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- Kačák_Event abstract "The Kačák Event (Czech pronunciation: [kat͡ʃaːk]) or Kačák-otomari Event is a widely recognised bioevent or series of events that occurred close to the end of the Eifelian Age of the Middle Devonian Epoch. It involved a global eustatic rise in sea-level. It was named for the Kačák Member of the Srbsko Formation in Bohemia, where it is represented by a black shale interval within a sequence of limestone. In marine environments, this appears as an anoxic event, often forming potential hydrocarbon source rocks such as the Marcellus Shale. Within the Old Red Sandstone continent, it is represented by the Achanarras lake, the deepest and most widespread lake that developed within the Orcadian Basin. The event is associated with significant extinctions, particularly amongst the Ammonoidea.".
- Kačák_Event wikiPageID "16743599".
- Kačák_Event wikiPageLength "7854".
- Kačák_Event wikiPageOutDegree "42".
- Kačák_Event wikiPageRevisionID "666241038".
- Kačák_Event wikiPageWikiLink Age_(geology).
- Kačák_Event wikiPageWikiLink Ammonoidea.
- Kačák_Event wikiPageWikiLink Anoxic_event.
- Kačák_Event wikiPageWikiLink Bioevent.
- Kačák_Event wikiPageWikiLink Black_shale.
- Kačák_Event wikiPageWikiLink Bohemia.
- Kačák_Event wikiPageWikiLink Cantabria.
- Kačák_Event wikiPageWikiLink Carnic_Alps.
- Kačák_Event wikiPageWikiLink Category:Middle_Devonian_extinctions.
- Kačák_Event wikiPageWikiLink Conodont.
- Kačák_Event wikiPageWikiLink Cubic_foot.
- Kačák_Event wikiPageWikiLink Devonian.
- Kačák_Event wikiPageWikiLink Eifel.
- Kačák_Event wikiPageWikiLink Euramerica.
- Kačák_Event wikiPageWikiLink Eustatic.
- Kačák_Event wikiPageWikiLink Graz.
- Kačák_Event wikiPageWikiLink Hydrocarbon.
- Kačák_Event wikiPageWikiLink Insolation.
- Kačák_Event wikiPageWikiLink Late_Devonian_extinction.
- Kačák_Event wikiPageWikiLink Limestone.
- Kačák_Event wikiPageWikiLink Marcellus_Formation.
- Kačák_Event wikiPageWikiLink Marine_habitats.
- Kačák_Event wikiPageWikiLink Marine_transgression.
- Kačák_Event wikiPageWikiLink Monsoon.
- Kačák_Event wikiPageWikiLink Montagne_Noire.
- Kačák_Event wikiPageWikiLink Morocco.
- Kačák_Event wikiPageWikiLink New_York.
- Kačák_Event wikiPageWikiLink New_York_State.
- Kačák_Event wikiPageWikiLink Omsk.
- Kačák_Event wikiPageWikiLink Ontario.
- Kačák_Event wikiPageWikiLink Orcadian_Basin.
- Kačák_Event wikiPageWikiLink Rheic_Ocean.
- Kačák_Event wikiPageWikiLink Sea_level.
- Kačák_Event wikiPageWikiLink Shale.
- Kačák_Event wikiPageWikiLink Shale_gas.
- Kačák_Event wikiPageWikiLink Solar_irradiance.
- Kačák_Event wikiPageWikiLink Source_rock.
- Kačák_Event wikiPageWikiLink Tentaculita.
- Kačák_Event wikiPageWikiLink Total_organic_carbon.
- Kačák_Event wikiPageWikiLink Trillion_cubic_feet.
- Kačák_Event wikiPageWikiLink United_States_Department_of_Energy.
- Kačák_Event wikiPageWikiLink United_States_Geological_Survey.
- Kačák_Event wikiPageWikiLink Δ13C.
- Kačák_Event wikiPageWikiLinkText "Kačák Event".
- Kačák_Event hasPhotoCollection Kačák_Event.
- Kačák_Event wikiPageUsesTemplate Template:IPA-cs.
- Kačák_Event wikiPageUsesTemplate Template:Reflist.
- Kačák_Event subject Category:Middle_Devonian_extinctions.
- Kačák_Event comment "The Kačák Event (Czech pronunciation: [kat͡ʃaːk]) or Kačák-otomari Event is a widely recognised bioevent or series of events that occurred close to the end of the Eifelian Age of the Middle Devonian Epoch. It involved a global eustatic rise in sea-level. It was named for the Kačák Member of the Srbsko Formation in Bohemia, where it is represented by a black shale interval within a sequence of limestone.".
- Kačák_Event label "Kačák Event".
- Kačák_Event sameAs m.0j45zph.
- Kačák_Event sameAs Q6381859.
- Kačák_Event sameAs Q6381859.
- Kačák_Event wasDerivedFrom Kačák_Event?oldid=666241038.
- Kačák_Event isPrimaryTopicOf Kačák_Event.