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List Of Fossiliferous Stratigraphic Units In Louisiana
This article contains a list of fossil-bearing stratigraphic units in the state of Louisiana, U.S. Sites See also * Paleontology in Louisiana References * {{DEFAULTSORT:Fossiliferous stratigraphic units in Louisiana Louisiana Louisiana , group=pronunciation (French: ''La Louisiane'') is a state in the Deep South and South Central regions of the United States. It is the 20th-smallest by area and the 25th most populous of the 50 U.S. states. Louisiana is borde ... Stratigraphic units Stratigraphy of Louisiana Louisiana geography-related lists United States geology-related lists . ...
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Stratigraphic Units
A stratigraphic unit is a volume of Rock (geology), rock of identifiable origin and relative age range that is defined by the distinctive and dominant, easily mapped and recognizable petrology, petrographic, lithology, lithologic or paleontology, 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 rock, 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 lithostratigraph ...
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Logansport Formation
The Logansport Formation is a geologic formation in Louisiana. It preserves fossils dating back to the Paleogene period. See also * List of fossiliferous stratigraphic units in Louisiana * Paleontology in Louisiana Paleontology in Louisiana refers to paleontological research occurring within or conducted by people from the U.S. state of Louisiana. Outcrops of fossil-bearing sediments and sedimentary rocks within Louisiana are quite rare. In part, this is beca ... References * Paleogene Louisiana {{Louisiana-geologic-formation-stub ...
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Louisiana Geography-related Lists
Louisiana , group=pronunciation (French: ''La Louisiane'') is a state in the Deep South and South Central regions of the United States. It is the 20th-smallest by area and the 25th most populous of the 50 U.S. states. Louisiana is bordered by the state of Texas to the west, Arkansas to the north, Mississippi to the east, and the Gulf of Mexico to the south. A large part of its eastern boundary is demarcated by the Mississippi River. Louisiana is the only U.S. state with political subdivisions termed parishes, which are equivalent to counties, making it one of only two U.S. states not subdivided into counties (the other being Alaska and its boroughs). The state's capital is Baton Rouge, and its largest city is New Orleans, with a population of roughly 383,000 people. Some Louisiana urban environments have a multicultural, multilingual heritage, being so strongly influenced by a mixture of 18th century Louisiana French, Dominican Creole, Spanish, French Canadian, Acadian, ...
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Stratigraphy Of Louisiana
Stratigraphy is a branch of geology concerned with the study of rock layers (strata) and layering (stratification). It is primarily used in the study of sedimentary and layered volcanic rocks. Stratigraphy has three related subfields: lithostratigraphy (lithologic stratigraphy), biostratigraphy (biologic stratigraphy), and chronostratigraphy (stratigraphy by age). Historical development Catholic priest Nicholas Steno established the theoretical basis for stratigraphy when he introduced the law of superposition, the principle of original horizontality and the principle of lateral continuity in a 1669 work on the fossilization of organic remains in layers of sediment. The first practical large-scale application of stratigraphy was by William Smith in the 1790s and early 19th century. Known as the "Father of English geology", Smith recognized the significance of strata or rock layering and the importance of fossil markers for correlating strata; he created the first geologic ...
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Fossiliferous Stratigraphic Units Of The United States
A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved in amber, hair, petrified wood and DNA remnants. The totality of fossils is known as the ''fossil record''. Paleontology is the study of fossils: their age, method of formation, and evolutionary significance. Specimens are usually considered to be fossils if they are over 10,000 years old. The oldest fossils are around 3.48 billion years old to 4.1 billion years old. Early edition, published online before print. The observation in the 19th century that certain fossils were associated with certain rock strata led to the recognition of a geological timescale and the relative ages of different fossils. The development of radiometric dating techniques in the early 20th century allowed scientists to quantitatively measure the absolute ...
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Paleontology In Louisiana
Paleontology in Louisiana refers to paleontological research occurring within or conducted by people from the U.S. state of Louisiana. Outcrops of fossil-bearing sediments and sedimentary rocks within Louisiana are quite rare. In part, this is because Louisiana’s semi-humid climate results in the rapid weathering and erosion of any exposures and the growth of thick vegetation that conceal any fossil-bearing strata. In addition, Holocene alluvial sediments left behind by rivers like the Mississippi, Red, and Ouachita, as well as marsh deposits, cover about 55% of Louisiana and deeply bury local fossiliferous strata. Nevertheless, paleontologists and geologists have succeeded in reconstructing much of the state's prehistory. Around the beginning of the Cambrian, Louisiana was part of a landmass called Rodinia. This supercontinent began to break up into the northern Laurentia and southern Gondwana. This division split off local rock which would become part of the southern supercontin ...
