Having no exact correspondcnt in thc stratigraphical columns, nor in thc ficld, this biozonc practically has no sense. The type section of the Recea Member nom. Doman; Plcşa;

HUZA Dr. Dacia Oradea. Thc lithostratigraphical units in that thc lov. Sincmurian Eastcrn Carpathians; thc Svţa Formation nom. Hettangian pro parteOgaşul Vod,înischi Sandstone Mcmber nom.

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Hcttangian pro parte Sinemurian. Ogaşul Murguccva Limestonc Mcmbcr nom.

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Plicnsbachian - Toarcian pro parteMehadia Formation nom. Hettangian pro parteValea Marc Clay Membcr nom. Toarcianthe Cioclovina Formation nom. Hettangian pro parteDealul Ţitla Sandstone Member nom. Hettangian pro parte - Sinemurianthe Codlea-Vulcan Formation nom.

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Hettangian - Pliensbachian with Codlea Conglomerate Member nom. Hettangian pro parteVulcan Sandstone Member nom. Hettangian pro parte - SinemurianHolbav Clay Member nom. Pliensbachian in Southern Carpathians; the Şuncuiuş Formation nom nov.

Hettangian - lower Sinemurian with Dumbrava Member nom. Hettangian pro parteRecea Member nom. Hettangian pro parte - lower Sinemurian in Apuseni Mountains.

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I\HIZEllL TARII CRIŞllRILOR NYMPHAEA FOLIA NATURAE BIHARIAE XXVII

Numcrous scientists, like Kudernatsch, HantkenBockhRamerRoth von Telcgd, a,BeneHalavatsNăstăseanuRăileanu et al. Up to the prcsent, authors defined very few lower Jurassic lithostratigraphical units from Roman ia.

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Moreover, only those from thc papers of Bucur, referring to the Reşiţa - Moldova Nouă zone, bear valid names.

Howevcr, wc should define and name all lithostratigraphical units, and this must be in concordance with the stratigraphical rules and recommendations HedbergVan EysingaHarland el al. This is the first scope of the present paper. The second one is the elaboration of a synthesis of all the lower Jurassic macroflora-bearing lithostratigraphic units from Romania. They contain severa!

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Typc section: Cristian Figs. Definition: Grcy sandstoncs with grcy-whitish clay lcns, coals. Typc section: Cristian - Valea Schnccbrich Figs. Ddinition: Succession of conglomerates, sandstones, coal-bearing clays, coals, coal- sandstones. Upper limit: above of the last sandstone bank with Gryphaea cymbium; discordance or erosion limit. Type section: Sviniţa Figs.

Age: Hettangian pro parte - Toarcian pro parte.

Localion or the type section of the Cristian Formation nom. The type section of the Cristian Formation nom. Based on thc scction of Jekelius Stratigraphical column of the m acrofl ora locality Cristian. Based on th e data publi shed by SturToul aJekelius 19 15,Krasser 1SemakaMutihac Dcfinition: White-violet or ycllowish gross quartz-conglomeratcs, m massive banks.

Lithofacial variations: conglomcratcs and sandstoncs, sandstonc-conglomcratcs, conglomerates with clay intcrcalations, microconglomcratcs and conglomcrates, conglomcratc-sandstoncs. Type section: Sviniţa - Culmea Şarlova Figs.

HUZA Dr. Dacia Oradea. Thc lithostratigraphical units in that thc lov.

Definition: White or brownish siliceous sandstones, schistose-argillaceous violet sandstones with coal intercalations, grey-black mica-sandstones. Lithofacial variations: argillaccous sandstones, limestone-sandstones, clays, coal-bearing clays and sandstoncs, argillaceous schists and coals, limestone-schists, sandy-argillaceous schists with limestone intcrcalations, marlargillaceous siltstones, marls.

Type section: Sviniţa - Ogaşul Vodânischi Figs. Definition: Violet-grey-black limestone-sandstones with diaclases filled with calcite, green-bluish sandstones. Lithofacial variations: yellow-grey sandstones with clay and mari intercalations, mari- sandstones and quartzite-sandstones, limestone-sandstones, marlargillaceous siltstones, sandy-argillaceous schists, black argillaceous schists with coal lens, sandy clays, clays, marls and siltstone-clays, marls and limestones, marl-limestones, marls and organogene limestones, sandstone-limestones, limestones.

Location of the type section of the Sviniţa Formation nom. Black arrow indicates the location of thc typc section.

