HOME TheInfoList.com
Providing Lists of Related Topics to Help You Find Great Stuff
[::MainTopicLength::#1500] [::ListTopicLength::#1000] [::ListLength::#15] [::ListAdRepeat::#3]

picture info

Poales
See textDiversityAbout 1,050 genera[citation needed]The Poales
Poales
are a large order of flowering plants in the monocotyledons, and includes families of plants such as the grasses, bromeliads, and sedges. Sixteen plant families are currently recognized by botanists to be part of Poales.Contents1 Description 2 Taxonomy2.1 Evolution and phylogeny 2.2 Diversity3 Uses 4 References 5 External linksDescription[edit] Billbergia pyramidalis
Billbergia pyramidalis
of family BromeliaceaeThe flowers are typically small, enclosed by bracts, and arranged in inflorescences (except in three species of the genus Mayaca, which possess very reduced, one-flowered inflorescences)
[...More...]

"Poales" on:
Wikipedia
Google
Yahoo

Late Cretaceous
The Late Cretaceous
Cretaceous
(100.5–66 Ma) is the younger of two epochs into which the Cretaceous
Cretaceous
period is divided in the geologic timescale. Rock strata from this epoch form the Upper Cretaceous
Cretaceous
series
[...More...]

"Late Cretaceous" on:
Wikipedia
Google
Yahoo

picture info

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
[...More...]

"Neogene" on:
Wikipedia
Google
Yahoo

picture info

Inflorescence
An inflorescence is a group or cluster of flowers arranged on a stem that is composed of a main branch or a complicated arrangement of branches. Morphologically, it is the modified part of the shoot of seed plants where flowers are formed. The modifications can involve the length and the nature of the internodes and the phyllotaxis, as well as variations in the proportions, compressions, swellings, adnations, connations and reduction of main and secondary axes. Inflorescence
Inflorescence
can also be defined as the reproductive portion of a plant that bears a cluster of flowers in a specific pattern. The stem holding the whole inflorescence is called a peduncle and the major axis (incorrectly referred to as the main stem) holding the flowers or more branches within the inflorescence is called the rachis. The stalk of each single flower is called a pedicel
[...More...]

"Inflorescence" on:
Wikipedia
Google
Yahoo

picture info

Order (biology)
In biological classification, the order (Latin: ordo) isa taxonomic rank used in the classification of organisms and recognized by the nomenclature codes. Other well-known ranks are life, domain, kingdom, phylum, class, family, genus, and species, with order fitting in between class and family. An immediately higher rank, superorder, may be added directly above order, while suborder would be a lower rank. a taxonomic unit, a taxon, in that rank. In that case the plural is orders (Latin ordines).Example: All owls belong to the order Strigiformes.What does and does not belong to each order is determined by a taxonomist, as is whether a particular order should be recognized at all. Often there is no exact agreement, with different taxonomists each taking a different position. There are no hard rules that a taxonomist needs to follow in describing or recognizing an order
[...More...]

"Order (biology)" on:
Wikipedia
Google
Yahoo

picture info

Biodiversity
Biodiversity, a portmanteau of "bio" (life) and "diversity", generally refers to the variety and variability of life on Earth. According to the United Nations Environment Programme
United Nations Environment Programme
(UNEP), biodiversity typically measures variation at the genetic, the species, and the ecosystem level.[1] Terrestrial biodiversity tends to be greater near the equator,[2] which seems to be the result of the warm climate and high primary productivity.[3] Biodiversity
Biodiversity
is not distributed evenly on Earth, and is richest in the tropics
[...More...]

"Biodiversity" on:
Wikipedia
Google
Yahoo

picture info

John Kunkel Small
John Kunkel Small
John Kunkel Small
(January 31, 1869 – January 20, 1938) was an American botanist. Born on January 31, 1869 in Harrisburg Pennsylvania, Kunkel studied botany at Franklin & Marshall College and Columbia University.Family of John Kunkel Small
John Kunkel Small
in the Florida Everglades
Florida Everglades
near Lake Okeechobee aboard the boat "Lida", 1913. Small frequently brought his family with him on his botanical and ethnographic excursions. From left to right: George K. Small, Kathryn Wheeler Small, Elizabeth Wheeler Small, Elizabeth Small, and John Wheeler Small.He was the first Curator of Museums at The New York Botanical
Botanical
Garden, a post in which he served from 1898 until 1906. From 1906 to 1934 he was Head Curator and then from 1934 until his death he was Chief Research Associate and Curator
[...More...]

