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Dovžan Gorge Formation
The Dovžan Gorge Formation ()Novak, 2007 is a geologic formation in Slovenia. It preserves fossils dating back to the Permian period. The formation is named after the Dovžan Gorge The Dovžan Gorge ( or ''Dolžanova soteska'') is a gorge in Slovenia that was carved by the Tržič Bistrica River. The river flows through unique waterfalls over large rounded blocks of white quartz conglomerate. These large blocks tumbled into .... Fossil content The following fossils have been reported from the formation: ;Trilobites * '' Ditomopyge aff. kumpani'' * '' Paraphillipsia aff. taurica'' * '' Pseudophillipsia (Carniphillipsia) aff. caruancensis'' * '' Neoproetus sp.'' * '' Pseudophillipsia sp.'' ;Brachiopods * '' Capillomesolobus heritschi'' References Bibliography * * {{DEFAULTSORT:Dovzan Gorge Formation Geologic formations of Slovenia Permian System of Europe Asselian Limestone formations Reef deposits Permian southern paleotropical deposits Paleontology in Sloven ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Formation (stratigraphy)
A geological formation, or simply formation, is a body of rock having a consistent set of physical characteristics (lithology) that distinguishes it from adjacent bodies of rock, and which occupies a particular position in the layers of rock exposed in a geographical region (the stratigraphic column). It is the fundamental unit of lithostratigraphy, the study of strata or rock layers. A formation must be large enough that it can be mapped at the surface or traced in the subsurface. Formations are otherwise not defined by the thickness (geology), thickness of their rock strata, which can vary widely. They are usually, but not universally, tabular in form. They may consist of a single lithology (rock type), or of alternating beds of two or more lithologies, or even a heterogeneous mixture of lithologies, so long as this distinguishes them from adjacent bodies of rock. The concept of a geologic formation goes back to the beginnings of modern scientific geology. The term was used by ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pseudophillipsia
''Pseudophillipsia'' is a genus of trilobite, notable for being one of the last members of the group before the extinction at the end of the Permian. It first appeared during the Pennsylvanian Pennsylvanian may refer to: * A person or thing from Pennsylvania * Pennsylvanian (geology) The Pennsylvanian ( , also known as Upper Carboniferous or Late Carboniferous) is, on the International Commission on Stratigraphy, ICS geologic timesc ... or Late Carboniferous. There are several species and this genus has a range spanning Eurasia. References Phillipsiidae Proetida genera {{Librostoma-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reef Deposits
A reef is a ridge or shoal of rock, coral, or similar relatively stable material lying beneath the surface of a natural body of water. Many reefs result from natural, abiotic (non-living) processes such as deposition of sand or wave erosion planning down rock outcrops. However, reefs such as the coral reefs of tropical waters are formed by biotic (living) processes, dominated by corals and coralline algae. Artificial reefs, such as shipwrecks and other man-made underwater structures, may occur intentionally or as the result of an accident. These are sometimes designed to increase the physical complexity of featureless sand bottoms to attract a more diverse range of organisms. They provide shelter to various aquatic animals which help prevent extinction. Another reason reefs are put in place is for aquaculture, and fish farmers who are looking to improve their businesses sometimes invest in them. Reefs are often quite near to the surface, but not all definitions require this ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone Formations
Limestone is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different Polymorphism (materials science), crystal forms of calcium carbonate . Limestone forms when these minerals Precipitation (chemistry), precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly Dolomite (rock), dolomite, a closely related rock, which contains a high percentage of the mineral Dolomite (mineral), dolomite, . ''Magnesian li ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Permian System Of Europe
