Puzosia
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Puzosia
''Puzosia'' is a genus of desmoceratid ammonites, and the type genus for the Puzosiinae, which lived during the middle part of the Cretaceous, from early Aptian to Maastrichtian (125.5 to 70.6 Ma). The generic name comes from the Serbian words "Puž" (snail) and "oce/ose" (axis), gaining its name from the shell's snail-like appearance. Subgenera and species * '' Puzosia (Anapuzosia)'' Matsumoto 1954 * '' Puzosia (Bhimaites)'' Matsumoto 1954 ** ''Puzosia (Bhimaites) bhima'' Stoliczka 1865 * '' Puzosia (Puzosia)'' Bayle 1878 ** ''Puzosia (Puzosia) mayoriana'' d'Orbigny 1841 ** ''Puzosia (Puzosia) planulatus'' Sowerby 1827 ** ''Puzosia alaskana'' Imlay 1960 ** ''Puzosia bistricta'' White 1887 ** ''Puzosia brasiliana'' Maury 1936 ** ''Puzosia crebrisulcata'' Kossmat 1898 ** ''Puzosia dilleri'' Anderson 1902 ** ''Puzosia garajauana'' Maury 1936 ** ''Puzosia lata'' Seitz 1931 ** ''Puzosia longmani'' Whitehouse 1926 ** ''Puzosia lytoceroides'' Haas 1952 ** ''Puzosia media'' Seitz 1 ...
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Puzosia (Puzosia)
''Puzosia'' is a genus of desmoceratid ammonites, and the type genus for the Puzosiinae, which lived during the middle part of the Cretaceous, from early Aptian to Maastrichtian (125.5 to 70.6 Ma). The generic name comes from the Serbian words "Puž" (snail) and "oce/ose" (axis), gaining its name from the shell's snail-like appearance. Subgenera and species * '' Puzosia (Anapuzosia)'' Matsumoto 1954 * '' Puzosia (Bhimaites)'' Matsumoto 1954 ** ''Puzosia (Bhimaites) bhima'' Stoliczka 1865 * '' Puzosia (Puzosia)'' Bayle 1878 ** ''Puzosia (Puzosia) mayoriana'' d'Orbigny 1841 ** ''Puzosia (Puzosia) planulatus'' Sowerby 1827 ** ''Puzosia alaskana'' Imlay 1960 ** ''Puzosia bistricta'' White 1887 ** ''Puzosia brasiliana'' Maury 1936 ** ''Puzosia crebrisulcata'' Kossmat 1898 ** ''Puzosia dilleri'' Anderson 1902 ** ''Puzosia garajauana'' Maury 1936 ** ''Puzosia lata'' Seitz 1931 ** ''Puzosia longmani'' Whitehouse 1926 ** ''Puzosia lytoceroides'' Haas 1952 ** ''Puzosia media'' Seitz 19 ...
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Puzosia (Anapuzosia)
''Puzosia'' is a genus of desmoceratid ammonites, and the type genus for the Puzosiinae, which lived during the middle part of the Cretaceous, from early Aptian to Maastrichtian (125.5 to 70.6 Ma). The generic name comes from the Serbian words "Puž" (snail) and "oce/ose" (axis), gaining its name from the shell's snail-like appearance. Subgenera and species * '' Puzosia (Anapuzosia)'' Matsumoto 1954 * '' Puzosia (Bhimaites)'' Matsumoto 1954 ** ''Puzosia (Bhimaites) bhima'' Stoliczka 1865 * ''Puzosia (Puzosia)'' Bayle 1878 ** ''Puzosia (Puzosia) mayoriana'' d'Orbigny 1841 ** ''Puzosia (Puzosia) planulatus'' Sowerby 1827 ** ''Puzosia alaskana'' Imlay 1960 ** ''Puzosia bistricta'' White 1887 ** ''Puzosia brasiliana'' Maury 1936 ** ''Puzosia crebrisulcata'' Kossmat 1898 ** ''Puzosia dilleri'' Anderson 1902 ** ''Puzosia garajauana'' Maury 1936 ** ''Puzosia lata'' Seitz 1931 ** ''Puzosia longmani'' Whitehouse 1926 ** ''Puzosia lytoceroides'' Haas 1952 ** ''Puzosia media'' Seitz 193 ...
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Puzosia Bhimaites Species Burmese Amber PNAS Fig2 A
''Puzosia'' is a genus of desmoceratid ammonites, and the type genus for the Puzosiinae, which lived during the middle part of the Cretaceous, from early Aptian to Maastrichtian (125.5 to 70.6 Ma). The generic name comes from the Serbian words "Puž" (snail) and "oce/ose" (axis), gaining its name from the shell's snail-like appearance. Subgenera and species * ''Puzosia (Anapuzosia)'' Matsumoto 1954 * '' Puzosia (Bhimaites)'' Matsumoto 1954 ** ''Puzosia (Bhimaites) bhima'' Stoliczka 1865 * ''Puzosia (Puzosia)'' Bayle 1878 ** ''Puzosia (Puzosia) mayoriana'' d'Orbigny 1841 ** ''Puzosia (Puzosia) planulatus'' Sowerby 1827 ** ''Puzosia alaskana'' Imlay 1960 ** ''Puzosia bistricta'' White 1887 ** ''Puzosia brasiliana'' Maury 1936 ** ''Puzosia crebrisulcata'' Kossmat 1898 ** ''Puzosia dilleri'' Anderson 1902 ** ''Puzosia garajauana'' Maury 1936 ** ''Puzosia lata'' Seitz 1931 ** ''Puzosia longmani'' Whitehouse 1926 ** ''Puzosia lytoceroides'' Haas 1952 ** ''Puzosia media'' Seitz 1931 ...
