Ossified meniscus and cyamo-fabella in some fossil sloths : a morpho-functional interpretation
Identifieur interne : 000506 ( PascalFrancis/Corpus ); précédent : 000505; suivant : 000507Ossified meniscus and cyamo-fabella in some fossil sloths : a morpho-functional interpretation
Auteurs : Rodolfo Salas ; Francois Pujos ; Christian De MuizonSource :
- Geobios : (Lyon) [ 0016-6995 ] ; 2005.
Descripteurs français
- Pascal (Inist)
English descriptors
- KwdEn :
Abstract
An articulated skeleton of Thalassocnus natans (Xenarthra : Nothrotheriidae) and a review of some other fossil sloths provide new information on sesamoid bones located at the knee joint. A sesamoid bone and an ossified meniscus have been identified at this joint. The cyanofabella (posterior sesamoid of the tibio-femoral articulation) of T. natans may act like a pulley through which the tendon of the m. gastrocnemius would have passed. The ossified meniscus, which is also present in Megatheriidae and Mylodontidae, could be related to the pedolateral stance and a large rotation of the knee joint during locomotion.
Notice en format standard (ISO 2709)
Pour connaître la documentation sur le format Inist Standard.
pA |
|
---|
Format Inist (serveur)
NO : | PASCAL 05-0286905 INIST |
---|---|
ET : | Ossified meniscus and cyamo-fabella in some fossil sloths : a morpho-functional interpretation |
AU : | SALAS (Rodolfo); PUJOS (Francois); DE MUIZON (Christian) |
AF : | Museo de Historia Natural-UNMSM, Dpto. de Paleontología de Vertebrados, Apdo. 14-0434/Lima/Pérou (1 aut.); Instituto Froncés de Estudios Andinos, Casilla 18-1217, Contralmirante Montero 141/Lima/Pérou (1 aut., 2 aut.); UMR 8569 du CNRS, Département Histoire de la Terre, Muséum national d'Histoire naturelle, 8, rue Buffon/75005 Paris/France (2 aut., 3 aut.) |
DT : | Publication en série; Niveau analytique |
SO : | Geobios : (Lyon); ISSN 0016-6995; France; Da. 2005; Vol. 38; No. 3; Pp. 389-394; Abs. français/espagnol; Bibl. 22 ref. |
LA : | Anglais |
EA : | An articulated skeleton of Thalassocnus natans (Xenarthra : Nothrotheriidae) and a review of some other fossil sloths provide new information on sesamoid bones located at the knee joint. A sesamoid bone and an ossified meniscus have been identified at this joint. The cyanofabella (posterior sesamoid of the tibio-femoral articulation) of T. natans may act like a pulley through which the tendon of the m. gastrocnemius would have passed. The ossified meniscus, which is also present in Megatheriidae and Mylodontidae, could be related to the pedolateral stance and a large rotation of the knee joint during locomotion. |
CC : | 227A04; 224A; 001E01Q04; 001E01I |
FD : | Interprétation; Squelette; Xenarthra; Ossement; Miocène sup; Locomotion; Anatomie; Biostratigraphie; Anatomie locomotion; Pliocène; Megatheriidae; Nothrotheriidae; Mylodontidae; Pérou |
FG : | Edentata; Eutheria; Theria; Mammalia; Tetrapoda; Vertebrata; Chordata; Miocène; Néogène; Tertiaire sup; Tertiaire; Cénozoïque; Phanérozoïque; Amérique du Sud |
ED : | interpretation; skeletons; Xenarthra; bones; upper Miocene; locomotion; anatomy; biostratigraphy; extremities; Pliocene; Peru |
EG : | Edentata; Eutheria; Theria; Mammalia; Tetrapoda; Vertebrata; Chordata; Miocene; Neogene; upper Tertiary; Tertiary; Cenozoic; Phanerozoic; South America |
SD : | Interpretación; Xenarthra; Osamenta; Mioceno sup; Locomoción; Anatomía; Bioestratigrafía; Anatomía locomoción; Plioceno; Perú |
LO : | INIST-14199.354000124794660090 |
ID : | 05-0286905 |
Links to Exploration step
Pascal:05-0286905Le document en format XML