"John Kunkel Small" on:
Wikipedia
Google
Yahoo

picture info

Starch
Starch
Starch
or amylum is a polymeric carbohydrate consisting of a large number of glucose units joined by glycosidic bonds. This polysaccharide is produced by most green plants as energy storage. It is the most common carbohydrate in human diets and is contained in large amounts in staple foods like potatoes, wheat, maize (corn), rice, and cassava. Pure starch is a white, tasteless and odorless powder that is insoluble in cold water or alcohol. It consists of two types of molecules: the linear and helical amylose and the branched amylopectin. Depending on the plant, starch generally contains 20 to 25% amylose and 75 to 80% amylopectin by weight.[4] Glycogen, the glucose store of animals, is a more highly branched version of amylopectin. In industry, starch is converted into sugars, for example by malting, and fermented to produce ethanol in the manufacture of beer, whisky and biofuel. It is processed to produce many of the sugars used in processed foods
[...More...]

"Starch" on:
Wikipedia
Google
Yahoo

Prionia
Falcaria is a genus of moths belonging to the subfamily Drepaninae.[1] Description[edit] Palpi slender and not reaching beyond the frons. Antennae bipectinated in both sexes to near apex, the branches longer in male than in female. Hind tibia not dilated. Fore wings produced at apex. The outer margin usually excurved at middle. vein 3 from close to angle of cell. Veins 7 to 9 stalked from before upper angle and vein 11 anastomosing with vein 12. Hind wings with vein 3 from before angle of cell.[2] Species[edit]Falcaria lacertinaria Linnaeus, 1758 Falcaria bilineata Packard, 1864References[edit]^ LepIndex ^ Hampson G. F. (1892). "The Fauna Of British India Including Ceylon And Burma Moths Vol-iii". Digital Library of India
[...More...]

"Prionia" on:
Wikipedia
Google
Yahoo

picture info

Plant
Plants are mainly multicellular, predominantly photosynthetic eukaryotes of the kingdom Plantae. They form the clade Viridiplantae (Latin for "green plants") that includes the flowering plants, conifers and other gymnosperms, ferns, clubmosses, hornworts, liverworts, mosses and the green algae, and excludes the red and brown algae. Historically, plants were treated as one of two kingdoms including all living things that were not animals, and all algae and fungi were treated as plants. However, all current definitions of Plantae exclude the fungi and some algae, as well as the prokaryotes (the archaea and bacteria). Green plants have cell walls containing cellulose and obtain most of their energy from sunlight via photosynthesis by primary chloroplasts that are derived from endosymbiosis with cyanobacteria. Their chloroplasts contain chlorophylls a and b, which gives them their green color
[...More...]

"Plant" on:
Wikipedia
Google
Yahoo

picture info

Taxonomy (biology)
Taxonomy (from Ancient Greek τάξις (taxis), meaning 'arrangement', and -νομία (-nomia), meaning 'method') is the science of defining and naming groups of biological organisms on the basis of shared characteristics. Organisms are grouped together into taxa (singular: taxon) and these groups are given a taxonomic rank; groups of a given rank can be aggregated to form a super-group of higher rank, thus creating a taxonomic hierarchy. The principal ranks in modern use are domain, kingdom, phylum (division is sometimes used in botany in place of phylum), class, order, family, genus and species
[...More...]

"Taxonomy (biology)" on:
Wikipedia
Google
Yahoo

picture info

Cronquist System
The Cronquist system
Cronquist system
is a taxonomic classification system of flowering plants. It was developed by Arthur Cronquist in a series of monographs and texts, including The Evolution and Classification of Flowering Plants (1968; 2nd edition, 1988) and An Integrated System of Classification of Flowering Plants (1981) (see Bibliography). Cronquist's system places flowering plants into two broad classes, Magnoliopsida
Magnoliopsida
(dicotyledons) and Liliopsida (monocotyledons). Within these classes, related orders are grouped into subclasses. While the scheme was widely used, in either the original form or in adapted versions, many botanists now use the Angiosperm Phylogeny Group classification for the orders and families of flowering plants, first developed in 1998
[...More...]

"Cronquist System" on:
Wikipedia
Google
Yahoo

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
[...More...]

"Paleogene" on:
Wikipedia
Google
Yahoo

picture info

Megaannum
A year is the orbital period of the Earth
Earth
moving in its orbit around the Sun. Due to the Earth's axial tilt, the course of a year sees the passing of the seasons, marked by changes in weather, the hours of daylight, and, consequently, vegetation and soil fertility. In temperate and subpolar regions around the planet, four seasons are generally recognized: spring, summer, autumn and winter. In tropical and subtropical regions several geographical sectors do not present defined seasons; but in the seasonal tropics, the annual wet and dry seasons are recognized and tracked. The current year is 2018. A calendar year is an approximation of the number of days of the Earth's orbital period as counted in a given calendar. The Gregorian, or modern, calendar, presents its calendar year to be either a common year of 365 days or a leap year of 366 days, as do the Julian calendars; see below
[...More...]

"Megaannum" on:
Wikipedia
Google
Yahoo

picture info

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
[...More...]

"Cretaceous" on:
Wikipedia
Google
Yahoo

picture info

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
[...More...]

"Jurassic" on:
Wikipedia
Google
Yahoo
.