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Aspidotis
''Aspidotis'' is a small genus of leptosporangiate ferns known commonly as laceferns. Most species are native to slopes, ridges, and rocky outcroppings, primarily in California and Mexico, although one species included in the genus by some authorities is widely distributed in eastern Africa. Description Members of ''Aspidotis'' are small ferns, with shiny, tufted fronds generally less than 35 centimeters long (although ''A. schimperi'' may be larger). Fertile leaves have false indusia formed by the leaves' inrolled margins, which partially conceal the spore-bearing sori. Taxonomy The taxonomy of laceferns has been considerably refined since they were first described in the late 1800s. Species currently placed in ''Aspidotis'' were originally assigned to a section of '' Hypolepis'', then to '' Cheilanthes''. David Lellinger established ''Aspidotis'' as a distinct genus based on characteristic features of its false indusia and its leaves, including their shiny surface, altho ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aspidotis Densa
''Aspidotis densa'' is a species of fern in the Cheilanthoid subfamily, known by the common name Indian's dream or Serpentine fern or dense lace fern. It is native to the west coast of North America from British Columbia to California and east to the Rocky Mountains in Idaho, Montana, and Wyoming; there is a disjunct population on serpentine soils in Quebec. Hitchcock, C.L. and Cronquist, A. 2018. Flora of the Pacific Northwest, 2nd Edition, p. 55. University of Washington Press, Seattle. Description This fern has leaves on long wiry brown to black petioles (stem below the leaf), with the leaf blade occupying less than half of the total length of the leaf when including the petiole. The leaves emerge from a short creeping rhizome covered with firm narrow scales. Where the petiole joins the leaf, the stem color grades to green and acquires a groove on its adaxial (top) surface. The leaf blades are medium to dark green, sometimes with a glaucous or bluish cast. The leaf blade is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aspidotis Schimperi
''Aspidotis'' is a small genus of leptosporangiate ferns known commonly as laceferns. Most species are native to slopes, ridges, and rocky outcroppings, primarily in California and Mexico, although one species included in the genus by some authorities is widely distributed in eastern Africa. Description Members of ''Aspidotis'' are small ferns, with shiny, tufted fronds generally less than 35 centimeters long (although ''A. schimperi'' may be larger). Fertile leaves have false indusia formed by the leaves' inrolled margins, which partially conceal the spore-bearing sori. Taxonomy The taxonomy of laceferns has been considerably refined since they were first described in the late 1800s. Species currently placed in ''Aspidotis'' were originally assigned to a section of '' Hypolepis'', then to '' Cheilanthes''. David Lellinger established ''Aspidotis'' as a distinct genus based on characteristic features of its false indusia and its leaves, including their shiny surface, altho ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aspidotis Meifolia
''Aspidotis'' is a small genus of leptosporangiate ferns known commonly as laceferns. Most species are native to slopes, ridges, and rocky outcroppings, primarily in California and Mexico, although one species included in the genus by some authorities is widely distributed in eastern Africa. Description Members of ''Aspidotis'' are small ferns, with shiny, tufted fronds generally less than 35 centimeters long (although ''A. schimperi'' may be larger). Fertile leaves have false indusia formed by the leaves' inrolled margins, which partially conceal the spore-bearing sori. Taxonomy The taxonomy of laceferns has been considerably refined since they were first described in the late 1800s. Species currently placed in ''Aspidotis'' were originally assigned to a section of '' Hypolepis'', then to '' Cheilanthes''. David Lellinger established ''Aspidotis'' as a distinct genus based on characteristic features of its false indusia and its leaves, including their shiny surface, altho ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aspidotis Californica
''Aspidotis californica'' is a species of fern known by the common name California lacefern. It is native to California and Baja California. It grows in rock cracks and crevices in many types of habitat, including Chaparral, Yellow pine forest Ponderosa pine forest is a plant association and plant community dominated by ponderosa pine and found in western North America. It is found from the Rocky Mountains to the Pacific Coast Ranges in the Western United States and Western Canada. In ..., Foothill oak woodland, and Valley grassland. Description ''Aspidotis californica'' has leaves that are thin and dissected into many triangular leaflets which are subdivided into small segments with curled teeth. The leaf segments bear sori containing sporangia, with the edges of the leaves rolled under to create a false indusium over the sori. References External linksCalflora Database: ''Aspidotis californica'' (California lace fern) [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aspidotis Carlotta-halliae
''Aspidotis carlotta-halliae'' is a species of perennial fern known by the common names tufted lacefern and Carlotta Hall's lace fern. It is endemic to California, where it is found in the Central Coast Ranges and coastal hillsides, often on serpentine soils. This species is a fertile hybrid between ''Aspidotis californica'' and ''Aspidotis densa''. The fern was named for fern collector Carlotta Case Hall, who coauthored the 1912 botanical guide ''A Yosemite Flora'' with her husband, botanist Harvey Monroe Hall. Description In appearance it is intermediate between the two other ferns. It has leathery triangular leaves divided into many pairs of leaflets, which are each subdivided into many coarse, irregularly toothed segments. The stipe is very thin and dark. The undersides of the segments are lined with sori containing sporangia. It is found between to in elevation The elevation of a geographic location is its height above or below a fixed reference point, most common ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pteridaceae
