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- W106305137 abstract "Magyarorszagon pliensbachi es toarci kepződmenyek a Bakony, Gerecse es Mecsek hegysegek retegsoraiban tanulmanyozhatok. A Bakonyban legreszletesebben a Bakonycsernyei Tűzkoves arok ostracoda faunaja kerult vizsgalatra. A pliensbachi es toarci fauna karakterisztikusan elterő, legfeltűnőbb a Healdidae csalad kepviselőinek hianya a toarci emeletben. E valtozas - Nyugat-Europatol elterően - mar a tenuicostatum zonaban is eszlelhető, ez az erősen kimelyult medence kovetkezmenye. Ezert hianyoznak a Cytheridae-k is. A Gerecse hegyseg ostracoda faunaja nagyon hasonlo a Bakony hegysegehez. A Healdidae-k es Cytheridae-k eltűnnek a toarciban a medence melyulese kovetkezteben. Cytheridae-k alarendelten meg előfordulnak. A Mecsek hegysegben a melyszublitoralis Healdidae egyuttest a tenuicostatum zona felett sekely szublitoralis Cytheridae-k dominanciajaval jellemezhető egyuttes valtja fel. Ez a vizmedence melysegenek csokkenesere utal. | The Pliensbachian and Toarcian sections in the Bakony, Gerecse and Mecsek Mountains were investigated. In the Bakony Mountains the Pliensbachian and Toarcian ostracod faunas show significant differences which are usually interpreted as related to the Lower Toarcian anoxic event. Main change is the disappearance of the Healdidae in the Lower Toarcian. The ostracod fauna of the Gerecse is very similar to that in the Bakony, here Healdidae and Cytheridae disappear in the Toarcian also, do to the deepening of the basin. In the Mecsek the deep sublittoral Healdidae assemblage is replaced by an assemblage dominated by shallow sublittoral Cytheridae above Tenuicostatum Zone, indicating the waterdepth changing to shallower." @default.
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- W106305137 date "2009-01-01" @default.
- W106305137 modified "2023-10-18" @default.
- W106305137 title "Júra faunák visszatérése a toarci anoxikus sokk után (magyarországi vizsgálatok) = Return of the Jurassic fauna after the Toarcian anoxic shock, studied in the sections of Hungary" @default.
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