<record><TEI><teiHeader><fileDesc><titleStmt><title xml:lang="en" level="a">Ossified meniscus and cyamo-fabella in some fossil sloths : a morpho-functional interpretation</title>
<author><name sortKey="Salas, Rodolfo" sort="Salas, Rodolfo" uniqKey="Salas R" first="Rodolfo" last="Salas">Rodolfo Salas</name>
<affiliation><inist:fA14 i1="01"><s1>Museo de Historia Natural-UNMSM, Dpto. de Paleontología de Vertebrados, Apdo. 14-0434</s1>
<s2>Lima</s2>
<s3>PER</s3>
<sZ>1 aut.</sZ>
</inist:fA14>
</affiliation>
<affiliation><inist:fA14 i1="02"><s1>Instituto Froncés de Estudios Andinos, Casilla 18-1217, Contralmirante Montero 141</s1>
<s2>Lima</s2>
<s3>PER</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="Pujos, Francois" sort="Pujos, Francois" uniqKey="Pujos F" first="Francois" last="Pujos">Francois Pujos</name>
<affiliation><inist:fA14 i1="02"><s1>Instituto Froncés de Estudios Andinos, Casilla 18-1217, Contralmirante Montero 141</s1>
<s2>Lima</s2>
<s3>PER</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
</inist:fA14>
</affiliation>
<affiliation><inist:fA14 i1="03"><s1>UMR 8569 du CNRS, Département Histoire de la Terre, Muséum national d'Histoire naturelle, 8, rue Buffon</s1>
<s2>75005 Paris</s2>
<s3>FRA</s3>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="De Muizon, Christian" sort="De Muizon, Christian" uniqKey="De Muizon C" first="Christian" last="De Muizon">Christian De Muizon</name>
<affiliation><inist:fA14 i1="03"><s1>UMR 8569 du CNRS, Département Histoire de la Terre, Muséum national d'Histoire naturelle, 8, rue Buffon</s1>
<s2>75005 Paris</s2>
<s3>FRA</s3>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
</titleStmt>
<publicationStmt><idno type="wicri:source">INIST</idno>
<idno type="inist">05-0286905</idno>
<date when="2005">2005</date>
<idno type="stanalyst">PASCAL 05-0286905 INIST</idno>
<idno type="RBID">Pascal:05-0286905</idno>
<idno type="wicri:Area/PascalFrancis/Corpus">000506</idno>
</publicationStmt>
<sourceDesc><biblStruct><analytic><title xml:lang="en" level="a">Ossified meniscus and cyamo-fabella in some fossil sloths : a morpho-functional interpretation</title>
<author><name sortKey="Salas, Rodolfo" sort="Salas, Rodolfo" uniqKey="Salas R" first="Rodolfo" last="Salas">Rodolfo Salas</name>
<affiliation><inist:fA14 i1="01"><s1>Museo de Historia Natural-UNMSM, Dpto. de Paleontología de Vertebrados, Apdo. 14-0434</s1>
<s2>Lima</s2>
<s3>PER</s3>
<sZ>1 aut.</sZ>
</inist:fA14>
</affiliation>
<affiliation><inist:fA14 i1="02"><s1>Instituto Froncés de Estudios Andinos, Casilla 18-1217, Contralmirante Montero 141</s1>
<s2>Lima</s2>
<s3>PER</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="Pujos, Francois" sort="Pujos, Francois" uniqKey="Pujos F" first="Francois" last="Pujos">Francois Pujos</name>
<affiliation><inist:fA14 i1="02"><s1>Instituto Froncés de Estudios Andinos, Casilla 18-1217, Contralmirante Montero 141</s1>
<s2>Lima</s2>
<s3>PER</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
</inist:fA14>
</affiliation>
<affiliation><inist:fA14 i1="03"><s1>UMR 8569 du CNRS, Département Histoire de la Terre, Muséum national d'Histoire naturelle, 8, rue Buffon</s1>
<s2>75005 Paris</s2>
<s3>FRA</s3>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="De Muizon, Christian" sort="De Muizon, Christian" uniqKey="De Muizon C" first="Christian" last="De Muizon">Christian De Muizon</name>
<affiliation><inist:fA14 i1="03"><s1>UMR 8569 du CNRS, Département Histoire de la Terre, Muséum national d'Histoire naturelle, 8, rue Buffon</s1>
<s2>75005 Paris</s2>
<s3>FRA</s3>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
</analytic>
<series><title level="j" type="main">Geobios : (Lyon)</title>
<title level="j" type="abbreviated">Geobios : (Lyon)</title>
