EdenteV2, PascalFrancis, Corpus, bibRecord, 000197

Nouveaux paresseux terrestres (Mammalia, Xenarthra, Mylodontidae) du Néogène de l'Altiplano bolivien

Identifieur interne : 000197 ( PascalFrancis/Corpus ); précédent : 000196; suivant : 000198

Nouveaux paresseux terrestres (Mammalia, Xenarthra, Mylodontidae) du Néogène de l'Altiplano bolivien

Auteurs : Pierre-Antoine Saint-Andre ; François Pujos ; Cástor Cartelle ; Gerardo De Iuliis ; Timothy J. Gaudin ; H. Gregory Mcdonald ; Bernardino Mamani Quispe

Source :

Geodiversitas [ 1280-9659 ] ; 2010.

RBID : Pascal:10-0319855

Descripteurs français

Pascal (Inist)
- Mammalia, Xenarthra, Néogène, Tuf volcanique, Miocène, Pliocène moyen, Anatomie, Taxon nouveau, Miocène sup, Pliocène inf, Biostratigraphie, Mylodontidae, Pleurolestodon dalenzae, Simomylodon uccasamamensis, Altiplano, Bolivie.

English descriptors

KwdEn :
- Altiplano, Bolivia, Mammalia, Miocene, Neogene, Xenarthra, anatomy, biostratigraphy, lower Pliocene, middle Pliocene, new taxa, tuff, upper Miocene.

Abstract

Two new Mylodontinae (Xenarthra, Tardigrada, Mylodontoidea) from the Bolivian Altiplano are described. One of them, Pleurolestodon dalenzae n. sp., was discovered a few meters below a volcanic tuff, Toba 76, that may be used as a reference stratigraphic level and is dated at 5.4 Ma; it could be Huayquerian (late Miocene) or at the Huayquerian-Montehermosan boundary in age. The other taxon, Simomylodon uccasamamensis n. gen., n. sp., was recovered from many localities of a horizon bounded below by Toba 76 and above by another volcanic level, the 2.8 Ma Ayo Ayo tuff; its age is Montehermosan-Chapadmalalan (early and middle Pliocene). Analysis of these taxa indicates that they are Mylodontidae more closely related to Glossotherium, Glossotheridium, Kiyumylodon and Paramylodon than to Lestodon or Thinobadistes.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