Pteridaceae is a family of ferns in the order Polypodiales, including some 1150 known species in ca 45 genera (depending on taxonomic opinions), divided over five subfamilies. The family includes four groups of genera that are sometimes recognized as separate families: the adiantoid, cheilanthoid, pteridoid, and hemionitidoid ferns. Relationships among these groups remain unclear, and although some recent genetic analyses of the Pteridales suggest that neither the family Pteridaceae nor the major groups within it are all monophyletic, as yet these analyses are insufficiently comprehensive and robust to provide good support for a revision of the order at the family level. Description Members of Pteridaceae have creeping or erect rhizomes. The leaves are almost always compound and have linear sori that are typically on the margins of the leaves and lack a true indusium, typically being protected by a false indusium formed from the reflexed margin of the leaf. Taxonomy Tradi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Serpentine Soil
Serpentine soil is an uncommon soil type produced by weathered ultramafic rock such as peridotite and its metamorphic derivatives such as serpentinite. More precisely, serpentine soil contains minerals of the serpentine subgroup, especially antigorite, lizardite, and chrysotile or white asbestos, all of which are commonly found in ultramafic rocks. The term "serpentine" is commonly used to refer to both the soil type and the mineral group which forms its parent materials. Serpentine soils exhibit distinct chemical and physical properties and are generally regarded as poor soils for agriculture. The soil is often reddish, brown, or gray in color due to its high iron and low organic content. Geologically, areas with serpentine bedrock are characteristically steep, rocky, and vulnerable to erosion, which causes many serpentine soils to be rather shallow. The shallow soils and sparse vegetation lead to elevated soil temperatures and dry conditions. Due to their ultramafic origin, ser ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fern
A fern (Polypodiopsida or Polypodiophyta ) is a member of a group of vascular plants (plants with xylem and phloem) that reproduce via spores and have neither seeds nor flowers. The polypodiophytes include all living pteridophytes except the lycopods, and differ from mosses and other bryophytes 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. Ferns first ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Edwin Bingham Copeland
Edwin Bingham Copeland (September 30, 1873 – March 16, 1964) was an American botanist and agriculturist. He is known for founding the University of the Philippines College of Agriculture at Los Baños, Laguna and for being one of the America's leading pteridologists (one who studies ferns). Life In 1903, he and his family moved to the Philippines, where he worked as a Systematic Botanist for the Bureau of Science. Wagner, W.H. Jr. 1964Edwin Bingham Copeland (1873–1964) and his contributions to Pteridology American Fern Journal 54(4): 177–188. In 1909, he founded the University of the Philippines College of Agriculture at Los Baños, Laguna, now part of the University of the Philippines Los Baños, and served as its dean and also as a professor of plant physiology for eight years (1909–1917). In 1917, he returned to the United States and was a leading rice grower in Chico, California. In 1927, he began work as an Associate Curator at the University of California, Berkel ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Greek Language
Greek ( el, label=Modern Greek, Ελληνικά, Elliniká, ; grc, Ἑλληνική, Hellēnikḗ) is an independent branch of the Indo-European family of languages, native to Greece, Cyprus, southern Italy (Calabria and Salento), southern Albania, and other regions of the Balkans, the Black Sea coast, Asia Minor, and the Eastern Mediterranean. It has the longest documented history of any Indo-European language, spanning at least 3,400 years of written records. Its writing system is the Greek alphabet, which has been used for approximately 2,800 years; previously, Greek was recorded in writing systems such as Linear B and the Cypriot syllabary. The alphabet arose from the Phoenician script and was in turn the basis of the Latin, Cyrillic, Armenian, Coptic, Gothic, and many other writing systems. The Greek language holds a very important place in the history of the Western world. Beginning with the epics of Homer, ancient Greek literature includes many works of lasting impo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ultramafic
Ultramafic rocks (also referred to as ultrabasic rocks, although the terms are not wholly equivalent) are igneous and meta-igneous rocks with a very low silica content (less than 45%), generally >18% MgO, high FeO, low potassium, and are composed of usually greater than 90% mafic minerals (dark colored, high magnesium and iron content). The Earth's mantle is composed of ultramafic rocks. Ultrabasic is a more inclusive term that includes igneous rocks with low silica content that may not be extremely enriched in Fe and Mg, such as carbonatites and ultrapotassic igneous rocks. Intrusive ultramafic rocks Intrusive ultramafic rocks are often found in large, layered ultramafic intrusions where differentiated rock types often occur in layers. Such cumulate rock types do not represent the chemistry of the magma from which they crystallized. The ultramafic intrusives include the dunites, peridotites and pyroxenites. Other rare varieties include troctolite which has a greater percenta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Edaphic
Edaphology (from Greek , ''edaphos'', "ground",, ''-logia'') is concerned with the influence of soils on living beings, particularly plants. It is one of two main divisions of soil science, the other being pedology. Edaphology includes the study of how soil influences humankind's use of land for plant growth as well as people's overall use of the land. General subfields within edaphology are agricultural soil science (known by the term agrology in some regions) and environmental soil science. (Pedology deals with pedogenesis, soil morphology, and soil classification.) In Russia, edaphology is considered equivalent to pedology, but is recognized to have an applied sense consistent with agrophysics and agrochemistry outside Russia. History Xenophon (431–355 BC), and Cato (234–149 BC), were early edaphologists. Xenophon noted the beneficial effect of turning a cover crop into the earth. Cato wrote De Agri Cultura ("On Farming") which recommended tillage, crop rotatio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
