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Fungus
Dikarya
Dikarya
(inc. Deuteromycota)AscomycotaPezizomycotina Saccharomycotina TaphrinomycotinaBasidiomycotaAgaricomycotina Pucciniomycotina UstilaginomycotinaSubphyla incertae sedisEntomophthoromycotina Kickxellomycotina Mucoromycotina ZoopagomycotinaA fungus (plural: fungi[3] or funguses[4]) is any member of the group of eukaryotic organisms that includes microorganisms such as yeasts and molds, as well as the more familiar mushrooms. These organisms are classified as a kingdom, Fungi, which is separate from the other eukaryotic life kingdoms of plants and animals. A characteristic that places fungi in a different kingdom from plants, bacteria, and some protists is chitin in their cell walls. Similar to animals, fungi are heterotrophs; they acquire their food by absorbing dissolved molecules, typically by secreting digestive enzymes into their environment. Fungi do not photosynthesise
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Carl Linnaeus
Carl Linnaeus
Linnaeus
(/lɪˈniːəs, lɪˈneɪəs/;[1][2] 23 May[note 1] 1707 – 10 January 1778), also known after his ennoblement as Carl von Linné[3] (Swedish pronunciation: [kɑːɭ fɔn lɪˈneː] ( listen)), was a Swedish botanist, physician and zoologist, who formalised the modern system of naming organisms called binomial nomenclature. He is known by the epithet "father of modern taxonomy".[4] Many of his writings were in Latin
Latin
and his name is rendered in Latin
Latin
as Carolus Linnæus (after 1761 Carolus a Linné). Linnaeus
Linnaeus
was born in the countryside of Småland, in southern Sweden. He received most of his higher education at Uppsala University
Uppsala University
and began giving lectures in botany there in 1730
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Triassic
The Triassic
Triassic
( /traɪˈæsɪk/) is a geologic period and system which spans 50.9 million years from the end of the Permian
Permian
Period 251.9 million years ago (Mya), to the beginning of the Jurassic
Jurassic
Period 201.3 Mya.[8] The Triassic
Triassic
is the first period of the Mesozoic
Mesozoic
Era. Both the start and end of the period are marked by major extinction events.[9] The Triassic
Triassic
began in the wake of the Permian– Triassic
Triassic
extinction event, which left the earth's biosphere impoverished; it would take well into the middle of this period for life to recover its former diversity. Therapsids and archosaurs were the chief terrestrial vertebrates during this time
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Plural
The plural (sometimes abbreviated PL), in many languages, is one of the values of the grammatical category of number. Plural of nouns typically denote a quantity other than the default quantity represented by a noun, which is generally one (the form that represents this default quantity is said to be of singular number). Most commonly, therefore, plurals are used to denote two or more of something, although they may also denote more than fractional, zero or negative amounts. An example of a plural is the English word cats, which corresponds to the singular cat. Words of other types, such as verbs, adjectives and pronouns, also frequently have distinct plural forms, which are used in agreement with the number of their associated nouns. Some languages also have a dual (denoting exactly two of something) or other systems of number categories
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Royall T. Moore
Michigan State College Harvard UniversityKnown for New species Fungal diversity and developmentAwards Benefactor's Medal, British Mycological Society Doctor of ScienceScientific careerFields MycologyDoctoral advisor Ivan Mackenzie LambAuthor abbrev. (botany) R.T. MooreRoyall Tyler Moore (October 11, 1930 – August 17, 2014) was an American-born mycologist and mycology professor.Contents1 Education and work 2 Selected publications 3 See also 4 ReferencesEducation and work[edit] He received his doctorate from the Harvard University
Harvard University
in 1959, writing his dissertation on the fungal genus Sporidesmium
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Aspergillus
See List of Aspergillus
Aspergillus
species Aspergillus
Aspergillus
(/ˌæspərˈdʒɪləs/) is a genus consisting of a few hundred mold species found in various climates worldwide. Aspergillus
Aspergillus
was first catalogued in 1729 by the Italian priest and biologist Pier Antonio Micheli
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Incertae Sedis
Incertae sedis
Incertae sedis
( Latin
Latin
for "of uncertain placement")[1] is a term used for a taxonomic group where its broader relationships are unknown or undefined.[2] Alternatively, such groups are frequently referred to as "enigmatic taxa".[3] I
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Amanita Muscaria
cap is flat or convexhymenium is freestipe has a ring and volvaspore print is whiteecology is mycorrhizaledibility: poisonous or psychoactive Amanita
Amanita