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A11	`01`	`1`		`@1 SAINT-ANDRE (Pierre-Antoine) @9 rép.`
A11	`02`	`1`		`@1 PUJOS (François)`
A11	`03`	`1`		`@1 CARTELLE (Cástor)`
A11	`04`	`1`		`@1 DE IULIIS (Gerardo)`
A11	`05`	`1`		`@1 GAUDIN (Timothy J.)`
A11	`06`	`1`		`@1 MCDONALD (H. Gregory)`
A11	`07`	`1`		`@1 MAMANI QUISPE (Bernardino)`
A14	`01`			`@1 Dpto de Geología y Paleontología, Instituto Argentino de Nivologia, Glaciologia y Ciencias Ambientales (IANIGLA), CCT-CONICET-Mendoza, Avda. Ruiz Leal s/n, Parque Gral. San Martín @2 5500 Mendoza @3 ARG @Z 2 aut.`
A14	`02`			`@1 PUC Minas, Avenida Dom José Gaspar, 290 Coração Eucarístico @2 Belo Horizonte, Minas Gerais @3 BRA @Z 3 aut.`
A14	`03`			`@1 Faculty of Community Services and Health Sciences, George Brown College of Applied Arts and Technology, 200 King Street East @2 Toronto, Ontario, M5A 1J5 @3 CAN @Z 4 aut.`
A14	`04`			`@1 Department of Biological and Environmental Sciences (Department 2653), University of Tennessee at Chattanooga, 615 McCallie Avenue @2 Chattanooga, TN 37403-2598 @3 USA @Z 5 aut.`
A14	`05`			`@1 Park Museum Management Program, National Park Service, 1201 Oakridge Drive, Suite 150 @2 Fort Collins, Colorado 80525 @3 USA @Z 6 aut.`
A14	`06`			`@1 Departamento de Paleontología, Museo Nacional de Historia Natural, Calle 26 s/n @2 Cota Cota, La Paz @3 BOL @Z 7 aut.`
A20				`@1 255-306`
A21				`@1 2010`
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A68	`01`	`1`	`ENG`	`@1 New ground sloths (Mammalia, Xenarthra, Mylodontidae) from the Neogene of the Bolivian Altiplano`
C01	`01`		`ENG`	@0 Two new Mylodontinae (Xenarthra, Tardigrada, Mylodontoidea) from the Bolivian Altiplano are described. One of them, Pleurolestodon dalenzae n. sp., was discovered a few meters below a volcanic tuff, Toba 76, that may be used as a reference stratigraphic level and is dated at 5.4 Ma; it could be Huayquerian (late Miocene) or at the Huayquerian-Montehermosan boundary in age. The other taxon, Simomylodon uccasamamensis n. gen., n. sp., was recovered from many localities of a horizon bounded below by Toba 76 and above by another volcanic level, the 2.8 Ma Ayo Ayo tuff; its age is Montehermosan-Chapadmalalan (early and middle Pliocene). Analysis of these taxa indicates that they are Mylodontidae more closely related to Glossotherium, Glossotheridium, Kiyumylodon and Paramylodon than to Lestodon or Thinobadistes.
C02	`01`	`2`		`@0 001E01Q04`
C02	`02`	`2`		`@0 001E01I`
C02	`03`	`2`		`@0 227A04`
C02	`04`	`2`		`@0 224A`
C03	`01`	`2`	`FRE`	`@0 Mammalia @2 NY @5 01`
C03	`01`	`2`	`ENG`	`@0 Mammalia @2 NY @5 01`
C03	`01`	`2`	`SPA`	`@0 Mammalia @2 NY @5 01`
C03	`02`	`2`	`FRE`	`@0 Xenarthra @2 NY @5 02`
C03	`02`	`2`	`ENG`	`@0 Xenarthra @2 NY @5 02`
C03	`02`	`2`	`SPA`	`@0 Xenarthra @2 NY @5 02`
C03	`03`	`2`	`FRE`	`@0 Néogène @2 NX @5 03`
C03	`03`	`2`	`ENG`	`@0 Neogene @2 NX @5 03`
C03	`03`	`2`	`SPA`	`@0 Neógeno @2 NX @5 03`
C03	`04`	`2`	`FRE`	`@0 Tuf volcanique @2 NV @5 04`
C03	`04`	`2`	`ENG`	`@0 tuff @2 NV @5 04`
C03	`04`	`2`	`SPA`	`@0 Toba volcánica @2 NV @5 04`
C03	`05`	`2`	`FRE`	`@0 Miocène @2 NX @5 05`
