|
Carpolestes
''Carpolestes'' ("fruit thief" from Ancient Greek κᾰρπός (karpós), “fruit, grain” + λῃστής (lēistḗs), “thief”) is a genus of extinct primate-like mammals from the late Paleocene of North America. It first existed around 58 million years ago. The three species of ''Carpolestes'' appear to form a lineage, with the earliest occurring species, '' C. dubius'', ancestral to the type species, '' C. nigridens'', which, in turn, was ancestral to the most recently occurring species, '' C. simpsoni''. Carpolestes had flattened fingernails on its feet but with claws on its fingers. Morphologically it supports Robert Sussman's theorySussman, Robert “Primate origins and the Evolution of Angiosperms” in American Journal of Primatology Vol 23, No.4 (1991) pp209-223 of the co-evolution of tropical fruiting Angiosperms and early primates where Angiosperms provide nectar and fruits in return for dispersing the seed for tropical rainforest plants. It appears to ha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carpolestes Nigridens
''Carpolestes'' ("fruit thief" from Ancient Greek κᾰρπός (karpós), “fruit, grain” + λῃστής (lēistḗs), “thief”) is a genus of extinct primate-like mammals from the late Paleocene of North America. It first existed around 58 million years ago. The three species of ''Carpolestes'' appear to form a lineage, with the earliest occurring species, '' C. dubius'', ancestral to the type species, '' C. nigridens'', which, in turn, was ancestral to the most recently occurring species, '' C. simpsoni''. Carpolestes had flattened fingernails on its feet but with claws on its fingers. Morphologically it supports Robert Sussman's theorySussman, Robert “Primate origins and the Evolution of Angiosperms” in American Journal of Primatology Vol 23, No.4 (1991) pp209-223 of the co-evolution of tropical fruiting Angiosperms and early primates where Angiosperms provide nectar and fruits in return for dispersing the seed for tropical rainforest plants. It appears to have b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carpolestes Dubius
''Carpolestes'' ("fruit thief" from Ancient Greek κᾰρπός (karpós), “fruit, grain” + λῃστής (lēistḗs), “thief”) is a genus of extinct primate-like mammals from the late Paleocene of North America. It first existed around 58 million years ago. The three species of ''Carpolestes'' appear to form a lineage, with the earliest occurring species, '' C. dubius'', ancestral to the type species, '' C. nigridens'', which, in turn, was ancestral to the most recently occurring species, '' C. simpsoni''. Carpolestes had flattened fingernails on its feet but with claws on its fingers. Morphologically it supports Robert Sussman's theorySussman, Robert “Primate origins and the Evolution of Angiosperms” in American Journal of Primatology Vol 23, No.4 (1991) pp209-223 of the co-evolution of tropical fruiting Angiosperms and early primates where Angiosperms provide nectar and fruits in return for dispersing the seed for tropical rainforest plants. It appears to have b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carpolestes Twelvemilensis
''Carpolestes'' ("fruit thief" from Ancient Greek κᾰρπός (karpós), “fruit, grain” + λῃστής (lēistḗs), “thief”) is a genus of extinct primate-like mammals from the late Paleocene of North America. It first existed around 58 million years ago. The three species of ''Carpolestes'' appear to form a lineage, with the earliest occurring species, '' C. dubius'', ancestral to the type species, '' C. nigridens'', which, in turn, was ancestral to the most recently occurring species, '' C. simpsoni''. Carpolestes had flattened fingernails on its feet but with claws on its fingers. Morphologically it supports Robert Sussman's theorySussman, Robert “Primate origins and the Evolution of Angiosperms” in American Journal of Primatology Vol 23, No.4 (1991) pp209-223 of the co-evolution of tropical fruiting Angiosperms and early primates where Angiosperms provide nectar and fruits in return for dispersing the seed for tropical rainforest plants. It appears to have b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carpolestes Simpsoni
''Carpolestes simpsoni'' is an extinct species of Plesiadapiformes, which is one of the earliest primate-like mammals appearing in the fossil record during the late Paleocene. ''C. simpsoni'' had grasping digits but no forward-facing eyes. Weighing about 100 grams, ''C. simpsoni'' appeared adapted for an arboreal habitat. One large, nail Nail or Nails may refer to: In biology * Nail (anatomy), toughened protective protein-keratin (known as alpha-keratin, also found in hair) at the end of an animal digit, such as fingernail * Nail (beak), a plate of hard horny tissue at the tip ...-tipped toe opposed other toes, allowing a firm grip on branches. Like other species of '' Carpolestes'', the dental morphology of ''C. simpsoni'' is specially adapted to eating fruit, seeds, and invertebrates. References External links Mikko's Phylogeny Archive Plesiadapiformes Paleocene mammals Prehistoric mammals of North America {{paleo-mammal-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clarkforkian
The Clarkforkian North American Stage, on the geologic timescale, is the North American faunal stage according to the North American Land Mammal Ages chronology (NALMA), typically set from 56,800,000 to 55,400,000 years BP lasting . Considered to be within the Paleocene, more specifically the Late Paleocene, the Clarkforkian shares its upper boundary with the Thanetian. The Clarkforkian is preceded by the Tiffanian and followed by the Wasatchian NALMA stages. Substages It is considered to contain the following substages: *Cf3: (shares the upper boundary) and lower boundary source of the base of Clarkforkian (approximate) and upper boundary source of the base of the Ypresian (approximate). *Cf2: Is the lower boundary source of the base of the Clarkforkian (approximate) *Cf1: Upper boundary source of the base of the Ypresian (approximate) Fauna Notable mammals Multituberculata - non-therian mammals * '' Ectypodus'', neoplagiaulacid multituberculate Metatheria - marsupi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paleocene
