Kingena
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Kingena
''Kingena'' is an extinct genus of primarily Cretaceous-aged brachiopods of the family Kingenidae whose fossils are found in marine strata of Antarctica, Europe, and New Zealand. Early Paleocene-aged fossils from Denmark represent the youngest species. Taxonomy Nearctic members have been excluded from this genus by Owen in 1970 and instead represent a separate genus, ''Waconella''. Select species * ''Kingena blackmorei'' Owen, 1970 * ''Kingena concinna'' Owen, 1970 * ''Kingena elegans'' Owen, 1970 * ''Kingena limburgica'' Simon, 2005 * ''Kingena mesembrina'' (Etheridge, 1913) * ''Kingena pentangulata'' Woodward, 1833 * ''Kingena simiensis'' Waring, 1917 Sources

Terebratulida Prehistoric brachiopod genera Cretaceous brachiopods Paleogene brachiopods Cretaceous brachiopods of Europe Paleocene animals of Europe Extinct animals of Antarctica Cretaceous genus first appearances Maastrichtian genera Danian genera Paleocene genus extinctions {{brachiopod-stub ...
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Kingena Simiensis
''Kingena'' is an extinct genus of primarily Cretaceous-aged brachiopods of the family Kingenidae whose fossils are found in marine strata of Antarctica, Europe, and New Zealand. Early Paleocene-aged fossils from Denmark represent the youngest species. Taxonomy Nearctic members have been excluded from this genus by Owen in 1970 and instead represent a separate genus, '' Waconella''. Select species * ''Kingena blackmorei'' Owen, 1970 * '' Kingena concinna'' Owen, 1970 * '' Kingena elegans'' Owen, 1970 * ''Kingena limburgica ''Kingena'' is an extinct genus of primarily Cretaceous-aged brachiopods of the family Kingenidae whose fossils are found in marine strata of Antarctica, Europe, and New Zealand. Early Paleocene-aged fossils from Denmark represent the youngest s ...'' Simon, 2005 * '' Kingena mesembrina'' (Etheridge, 1913) * '' Kingena pentangulata'' Woodward, 1833 * '' Kingena simiensis'' Waring, 1917 Sources Terebratulida Prehistoric brachiopod genera ...
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Kingena Blackmorei
''Kingena'' is an extinct genus of primarily Cretaceous-aged brachiopods of the family Kingenidae whose fossils are found in marine strata of Antarctica, Europe, and New Zealand. Early Paleocene-aged fossils from Denmark represent the youngest species. Taxonomy Nearctic members have been excluded from this genus by Owen in 1970 and instead represent a separate genus, '' Waconella''. Select species * '' Kingena blackmorei'' Owen, 1970 * '' Kingena concinna'' Owen, 1970 * '' Kingena elegans'' Owen, 1970 * ''Kingena limburgica ''Kingena'' is an extinct genus of primarily Cretaceous-aged brachiopods of the family Kingenidae whose fossils are found in marine strata of Antarctica, Europe, and New Zealand. Early Paleocene-aged fossils from Denmark represent the youngest s ...'' Simon, 2005 * '' Kingena mesembrina'' (Etheridge, 1913) * '' Kingena pentangulata'' Woodward, 1833 * '' Kingena simiensis'' Waring, 1917 Sources Terebratulida Prehistoric brachiopod genera ...
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Kingena Pentangulata
''Kingena'' is an extinct genus of primarily Cretaceous-aged brachiopods of the family Kingenidae whose fossils are found in marine strata of Antarctica, Europe, and New Zealand. Early Paleocene-aged fossils from Denmark represent the youngest species. Taxonomy Nearctic members have been excluded from this genus by Owen in 1970 and instead represent a separate genus, '' Waconella''. Select species * ''Kingena blackmorei'' Owen, 1970 * '' Kingena concinna'' Owen, 1970 * '' Kingena elegans'' Owen, 1970 * ''Kingena limburgica'' Simon, 2005 * '' Kingena mesembrina'' (Etheridge, 1913) * '' Kingena pentangulata'' Woodward, 1833 * ''Kingena simiensis ''Kingena'' is an extinct genus of primarily Cretaceous-aged brachiopods of the family Kingenidae whose fossils are found in marine strata of Antarctica, Europe, and New Zealand. Early Paleocene-aged fossils from Denmark represent the yo ...'' Waring, 1917 Sources Terebratulida Prehistoric brachiopod genera ...
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Kingena Mesembrina
''Kingena'' is an extinct genus of primarily Cretaceous-aged brachiopods of the family Kingenidae whose fossils are found in marine strata of Antarctica, Europe, and New Zealand. Early Paleocene-aged fossils from Denmark represent the youngest species. Taxonomy Nearctic members have been excluded from this genus by Owen in 1970 and instead represent a separate genus, '' Waconella''. Select species * ''Kingena blackmorei'' Owen, 1970 * '' Kingena concinna'' Owen, 1970 * '' Kingena elegans'' Owen, 1970 * ''Kingena limburgica'' Simon, 2005 * '' Kingena mesembrina'' (Etheridge, 1913) * ''Kingena pentangulata'' Woodward, 1833 * ''Kingena simiensis ''Kingena'' is an extinct genus of primarily Cretaceous-aged brachiopods of the family Kingenidae whose fossils are found in marine strata of Antarctica, Europe, and New Zealand. Early Paleocene-aged fossils from Denmark represent the yo ...'' Waring, 1917 Sources Terebratulida Prehistoric brachiopod genera C ...
