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Tallahatta Formation
The Tallahatta Formation is a geologic formation found on the surface in Alabama, Florida, Georgia, and Mississippi. It is also located in the subsurface of Kentucky. The Tallahatta formation is part of the Claiborne Group and contains four members: the ''Basic City Shale'' in Mississippi, the ''Holy Springs Sand Member'' in Mississippi, the ''Meridian Sand Member'' in Alabama and Mississippi, and the ''Neshoba Sand Member'' in Mississippi. It preserves fossils dating back to the Paleogene period, specifically the Eocene. History As early as 1823, the rocks that would later become the Tallahatta Formation was referred to as "Buhrstone", a type of porous limestone. Other terms used to describe this rock were "Siliceous Claiborne" in Mississippi and the "Choctaw buhrstone" in Alabama. These rocks became known as the Tallahatta Formation in 1898. Originally, the Winona Formation was considered part of the Tallahatta as the Winona Sand Member before it was split off as a separate ...
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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 ...
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Bioturbation
Bioturbation is defined as the reworking of soils and sediments by animals or plants. It includes burrowing, ingestion, and defecation of sediment grains. Bioturbating activities have a profound effect on the environment and are thought to be a primary driver of biodiversity. The formal study of bioturbation began in the 1800s by Charles Darwin experimenting in his garden. The disruption of aquatic sediments and terrestrial soils through bioturbating activities provides significant ecosystem services. These include the alteration of nutrients in aquatic sediment and overlying water, shelter to other species in the form of burrows in terrestrial and water ecosystems, and soil production on land.Shaler, N. S., 1891, The origin and nature of soils, in Powell, J. W., ed., USGS 12th Annual report 1890-1891: Washington, D.C., Government Printing Office, p. 213-45. Bioturbators are deemed ecosystem engineers because they alter resource availability to other species through the physical ch ...
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Paleogene Georgia (U
The Paleogene ( ; also spelled Palaeogene or Palæogene; informally Lower Tertiary or Early Tertiary) is a geologic period and system that spans 43 million years from the end of the Cretaceous Period million years ago (Mya) to the beginning of the Neogene Period Mya. It is the beginning of the Cenozoic Era of the present Phanerozoic Eon. The earlier term Tertiary Period was used to define the span of time now covered by the Paleogene Period and subsequent Neogene Period; despite no longer being recognised as a formal stratigraphic term, 'Tertiary' is still widely found in earth science literature and remains in informal use. Paleogene is often abbreviated "Pg" (but the United States Geological Survey uses the abbreviation PE for the Paleogene on the Survey's geologic maps). During the Paleogene, mammals diversified from relatively small, simple forms into a large group of diverse animals in the wake of the Cretaceous–Paleogene extinction event that ended the preceding Cre ...
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Paleontology In Georgia (U
The location and boundaries of the U.S. state of Georgia Paleontology in Georgia refers to paleontological research occurring within or conducted by people from the U.S. state of Georgia. During the early part of the Paleozoic, Georgia was largely covered by seawater. Although no major Paleozoic discoveries have been uncovered in Georgia, the local fossil record documents a great diversity of ancient life in the state. Inhabitants of Georgia's early Paleozoic sea included corals, stromatolites, and trilobites. During the Carboniferous local sea levels dropped and a vast complex of richly vegetated delta formed in the state. These swampy deltas were home to early tetrapods which left behind footprints that would later fossilize. Little is known of Triassic Georgia and the Jurassic is absent altogether from the state's rock record. During the Cretaceous, however, southern Georgia was covered by a sea that was home to invertebrates and fishes. On land, the tree ''Araucaria'' grew ...
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List Of Fossiliferous Stratigraphic Units In Mississippi
This article contains a list of fossil-bearing stratigraphic units in the state of Mississippi, U.S. Sites See also * Paleontology in Mississippi References * {{DEFAULTSORT:Fossiliferous stratigraphic units in Mississippi Mississippi 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, p ... Stratigraphy of Mississippi Mississippi geography-related lists United States geology-related lists ...
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List Of Fossiliferous Stratigraphic Units In Georgia (U
See also * Paleontology in Georgia (U.S. state) References * {{DEFAULTSORT:Fossiliferous stratigraphic units in Georgia (U.S. state) Georgia 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, p ... Stratigraphy of Georgia (U.S. state) Georgia (U.S. state) geography-related lists United States geology-related lists ...
