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Statements

Subject Item
dbr:South_American_land_mammal_age
rdfs:label
Edad mamífero de América del Sur South American land mammal age South American Land Mammal Age
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Een South American Land Mammal Age (afgekort: SALMA) is een stratigrafische biozone, een correleerbare zone in lagen sedimentaire gesteente, die een bepaalde assemblage van fossielen van Zuid-Amerikaanse zoogdieren bevat. Hoewel biozones als biostratigrafische eenheden per definitie niet overal precies dezelfde ouderdom hoeven te hebben, worden SALMA's in de praktijk vaak als tijdschaal gebruikt. Het Cenozoïcum van Zuid-Amerika wordt dan in deze tijdsnedes (Engels: ages) of etages (Engels: stages) opgedeeld. Gebruikelijker is het de geologische tijdschaal in te delen in de tijsnedes van de ICS. Una edad mamífero de América del Sur (precedida por el código SALMA, del idioma inglés South American land mammal ages) es una división establecida para definir una escala biocronológica para y mediante la fauna de mamíferos sudamericanos, desde 64,5 Ma, durante el Paleógeno, hasta el Holoceno.​ Estos períodos se denominan edades, subedades, o intervalos entre ellas, así como también son llamadas «unidades bioestratigráficas» o «biozonas de asociación», y se establecieron utilizando nombres de las localidades geográficas donde los materiales fósiles que definen el periodo fueron obtenidos, caracterizando sus estratotipos, y definiendo sus taxones tipo.​​ The South American land mammal ages (SALMA) establish a geologic timescale for prehistoric South American fauna beginning 64.5 Ma during the Paleocene and continuing through to the Late Pleistocene (0.011 Ma). These periods are referred to as ages, stages, or intervals and were established using geographic place names where fossil materials where obtained.
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Albian
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4.73364E14 3.471336E15 Locations of SALMA type localities 14 The Drake Passage, separating South America from Antarctica, was formed since the latest Eocene
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2018-09-04 2013-12-12 2017-08-06 2018-08-10
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The paleogeographical history of South America, with the separation from Africa and Antarctica
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Earth2014 visualisation Antarctica.jpg Blakey 105Ma - COL.jpg Drake Passage - Lambert Azimuthal projection.png
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n175:21722-118331-1-PB.pdf n128:clyde_et_al._2014.pdf n123:(01)Zurita.pdf n71:347
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0001-05-14
dbo:abstract
The South American land mammal ages (SALMA) establish a geologic timescale for prehistoric South American fauna beginning 64.5 Ma during the Paleocene and continuing through to the Late Pleistocene (0.011 Ma). These periods are referred to as ages, stages, or intervals and were established using geographic place names where fossil materials where obtained. The basic unit of measure is the first/last boundary statement. This shows that the first appearance event of one taxon is known to predate the last appearance event of another. If two taxa are found in the same fossil quarry or at the same stratigraphic horizon, then their age-range zones overlap. Een South American Land Mammal Age (afgekort: SALMA) is een stratigrafische biozone, een correleerbare zone in lagen sedimentaire gesteente, die een bepaalde assemblage van fossielen van Zuid-Amerikaanse zoogdieren bevat. Hoewel biozones als biostratigrafische eenheden per definitie niet overal precies dezelfde ouderdom hoeven te hebben, worden SALMA's in de praktijk vaak als tijdschaal gebruikt. Het Cenozoïcum van Zuid-Amerika wordt dan in deze tijdsnedes (Engels: ages) of etages (Engels: stages) opgedeeld. Gebruikelijker is het de geologische tijdschaal in te delen in de tijsnedes van de ICS. Una edad mamífero de América del Sur (precedida por el código SALMA, del idioma inglés South American land mammal ages) es una división establecida para definir una escala biocronológica para y mediante la fauna de mamíferos sudamericanos, desde 64,5 Ma, durante el Paleógeno, hasta el Holoceno.​ Estos períodos se denominan edades, subedades, o intervalos entre ellas, así como también son llamadas «unidades bioestratigráficas» o «biozonas de asociación», y se establecieron utilizando nombres de las localidades geográficas donde los materiales fósiles que definen el periodo fueron obtenidos, caracterizando sus estratotipos, y definiendo sus taxones tipo.​​
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