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Wilcox Formation
The Wilcox Formation is a geologic formation in Tennessee. It preserves fossils dating back to the Paleogene period. The first hydrocarbon discover in the formation occurred in 1928, onshore Texas. Subsequent field discoveries included the Seven Sisters Field, the Fandando Field , and in 1940 the Sheridan Field in Colorado County, Texas. Notable offshore discoveries within the formation include BAHA No. 2, and in 2004, the giant Jack Field. See also * List of fossiliferous stratigraphic units in Tennessee * Paleontology in Tennessee * Jack 2 * Wilcox Group The Wilcox Group is an important geologic group in the Gulf of Mexico Basin and surrounding onshore areas from Mexico and Texas to Louisiana and Alabama. The group ranges in age from Paleocene to Eocene and is in Texas subdivided into the Calve ... References * Paleogene Louisiana Paleogene geology of Tennessee {{Tennessee-geologic-formation-stub ...
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Weches Formation
The Weches Formation is a greensand, slay, and shale geologic formation in Louisiana and Eastern Texas. It preserves fossils dating back to the Paleogene period, specifically the Eocene. Description The Weches Formation is a fossiliferous glauconite rich sand that graduates into a clay. It is considered one of the principal iron bearing beds in Eastern Texas, and is mined for sand in gravel in parts of Texas where exposed. The Weches Formation was originally called the Weches Greensand, and was considered a member of the Mount Selman Formation before being raised to formation status. See also * List of fossiliferous stratigraphic units in Louisiana * List of fossiliferous stratigraphic units in Texas * Paleontology in Louisiana Paleontology in Louisiana refers to paleontological research occurring within or conducted by people from the U.S. state of Louisiana. Outcrops of fossil-bearing sediments and sedimentary rocks within Louisiana are quite rare. In part, this is beca . ...
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Mosley Hill Formation
The Mosley Hill Formation is a geologic formation in Louisiana. It preserves fossils dating back to the Paleogene period. See also * List of fossiliferous stratigraphic units in Louisiana * Paleontology in Louisiana Paleontology in Louisiana refers to paleontological research occurring within or conducted by people from the U.S. state of Louisiana. Outcrops of fossil-bearing sediments and sedimentary rocks within Louisiana are quite rare. In part, this is beca ... References * Geologic formations of Louisiana Paleogene Louisiana {{Louisiana-geologic-formation-stub ...
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Byram Marl
The Byram Marl is a geologic formation in Mississippi. It preserves fossils dating back to the Paleogene period. See also * List of fossiliferous stratigraphic units in Mississippi * Paleontology in Mississippi The location of the state of Mississippi Paleontology in Mississippi refers to paleontological research occurring within or conducted by people from the U.S. state of Mississippi. The oldest rocks in Mississippi date back to the Late Devonian. ... References * Paleogene Mississippi Paleogene Louisiana {{Mississippi-geologic-formation-stub ...
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Vicksburg Group
The Vicksburg Group is a geologic group in Georgia. It preserves fossils dating back to the Paleogene period. See also * List of fossiliferous stratigraphic units in Georgia (U.S. state) See also * Paleontology in Georgia (U.S. state) References * {{DEFAULTSORT:Fossiliferous stratigraphic units in Georgia (U.S. state) Fossiliferous stratigraphic units of the United States, Georgia Paleontology in Georgia (U.S. state), ... * Paleontology in Georgia (U.S. state) References * Geologic groups of Georgia (U.S. state) {{US-geologic-formation-stub ...
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Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of the entire Phanerozoic. The name is derived from the Latin ''creta'', "chalk", which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation ''Kreide''. The Cretaceous was a period with a relatively warm climate, resulting in high eustatic sea levels that created numerous shallow inland seas. These oceans and seas were populated with now- extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was ice free, and forests extended to the poles. During this time, new groups of mammals and birds appeared. During the Early Cretaceous, flowering plants appeared and began to rapidly diversify, becoming the dominant group of plants across the Earth b ...
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