C03	`05`	`2`	`ENG`	`@0 Miocene @2 NX @5 05`
C03	`05`	`2`	`SPA`	`@0 Mioceno @2 NX @5 05`
C03	`06`	`2`	`FRE`	`@0 Pliocène moyen @2 NX @5 06`
C03	`06`	`2`	`ENG`	`@0 middle Pliocene @2 NX @5 06`
C03	`06`	`2`	`SPA`	`@0 Plioceno medio @2 NX @5 06`
C03	`07`	`2`	`FRE`	`@0 Anatomie @5 07`
C03	`07`	`2`	`ENG`	`@0 anatomy @5 07`
C03	`07`	`2`	`SPA`	`@0 Anatomía @5 07`
C03	`08`	`2`	`FRE`	`@0 Taxon nouveau @5 08`
C03	`08`	`2`	`ENG`	`@0 new taxa @5 08`
C03	`08`	`2`	`SPA`	`@0 Nuevo taxón @5 08`
C03	`09`	`2`	`FRE`	`@0 Miocène sup @2 NX @5 09`
C03	`09`	`2`	`ENG`	`@0 upper Miocene @2 NX @5 09`
C03	`09`	`2`	`SPA`	`@0 Mioceno sup @2 NX @5 09`
C03	`10`	`2`	`FRE`	`@0 Pliocène inf @2 NX @5 10`
C03	`10`	`2`	`ENG`	`@0 lower Pliocene @2 NX @5 10`
C03	`10`	`2`	`SPA`	`@0 Plioceno inf @2 NX @5 10`
C03	`11`	`2`	`FRE`	`@0 Biostratigraphie @5 11`
C03	`11`	`2`	`ENG`	`@0 biostratigraphy @5 11`
C03	`11`	`2`	`SPA`	`@0 Bioestratigrafía @5 11`
C03	`12`	`2`	`FRE`	`@0 Mylodontidae @4 INC @5 52`
C03	`13`	`2`	`FRE`	`@0 Pleurolestodon dalenzae @4 INC @5 53`
C03	`14`	`2`	`FRE`	`@0 Simomylodon uccasamamensis @4 INC @5 54`
C03	`15`	`2`	`FRE`	`@0 Altiplano @2 NG @5 61`
C03	`15`	`2`	`ENG`	`@0 Altiplano @2 NG @5 61`
C03	`16`	`2`	`FRE`	`@0 Bolivie @2 NG @5 62`
C03	`16`	`2`	`ENG`	`@0 Bolivia @2 NG @5 62`
C03	`16`	`2`	`SPA`	`@0 Bolivia @2 NG @5 62`
C07	`01`	`2`	`FRE`	`@0 Tetrapoda @2 NY`
C07	`01`	`2`	`ENG`	`@0 Tetrapoda @2 NY`
C07	`01`	`2`	`SPA`	`@0 Tetrapoda @2 NY`
C07	`02`	`2`	`FRE`	`@0 Vertebrata @2 NY`
C07	`02`	`2`	`ENG`	`@0 Vertebrata @2 NY`
C07	`02`	`2`	`SPA`	`@0 Vertebrata @2 NY`
C07	`03`	`2`	`FRE`	`@0 Chordata`
C07	`03`	`2`	`ENG`	`@0 Chordata`
C07	`03`	`2`	`SPA`	`@0 Chordata`
C07	`04`	`2`	`FRE`	`@0 Edentata @2 NY`
C07	`04`	`2`	`ENG`	`@0 Edentata @2 NY`
C07	`04`	`2`	`SPA`	`@0 Edentata @2 NY`
C07	`05`	`2`	`FRE`	`@0 Eutheria @2 NY`
C07	`05`	`2`	`ENG`	`@0 Eutheria @2 NY`
C07	`06`	`2`	`FRE`	`@0 Theria @2 NY`
C07	`06`	`2`	`ENG`	`@0 Theria @2 NY`
C07	`07`	`2`	`FRE`	`@0 Tertiaire sup @2 NX`
C07	`07`	`2`	`ENG`	`@0 upper Tertiary @2 NX`
C07	`08`	`2`	`FRE`	`@0 Tertiaire @2 NX`
C07	`08`	`2`	`ENG`	`@0 Tertiary @2 NX`
C07	`08`	`2`	`SPA`	`@0 Terciario @2 NX`
C07	`09`	`2`	`FRE`	`@0 Cénozoïque @2 NX`
C07	`09`	`2`	`ENG`	`@0 Cenozoic @2 NX`
C07	`09`	`2`	`SPA`	`@0 Cenozoico @2 NX`
C07	`10`	`2`	`FRE`	`@0 Phanérozoïque @2 NX`
C07	`10`	`2`	`ENG`	`@0 Phanerozoic @2 NX`
C07	`10`	`2`	`SPA`	`@0 Fanerozoico @2 NX`
C07	`11`	`2`	`FRE`	`@0 Pyroclastite @2 NV`
C07	`11`	`2`	`ENG`	`@0 pyroclastics @2 NV`
C07	`12`	`2`	`FRE`	`@0 Roche volcanique @2 NV`
C07	`12`	`2`	`ENG`	`@0 volcanic rocks @2 NV`
C07	`12`	`2`	`SPA`	`@0 Roca volcánica @2 NV`
C07	`13`	`2`	`FRE`	`@0 Roche ignée @2 NV`
C07	`13`	`2`	`ENG`	`@0 igneous rocks @2 NV`
C07	`13`	`2`	`SPA`	`@0 Roca ignea @2 NV`
C07	`14`	`2`	`FRE`	`@0 Pliocène @2 NX`
C07	`14`	`2`	`ENG`	`@0 Pliocene @2 NX`
C07	`14`	`2`	`SPA`	`@0 Plioceno @2 NX`
C07	`15`	`2`	`FRE`	`@0 Andes @2 NG`
C07	`15`	`2`	`ENG`	`@0 Andes @2 NG`
C07	`15`	`2`	`SPA`	`@0 Andes @2 NG`
C07	`16`	`2`	`FRE`	`@0 Amérique du Sud @2 564`
C07	`16`	`2`	`ENG`	`@0 South America @2 564`
C07	`16`	`2`	`SPA`	`@0 America del sur @2 564`
N21				`@1 200`