muscaria, commonly known as the fly agaric or fly amanita, is a basidiomycete mushroom, one of many in the genus Amanita. It is also a muscimol mushroom. Native throughout the temperate and boreal regions of the Northern Hemisphere, Amanita
Amanita
muscaria has been unintentionally introduced to many countries in the Southern Hemisphere, generally as a symbiont with pine and birch plantations, and is now a true cosmopolitan species
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Neogene
The Neogene
Neogene
( /ˈniːəˌdʒiːn/)[6][7] (informally Upper Tertiary or Late Tertiary) is a geologic period and system that spans 20.45 million years from the end of the Paleogene Period 23.03 million years ago (Mya) to the beginning of the present Quaternary
Quaternary
Period 2.58 Mya. The Neogene
Neogene
is sub-divided into two epochs, the earlier Miocene
Miocene
and the later Pliocene. Some geologists assert that the Neogene
Neogene
cannot be clearly delineated from the modern geological period, the Quaternary. During this period, mammals and birds continued to evolve into roughly modern forms, while other groups of life remained relatively unchanged. Early hominids, the ancestors of humans, appeared in Africa near the end of the period
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Paleogene
The Paleogene (/ˈpæliədʒiːn, ˈpeɪliə-/; 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
Cretaceous
Period 66 million years ago (Mya) to the beginning of the Neogene
Neogene
Period 23.03 Mya
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Cretaceous
The Cretaceous
Cretaceous
( /krɪˈteɪʃəs/, kri-TAY-shəs) is a geologic period and system that spans 79 million years from the end of the Jurassic
Jurassic
Period 145 million years ago (mya) to the beginning of the Paleogene Period 66 mya. It is the last period of the Mesozoic
Mesozoic
Era. The Cretaceous
Cretaceous
Period is usually abbreviated K, for its German translation Kreide (chalk). The Cretaceous
Cretaceous
was a period with a relatively warm climate, resulting in high eustatic sea levels that created numerous shallow inland seas. These oceans and seas were populated with now-extinct marine reptiles, ammonites and rudists, while dinosaurs continued to dominate on land. During this time, new groups of mammals and birds, as well as flowering plants, appeared
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Jurassic
The Jurassic
Jurassic
( /dʒʊˈræsɪk/; from Jura Mountains) was a geologic period and system that spanned 56 million years from the end of the Triassic
Triassic
Period 201.3 million years ago (Mya) to the beginning of the Cretaceous
Cretaceous
Period 145 Mya.[note 1] The Jurassic
Jurassic
constituted the middle period of the Mesozoic
Mesozoic
Era, also known as the Age of Reptiles. The start of the period was marked by the major Triassic–Jurassic extinction event
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Permian
The Permian
Permian
is a geologic period and system which spans 46.7 million years from the end of the Carboniferous
Carboniferous
Period 298.9 million years ago (Mya), to the beginning of the Triassic
Triassic
period 251.902 Mya. It is the last period of the Paleozoic
Paleozoic
era; the following Triassic
Triassic
period belongs to the Mesozoic
Mesozoic
era. The concept of the Permian
Permian
was introduced in 1841 by geologist Sir Roderick Murchison, who named it after the city of Perm. The Permian
Permian
witnessed the diversification of the early amniotes into the ancestral groups of the mammals, turtles, lepidosaurs, and archosaurs. The world at the time was dominated by two continents known as Pangaea
Pangaea
and Siberia, surrounded by a global ocean called Panthalassa
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Carboniferous
The Carboniferous
Carboniferous
is a geologic period and system that spans 60 million years from the end of the Devonian
Devonian
Period 358.9 million years ago (Mya), to the beginning of the Permian
Permian
Period, 298.9 Mya
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Silurian
The Silurian
Silurian
is a geologic period and system spanning 24.6 million years from the end of the Ordovician
Ordovician
Period, at 443.8 million years ago (Mya), to the beginning of the Devonian
Devonian
Period, 419.2 Mya.[8] As with other geologic periods, the rock beds that define the period's start and end are well identified, but the exact dates are uncertain by several million years. The base of the Silurian
Silurian
is set at a series of major Ordovician–Silurian extinction events
Ordovician–Silurian extinction events
when 60% of marine species were wiped out. A significant evolutionary milestone during the Silurian
Silurian
was the diversification of jawed and bony fish
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Ordovician
The Ordovician
Ordovician
( /ɔːrdəˈvɪʃən/) is a geologic period and system, the second of six periods of the Paleozoic
Paleozoic
Era
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