Английская Википедия:Asteriacites
Шаблон:Short description Шаблон:Ichnobox
Asteriacites is the name given to five-rayed trace fossils found in marine sedimentary rocks (Mángano et al., 1999; Wilson and Rigby, 2000). They record the burrows of ophiuroid and asteroid sea stars on the sea floor. Asteriacites are found in European and American rocks, from the Ordovician period onwards, and are especially numerous in the Triassic and Jurassic systems.[1][2][3]
Dense assemblages of Asteriacites ('Asteriacites beds') are considered proxies for marine settings, low bioturbation intensity, shallow tiering, high sedimentation rate and/or event-bed deposition, significant levels of hydrodynamic energy, and low predation pressure.[3]
Gallery
-
Asteriacites from the Devonian of northeastern Ohio; this trace was made by an asteroid echinoderm
-
Bedding plane view of Asteriacites from the Snapper Point Formation (Permian), New South Wales
References
Шаблон:Commons category Шаблон:Reflist
Шаблон:Trace-fossil-stub
Шаблон:Paleo-echinoderm-stub
- ↑ Шаблон:Cite journal
- ↑ Шаблон:Cite journal
- ↑ 3,0 3,1 Baucon, A., Neto de Carvalho, C. 2016. Stars of the aftermath: Asteriacites beds from the Lower Triassic of the Carnic Alps (Werfen Formation, Sauris di Sopra), Italy. Palaios 31. Abstract available at http://www.tracemaker.com
- Страницы с неработающими файловыми ссылками
- Английская Википедия
- Prehistoric Asterozoa genera
- Devonian echinoderms
- Silurian echinoderms
- Silurian animals of North America
- Paleozoic echinoderms of North America
- Devonian trace fossils
- Trace fossils
- Страницы, где используется шаблон "Навигационная таблица/Телепорт"
- Страницы с телепортом
- Википедия
- Статья из Википедии
- Статья из Английской Википедии