List Of Fossiliferous Stratigraphic Units In Austria
This is a list of fossiliferous stratigraphic units in Austria. __NOTOC__ List of fossiliferous stratigraphic units See also * List of fossiliferous stratigraphic units in Europe ** List of fossiliferous stratigraphic units in Germany ** List of fossiliferous stratigraphic units in Czech Republic ** List of fossiliferous stratigraphic units in Slovakia ** List of fossiliferous stratigraphic units in Hungary ** List of fossiliferous stratigraphic units in Slovenia ** List of fossiliferous stratigraphic units in Italy See also * Lists of fossiliferous stratigraphic units in Europe These lists of fossiliferous stratigraphic units in Europe enumerate the rock layers which preserve the fossilized remains of ancient life in Europe by the modern countries wher ... ** List of fossiliferous stratigraphic units in Switzerland References * {{DEFAULTSORT:Fossiliferous stratigraphic units in Austria * * Austria Austria geography-related lists ...
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Yellow Pog
Yellow is the color between green and orange on the spectrum of light. It is evoked by light with a dominant wavelength of roughly 575585 nm. It is a primary color in subtractive color systems, used in painting or color printing. In the RGB color model, used to create colors on television and computer screens, yellow is a secondary color made by combining red and green at equal intensity. Carotenoids give the characteristic yellow color to autumn leaves, corn, canaries, daffodils, and lemons, as well as egg yolks, buttercups, and bananas. They absorb light energy and protect plants from photo damage in some cases. Sunlight has a slight yellowish hue when the Sun is near the horizon, due to atmospheric scattering of shorter wavelengths (green, blue, and violet). Because it was widely available, yellow ochre pigment was one of the first colors used in art; the Lascaux cave in France has a painting of a yellow horse 17,000 years old. Ochre and orpiment pigments were used t ...
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Trogkofel Formation
The Trogkofel Formation is a geologic formation in Austria, Slovenia and Italy. It preserves fossils dating back to the Sakmarian to Artinskian stages of the Permian period.Trogkofel Formation
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Fossil content

The following fossils were reported from the formation: * '' Alternifenestella subquadratopora'' * '' Alternifenestella tuberculifera'' * ''
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Eibiswald Formation
The Eibiswald Formation is a geologic formation in Austria. It preserves fossils dated to the Langhian age of the Miocene epoch.Eibiswald Formation
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Burgschleinitz Formation
The Burgschleinitz Formation is a geologic formation in Austria. It preserves fossils dated to the Neogene period.Burgschleinitz Formation
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Leitha Formation
The Leitha Limestone is a geologic formation in Austria, Czech Republic, Hungary and Poland. It preserves fossils dated to the Middle to Late Miocene period. Fossil content Various fossils have been found in the formation: * '' Aetobatis irregularis'' * '' Araloselachus cuspidata'' * '' Carcharias (Hypoprion) sp.'' * '' Carcharias (Aprionodon) cf. collata'' * ''Carcharodon hastalis'' * '' Cetotherium priscum'' * '' Coris sigismundi'' * '' Eugaleus latus'' * ''Galeocerdo aduncus'' * ''Galeus aduncus'' * '' Galeus cf. canis'' * '' Halitherium schinzii'' * '' Heterodelphis leiodontus'' * ''Hemipristis serra'' * ''Isurus desorii'' * '' Kentriodon fuchsii'' * Megalodon * '' Metaxytherium medium'' * '' Myliobatis cf. meridionalis'' * '' Notidanus primigenius'' * '' Odontaspis acutissima'' * '' Odontaspis macrota'' * '' Oxyrhina xyphodon'' * '' Pachyacanthus suessii'' * '' Prionodon sp.'' * '' Raja sp.'' * '' Sparus sp.'' * '' Symphodus westneati'' * '' Wainwrightilabrus agassizi'' ...
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Leitha Limestone Formation
The Leitha Limestone is a geologic formation in Austria, Czech Republic, Hungary and Poland. It preserves fossils dated to the Middle to Late Miocene period. Fossil content Various fossils have been found in the formation: * '' Aetobatis irregularis'' * '' Araloselachus cuspidata'' * '' Carcharias (Hypoprion) sp.'' * '' Carcharias (Aprionodon) cf. collata'' * ''Carcharodon hastalis'' * '' Cetotherium priscum'' * '' Coris sigismundi'' * '' Eugaleus latus'' * ''Galeocerdo aduncus'' * ''Galeus aduncus'' * '' Galeus cf. canis'' * '' Halitherium schinzii'' * '' Heterodelphis leiodontus'' * ''Hemipristis serra'' * ''Isurus desorii'' * '' Kentriodon fuchsii'' * Megalodon * '' Metaxytherium medium'' * '' Myliobatis cf. meridionalis'' * '' Notidanus primigenius'' * '' Odontaspis acutissima'' * '' Odontaspis macrota'' * '' Oxyrhina xyphodon'' * '' Pachyacanthus suessii'' * '' Prionodon sp.'' * '' Raja sp.'' * '' Sparus sp.'' * '' Symphodus westneati'' * '' Wainwrightilabrus agassizi'' ...
