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Cylostrobus
''Cylostrobus'' is genus of Lycopsida most like ''Pleuromeia'', but with very compact and round cones. It is known from the Early Triassic of Australia, coincident with a marked greenhouse spike at the end of the Early Triassic. The genus ''Cylostrobus'' was erected for the compact cone only, in the paleobotanical system of form genera, but these small plants are well enough understood that the name ''Cylostrobus sydneyensis'' is used for the whole plant, rather than the old name ''Pleuromeia longicaulis''. Other species of ''Pleuromeia'' have attached cones that are less compact and produce different spores. See also * Evolution of plants The evolution of plants has resulted in a wide range of complexity, from the earliest algal mats, through multicellular marine and freshwater green algae, terrestrial bryophytes, lycopods and ferns, to the complex gymnosperms and angiosperms (fl ... References Prehistoric lycophytes Triassic plants Prehistoric lycophyte g ...
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Cylostrobus Indicus
''Cylostrobus'' is genus of Lycopsida most like ''Pleuromeia'', but with very compact and round cones. It is known from the Early Triassic of Australia, coincident with a marked greenhouse spike at the end of the Early Triassic The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period .... The genus ''Cylostrobus'' was erected for the compact cone only, in the paleobotanical system of form genera, but these small plants are well enough understood that the name ''Cylostrobus sydneyensis'' is used for the whole plant, rather than the old name ''Pleuromeia longicaulis''. Other species of ''Pleuromeia'' have attached cones that are less compact and produce different spores. See also * Evolution of plants References Prehistoric lycophytes Triassic plants Prehistoric lycophyte ...
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Cylostrobus Ornatus
''Cylostrobus'' is genus of Lycopsida most like ''Pleuromeia'', but with very compact and round cones. It is known from the Early Triassic of Australia, coincident with a marked greenhouse spike at the end of the Early Triassic The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period .... The genus ''Cylostrobus'' was erected for the compact cone only, in the paleobotanical system of form genera, but these small plants are well enough understood that the name ''Cylostrobus sydneyensis'' is used for the whole plant, rather than the old name ''Pleuromeia longicaulis''. Other species of ''Pleuromeia'' have attached cones that are less compact and produce different spores. See also * Evolution of plants References Prehistoric lycophytes Triassic plants Prehistoric lycophyte ...
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Cylostrobus Sydneyensis
''Cylostrobus'' is genus of Lycopsida most like ''Pleuromeia'', but with very compact and round cones. It is known from the Early Triassic of Australia, coincident with a marked greenhouse spike at the end of the Early Triassic The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period .... The genus ''Cylostrobus'' was erected for the compact cone only, in the paleobotanical system of form genera, but these small plants are well enough understood that the name ''Cylostrobus sydneyensis'' is used for the whole plant, rather than the old name ''Pleuromeia longicaulis''. Other species of ''Pleuromeia'' have attached cones that are less compact and produce different spores. See also * Evolution of plants References Prehistoric lycophytes Triassic plants Prehistoric lycophyte ...
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Cylostrobus Sydneyensis Apex
''Cylostrobus'' is genus of Lycopsida most like ''Pleuromeia'', but with very compact and round cones. It is known from the Early Triassic of Australia, coincident with a marked greenhouse spike at the end of the Early Triassic The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period .... The genus ''Cylostrobus'' was erected for the compact cone only, in the paleobotanical system of form genera, but these small plants are well enough understood that the name ''Cylostrobus sydneyensis'' is used for the whole plant, rather than the old name ''Pleuromeia longicaulis''. Other species of ''Pleuromeia'' have attached cones that are less compact and produce different spores. See also * Evolution of plants References Prehistoric lycophytes Triassic plants Prehistoric lycophyte ...
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Cylostrobus Sydneyensis Corm
''Cylostrobus'' is genus of Lycopsida most like ''Pleuromeia'', but with very compact and round cones. It is known from the Early Triassic of Australia, coincident with a marked greenhouse spike at the end of the Early Triassic The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period .... The genus ''Cylostrobus'' was erected for the compact cone only, in the paleobotanical system of form genera, but these small plants are well enough understood that the name ''Cylostrobus sydneyensis'' is used for the whole plant, rather than the old name ''Pleuromeia longicaulis''. Other species of ''Pleuromeia'' have attached cones that are less compact and produce different spores. See also * Evolution of plants References Prehistoric lycophytes Triassic plants Prehistoric lycophyte ...
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Species
In biology, a species is the basic unit of classification and a taxonomic rank of an organism, as well as a unit of biodiversity. A species is often defined as the largest group of organisms in which any two individuals of the appropriate sexes or mating types can produce fertile offspring, typically by sexual reproduction. Other ways of defining species include their karyotype, DNA sequence, morphology, behaviour or ecological niche. In addition, paleontologists use the concept of the chronospecies since fossil reproduction cannot be examined. The most recent rigorous estimate for the total number of species of eukaryotes is between 8 and 8.7 million. However, only about 14% of these had been described by 2011. All species (except viruses) are given a two-part name, a "binomial". The first part of a binomial is the genus to which the species belongs. The second part is called the specific name or the specific epithet (in botanical nomenclature, also sometimes i ...