<idno type="ISSN">0016-6995</idno>
<imprint><date when="2005">2005</date>
</imprint>
</series>
</biblStruct>
</sourceDesc>
<seriesStmt><title level="j" type="main">Geobios : (Lyon)</title>
<title level="j" type="abbreviated">Geobios : (Lyon)</title>
<idno type="ISSN">0016-6995</idno>
</seriesStmt>
</fileDesc>
<profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Peru</term>
<term>Pliocene</term>
<term>Xenarthra</term>
<term>anatomy</term>
<term>biostratigraphy</term>
<term>bones</term>
<term>extremities</term>
<term>interpretation</term>
<term>locomotion</term>
<term>skeletons</term>
<term>upper Miocene</term>
</keywords>
<keywords scheme="Pascal" xml:lang="fr"><term>Interprétation</term>
<term>Squelette</term>
<term>Xenarthra</term>
<term>Ossement</term>
<term>Miocène sup</term>
<term>Locomotion</term>
<term>Anatomie</term>
<term>Biostratigraphie</term>
<term>Anatomie locomotion</term>
<term>Pliocène</term>
<term>Megatheriidae</term>
<term>Nothrotheriidae</term>
<term>Mylodontidae</term>
<term>Pérou</term>
</keywords>
</textClass>
</profileDesc>
</teiHeader>
<front><div type="abstract" xml:lang="en">An articulated skeleton of Thalassocnus natans (Xenarthra : Nothrotheriidae) and a review of some other fossil sloths provide new information on sesamoid bones located at the knee joint. A sesamoid bone and an ossified meniscus have been identified at this joint. The cyanofabella (posterior sesamoid of the tibio-femoral articulation) of T. natans may act like a pulley through which the tendon of the m. gastrocnemius would have passed. The ossified meniscus, which is also present in Megatheriidae and Mylodontidae, could be related to the pedolateral stance and a large rotation of the knee joint during locomotion.</div>
</front>
</TEI>
<inist><standard h6="B"><pA><fA01 i1="01" i2="1"><s0>0016-6995</s0>
</fA01>
<fA03 i2="1"><s0>Geobios : (Lyon)</s0>
</fA03>
<fA05><s2>38</s2>
</fA05>
<fA06><s2>3</s2>
</fA06>
<fA08 i1="01" i2="1" l="ENG"><s1>Ossified meniscus and cyamo-fabella in some fossil sloths : a morpho-functional interpretation</s1>
</fA08>
<fA11 i1="01" i2="1"><s1>SALAS (Rodolfo)</s1>
</fA11>
<fA11 i1="02" i2="1"><s1>PUJOS (Francois)</s1>
</fA11>
<fA11 i1="03" i2="1"><s1>DE MUIZON (Christian)</s1>
</fA11>
<fA14 i1="01"><s1>Museo de Historia Natural-UNMSM, Dpto. de Paleontología de Vertebrados, Apdo. 14-0434</s1>
<s2>Lima</s2>
<s3>PER</s3>
<sZ>1 aut.</sZ>
</fA14>
<fA14 i1="02"><s1>Instituto Froncés de Estudios Andinos, Casilla 18-1217, Contralmirante Montero 141</s1>
<s2>Lima</s2>
<s3>PER</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
</fA14>
<fA14 i1="03"><s1>UMR 8569 du CNRS, Département Histoire de la Terre, Muséum national d'Histoire naturelle, 8, rue Buffon</s1>
<s2>75005 Paris</s2>
<s3>FRA</s3>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
</fA14>
<fA20><s1>389-394</s1>
</fA20>
<fA21><s1>2005</s1>
</fA21>
<fA23 i1="01"><s0>ENG</s0>
</fA23>
<fA24 i1="01"><s0>fre</s0>
</fA24>
<fA24 i1="02"><s0>spa</s0>
</fA24>
<fA43 i1="01"><s1>INIST</s1>
<s2>14199</s2>
<s5>354000124794660090</s5>
</fA43>
<fA44><s0>0000</s0>
<s1>© 2005 INIST-CNRS. All rights reserved.</s1>
</fA44>
<fA45><s0>22 ref.</s0>
</fA45>
<fA47 i1="01" i2="1"><s0>05-0286905</s0>
</fA47>
<fA60><s1>P</s1>
</fA60>
<fA61><s0>A</s0>
</fA61>
<fA64 i1="01" i2="1"><s0>Geobios : (Lyon)</s0>
</fA64>
<fA66 i1="01"><s0>FRA</s0>
</fA66>
