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The Vitaceae are a family of flowering plants, with 14 genera and around 910 known species, including common plants such as grapevines and Virginia creeper. The family name is derived from the genus Vitis.
Pica is a genus of seven species of birds in the family Corvidae in both the New World and the Old. It is one of several corvid genera whose members are known as magpies.
Paleobotany, also spelled as palaeobotany, is the branch of botany dealing with the recovery and identification of plant remains from geological contexts, and their use for the biological reconstruction of past environments (paleogeography), and the evolutionary history of plants, with a bearing upon the evolution of life in general. A synonym is paleophytology. It is a component of paleontology and paleobiology. The prefix palaeo- or paleo- means "ancient, old", and is derived from the Greek adjective παλαιός, palaios. Paleobotany includes the study of terrestrial plant fossils, as well as the study of prehistoric marine photoautotrophs, such as photosynthetic algae, seaweeds or kelp. A closely related field is palynology, which is the study of fossilized and extant spores and pollen.
Sparganium (bur-reed) is a genus of flowering plants, described as a genus by Linnaeus in 1753. It is widespread in wet areas in temperate regions of both the Northern and Southern Hemispheres. The plants are perennial marsh plants that can grow to 3.5 m, with epicene flowers.
Nicolia is a genus of fossilized wood from the Late Cretaceous to Pleistocene of Belgium, Ethiopia, Egypt, New Caledonia, New Zealand, and Tunisia. The type species is N. aegyptiaca.
Acacia, commonly known as wattles or acacias, is a genus of about 1,084 species of shrubs and trees in the subfamily Mimosoideae of the pea family Fabaceae. Initially, it comprised a group of plant species native to Africa, South America, and Australasia, but is now reserved for species mainly from Australia, with others from New Guinea, Southeast Asia, and the Indian Ocean. The genus name is Neo-Latin, borrowed from the Greek ἀκακία, a term used in antiquity to describe a preparation extracted from Vachellia nilotica, the original type species.
Loranthus is a genus of parasitic plants that grow on the branches of woody trees. It belongs to the family Loranthaceae, the showy mistletoe family. In most earlier systematic treatments it contains all mistletoe species with bisexual flowers, though some species have reversed to unisexual flowers. Other treatments restrict the genus to a few species. The systematic situation of Loranthus is not entirely clear.
Aporrhais is a genus of medium-sized sea snails, marine gastropod mollusks in the family Aporrhaidae and the superfamily Stromboidea.
Paleontology in Michigan refers to paleontological research occurring within or conducted by people from the U.S. state of Michigan. During the Precambrian, the Upper Peninsula was home to filamentous algae. The remains it left behind are among the oldest known fossils in the world. During the early part of the Paleozoic Michigan was covered by a shallow tropical sea which was home to a rich invertebrate fauna including brachiopods, corals, crinoids, and trilobites. Primitive armored fishes and sharks were also present. Swamps covered the state during the Carboniferous. There are little to no sedimentary deposits in the state for an interval spanning from the Permian to the end of the Neogene. Deposition resumed as glaciers transformed the state's landscape during the Pleistocene. Michigan was home to large mammals like mammoths and mastodons at that time. The Holocene American mastodon, Mammut americanum, is the Michigan state fossil. The Petoskey stone, which is made of fossil coral, is the state stone of Michigan.
Paleontology in North Carolina refers to paleontological research occurring within or conducted by people from the U.S. state of North Carolina. Fossils are common in North Carolina. According to author Rufus Johnson, "almost every major river and creek east of Interstate 95 has exposures where fossils can be found". The fossil record of North Carolina spans from Eocambrian remains that are 600 million years old, to the Pleistocene 10,000 years ago.
Paleontology in Rhode Island refers to paleontological research occurring within or conducted by people from the U.S. state of Rhode Island. Rhode Island has a relatively sparse fossil record. Among its more common fossils are plant remains that are frequently associated with the state's coal beds. During the early Paleozoic, Rhode Island was at least partially submerged under a sea inhabited by trilobites. During the Carboniferous period the state became a swampy environment where lush vegetation included trees more than 50 feet high. Local animal life included arachnids and insects like cockroaches. Rift basins formed locally during the Permian. The ensuing Triassic and Jurassic periods are absent from the state's rock record. Little is known about the state's Cretaceous history. The Paleogene and Neogene periods are also missing from Rhode Island's rock record. During the Pleistocene the state was subjected to glacial activity. Notable local fossil finds have included previously unknown kinds of insect and abundant ancient amphibian trackways.
Paleontology in Missouri refers to paleontological research occurring within or conducted by people from the U.S. state of Missouri. The geologic column of Missouri spans all of geologic history from the Precambrian to present with the exception of the Permian, Triassic, and Jurassic. Brachiopods are probably the most common fossils in Missouri.