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Marine Regression
A marine regression is a geological process occurring when areas of submerged seafloor are exposed above the sea level. The opposite event, marine transgression, occurs when flooding from the sea covers previously-exposed land. Evidence of marine regressions and transgressions occurs throughout the fossil record, and the fluctuations are thought to have caused or contributed to several mass extinctions, such as the Permian-Triassic extinction event (250 million years ago) and Cretaceous–Paleogene extinction event (66 Ma). During the Permian-Triassic extinction, the largest extinction event in the Earth's history, the global sea level fell 250 m (820 ft). A major regression could itself cause marine organisms in shallow seas to go extinct, but mass extinctions tend to involve both terrestrial and aquatic species, and it is harder to see how a marine regression could cause widespread extinctions of land animals. Regressions are, therefore, seen as correlates or symptoms of major ...
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Unconformity
An unconformity is a buried erosional or non-depositional surface separating two rock masses or strata of different ages, indicating that sediment deposition was not continuous. In general, the older layer was exposed to erosion for an interval of time before deposition of the younger layer, but the term is used to describe any break in the sedimentary geologic record. The significance of angular unconformity (see below) was shown by James Hutton, who found examples of Hutton's Unconformity at Jedburgh in 1787 and at Siccar Point in 1788. The rocks above an unconformity are younger than the rocks beneath (unless the sequence has been overturned). An unconformity represents time during which no sediments were preserved in a region or were subsequently eroded before the next deposition. The local record for that time interval is missing and geologists must use other clues to discover that part of the geologic history of that area. The interval of geologic time not represented is ...
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Glauconite
Glauconite is an iron potassium phyllosilicate ( mica group) mineral of characteristic green color which is very friable and has very low weathering resistance. It crystallizes with a monoclinic geometry. Its name is derived from the Greek () meaning 'bluish green', referring to the common blue-green color of the mineral; its sheen ( mica glimmer) and blue-green color. Its color ranges from olive green, black green to bluish green, and yellowish on exposed surfaces due to oxidation. In the Mohs scale it has hardness of 2. The relative specific gravity range is 2.4 - 2.95. It is normally found in dark green rounded brittle pellets, and with the dimension of a sand grain size. It can be confused with chlorite (also of green color) or with a clay mineral. Glauconite has the chemical formula . Glauconite particles are one of the main components of greensand, glauconitic siltstone and glauconitic sandstone. Glauconite has been called a marl in an old and broad sense of that word. ...
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Neshoba County, Mississippi
Neshoba County is located in the central part of the U.S. state of Mississippi. As of the 2020 census, the population was 29,087. Its county seat is Philadelphia. It was named after ''Nashoba'', a Choctaw chief. His name means "wolf" in the Choctaw language. The county is known for the Neshoba County Fair and harness horse races. It is home of the Williams Brothers Store, which has been in operation since the early 1900s. In June 1964, civil rights workers James Chaney, Andrew Goodman, and Michael Schwerner were chased down, tortured, and murdered by members of the Ku Klux Klan. They were buried in an earthen dam on private property off of Highway 21; Goodman was still alive. Initially treated as a missing persons case, their disappearance provoked national outrage and contributed significantly to the July enactment of the Civil Rights Act by President Johnson. The Mississippi Band of Choctaw Indians (MBCI), a federally recognized tribe, is based here and has developed ...
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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 Calvert Bluff, Simsboro and Hooper Formations, and in Alabama into the Nanafalia and Hatchetigbee Formations. Other subdivisions are the Lower, Middle and Upper Wilcox Subgroups, and the Carrizo and Indio Formations. Lithologies The group comprises mostly mudstone with secondary sandstone and lignite beds, ironstone concretions, as well as siltstones, conglomerates and limestones. The total thickness is about .Wilcox Group, Texas
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Meridian, Mississippi
Meridian is the List of municipalities in Mississippi, seventh largest city in the U.S. state of Mississippi, with a population of 41,148 at the 2010 United States Census, 2010 census and an estimated population in 2018 of 36,347. It is the county seat of Lauderdale County, Mississippi, Lauderdale County and the principal city of the Meridian, Mississippi Micropolitan Statistical Area. Along major highways, the city is east of Jackson, Mississippi; southwest of Birmingham, Alabama; northeast of New Orleans, Louisiana; and southeast of Memphis, Tennessee. Established in 1860, at the junction of the Mobile and Ohio Railroad and Southern Railway (U.S.), Southern Railway of Mississippi, Meridian built an economy based on the railways and goods transported on them, and it became a strategic trading center. During the American Civil War, General William Tecumseh Sherman burned much of the city to the ground in the Battle of Meridian (February 1864). Rebuilt after the war, the city e ...
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