Format Inist (serveur)

NO :	PASCAL 10-0319855 INIST
FT :	Nouveaux paresseux terrestres (Mammalia, Xenarthra, Mylodontidae) du Néogène de l'Altiplano bolivien
ET :	(New ground sloths (Mammalia, Xenarthra, Mylodontidae) from the Neogene of the Bolivian Altiplano)
AU :	SAINT-ANDRE (Pierre-Antoine); PUJOS (François); CARTELLE (Cástor); DE IULIIS (Gerardo); GAUDIN (Timothy J.); MCDONALD (H. Gregory); MAMANI QUISPE (Bernardino)
AF :	Dpto de Geología y Paleontología, Instituto Argentino de Nivologia, Glaciologia y Ciencias Ambientales (IANIGLA), CCT-CONICET-Mendoza, Avda. Ruiz Leal s/n, Parque Gral. San Martín/5500 Mendoza/Argentine (2 aut.); PUC Minas, Avenida Dom José Gaspar, 290 Coração Eucarístico/Belo Horizonte, Minas Gerais/Brésil (3 aut.); Faculty of Community Services and Health Sciences, George Brown College of Applied Arts and Technology, 200 King Street East/Toronto, Ontario, M5A 1J5/Canada (4 aut.); Department of Biological and Environmental Sciences (Department 2653), University of Tennessee at Chattanooga, 615 McCallie Avenue/Chattanooga, TN 37403-2598/Etats-Unis (5 aut.); Park Museum Management Program, National Park Service, 1201 Oakridge Drive, Suite 150/Fort Collins, Colorado 80525/Etats-Unis (6 aut.); Departamento de Paleontología, Museo Nacional de Historia Natural, Calle 26 s/n/Cota Cota, La Paz/Bolivie (7 aut.)
DT :	Publication en série; Niveau analytique
SO :	Geodiversitas; ISSN 1280-9659; France; Da. 2010; Vol. 32; No. 2; Pp. 255-306; Abs. anglais; Bibl. 2 p.1/4
LA :	Français
EA :	Two new Mylodontinae (Xenarthra, Tardigrada, Mylodontoidea) from the Bolivian Altiplano are described. One of them, Pleurolestodon dalenzae n. sp., was discovered a few meters below a volcanic tuff, Toba 76, that may be used as a reference stratigraphic level and is dated at 5.4 Ma; it could be Huayquerian (late Miocene) or at the Huayquerian-Montehermosan boundary in age. The other taxon, Simomylodon uccasamamensis n. gen., n. sp., was recovered from many localities of a horizon bounded below by Toba 76 and above by another volcanic level, the 2.8 Ma Ayo Ayo tuff; its age is Montehermosan-Chapadmalalan (early and middle Pliocene). Analysis of these taxa indicates that they are Mylodontidae more closely related to Glossotherium, Glossotheridium, Kiyumylodon and Paramylodon than to Lestodon or Thinobadistes.
CC :	001E01Q04; 001E01I; 227A04; 224A
FD :	Mammalia; Xenarthra; Néogène; Tuf volcanique; Miocène; Pliocène moyen; Anatomie; Taxon nouveau; Miocène sup; Pliocène inf; Biostratigraphie; Mylodontidae; Pleurolestodon dalenzae; Simomylodon uccasamamensis; Altiplano; Bolivie
FG :	Tetrapoda; Vertebrata; Chordata; Edentata; Eutheria; Theria; Tertiaire sup; Tertiaire; Cénozoïque; Phanérozoïque; Pyroclastite; Roche volcanique; Roche ignée; Pliocène; Andes; Amérique du Sud
ED :	Mammalia; Xenarthra; Neogene; tuff; Miocene; middle Pliocene; anatomy; new taxa; upper Miocene; lower Pliocene; biostratigraphy; Altiplano; Bolivia
EG :	Tetrapoda; Vertebrata; Chordata; Edentata; Eutheria; Theria; upper Tertiary; Tertiary; Cenozoic; Phanerozoic; pyroclastics; volcanic rocks; igneous rocks; Pliocene; Andes; South America
SD :	Mammalia; Xenarthra; Neógeno; Toba volcánica; Mioceno; Plioceno medio; Anatomía; Nuevo taxón; Mioceno sup; Plioceno inf; Bioestratigrafía; Bolivia
LO :	INIST-801C.354000180727780040
ID :	10-0319855

