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Santa Juana Formation
Santa Juana Formation a Late Triassic (Carnian stage) sedimentary rock formation near Santa Juana in the lower course of the Biobío River in south-central Chile.Santa Juana Formation at .org Lithologies range from conglomerate , sandstone, |
Geological Formation
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] |
Alluvial
Alluvium (, ) is loose clay, silt, sand, or gravel that has been deposited by running water in a stream bed, on a floodplain, in an alluvial fan or beach, or in similar settings. Alluvium is also sometimes called alluvial deposit. Alluvium is typically geologically young and is not consolidated into solid rock. Sediments deposited underwater, in seas, estuaries, lakes, or ponds, are not described as alluvium. Floodplain alluvium can be highly fertile, and supported some of the earliest human civilizations. Definitions The present consensus is that "alluvium" refers to loose sediments of all types deposited by running water in floodplains or in alluvial fans or related landforms. However, the meaning of the term has varied considerably since it was first defined in the French dictionary of Antoine Furetière, posthumously published in 1690. Drawing upon concepts from Roman law, Furetière defined '' alluvion'' (the French term for alluvium) as new land formed by deposition ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dicroidium
''Dicroidium'' is an extinct genus of fork-leaved seed plants. It is the archetypal genus of the corystosperms, an extinct group of seed plants, often called " seed ferns", assigned to the order Corystospermales or Umkomasiales. Species of ''Dicroidium,'' which grew as large trees, were widely distributed and dominant over Gondwana during the Triassic (). Their fossils are known from South Africa, the Arabian Peninsula, Australia, New Zealand, South America, Madagascar, the Indian subcontinent and Antarctica. Description Within the form genus classification system used in paleobotany, the genus ''Dicroidium'' refers specifically to the leaves. Some authors have suggested dividing ''Dicroidium'' up into several genera, including ''Dicroidiopsis, Diplasiophyllum, Zuberia'', ''Xylopteris'', ''Johnstonia'' and ''Tetraptilon,'' but this is rejected by other authors. The leaves of ''Dicroidium'' bifurcate (fork) at their base, which is characteristic of all species. The leaves are h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cladophlebis
''Cladophlebis'' is an extinct form genus of fern, which has been reported from the Permian to the end of the Cretaceous and from all continents of the world. Description Some pinnules have smooth edges and some have serrated edges. The midrib is distinct and the lateral veins are dichotomous (two branches) to the end. This fern had rizoma. used to refer to Paleozoic and Mesozoic fern leaves that have "fern fronds with pinnules that are attached to the rachis, and have a median vein that runs to the apex of the pinnule, and veins from that are curved and dichotomise".''Cladophlebis'' at Fossilworks
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Baiera
''Baiera'' is a genus of prehistoric gymnosperms in the order Ginkgoales. It is one of the oldest fossil foliage types of Ginkgoales, and is related to the genera ''Ginkgo'' and ''Ginkgoites''. Fossils of ''Baiera'' are found worldwide, and have been known from the Permian to the Cretaceous. Description ''Baiera'' species are characterized by fan-shaped leaves,Pott, Christian & Burgh, J. & van Konijnenburg-van Cittert, Johanna. (2016). New Ginkgophytes from the Upper Triassic–Lower Cretaceous of Spitsbergen and Edgeøya (Svalbard, Arctic Norway): The History of Ginkgoales on Svalbard. International Journal of Plant Sciences. 177. 175-197. 10.1086/684194. are deeply lobed into four segments, deeply incised into slender segments, and are distinguished from '' Sphenobaiera'' by a petiole. ''B. africana'' is characterized by its symmetrical and triangular leaves. Classification Karl Friedrich Wilhelm Braun first introduced the name ''Baiera'' in 1843 to refer to fossils in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Asterotheca
''Asterotheca'' is a genus of seedless, spore, spore-bearing, Vascular plant, vascularized ferns dating from the Carboniferous of the Paleozoic to the Triassic of the Mesozoic. Description ''Asterotheca sp.'' is a vascularized, seedless fern that reproduces via spores that require the presence of water. This genus of fern lived from the Carboniferous to the Triassic and is an ancestor to all modern seed plants. The leaves of ''Asterotheca'' (and all ferns) are called fronds. Fossilized specimens show large, morphologically complex structures that consist of leaf segments called Pinnation, pinnae. Each pinna consists of four to eight sporangia. ''Asterotheca'' fronds are Pinnation, unipinnate because there is only a single row of pinnae on each side of the rachis, or main central stem. ''Asterotheca cyathea'' displays open dichotomous branching, dichotomous unipinnate segments, each with four to five eusporangia. Synonyms In the field of paleobotany, different parts of plant ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gondwana
Gondwana ( ; ) was a large landmass, sometimes referred to as a supercontinent. The remnants of Gondwana make up around two-thirds of today's continental area, including South America, Africa, Antarctica, Australia (continent), Australia, Zealandia, Arabian Peninsula, Arabia, and the Indian subcontinent. Gondwana was formed by the Accretion (geology), accretion of several cratons (large stable blocks of the Earth's crust), beginning with the East African Orogeny, the collision of India and Geography of Madagascar, Madagascar with East Africa, and culminating in with the overlapping Brasiliano orogeny, Brasiliano and Kuunga orogeny, Kuunga orogenies, the collision of South America with Africa, and the addition of Australia and Antarctica, respectively. Eventually, Gondwana became the largest piece of continental crust of the Paleozoic Era, covering an area of some , about one-fifth of the Earth's surface. It fused with Laurasia during the Carboniferous to form Pan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rift
In geology, a rift is a linear zone where the lithosphere is being pulled apart and is an example of extensional tectonics. Typical rift features are a central linear downfaulted depression, called a graben, or more commonly a half-graben with normal faulting and rift-flank uplifts mainly on one side. Where rifts remain above sea level they form a rift valley, which may be filled by water forming a rift lake. The axis of the rift area may contain volcanic rocks, and active volcanism is a part of many, but not all, active rift systems. Major rifts occur along the central axis of most mid-ocean ridges, where new oceanic crust and lithosphere is created along a divergent boundary between two tectonic plates. ''Failed rifts'' are the result of continental rifting that failed to continue to the point of break-up. Typically the transition from rifting to spreading develops at a triple junction where three converging rifts meet over a hotspot. Two of these evolve to t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