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Puzosia (Bhimaites)
''Puzosia'' (''Bhimaites'') is a subgenus of desmoceratid ammonites with a subinvolute, mostly smooth, high whorled shell with convex or flat sides and frequent constrictions on the venter. It is included in the subfamily Puzosiinae and has been found in Upper Albian and Cenomanian sediments in Angola, South Africa, and southern India. In 2019, a ''Bhimaites'' shell was found fossilized in a 99 million-year-old chunk of Burmese amber from Myanmar Myanmar, ; UK pronunciations: US pronunciations incl. . Note: Wikipedia's IPA conventions require indicating /r/ even in British English although only some British English speakers pronounce r at the end of syllables. As John C. Wells, Joh ..., marking the first known discovery of an ammonite preserved in amber. The ammonite's shell was presumably picked up and preserved after the resin fell off a tree and tumbled across the seashore. References ;Notes ;Bibliography *Arkell, et al., 1957. Mesozoic Ammonoidea; Treatise on In ...
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Burmese Amber
Burmese amber, also known as Burmite or Kachin amber, is amber from the Hukawng Valley in northern Myanmar. The amber is dated to around 100 million years ago, during the latest Albian to earliest Cenomanian ages of the mid-Cretaceous period. The amber is of significant palaeontological interest due to the diversity of flora and fauna contained as inclusions, particularly arthropods including insects and arachnids but also birds, lizards, snakes, frogs and fragmentary dinosaur remains. The amber has been known and commercially exploited since the first century AD, and has been known to science since the mid-nineteenth century. Research on the deposit has attracted controversy due to its alleged role in funding internal conflict in Myanmar and hazardous working conditions in the mines where it is collected. Geological context, depositional environment and age The amber is found within the Hukawng Basin, a large Cretaceous-Cenozoic sedimentary basin within northern Myanmar. The s ...
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Desmoceratidae
Desmoceratidae is a family belonging to the ammonite superfamily Desmoceratoidea. with and (1996), ''Mollusca 4 Revised , Cretaceous Ammonoidea'', vol. 4, in ''Treatise on Invertebrate Paleontology'', Part L (Roger L. Kaesler et el. eds.), Boulder, Colorado: The Geological Society of America & Lawrence, Kansas: University of Kansas Press, 69-71.Desmoceratidae
a
Paleobiology database
retrieved on July 8, 2012. They are an extinct group of , shelled
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Cretaceous Asia
The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of the entire Phanerozoic. The name is derived from the Latin ''creta'', "chalk", which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation ''Kreide''. The 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. The world was ice free, and forests extended to the poles. During this time, new groups of mammals and birds appeared. During the Early Cretaceous, flowering plants appeared and began to rapidly diversify, becoming the dominant group of plants across the Earth by the ...
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Cretaceous Africa
The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of the entire Phanerozoic. The name is derived from the Latin ''creta'', "chalk", which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation ''Kreide''. The 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. The world was ice free, and forests extended to the poles. During this time, new groups of mammals and birds appeared. During the Early Cretaceous, flowering plants appeared and began to rapidly diversify, becoming the dominant group of plants across the Earth by t ...
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Ammonites Of Asia
Ammonoids are a group of extinct marine mollusc animals in the subclass Ammonoidea of the class Cephalopoda. These molluscs, commonly referred to as ammonites, are more closely related to living coleoids (i.e., octopuses, squid and cuttlefish) than they are to shelled nautiloids such as the living ''Nautilus'' species. The earliest ammonites appeared during the Devonian, with the last species vanishing during the Cretaceous–Paleogene extinction event. Ammonites are excellent index fossils, and linking the rock layer in which a particular species or genus is found to specific geologic time periods is often possible. Their fossil shells usually take the form of planispirals, although some helically spiraled and nonspiraled forms (known as heteromorphs) have been found. The name "ammonite", from which the scientific term is derived, was inspired by the spiral shape of their fossilized shells, which somewhat resemble tightly coiled rams' horns. Pliny the Elder ( 79 AD near Pompe ...
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Ammonites Of Europe
Ammonoids are a group of extinct marine mollusc animals in the subclass Ammonoidea of the class Cephalopoda. These molluscs, commonly referred to as ammonites, are more closely related to living coleoids (i.e., octopuses, squid and cuttlefish) than they are to shelled nautiloids such as the living ''Nautilus'' species. The earliest ammonites appeared during the Devonian, with the last species vanishing during the Cretaceous–Paleogene extinction event. Ammonites are excellent index fossils, and linking the rock layer in which a particular species or genus is found to specific geologic time periods is often possible. Their fossil shells usually take the form of planispirals, although some helically spiraled and nonspiraled forms (known as heteromorphs) have been found. The name "ammonite", from which the scientific term is derived, was inspired by the spiral shape of their fossilized shells, which somewhat resemble tightly coiled rams' horns. Pliny the Elder ( 79 AD near Pompe ...
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Cretaceous Ammonites
The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of the entire Phanerozoic. The name is derived from the Latin ''creta'', "chalk", which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation ''Kreide''. The 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. The world was ice free, and forests extended to the poles. During this time, new groups of mammals and birds appeared. During the Early Cretaceous, flowering plants appeared and began to rapidly diversify, becoming the dominant group of plants across the Earth by the ...
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Cretaceous Europe
The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of the entire Phanerozoic. The name is derived from the Latin ''creta'', "chalk", which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation ''Kreide''. The 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. The world was ice free, and forests extended to the poles. During this time, new groups of mammals and birds appeared. During the Early Cretaceous, flowering plants appeared and began to rapidly diversify, becoming the dominant group of plants across the Earth by the ...
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