The Paleocene, ( ) or Palaeocene, is a geological epoch (geology), epoch that lasted from about 66 to 56 mya (unit), million years ago (mya). It is the first epoch of the Paleogene Period (geology), Period in the modern Cenozoic Era (geology), Era. The name is a combination of the Ancient Greek ''palaiós'' meaning "old" and the Eocene Epoch (which succeeds the Paleocene), translating to "the old part of the Eocene". The epoch is bracketed by two major events in Earth's history. The K–Pg extinction event, brought on by Chicxulub impact, an asteroid impact and possibly volcanism, marked the beginning of the Paleocene and killed off 75% of living species, most famously the non-avian dinosaurs. The end of the epoch was marked by the Paleocene–Eocene Thermal Maximum (PETM), which was a major climatic event wherein about 2,500–4,500 gigatons of carbon were released into the atmosphere and ocean systems, causing a spike in global temperatures and ocean acidification. In the Pal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Prehistoric Placental Genera
Prehistory, also known as pre-literary history, is the period of human history between the use of the first stone tools by hominins 3.3 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 5000 years ago. It took thousands of years for writing systems to be widely adopted, with writing spreading to almost all cultures by the 19th century. The end of prehistory therefore came at very different times in different places, and the term is less often used in discussing societies where prehistory ended relatively recently. In the early Bronze Age, Sumer in Mesopotamia, the Indus Valley Civilisation, and ancient Egypt were the first civilizations to develop their own scripts and to keep historical records, with their neighbors following. Most other civilizations reached the end of prehistory during the following Iron Age. T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paleontology In Wyoming
Paleontology in Wyoming includes research into the prehistoric life of the U.S. state of Wyoming as well as investigations conducted by Wyomingite researchers and institutions into ancient life occurring elsewhere. The fossil record of the US state of Wyoming spans from the Precambrian to recent deposits. Many fossil sites are spread throughout the state. Wyoming is such a spectacular source of fossils that author Marian Murray noted in 1974 that " en today, it is the expected thing that any great museum will send its representatives to Wyoming as often as possible." Murray has also written that nearly every major vertebrate paleontologist in United States history has collected fossils in Wyoming. Wyoming is a major source of dinosaur fossils. Wyoming's dinosaur fossils are curated by museums located all over the planet. During the Precambrian, Wyoming was covered by a shallow sea inhabited by stromatolite-forming bacteria. This sea remained in place during the early Paleozoic era ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paleontology In Montana
Paleontology in Montana refers to paleontological research occurring within or conducted by people from the U.S. state of Montana. The fossil record in Montana stretches all the way back to the Precambrian. During the Late Precambrian, western Montana was covered by a warm, shallow sea where local bacteria formed stromatolites and bottom-dwelling marine life left tracks on the sediment that would later fossilize. This sea remained in place during the early Paleozoic, although withdrew during the Silurian and Early Devonian, leaving a gap in the local rock record until its return. This sea was home to creatures including brachiopods, conodonts, crinoids, fish, and trilobites. During the Carboniferous the state was home to an unusual cartilaginous fish fauna. Later in the Paleozoic the sea began to withdraw, but with a brief return during the Permian. During the Triassic Montana was again covered in a sea whose inhabitants are the state's only known fossils from this time. Much of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fossils Of The United States
A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved in amber, hair, petrified wood and DNA remnants. The totality of fossils is known as the ''fossil record''. Paleontology is the study of fossils: their age, method of formation, and evolutionary significance. Specimens are usually considered to be fossils if they are over 10,000 years old. The oldest fossils are around 3.48 billion years old to 4.1 billion years old. Early edition, published online before print. The observation in the 19th century that certain fossils were associated with certain rock strata led to the recognition of a geological timescale and the relative ages of different fossils. The development of radiometric dating techniques in the early 20th century allowed scientists to quantitatively measure the absolute ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paleocene Mammals Of North America
The Paleocene, ( ) or Palaeocene, is a geological epoch that lasted from about 66 to 56 million years ago (mya). It is the first epoch of the Paleogene Period in the modern Cenozoic Era. The name is a combination of the Ancient Greek ''palaiós'' meaning "old" and the Eocene Epoch (which succeeds the Paleocene), translating to "the old part of the Eocene". The epoch is bracketed by two major events in Earth's history. The K–Pg extinction event, brought on by an asteroid impact and possibly volcanism, marked the beginning of the Paleocene and killed off 75% of living species, most famously the non-avian dinosaurs. The end of the epoch was marked by the Paleocene–Eocene Thermal Maximum (PETM), which was a major climatic event wherein about 2,500–4,500 gigatons of carbon were released into the atmosphere and ocean systems, causing a spike in global temperatures and ocean acidification. In the Paleocene, the continents of the Northern Hemisphere were still connected via so ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wasatchian
The Wasatchian North American Stage on the geologic timescale is the North American faunal stage according to the North American Land Mammal Ages chronology (NALMA), typically set from 55,400,000 to 50,300,000 years BP lasting . It is usually considered to be within the Eocene, more specifically the Early Eocene. The Wasatchian is preceded by the Clarkforkian and followed by the Bridgerian NALMA stages. Definition The age is named after the Wasatch Formation, a highly fossiliferous stratigraphic unit stretching across six of the United States from Idaho and Montana in the north through Utah and Wyoming to Colorado and New Mexico ) , population_demonym = New Mexican ( es, Neomexicano, Neomejicano, Nuevo Mexicano) , seat = Santa Fe , LargestCity = Albuquerque , LargestMetro = Tiguex , OfficialLang = None , Languages = English, Spanish ( New Mexican), Navajo, Ker ... in the south. Substages The Wasatchian is considered to contain the following substages: * Sand ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