Links to Exploration step

Pascal:10-0319855

Le document en format XML

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<author><name sortKey="Mamani Quispe, Bernardino" sort="Mamani Quispe, Bernardino" uniqKey="Mamani Quispe B" first="Bernardino" last="Mamani Quispe">Bernardino Mamani Quispe</name>
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<sourceDesc><biblStruct><analytic><title xml:lang="fr" level="a">Nouveaux paresseux terrestres (Mammalia, Xenarthra, Mylodontidae) du Néogène de l'Altiplano bolivien</title>
<author><name sortKey="Saint Andre, Pierre Antoine" sort="Saint Andre, Pierre Antoine" uniqKey="Saint Andre P" first="Pierre-Antoine" last="Saint-Andre">Pierre-Antoine Saint-Andre</name>
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<author><name sortKey="Pujos, Francois" sort="Pujos, Francois" uniqKey="Pujos F" first="François" last="Pujos">François Pujos</name>
<affiliation><inist:fA14 i1="01"><s1>Dpto de Geología y Paleontología, Instituto Argentino de Nivologia, Glaciologia y Ciencias Ambientales (IANIGLA), CCT-CONICET-Mendoza, Avda. Ruiz Leal s/n, Parque Gral. San Martín</s1>
<s2>5500 Mendoza</s2>
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<author><name sortKey="Cartelle, Castor" sort="Cartelle, Castor" uniqKey="Cartelle C" first="Cástor" last="Cartelle">Cástor Cartelle</name>
<affiliation><inist:fA14 i1="02"><s1>PUC Minas, Avenida Dom José Gaspar, 290 Coração Eucarístico</s1>
<s2>Belo Horizonte, Minas Gerais</s2>
<s3>BRA</s3>
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<author><name sortKey="De Iuliis, Gerardo" sort="De Iuliis, Gerardo" uniqKey="De Iuliis G" first="Gerardo" last="De Iuliis">Gerardo De Iuliis</name>
<affiliation><inist:fA14 i1="03"><s1>Faculty of Community Services and Health Sciences, George Brown College of Applied Arts and Technology, 200 King Street East</s1>
<s2>Toronto, Ontario, M5A 1J5</s2>
<s3>CAN</s3>
<sZ>4 aut.</sZ>
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<author><name sortKey="Gaudin, Timothy J" sort="Gaudin, Timothy J" uniqKey="Gaudin T" first="Timothy J." last="Gaudin">Timothy J. Gaudin</name>
<affiliation><inist:fA14 i1="04"><s1>Department of Biological and Environmental Sciences (Department 2653), University of Tennessee at Chattanooga, 615 McCallie Avenue</s1>
<s2>Chattanooga, TN 37403-2598</s2>
<s3>USA</s3>
<sZ>5 aut.</sZ>
</inist:fA14>
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</author>
<author><name sortKey="Mcdonald, H Gregory" sort="Mcdonald, H Gregory" uniqKey="Mcdonald H" first="H. Gregory" last="Mcdonald">H. Gregory Mcdonald</name>
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<s2>Fort Collins, Colorado 80525</s2>
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<author><name sortKey="Mamani Quispe, Bernardino" sort="Mamani Quispe, Bernardino" uniqKey="Mamani Quispe B" first="Bernardino" last="Mamani Quispe">Bernardino Mamani Quispe</name>
<affiliation><inist:fA14 i1="06"><s1>Departamento de Paleontología, Museo Nacional de Historia Natural, Calle 26 s/n</s1>
<s2>Cota Cota, La Paz</s2>
<s3>BOL</s3>
<sZ>7 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
</analytic>
<series><title level="j" type="main">Geodiversitas</title>
<title level="j" type="abbreviated">Geodiversitas</title>
<idno type="ISSN">1280-9659</idno>
<imprint><date when="2010">2010</date>
</imprint>
</series>
</biblStruct>
</sourceDesc>
<seriesStmt><title level="j" type="main">Geodiversitas</title>
<title level="j" type="abbreviated">Geodiversitas</title>
<idno type="ISSN">1280-9659</idno>
</seriesStmt>
</fileDesc>
<profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Altiplano</term>
<term>Bolivia</term>
<term>Mammalia</term>
<term>Miocene</term>
<term>Neogene</term>
<term>Xenarthra</term>
<term>anatomy</term>
<term>biostratigraphy</term>
<term>lower Pliocene</term>
<term>middle Pliocene</term>
<term>new taxa</term>
<term>tuff</term>
<term>upper Miocene</term>
</keywords>
<keywords scheme="Pascal" xml:lang="fr"><term>Mammalia</term>
<term>Xenarthra</term>
<term>Néogène</term>
<term>Tuf volcanique</term>
<term>Miocène</term>
<term>Pliocène moyen</term>
<term>Anatomie</term>
<term>Taxon nouveau</term>
<term>Miocène sup</term>
<term>Pliocène inf</term>
<term>Biostratigraphie</term>
<term>Mylodontidae</term>
<term>Pleurolestodon dalenzae</term>
<term>Simomylodon uccasamamensis</term>
<term>Altiplano</term>
<term>Bolivie</term>
</keywords>
</textClass>
</profileDesc>
</teiHeader>
<front><div type="abstract" xml:lang="en">Two new Mylodontinae (Xenarthra, Tardigrada, Mylodontoidea) from the Bolivian Altiplano are described. One of them, Pleurolestodon dalenzae n. sp., was discovered a few meters below a volcanic tuff, Toba 76, that may be used as a reference stratigraphic level and is dated at 5.4 Ma; it could be Huayquerian (late Miocene) or at the Huayquerian-Montehermosan boundary in age. The other taxon, Simomylodon uccasamamensis n. gen., n. sp., was recovered from many localities of a horizon bounded below by Toba 76 and above by another volcanic level, the 2.8 Ma Ayo Ayo tuff; its age is Montehermosan-Chapadmalalan (early and middle Pliocene). Analysis of these taxa indicates that they are Mylodontidae more closely related to Glossotherium, Glossotheridium, Kiyumylodon and Paramylodon than to Lestodon or Thinobadistes.</div>
