Within this famous site, we can observe:

- Regionally unique Lochkovian volcanites,

- Pragian trilobite-rich crinoidal limestones.

- Lower Emsian (Zlíchovian) steep, cone-shaped mudmounds with coral-stabilized flanks.

- Hydrothermal hot vent communities and trilobite lumachelles filling neptunian dykes.

- Rapid upper Emsian burial and overlying, fossiliferous hemipelagic, hypoxic marls.

- Eifelian to Givetian goniatite limestones.

- Hypoxic lower Frasnian styliolinites and Upper Frasnian Kellwasser Facies with cephalopod mass occurrences.

- Lower Famennian radiation interval with rich cheiloceratid fauna.

- The Eifelian/Givetian HOLLARD Mound and its methane seep environments

More details on :

https://www.researchgate.net/publication/324248737_The_world-famous_Devonian_mudmounds_at_Hamar_Laghdad_and_overlying_cephalopod-rich_strata

More Ahmed El Hassani's questions See All
Similar questions and discussions