod trace fossil Glaciichnium australis isp. nov. preserved mostly as unilobated or bilobated median trails, middle–late Eocene, Mount Wawel Formation, King George Island, Antarctica, slab ZPAL Tf.8/2007.25. A. Unilobate median trail passes into irregular trackway, produced probably in low cohesive substrate. B. A transition between unilobate and bilobate median trail. C. Unilobate and bilobate median trails as epichnial furrows. D. Hypichnial ridges, which are unilobated median trails resembling the trace fossil Helminthoidichnites.
Notes
Published as part of Uchman, Alfred, Gaździcki, Andrzej & Błażejowski, Błażej, 2018, Arthropod trace fossils from Eocene cold climate continental strata of King George Island, West Antarctica, pp. 383-396 in Acta Palaeontologica Polonica 63 (2) on page 390, DOI: 10.4202/app.00467.2018, http://zenodo.org/record/13262379
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- Is cited by
- Taxonomic treatment: http://treatment.plazi.org/id/03A1FA76FFA11A07E9B982EEFE25F9BE (URL)
- Is part of
- Journal article: 10.4202/app.00467.2018 (DOI)
- Journal article: urn:lsid:plazi.org:pub:FF98820EFFA51A0EE92E875DFFE8FFD1 (LSID)
- Journal article: http://publication.plazi.org/id/FF98820EFFA51A0EE92E875DFFE8FFD1 (URL)
- Journal article: https://zenodo.org/record/13262379 (URL)