</front>
</TEI>
<inist><standard h6="B"><pA><fA01 i1="01" i2="1"><s0>1280-9659</s0>
</fA01>
<fA03 i2="1"><s0>Geodiversitas</s0>
</fA03>
<fA05><s2>32</s2>
</fA05>
<fA06><s2>2</s2>
</fA06>
<fA08 i1="01" i2="1" l="FRE"><s1>Nouveaux paresseux terrestres (Mammalia, Xenarthra, Mylodontidae) du Néogène de l'Altiplano bolivien</s1>
</fA08>
<fA11 i1="01" i2="1"><s1>SAINT-ANDRE (Pierre-Antoine)</s1>
<s9>rép.</s9>
</fA11>
<fA11 i1="02" i2="1"><s1>PUJOS (François)</s1>
</fA11>
<fA11 i1="03" i2="1"><s1>CARTELLE (Cástor)</s1>
</fA11>
<fA11 i1="04" i2="1"><s1>DE IULIIS (Gerardo)</s1>
</fA11>
<fA11 i1="05" i2="1"><s1>GAUDIN (Timothy J.)</s1>
</fA11>
<fA11 i1="06" i2="1"><s1>MCDONALD (H. Gregory)</s1>
</fA11>
<fA11 i1="07" i2="1"><s1>MAMANI QUISPE (Bernardino)</s1>
</fA11>
<fA14 i1="01"><s1>Dpto de Geología y Paleontología, Instituto Argentino de Nivologia, Glaciologia y Ciencias Ambientales (IANIGLA), CCT-CONICET-Mendoza, Avda. Ruiz Leal s/n, Parque Gral. San Martín</s1>
<s2>5500 Mendoza</s2>
<s3>ARG</s3>
<sZ>2 aut.</sZ>
</fA14>
<fA14 i1="02"><s1>PUC Minas, Avenida Dom José Gaspar, 290 Coração Eucarístico</s1>
<s2>Belo Horizonte, Minas Gerais</s2>
<s3>BRA</s3>
<sZ>3 aut.</sZ>
</fA14>
<fA14 i1="03"><s1>Faculty of Community Services and Health Sciences, George Brown College of Applied Arts and Technology, 200 King Street East</s1>
<s2>Toronto, Ontario, M5A 1J5</s2>
<s3>CAN</s3>
<sZ>4 aut.</sZ>
</fA14>
<fA14 i1="04"><s1>Department of Biological and Environmental Sciences (Department 2653), University of Tennessee at Chattanooga, 615 McCallie Avenue</s1>
<s2>Chattanooga, TN 37403-2598</s2>
<s3>USA</s3>
<sZ>5 aut.</sZ>
</fA14>
<fA14 i1="05"><s1>Park Museum Management Program, National Park Service, 1201 Oakridge Drive, Suite 150</s1>
<s2>Fort Collins, Colorado 80525</s2>
<s3>USA</s3>
<sZ>6 aut.</sZ>
</fA14>
<fA14 i1="06"><s1>Departamento de Paleontología, Museo Nacional de Historia Natural, Calle 26 s/n</s1>
<s2>Cota Cota, La Paz</s2>
<s3>BOL</s3>
<sZ>7 aut.</sZ>
</fA14>
<fA20><s1>255-306</s1>
</fA20>
<fA21><s1>2010</s1>
</fA21>
<fA23 i1="01"><s0>FRE</s0>
</fA23>
<fA24 i1="01"><s0>eng</s0>
</fA24>
<fA43 i1="01"><s1>INIST</s1>
<s2>801C</s2>
<s5>354000180727780040</s5>
</fA43>
<fA44><s0>0000</s0>
<s1>© 2010 INIST-CNRS. All rights reserved.</s1>
</fA44>
<fA45><s0>2 p.1/4</s0>
</fA45>
<fA47 i1="01" i2="1"><s0>10-0319855</s0>
</fA47>
<fA60><s1>P</s1>
</fA60>
<fA61><s0>A</s0>
</fA61>
<fA64 i1="01" i2="1"><s0>Geodiversitas</s0>
</fA64>
<fA66 i1="01"><s0>FRA</s0>
</fA66>
<fA68 i1="01" i2="1" l="ENG"><s1>New ground sloths (Mammalia, Xenarthra, Mylodontidae) from the Neogene of the Bolivian Altiplano</s1>
</fA68>
<fC01 i1="01" l="ENG"><s0>Two new Mylodontinae (Xenarthra, Tardigrada, Mylodontoidea) from the Bolivian Altiplano are described. One of them, Pleurolestodon dalenzae n. sp., was discovered a few meters below a volcanic tuff, Toba 76, that may be used as a reference stratigraphic level and is dated at 5.4 Ma; it could be Huayquerian (late Miocene) or at the Huayquerian-Montehermosan boundary in age. The other taxon, Simomylodon uccasamamensis n. gen., n. sp., was recovered from many localities of a horizon bounded below by Toba 76 and above by another volcanic level, the 2.8 Ma Ayo Ayo tuff; its age is Montehermosan-Chapadmalalan (early and middle Pliocene). Analysis of these taxa indicates that they are Mylodontidae more closely related to Glossotherium, Glossotheridium, Kiyumylodon and Paramylodon than to Lestodon or Thinobadistes.</s0>
</fC01>
<fC02 i1="01" i2="2"><s0>001E01Q04</s0>
</fC02>
<fC02 i1="02" i2="2"><s0>001E01I</s0>
</fC02>
<fC02 i1="03" i2="2"><s0>227A04</s0>
</fC02>
<fC02 i1="04" i2="2"><s0>224A</s0>
</fC02>
<fC03 i1="01" i2="2" l="FRE"><s0>Mammalia</s0>
<s2>NY</s2>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="2" l="ENG"><s0>Mammalia</s0>
<s2>NY</s2>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="2" l="SPA"><s0>Mammalia</s0>
<s2>NY</s2>
<s5>01</s5>
</fC03>
<fC03 i1="02" i2="2" l="FRE"><s0>Xenarthra</s0>
<s2>NY</s2>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="2" l="ENG"><s0>Xenarthra</s0>
<s2>NY</s2>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="2" l="SPA"><s0>Xenarthra</s0>
<s2>NY</s2>
<s5>02</s5>
</fC03>
<fC03 i1="03" i2="2" l="FRE"><s0>Néogène</s0>
<s2>NX</s2>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="2" l="ENG"><s0>Neogene</s0>
<s2>NX</s2>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="2" l="SPA"><s0>Neógeno</s0>
<s2>NX</s2>
<s5>03</s5>
</fC03>
<fC03 i1="04" i2="2" l="FRE"><s0>Tuf volcanique</s0>
<s2>NV</s2>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="ENG"><s0>tuff</s0>
<s2>NV</s2>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="SPA"><s0>Toba volcánica</s0>
