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Calamitaceae
Calamitaceae is an extinct Family (biology), family of Equisetales, equisetalean plants related to the modern horsetails, known from the Carboniferous and Permian periods. Some members of this family like ''Arthropitys'' attained tree-like stature, with heights over , with extensive underground rhizomes. They were largely found in wetland environments. Proposed genera and species of Calamitaceae * ''Annularia''. ** ''A. stellata''. * ''Arthropitys''. * ''Asterophyllites'' (or incorrectly ''Asterophyllum''). * ''Astromyelon''. * ''Calamites''. ** ''C. carinatus''. ** ''C. suckowi''. ** ''C. undulatus''. * ''Calamocarpon''. * ''Calamostachys''. ** ''C. binneyana''. * ''Cingularia''. * ''Mazostachys''. * ''Paleostachya''. References External links Link to information and pictures Equisetales Carboniferous plants Prehistoric plant families Fern families Carboniferous first appearances Carboniferous extinctions {{carboniferous-plant-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Calamites
''Calamites'' is a genus of Extinction, extinct arborescent (tree-like) horsetails to which the modern horsetails (genus ''Equisetum'') are closely related. Unlike their Herbaceous plant, herbaceous modern cousins, these plants were medium-sized trees, growing to heights of . They were components of the understories of coal swamps of the Carboniferous, Carboniferous Period (around ). Taxonomy A number of organ taxon, organ taxa have been identified as part of a united organism, which has inherited the name ''Calamites'' in popular culture. ''Calamites'' correctly refers only to casts of the stem of Carboniferous/Permian sphenophytes, and as such is a form genus of little taxonomic value. There are two forms of casts, which can give mistaken impressions of the organisms. The most common is an internal cast of the hollow (or pith-filled) void in the centre of the trunk. This can cause some confusion: firstly, a fossil was probably surrounded with 4-5 times its width in (unprese ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Equisetales
Equisetales is an order of subclass Equisetidae with only one living family Family (from ) is a Social group, group of people related either by consanguinity (by recognized birth) or Affinity (law), affinity (by marriage or other relationship). It forms the basis for social order. Ideally, families offer predictabili ..., Equisetaceae, containing the genus '' Equisetum'' (horsetails), as well as a variety of extinct groups, including the tree-like Calamitaceae. Classification In the molecular phylogenetic classification of Smith et al. in 2006, Equisetales, in its present circumscription, was held to be the sole member of class Equisetopsida. The linear sequence of Christenhusz et al. (2011), intended for compatibility with the classification of Chase and Reveal (2009) which placed all land plants in Equisetopsida, made it the sole member of subclass Equisetidae, equivalent to Smith's Equisetopsida. The placement of Equisetales in subclass Equisetidae has subsequently ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Calamites Sp
''Calamites'' is a genus of extinct arborescent (tree-like) horsetails to which the modern horsetails (genus ''Equisetum'') are closely related. Unlike their herbaceous modern cousins, these plants were medium-sized trees, growing to heights of . They were components of the understories of coal swamps of the Carboniferous Period (around ). Taxonomy A number of organ taxa have been identified as part of a united organism, which has inherited the name ''Calamites'' in popular culture. ''Calamites'' correctly refers only to casts of the stem of Carboniferous/Permian sphenophytes, and as such is a form genus of little taxonomic value. There are two forms of casts, which can give mistaken impressions of the organisms. The most common is an internal cast of the hollow (or pith-filled) void in the centre of the trunk. This can cause some confusion: firstly, a fossil was probably surrounded with 4-5 times its width in (unpreserved) vascular tissue, so the organisms were much wider ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Annularia
''Annularia'' is a form taxon, applied to fossil foliage belonging to extinct plants of the genus ''Calamites'' in the order Equisetales. Description ''Annularia'' is a form taxon name given to leaves of ''Calamites''. In that species, the leaves formed radiating leaf whorls at each stem node, in a similar way to the branches of ''Equisetum'', an extant genus of horsetails. ''Annularia'' leaves are arranged in whorls of between 8 and 13 leaves. The leaf shape is quite variable, being oval in ''Annularia sphenophylloides'' and linear to lanceolate in ''Annularia radiata'', but they are always flat and of varying lengths. ''Calamites'' were arborescent and grew to a height of . Fossil records Fossils of this genus have been discovered in the Permian strata of Russia and in the Carboniferous (around ) strata of the United States, Canada, China and Europe. Calamitaceae - Annularia stellata.JPG, Specimen of ''Annularia stellata'' from Italy on display at the Museo Civico di Storia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Horsetail