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Pleuromeia Reconstructions
''Pleuromeia'' is an extinct genus of lycophytes. They are related to modern quillworts (''Isoetes''). ''Pleuromeia'' dominated vegetation during the Early Triassic all over Eurasia and elsewhere, in the aftermath of the collapse of floral communities during the Permian–Triassic extinction event, often occurring in monospecific assemblages. Its sedimentary context in monospecific assemblages on immature paleosols, is evidence that it was an opportunistic pioneer plant that grew on mineral soils with little competition. It spread to high latitudes with greenhouse climatic conditions. Conifers reoccurred in the Early Anisian, followed by the cycads and pteridosperms during the Late Anisian. Description ''Pleuromeia'' consisted of a single unbranched stem of variable thickness, which could grow to a maximum of in height. Around the stem were helically arranged leaves. It had a 2-4 lobed bulbous base to which numerous adventive roots are attached. ''Pleuromeia'' produced a sing ...
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Lycopsida
Lycopodiopsida is a class of vascular plants known as lycopods, lycophytes or other terms including the component lyco-. Members of the class are also called clubmosses, firmosses, spikemosses and quillworts. They have dichotomously branching stems bearing simple leaves called microphylls and reproduce by means of spores borne in sporangia on the sides of the stems at the bases of the leaves. Although living species are small, during the Carboniferous, extinct tree-like forms formed huge forests that dominated the landscape and contributed to coal deposits. The nomenclature and classification of plants with microphylls varies substantially among authors. A consensus classification for extant (living) species was produced in 2016 by the Pteridophyte Phylogeny Group (PPG I), which places them all in the class Lycopodiopsida, which includes the classes Isoetopsida and Selaginellopsida used in other systems. (See Table 2.) Alternative classification systems have used ranks fr ...
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Pleuromeia
''Pleuromeia'' is an extinct genus of lycophytes. They are related to modern quillworts (''Isoetes''). ''Pleuromeia'' dominated vegetation during the Early Triassic all over Eurasia and elsewhere, in the aftermath of the collapse of floral communities during the Permian–Triassic extinction event, often occurring in monospecific assemblages. Its sedimentary context in monospecific assemblages on immature paleosols, is evidence that it was an opportunistic pioneer plant that grew on mineral soils with little competition. It spread to high latitudes with greenhouse climatic conditions. Conifers reoccurred in the Early Anisian, followed by the cycads and pteridosperms during the Late Anisian. Description ''Pleuromeia'' consisted of a single unbranched stem of variable thickness, which could grow to a maximum of in height. Around the stem were helically arranged leaves. It had a 2-4 lobed bulbous base to which numerous adventive roots are attached. ''Pleuromeia'' produced a s ...
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Triassic
The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period of the Mesozoic Era. Both the start and end of the period are marked by major extinction events. The Triassic Period is subdivided into three epochs: Early Triassic, Middle Triassic and Late Triassic. The Triassic began in the wake of the Permian–Triassic extinction event, which left the Earth's biosphere impoverished; it was well into the middle of the Triassic before life recovered its former diversity. Three categories of organisms can be distinguished in the Triassic record: survivors from the extinction event, new groups that flourished briefly, and other new groups that went on to dominate the Mesozoic Era. Reptiles, especially archosaurs, were the chief terrestrial vertebrates during this time. A specialized subgroup of archo ...
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Form Genera
Form classification is the classification of organisms based on their morphology, which does not necessarily reflect their biological relationships. Form classification, generally restricted to palaeontology, reflects uncertainty; the goal of science is to move "form taxa" to biological taxa whose affinity is known. Form taxonomy is restricted to fossils that preserve too few characters for a conclusive taxonomic definition or assessment of their biological affinity, but whose study is made easier if a binomial name is available by which to identify them. The term "form classification" is preferred to "form taxonomy"; taxonomy suggests that the classification implies a biological affinity, whereas form classification is about giving a name to a group of morphologically-similar organisms that may not be related. A "parataxon" (not to be confused with parataxonomy), or "sciotaxon" (Gr. "shadow taxon"), is a classification based on incomplete data: for instance, the larval stage o ...
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Evolution Of Plants
The evolution of plants has resulted in a wide range of complexity, from the earliest algal mats, through multicellular marine and freshwater green algae, terrestrial bryophytes, lycopods and ferns, to the complex gymnosperms and angiosperms (flowering plants) of today. While many of the earliest groups continue to thrive, as exemplified by red and green algae in marine environments, more recently derived groups have displaced previously ecologically dominant ones; for example, the ascendance of flowering plants over gymnosperms in terrestrial environments. There is evidence that cyanobacteria and multicellular photosynthetic eukaryotes lived in freshwater communities on land as early as 1 billion years ago, and that communities of complex, multicellular photosynthesizing organisms existed on land in the late Precambrian, around . Evidence of the emergence of embryophyte land plants first occurs in the mid-Ordovician (~), and by the middle of the Devonian (~), many of the featur ...
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