<s2>NV</s2>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="2" l="FRE"><s0>Miocène</s0>
<s2>NX</s2>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="ENG"><s0>Miocene</s0>
<s2>NX</s2>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="SPA"><s0>Mioceno</s0>
<s2>NX</s2>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="2" l="FRE"><s0>Pliocène moyen</s0>
<s2>NX</s2>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="2" l="ENG"><s0>middle Pliocene</s0>
<s2>NX</s2>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="2" l="SPA"><s0>Plioceno medio</s0>
<s2>NX</s2>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="2" l="FRE"><s0>Anatomie</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="2" l="ENG"><s0>anatomy</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="2" l="SPA"><s0>Anatomía</s0>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="2" l="FRE"><s0>Taxon nouveau</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="2" l="ENG"><s0>new taxa</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="2" l="SPA"><s0>Nuevo taxón</s0>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="2" l="FRE"><s0>Miocène sup</s0>
<s2>NX</s2>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="2" l="ENG"><s0>upper Miocene</s0>
<s2>NX</s2>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="2" l="SPA"><s0>Mioceno sup</s0>
<s2>NX</s2>
<s5>09</s5>
</fC03>
<fC03 i1="10" i2="2" l="FRE"><s0>Pliocène inf</s0>
<s2>NX</s2>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="2" l="ENG"><s0>lower Pliocene</s0>
<s2>NX</s2>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="2" l="SPA"><s0>Plioceno inf</s0>
<s2>NX</s2>
<s5>10</s5>
</fC03>
<fC03 i1="11" i2="2" l="FRE"><s0>Biostratigraphie</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="ENG"><s0>biostratigraphy</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="SPA"><s0>Bioestratigrafía</s0>
<s5>11</s5>
</fC03>
<fC03 i1="12" i2="2" l="FRE"><s0>Mylodontidae</s0>
<s4>INC</s4>
<s5>52</s5>
</fC03>
<fC03 i1="13" i2="2" l="FRE"><s0>Pleurolestodon dalenzae</s0>
<s4>INC</s4>
<s5>53</s5>
</fC03>
<fC03 i1="14" i2="2" l="FRE"><s0>Simomylodon uccasamamensis</s0>
<s4>INC</s4>
<s5>54</s5>
</fC03>
<fC03 i1="15" i2="2" l="FRE"><s0>Altiplano</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="15" i2="2" l="ENG"><s0>Altiplano</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="16" i2="2" l="FRE"><s0>Bolivie</s0>
<s2>NG</s2>
<s5>62</s5>
</fC03>
<fC03 i1="16" i2="2" l="ENG"><s0>Bolivia</s0>
<s2>NG</s2>
<s5>62</s5>
</fC03>
<fC03 i1="16" i2="2" l="SPA"><s0>Bolivia</s0>
<s2>NG</s2>
<s5>62</s5>
</fC03>
<fC07 i1="01" i2="2" l="FRE"><s0>Tetrapoda</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="01" i2="2" l="ENG"><s0>Tetrapoda</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="01" i2="2" l="SPA"><s0>Tetrapoda</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="02" i2="2" l="FRE"><s0>Vertebrata</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="02" i2="2" l="ENG"><s0>Vertebrata</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="02" i2="2" l="SPA"><s0>Vertebrata</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="03" i2="2" l="FRE"><s0>Chordata</s0>
</fC07>
<fC07 i1="03" i2="2" l="ENG"><s0>Chordata</s0>
</fC07>
<fC07 i1="03" i2="2" l="SPA"><s0>Chordata</s0>
</fC07>
<fC07 i1="04" i2="2" l="FRE"><s0>Edentata</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="04" i2="2" l="ENG"><s0>Edentata</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="04" i2="2" l="SPA"><s0>Edentata</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="05" i2="2" l="FRE"><s0>Eutheria</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="05" i2="2" l="ENG"><s0>Eutheria</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="06" i2="2" l="FRE"><s0>Theria</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="06" i2="2" l="ENG"><s0>Theria</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="07" i2="2" l="FRE"><s0>Tertiaire sup</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="07" i2="2" l="ENG"><s0>upper Tertiary</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="08" i2="2" l="FRE"><s0>Tertiaire</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="08" i2="2" l="ENG"><s0>Tertiary</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="08" i2="2" l="SPA"><s0>Terciario</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="09" i2="2" l="FRE"><s0>Cénozoïque</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="09" i2="2" l="ENG"><s0>Cenozoic</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="09" i2="2" l="SPA"><s0>Cenozoico</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="10" i2="2" l="FRE"><s0>Phanérozoïque</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="10" i2="2" l="ENG"><s0>Phanerozoic</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="10" i2="2" l="SPA"><s0>Fanerozoico</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="11" i2="2" l="FRE"><s0>Pyroclastite</s0>
<s2>NV</s2>
</fC07>