''Equisetum'' (; horsetail) is the only living genus in Equisetaceae, a family of vascular plants that reproduce by spores rather than seeds. ''Equisetum'' is a "living fossil", the only living genus of the entire subclass Equisetidae, which for over 100 million years was much more diverse and dominated the understorey of late Paleozoic forests. Some equisetids were large trees reaching to tall. The genus '' Calamites'' of the family Calamitaceae, for example, is abundant in coal deposits from the Carboniferous period. The pattern of spacing of nodes in horsetails, wherein those toward the apex of the shoot are increasingly close together, is said to have inspired John Napier to invent logarithms. Modern horsetails first appeared during the Jurassic period. A superficially similar but entirely unrelated flowering plant genus, mare's tail ('' Hippuris''), is occasionally referred to as "horsetail", and adding to confusion, the name "mare's tail" is sometimes applied to ''Eq ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arthropitys
''Arthropitys'' is an extinct genus of calamitacean equisetale. The petrified fossils of ''Arthropitys bistriata'', the type species, can be found in the Leukersdorf Formation, Chemnitz petrified forest, Chemnitz, Germany. The genus existed from the Carboniferous (Bashkirian)C. W. Good. (1975). Pennsylvanian-Age Calamitean Cones, Elater-Bearing Spores, and Associated Vegetative Organs. ''Palaeontographica'' 153:28-99 until the Early Triassic (Olenekian).I. A. Dobruskina. (1982). Triassic Floras of Eurasia. ''Akademia Nauk SSSR, Transactions'' 365:1-196 History The first remains of ''Arthropitys'' were discovered in the early 16th century and were described by Georgius Agricola (1494–1555) in 1546. In the mid-18th century, gemstone prospector David Frenzel (1691–1772) found numerous examples of this wood in the hills in and around Chemnitz. One of Frenzel's 1751 finds is one of the few petrified wood specimens still possessing its roots. Later a collector, the Hilbers ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fern Families
The ferns (Polypodiopsida or Polypodiophyta) are a group of vascular plants (plants with xylem and phloem) that reproduce via spores and have neither seeds nor flowers. They differ from mosses by being vascular, i.e., having specialized tissues that conduct water and nutrients, and in having life cycles in which the branched sporophyte is the dominant phase. Ferns have complex leaves called megaphylls that are more complex than the microphylls of clubmosses. Most ferns are leptosporangiate ferns. They produce coiled fiddleheads that uncoil and expand into fronds. The group includes about 10,560 known extant species. Ferns are defined here in the broad sense, being all of the Polypodiopsida, comprising both the leptosporangiate ( Polypodiidae) and eusporangiate ferns, the latter group including horsetails, whisk ferns, marattioid ferns, and ophioglossoid ferns. The fern crown group, consisting of the leptosporangiates and eusporangiates, is estimated to have originated in t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Prehistoric Plant Families
Prehistory, also called pre-literary history, is the period of human history between the first known use of stone tools by hominins million years ago and the beginning of recorded history with the invention of writing systems. The use of symbols, marks, and images appears very early among humans, but the earliest known writing systems appeared years ago. It took thousands of years for writing systems to be widely adopted, with writing having spread to almost all cultures by the 19th century. The end of prehistory therefore came at different times in different places, and the term is less often used in discussing societies where prehistory ended relatively recently. It is based on an old conception of history that without written records there could be no history. The most common conception today is that history is based on evidence, however the concept of prehistory hasn't been completely discarded. In the early Bronze Age, Sumer in Mesopotamia, the Indus Valley Civilis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carboniferous Plants
The Carboniferous ( ) is a geologic period and system of the Paleozoic era that spans 60 million years, from the end of the Devonian Period Ma (million years ago) to the beginning of the Permian Period, Ma. It is the fifth and penultimate period of the Paleozoic era and the fifth period of the Phanerozoic eon. In North America, the Carboniferous is often treated as two separate geological periods, the earlier Mississippian and the later Pennsylvanian. The name ''Carboniferous'' means "coal-bearing", from the Latin ("coal") and ("bear, carry"), and refers to the many coal beds formed globally during that time. The first of the modern "system" names, it was coined by geologists William Conybeare and William Phillips in 1822, based on a study of the British rock succession. Carboniferous is the period during which both terrestrial animal and land plant life was well established. Stegocephalia (four-limbed vertebrates including true tetrapods), whose forerunners (tetrapodomor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