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Kingena Limburgica
''Kingena'' is an extinct genus of primarily Cretaceous-aged brachiopods of the family Kingenidae whose fossils are found in marine strata of Antarctica, Europe, and New Zealand. Early Paleocene-aged fossils from Denmark represent the youngest species. Taxonomy Nearctic members have been excluded from this genus by Owen in 1970 and instead represent a separate genus, ''Waconella''. Select species * ''Kingena blackmorei'' Owen, 1970 * ''Kingena concinna'' Owen, 1970 * ''Kingena elegans'' Owen, 1970 * ''Kingena limburgica'' Simon, 2005 * ''Kingena mesembrina'' (Etheridge, 1913) * ''Kingena pentangulata'' Woodward, 1833 * ''Kingena simiensis'' Waring, 1917 Sources

Terebratulida Prehistoric brachiopod genera Cretaceous brachiopods Paleogene brachiopods Cretaceous brachiopods of Europe Paleocene animals of Europe Extinct animals of Antarctica Cretaceous genus first appearances Maastrichtian genera Danian genera Paleocene genus extinctions {{brachiopod-stub ...
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Kingena Elegans
''Kingena'' is an extinct genus of primarily Cretaceous-aged brachiopods of the family Kingenidae whose fossils are found in marine strata of Antarctica, Europe, and New Zealand. Early Paleocene-aged fossils from Denmark represent the youngest species. Taxonomy Nearctic members have been excluded from this genus by Owen in 1970 and instead represent a separate genus, '' Waconella''. Select species * ''Kingena blackmorei'' Owen, 1970 * '' Kingena concinna'' Owen, 1970 * '' Kingena elegans'' Owen, 1970 * ''Kingena limburgica'' Simon, 2005 * ''Kingena mesembrina'' (Etheridge, 1913) * ''Kingena pentangulata'' Woodward, 1833 * ''Kingena simiensis ''Kingena'' is an extinct genus of primarily Cretaceous-aged brachiopods of the family Kingenidae whose fossils are found in marine strata of Antarctica, Europe, and New Zealand. Early Paleocene-aged fossils from Denmark represent the yo ...'' Waring, 1917 Sources Terebratulida Prehistoric brachiopod genera Cr ...
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Kingena Concinna
''Kingena'' is an extinct genus of primarily Cretaceous-aged brachiopods of the family Kingenidae whose fossils are found in marine strata of Antarctica, Europe, and New Zealand. Early Paleocene-aged fossils from Denmark represent the youngest species. Taxonomy Nearctic members have been excluded from this genus by Owen in 1970 and instead represent a separate genus, '' Waconella''. Select species * ''Kingena blackmorei'' Owen, 1970 * '' Kingena concinna'' Owen, 1970 * ''Kingena elegans'' Owen, 1970 * ''Kingena limburgica'' Simon, 2005 * ''Kingena mesembrina'' (Etheridge, 1913) * ''Kingena pentangulata'' Woodward, 1833 * ''Kingena simiensis ''Kingena'' is an extinct genus of primarily Cretaceous-aged brachiopods of the family Kingenidae whose fossils are found in marine strata of Antarctica, Europe, and New Zealand. Early Paleocene-aged fossils from Denmark represent the yo ...'' Waring, 1917 Sources Terebratulida Prehistoric brachiopod genera Cre ...
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Kingenidae
Kingenidae is a family of brachiopods belonging to the order Terebratulida Terebratulids are one of only three living orders of articulate brachiopods, the others being the Rhynchonellida and the Thecideida. Craniida and Lingulida include living brachiopods, but are inarticulates. The name, Terebratula, may be derived f .... Genera The following genera are included in Kingenidae: * '' Aldingia'' Thomson, 1916 * '' Belothyris'' Smirnova, 1960 * '' Dictyothyropsis'' Barczyk, 1969 * '' Dzirulina'' Nutsubidze, 1945 * '' Kingena'' Davidson, 1852 * '' Paraldingia'' Richardson, 1973 * '' Waconella'' Owen, 1970 * '' Zeuschneria'' Smirnova, 1975 * '' Zittelina'' Rollier, 1919 References {{Taxonbar, from=Q18548389 Brachiopods ...
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Cretaceous
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 b ...
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Cretaceous Genus First Appearances
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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Extinct Animals Of Antarctica
Extinction is the termination of a kind of organism or of a group of kinds ( taxon), usually a species. The moment of extinction is generally considered to be the death of the last individual of the species, although the capacity to breed and recover may have been lost before this point. Because a species' potential range may be very large, determining this moment is difficult, and is usually done retrospectively. This difficulty leads to phenomena such as Lazarus taxa, where a species presumed extinct abruptly "reappears" (typically in the fossil record) after a period of apparent absence. More than 99% of all species that ever lived on Earth, amounting to over five billion species, are estimated to have died out. It is estimated that there are currently around 8.7 million species of eukaryote globally, and possibly many times more if microorganisms, like bacteria, are included. Notable extinct animal species include non-avian dinosaurs, saber-toothed cats, do ...
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Paleocene Animals Of Europe
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 v ...
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