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The type section of the Sviniţa Formation nom. Based on the section of Răileanuwith modifications regarding the dating of the lower Jurassic units.

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Based on the data publi shed by R: ă il ea nu, R ăi l eanu, Patrulius et al. Dcfinition: Succcssion of conglomcrates, conglomcratcs and sandstoncs, clays, sandstoncs. Lowcr limit: ahovc thc crystalline fundament, or thc Permian breccias and conglomcratcs. Uppcr limit: below the first black sandstone-clay bank with G1Jphaca cymbium. Typc section: Mchadia Figs. Lower limit: above the crystallinc fundament, or thc Permian breccias and conglomeratcs.

Type section: Mehadia - Valea Ciumoasa Figs. Definition: Clays and sandstones. Upper limit: below the first black sandstone-clay bank with Gryphaea cymbium. Type section: Mehadia - Valea Mare Figs.

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Age: Png dating lae pro parte - Sinemurian. Location of the type section of the Mehadia Formation nom. Black arrow indicatcs thc location of the type section. The type section of the Mehadia Formation nom. Representcd scction: Mehadia - Valea Marc Figs.

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Age of reprcscnted section bcaring fossil plants: Plicnsbachian pro parte Cerna - Jiu zone The Schela Formation Mrazec se11s11 Preda Lithology of represented section: quartz-mctapsephites, coals, graphitoid metapellitcs, pirophilitic mctapellitcs, quartz-fcldspar- and quartz-metapsammites. Age of represented doar nottingham dating bearing fossil plants: Hettangian - Sinemunan Reşiţa - Moldova Nouă zone The Steierdorf Formation Bucur Lithology of represented sections: gross quartz-conglomeratcs, conglomerates and sandstones, microconglomerates, conglomerate-sandstoncs, microconglomcrate-sandstones, gross sandstones and microconglomeratcs, mica- and quartz-sandstones, argillaceous sandstones, clays and refractory clays, coalbearing clays, coals, black bituminous argillites with spherosiderite concretions and thin coal intcrcalations.

Bascd on thc data publishcd by ManolescuSemakaZbcrca ct al.

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Biţoianu in Petrescu ct al. Daman Figs. A~c of reprcsented scctions bcaring fossil plants: Hcttangian ~ bachian t Represented sections: Anina, Daman Figs. Age of represented sections bearing fossil plants: Hettangian pro parte The Valea Terezia Sandstone Member Bucur Lithology of represented sections: sandstones, subordinate microconglomerates, conglomerate-sandstones, microconglomerate-sandstones, gross sandstones and microconglomerates, mica- and quartz-sandstoncs, argillaceous sandstones, clays and refractory clays, coal-bearing clays, coals.

Upper limit in rcpresented scctions: bclow thc first black bituminous argillite packet of the Uteriş Member. Reprcsented sections: Anina, Do man Figs. Age of represented sections bearing fossil plants: Pliensbachian. Based on the data published by Etting hausen l a, l 52bAndrae lFoetterle lSturH antken l 78StaubRoth v.

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Telegd png dating lae,b,H a l avătschrcter l 9 l 2PappKrasser 19 16, 1ThomasLangerBarbu 1 95 1 Răileanu et al. Location of the type section of the Va lea odo!

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Mari Member nom. Geologica ketch based png dating lae. Black arrow indicates th e location of the type section. The type section of th e Va lea Sodol Mari Member nom.

B ased on the section of Bene 1 and the comments of Halavâts The Va lea Sodol Mari M ember nom. Toa rcian corresponds to the term no.

Stratigraphical column of the macrofl ora locali ty Doman. B png dating lae on the data published by H antkenBene 1H a l avă t sStaubMateescuR ăi l ea nu et a l.

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Rcprcscntcd sections: Anina, Doman Figs. Dcfinition: Marls and limcstonc-marls with sandstonc-marl intcrcalations. Typc scction: Doman - Valea Sodol Figs. Dcfinition: Succcssion of conglomerates in massivc banks, conglomerates and ferruginous sandstones, sandstoncs with coal rcmains, sandstones and clays. Type section: Cioclovina Figs.

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Dcfinition: Conglomerates in massive banks, subordinate conglomerates and fcm1ginous sandstones. Lower limit: above thc crystalline fundament.

Location of t he typ ioclovina Formation nom. Black arrow indicates the location of th e type section.