The Permian ( ) is a geologic period and stratigraphic system which spans 47 million years, from the end of the Carboniferous Period million years ago (Mya), to the beginning of the Triassic Period 251.902 Mya. It is the sixth and last period of the Paleozoic Era; the following Triassic Period belongs to the Mesozoic Era. The concept of the Permian was introduced in 1841 by geologist Sir Roderick Murchison, who named it after the region of Perm in Russia. The Permian witnessed the diversification of the two groups of amniotes, the synapsids and the sauropsids (reptiles). The world at the time was dominated by the supercontinent Pangaea, which had formed due to the collision of Euramerica and Gondwana during the Carboniferous. Pangaea was surrounded by the superocean Panthalassa. The Carboniferous rainforest collapse left behind vast regions of desert within the continental interior. Amniotes, which could better cope with these drier conditions, rose to dominance in place of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geologic Formations Of Slovenia
Geology (). is a branch of natural science concerned with the Earth and other astronomical objects, the rocks of which they are composed, and the processes by which they change over time. Modern geology significantly overlaps all other Earth sciences, including hydrology. It is integrated with Earth system science and planetary science. Geology describes the structure of the Earth on and beneath its surface and the processes that have shaped that structure. Geologists study the mineralogical composition of rocks in order to get insight into their history of formation. Geology determines the relative ages of rocks found at a given location; geochemistry (a branch of geology) determines their absolute ages. By combining various petrological, crystallographic, and paleontological tools, geologists are able to chronicle the geological history of the Earth as a whole. One aspect is to demonstrate the age of the Earth. Geology provides evidence for plate tectonics, the evolutionary ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Senckenbergiana Lethaea
This is a list of academic journals An academic journal (or scholarly journal or scientific journal) is a periodical publication in which scholarship relating to a particular academic discipline is published. They serve as permanent and transparent forums for the dissemination, scr ..., monographic series, and other serials published by E. Schweizerbart. A B C D E F G H I J K L M N P Q R S T U V W Z {{columns-list, colwidth=30em, *''Zeitschrift der Deutschen Gesellschaft für Geowissenschaften'' *''Zeitschrift für Angewandte Geologie'' *'' Zeitschrift für Geomorphologie'' **'' Zeitschrift für Geomorphologie, Supplement Volumes'' **'' Zeitschrift für Geomorphologie, Supplementary Issues'' *''Zentralblatt für Geologie und Paläontologie'' **''Zentralblatt für Geologie und Paläontologie, Teil I'' **''Zentralblatt für Geologie und Paläontologie, Teil II'' *''Ziegler Catalogue of Conodonts'' *''Zoologica'' External linksSeri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paraphillipsia
''Paraphillipsia'' is a genus of proetid trilobite in the family Phillipsiidae. It is notable for being one of the last trilobites to go extinct during the Permian–Triassic extinction event The Permian–Triassic extinction event (also known as the P–T extinction event, the Late Permian extinction event, the Latest Permian extinction event, the End-Permian extinction event, and colloquially as the Great Dying,) was an extinction .... Species *''P. aglypta'' *''P. inflata'' *''P. karpinskyi'' *''P. levigata'' *''P. midlemissi'' *''P. pahara'' *''P. taurica'' (synonymous with ''P. kussicum'', ''P. anfensis'', and ''P. netschaewi'') *''P. vnweberi'' References {{Trilobite-stub Proetida genera Permian trilobites Permian–Triassic extinction event Cummingellinae ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Asselian
In the geologic timescale, the Asselian is the earliest geochronologic age or lowermost chronostratigraphic stage of the Permian. It is a subdivision of the Cisuralian Epoch or Series. The Asselian lasted between and million years ago (Ma). It was preceded by the Gzhelian (the latest or uppermost subdivision in the Carboniferous) and followed by the Sakmarian. Stratigraphy The Asselian Stage was introduced into scientific literature in 1954, when the Russian stratigrapher V.E. Ruzhenchev split it off from the Artinskian. At the time, the Artinskian still encompassed most of the lower Permian – its current definitions are more restricted. The Asselian is named after the Assel River in the southern Ural Mountains of Kazakhstan and Bashkortostan. The base of the Asselian Stage is equivalent to the base of the Cisuralian Series and the Permian System. It is defined as the point in the stratigraphic record where fossils of the conodont '' Streptognathodus isolatus'' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