<fC07 i1="11" i2="2" l="ENG"><s0>pyroclastics</s0>
<s2>NV</s2>
</fC07>
<fC07 i1="12" i2="2" l="FRE"><s0>Roche volcanique</s0>
<s2>NV</s2>
</fC07>
<fC07 i1="12" i2="2" l="ENG"><s0>volcanic rocks</s0>
<s2>NV</s2>
</fC07>
<fC07 i1="12" i2="2" l="SPA"><s0>Roca volcánica</s0>
<s2>NV</s2>
</fC07>
<fC07 i1="13" i2="2" l="FRE"><s0>Roche ignée</s0>
<s2>NV</s2>
</fC07>
<fC07 i1="13" i2="2" l="ENG"><s0>igneous rocks</s0>
<s2>NV</s2>
</fC07>
<fC07 i1="13" i2="2" l="SPA"><s0>Roca ignea</s0>
<s2>NV</s2>
</fC07>
<fC07 i1="14" i2="2" l="FRE"><s0>Pliocène</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="14" i2="2" l="ENG"><s0>Pliocene</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="14" i2="2" l="SPA"><s0>Plioceno</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="15" i2="2" l="FRE"><s0>Andes</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="15" i2="2" l="ENG"><s0>Andes</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="15" i2="2" l="SPA"><s0>Andes</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="16" i2="2" l="FRE"><s0>Amérique du Sud</s0>
<s2>564</s2>
</fC07>
<fC07 i1="16" i2="2" l="ENG"><s0>South America</s0>
<s2>564</s2>
</fC07>
<fC07 i1="16" i2="2" l="SPA"><s0>America del sur</s0>
<s2>564</s2>
</fC07>
<fN21><s1>200</s1>
</fN21>
</pA>
</standard>
<server><NO>PASCAL 10-0319855 INIST</NO>
<FT>Nouveaux paresseux terrestres (Mammalia, Xenarthra, Mylodontidae) du Néogène de l'Altiplano bolivien</FT>
<ET>(New ground sloths (Mammalia, Xenarthra, Mylodontidae) from the Neogene of the Bolivian Altiplano)</ET>
<AU>SAINT-ANDRE (Pierre-Antoine); PUJOS (François); CARTELLE (Cástor); DE IULIIS (Gerardo); GAUDIN (Timothy J.); MCDONALD (H. Gregory); MAMANI QUISPE (Bernardino)</AU>
<AF>Dpto de Geología y Paleontología, Instituto Argentino de Nivologia, Glaciologia y Ciencias Ambientales (IANIGLA), CCT-CONICET-Mendoza, Avda. Ruiz Leal s/n, Parque Gral. San Martín/5500 Mendoza/Argentine (2 aut.); PUC Minas, Avenida Dom José Gaspar, 290 Coração Eucarístico/Belo Horizonte, Minas Gerais/Brésil (3 aut.); Faculty of Community Services and Health Sciences, George Brown College of Applied Arts and Technology, 200 King Street East/Toronto, Ontario, M5A 1J5/Canada (4 aut.); Department of Biological and Environmental Sciences (Department 2653), University of Tennessee at Chattanooga, 615 McCallie Avenue/Chattanooga, TN 37403-2598/Etats-Unis (5 aut.); Park Museum Management Program, National Park Service, 1201 Oakridge Drive, Suite 150/Fort Collins, Colorado 80525/Etats-Unis (6 aut.); Departamento de Paleontología, Museo Nacional de Historia Natural, Calle 26 s/n/Cota Cota, La Paz/Bolivie (7 aut.)</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>Geodiversitas; ISSN 1280-9659; France; Da. 2010; Vol. 32; No. 2; Pp. 255-306; Abs. anglais; Bibl. 2 p.1/4</SO>
<LA>Français</LA>
<EA>Two new Mylodontinae (Xenarthra, Tardigrada, Mylodontoidea) from the Bolivian Altiplano are described. One of them, Pleurolestodon dalenzae n. sp., was discovered a few meters below a volcanic tuff, Toba 76, that may be used as a reference stratigraphic level and is dated at 5.4 Ma; it could be Huayquerian (late Miocene) or at the Huayquerian-Montehermosan boundary in age. The other taxon, Simomylodon uccasamamensis n. gen., n. sp., was recovered from many localities of a horizon bounded below by Toba 76 and above by another volcanic level, the 2.8 Ma Ayo Ayo tuff; its age is Montehermosan-Chapadmalalan (early and middle Pliocene). Analysis of these taxa indicates that they are Mylodontidae more closely related to Glossotherium, Glossotheridium, Kiyumylodon and Paramylodon than to Lestodon or Thinobadistes.</EA>
<CC>001E01Q04; 001E01I; 227A04; 224A</CC>
<FD>Mammalia; Xenarthra; Néogène; Tuf volcanique; Miocène; Pliocène moyen; Anatomie; Taxon nouveau; Miocène sup; Pliocène inf; Biostratigraphie; Mylodontidae; Pleurolestodon dalenzae; Simomylodon uccasamamensis; Altiplano; Bolivie</FD>
<FG>Tetrapoda; Vertebrata; Chordata; Edentata; Eutheria; Theria; Tertiaire sup; Tertiaire; Cénozoïque; Phanérozoïque; Pyroclastite; Roche volcanique; Roche ignée; Pliocène; Andes; Amérique du Sud</FG>
<ED>Mammalia; Xenarthra; Neogene; tuff; Miocene; middle Pliocene; anatomy; new taxa; upper Miocene; lower Pliocene; biostratigraphy; Altiplano; Bolivia</ED>
<EG>Tetrapoda; Vertebrata; Chordata; Edentata; Eutheria; Theria; upper Tertiary; Tertiary; Cenozoic; Phanerozoic; pyroclastics; volcanic rocks; igneous rocks; Pliocene; Andes; South America</EG>
<SD>Mammalia; Xenarthra; Neógeno; Toba volcánica; Mioceno; Plioceno medio; Anatomía; Nuevo taxón; Mioceno sup; Plioceno inf; Bioestratigrafía; Bolivia</SD>
<LO>INIST-801C.354000180727780040</LO>
<ID>10-0319855</ID>
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Nouveaux paresseux terrestres (Mammalia, Xenarthra, Mylodontidae) du Néogène de l'Altiplano bolivien

Nouveaux paresseux terrestres (Mammalia, Xenarthra, Mylodontidae) du Néogène de l'Altiplano bolivien

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