Paleontology in Texas refers to paleontological research occurring within or conducted by people from the U.S. state of Texas. Author Marian Murray has said that "Texas is as big for fossils as it is for everything else." Some of the most important fossil finds in United States history have come from Texas. Fossils can be found throughout most of the state. The fossil record of Texas spans almost the entire geologic column from Precambrian to Pleistocene. Shark teeth are probably the state's most common fossil. During the early Paleozoic era Texas was covered by a sea that would later be home to creatures like brachiopods, cephalopods, graptolites, and trilobites. Little is known about the state's Devonian and early Carboniferous life. Evidence indicates that during the late Carboniferous the state was home to marine life, land plants and early reptiles. During the Permian, the seas largely shrank away, but nevertheless coral reefs formed in the state. The rest of Texas was a coastal plain inhabited by early relatives of mammals like Dimetrodon and Edaphosaurus. During the Triassic, a great river system formed in the state that was inhabited by crocodile-like phytosaurs. Little is known about Jurassic Texas, but there are fossil aquatic invertebrates of this age like ammonites in the state. During the Early Cretaceous local large sauropods and theropods left a great abundance of footprints. Later in the Cretaceous, the state was covered by the Western Interior Seaway and home to creatures like mosasaurs, plesiosaurs, and few icthyosaurs. Early Cenozoic Texas still contained areas covered in seawater where invertebrates and sharks lived. On land the state would come to be home to creatures like glyptodonts, mammoths, mastodons, saber-toothed cats, giant ground sloths, titanotheres, uintatheres, and dire wolves. Archaeological evidence suggests that local Native Americans knew about local fossils. Formally trained scientists were already investigating the state's fossils by the late 1800s. In 1938, a major dinosaur footprint find occurred near Glen Rose. Pleurocoelus was the Texas state dinosaur from 1997 to 2009, when it was replaced by Paluxysaurus jonesi after the Texan fossils once referred to the former species were reclassified to a new genus.
Paleontology in Idaho refers to paleontological research occurring within or conducted by people from the U.S. state of Idaho. The fossil record of Idaho spans much of the geologic column from the Precambrian onward. During the Precambrian, bacteria formed stromatolites while worms left behind trace fossils. The state was mostly covered by a shallow sea during the majority of the Paleozoic era. This sea became home to creatures like brachiopods, corals and trilobites. Idaho continued to be a largely marine environment through the Triassic and Jurassic periods of the Mesozoic era, when brachiopods, bryozoans, corals, ichthyosaurs and sharks inhabited the local waters. The eastern part of the state was dry land during the ensuing Cretaceous period when dinosaurs roamed the area and trees grew which would later form petrified wood.
Euryale is a genus of flowering plants of the family Nymphaeaceae.
Macroneuropteris is a genus of Carboniferous seed plants in the order Medullosales. The genus is best known for the species Macroneuropteris scheuchzeri, a medium-size tree that was common throughout the late Carboniferous Euramerica. Three similar species, M. macrophylla, M. britannica and M. subauriculata are also included in the genus.
Conomedusites was a creature from the Ediacaran biota. The Ediacaran period ranged from 635 to 539 million years ago. Its fossil was first discovered in 1966 by Martin F. Glaessner and Mary Wade in South Australia. Conomedusites is believed to have been part of the phylum Cnidaria due to its similar structure to jellyfish and other cnidarians, but this is not known for certain. Conomedusites is thought to have been a stationary osmotroph.
Schizophoria is an extinct genus of brachiopod belonging to the superfamily Enteletoidea. Specimens have been found in Devonian through Permian beds in North America, Australia, central and southeast Asia, and eastern Europe.
Tritia pygmaea is an extinct species of sea snail, a marine gastropod mollusc in the family Nassariidae, the nassa mud snails or dog whelks.
It is suggested a late Pliocene age (Reuverian) for this flora. Palynofloras from drill cores in the surroundings of Frankfurt am Main and Hanau also suggests a late Pliocene age. The Pliocene flora of Frankfurt am Main described by Karl Mädler during the first half of the twentieth century is a key flora for the European Pliocene.
References
- ↑ Columbian Cyclopedia. (1897). United States: Garretson, Cox.
- 1 2 PBDB Taxon. (n.d.). Retrieved from https://paleobiodb.org/classic/checkTaxonInfo?taxon_no=134692&is_real_user=1
- ↑ Mindat.org. (2016). Mindat.org. https://www.mindat.org/taxon-8623412.html
- ↑ Palaeozoic Plants from Central Shansi. (1927). China: Alexander Doweld.
- ↑ Wallerius, J. G. (1750). Mineralogie, oder mineralreich: von ihm eingeteilt und beschrieben. Germany: C.G. Nicolai.
- ↑ Seward, A. C. (2011). Fossil Plants: A Text-Book for Students of Botany and Geology. United Kingdom: Cambridge University Press.
- ↑ Geophytology: A Journal of Palaeobotany and Allied Sciences. (1971). India: Palaeobotanical Society..
- ↑ Cleal, C. J., & Thomas, B. A. (2018). Nomenclatural status of the palaeobotanical “artificial taxa” established in Brongniart’s 1822 “Classification” paper (journal-article). (Fossil Imprint), Fossil Imprint (Vols. 74–74, pp. 9–28). Praha. https://doi.org/10.2478/if-2018-0001
- ↑ Wang, Q. (2011, February). (1996) Proposal to conserve the name Carpolithus with that spelling (fossil spermatopsida). Retrieved December 18, 2024, from https://www.researchgate.net/publication/331030201_1996_Proposal_to_conserve_the_name_Carpolithus_with_that_spelling_fossil_Spermatopsida
- ↑ Fossil Plants: a Text-book for Students of Botany and Geology. Vol. Iii.. (n.d.). (n.p.): CUP Archive.
- ↑ Andrews, H. N. (1970). Index of Generic Names of Fossil Plants, 1820-1965. South Africa: U.S. Government Printing Office.
- ↑ Memoir. (1977). United States: The Society.
- ↑ Histoire Naturelle Eclaircie Dans Une de Ses Parties Principales, L'oryctologie, Qui Traite Des Terres, Des Pierres, Des Metaux, Des Mineraux Et Autyres Fossiles. (1755). France: Avec Approbations et privilege du Roy.