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Baden Group
Baden (; ) is a historical territory in South Germany, in earlier times on both sides of the Upper Rhine but since the Napoleonic Wars only East of the Rhine. History The margraves of Baden originated from the House of Zähringen. Baden is named after the margraves' residence, in Baden-Baden. Hermann II of Baden first claimed the title of Margrave of Baden in 1112. A united Margraviate of Baden existed from this time until 1535, when it was split into the two Margraviates of Baden-Durlach and Baden-Baden. Following a devastating fire in Baden-Baden in 1689, the capital was moved to Rastatt. The two parts were reunited in 1771 under Margrave Charles Frederick. The restored Margraviate with its capital Karlsruhe was elevated to the status of electorate in 1803. In 1806, the Electorate of Baden, receiving territorial additions, became the Grand Duchy of Baden. The Grand Duchy of Baden was a state within the German Confederation until 1866 and the German Empire until 1918, s ...
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Baden Tegel Formation
Baden (; ) is a historical territory in South Germany, in earlier times on both sides of the Upper Rhine but since the Napoleonic Wars only East of the Rhine. History The margraves of Baden originated from the House of Zähringen. Baden is named after the margraves' residence, in Baden-Baden. Hermann II of Baden first claimed the title of Margrave of Baden in 1112. A united Margraviate of Baden existed from this time until 1535, when it was split into the two Margraviates of Baden-Durlach and Baden-Baden. Following a devastating fire in Baden-Baden in 1689, the capital was moved to Rastatt. The two parts were reunited in 1771 under Margrave Charles Frederick. The restored Margraviate with its capital Karlsruhe was elevated to the status of electorate in 1803. In 1806, the Electorate of Baden, receiving territorial additions, became the Grand Duchy of Baden. The Grand Duchy of Baden was a state within the German Confederation until 1866 and the German Empire until 1918, s ...
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Neogene
The Neogene ( ), informally Upper Tertiary or Late Tertiary, is a geologic period and system that spans 20.45 million years from the end of the Paleogene Period million years ago ( Mya) to the beginning of the present Quaternary Period Mya. The Neogene is sub-divided into two epochs, the earlier Miocene and the later Pliocene. Some geologists assert that the Neogene cannot be clearly delineated from the modern geological period, the Quaternary. The term "Neogene" was coined in 1853 by the Austrian palaeontologist Moritz Hörnes (1815–1868). During this period, mammals and birds continued to evolve into modern forms, while other groups of life remained relatively unchanged. The first humans (''Homo habilis'') appeared in Africa near the end of the period. Some continental movements took place, the most significant event being the connection of North and South America at the Isthmus of Panama, late in the Pliocene. This cut off the warm ocean currents from the Pacific to th ...
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Baden Formation
Baden (; ) is a historical territory in South Germany, in earlier times on both sides of the Upper Rhine but since the Napoleonic Wars only East of the Rhine. History The margraves of Baden originated from the House of Zähringen. Baden is named after the margraves' residence, in Baden-Baden. Herman II, Margrave of Baden, Hermann II of Baden first claimed the title of Margrave of Baden in 1112. A united Margraviate of Baden existed from this time until 1535, when it was split into the two Margraviates of Baden-Durlach and Baden-Baden. Following a devastating fire in Baden-Baden in 1689, the capital was moved to Rastatt. The two parts were reunited in 1771 under Charles Frederick, Grand Duke of Baden, Margrave Charles Frederick. The restored Margraviate with its capital Karlsruhe was elevated to the status of Prince-elector, electorate in 1803. In 1806, the Electorate of Baden, receiving territorial additions, became the Grand Duchy of Baden. The Grand Duchy of Baden was a ...
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Austria
Austria, , bar, Östareich officially the Republic of Austria, is a country in the southern part of Central Europe, lying in the Eastern Alps. It is a federation of nine states, one of which is the capital, Vienna, the most populous city and state. A landlocked country, Austria is bordered by Germany to the northwest, the Czech Republic to the north, Slovakia to the northeast, Hungary to the east, Slovenia and Italy to the south, and Switzerland and Liechtenstein to the west. The country occupies an area of and has a population of 9 million. Austria emerged from the remnants of the Eastern and Hungarian March at the end of the first millennium. Originally a margraviate of Bavaria, it developed into a duchy of the Holy Roman Empire in 1156 and was later made an archduchy in 1453. In the 16th century, Vienna began serving as the empire's administrative capital and Austria thus became the heartland of the Habsburg monarchy. After the dissolution of the H ...
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Stratigraphic Unit
A stratigraphic unit is a volume of rock of identifiable origin and relative age range that is defined by the distinctive and dominant, easily mapped and recognizable petrographic, lithologic or paleontologic features (facies) that characterize it. Units must be ''mappable'' and ''distinct'' from one another, but the contact need not be particularly distinct. For instance, a unit may be defined by terms such as "when the sandstone component exceeds 75%". Lithostratigraphic units Sequences of sedimentary and volcanic rocks are subdivided the basis of their shared or associated lithology. Formally identified lithostratigraphic units are structured in a hierarchy of lithostratigraphic rank, higher rank units generally comprising two or more units of lower rank. Going from smaller to larger in rank, the main lithostratigraphic ranks are Bed, Member, Formation, Group and Supergroup. Formal names of lithostratigraphic units are assigned by geological surveys. Units of formation or hi ...
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