<fC01 i1="01" l="ENG"><s0>An articulated skeleton of Thalassocnus natans (Xenarthra : Nothrotheriidae) and a review of some other fossil sloths provide new information on sesamoid bones located at the knee joint. A sesamoid bone and an ossified meniscus have been identified at this joint. The cyanofabella (posterior sesamoid of the tibio-femoral articulation) of T. natans may act like a pulley through which the tendon of the m. gastrocnemius would have passed. The ossified meniscus, which is also present in Megatheriidae and Mylodontidae, could be related to the pedolateral stance and a large rotation of the knee joint during locomotion.</s0>
</fC01>
<fC02 i1="01" i2="2"><s0>227A04</s0>
</fC02>
<fC02 i1="02" i2="2"><s0>224A</s0>
</fC02>
<fC02 i1="03" i2="2"><s0>001E01Q04</s0>
</fC02>
<fC02 i1="04" i2="2"><s0>001E01I</s0>
</fC02>
<fC03 i1="01" i2="2" l="FRE"><s0>Interprétation</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="2" l="ENG"><s0>interpretation</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="2" l="SPA"><s0>Interpretación</s0>
<s5>01</s5>
</fC03>
<fC03 i1="02" i2="2" l="FRE"><s0>Squelette</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="2" l="ENG"><s0>skeletons</s0>
<s5>02</s5>
</fC03>
<fC03 i1="03" i2="2" l="FRE"><s0>Xenarthra</s0>
<s2>NY</s2>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="2" l="ENG"><s0>Xenarthra</s0>
<s2>NY</s2>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="2" l="SPA"><s0>Xenarthra</s0>
<s2>NY</s2>
<s5>03</s5>
</fC03>
<fC03 i1="04" i2="2" l="FRE"><s0>Ossement</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="ENG"><s0>bones</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="SPA"><s0>Osamenta</s0>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="2" l="FRE"><s0>Miocène sup</s0>
<s2>NX</s2>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="ENG"><s0>upper Miocene</s0>
<s2>NX</s2>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="SPA"><s0>Mioceno sup</s0>
<s2>NX</s2>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="2" l="FRE"><s0>Locomotion</s0>
<s5>07</s5>
</fC03>
<fC03 i1="06" i2="2" l="ENG"><s0>locomotion</s0>
<s5>07</s5>
</fC03>
<fC03 i1="06" i2="2" l="SPA"><s0>Locomoción</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="2" l="FRE"><s0>Anatomie</s0>
<s5>08</s5>
</fC03>
<fC03 i1="07" i2="2" l="ENG"><s0>anatomy</s0>
<s5>08</s5>
</fC03>
<fC03 i1="07" i2="2" l="SPA"><s0>Anatomía</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="2" l="FRE"><s0>Biostratigraphie</s0>
<s5>10</s5>
</fC03>
<fC03 i1="08" i2="2" l="ENG"><s0>biostratigraphy</s0>
<s5>10</s5>
</fC03>
<fC03 i1="08" i2="2" l="SPA"><s0>Bioestratigrafía</s0>
<s5>10</s5>
</fC03>
<fC03 i1="09" i2="2" l="FRE"><s0>Anatomie locomotion</s0>
<s5>11</s5>
</fC03>
<fC03 i1="09" i2="2" l="ENG"><s0>extremities</s0>
<s5>11</s5>
</fC03>
<fC03 i1="09" i2="2" l="SPA"><s0>Anatomía locomoción</s0>
<s5>11</s5>
</fC03>
<fC03 i1="10" i2="2" l="FRE"><s0>Pliocène</s0>
<s2>NX</s2>
<s5>12</s5>
</fC03>
<fC03 i1="10" i2="2" l="ENG"><s0>Pliocene</s0>
<s2>NX</s2>
<s5>12</s5>
</fC03>
<fC03 i1="10" i2="2" l="SPA"><s0>Plioceno</s0>
<s2>NX</s2>
<s5>12</s5>
</fC03>
<fC03 i1="11" i2="2" l="FRE"><s0>Megatheriidae</s0>
<s4>INC</s4>
<s5>52</s5>
</fC03>
<fC03 i1="12" i2="2" l="FRE"><s0>Nothrotheriidae</s0>
<s4>INC</s4>
<s5>53</s5>
</fC03>
<fC03 i1="13" i2="2" l="FRE"><s0>Mylodontidae</s0>
<s4>INC</s4>
<s5>54</s5>
</fC03>
<fC03 i1="14" i2="2" l="FRE"><s0>Pérou</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="14" i2="2" l="ENG"><s0>Peru</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="14" i2="2" l="SPA"><s0>Perú</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC07 i1="01" i2="2" l="FRE"><s0>Edentata</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="01" i2="2" l="ENG"><s0>Edentata</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="01" i2="2" l="SPA"><s0>Edentata</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="02" i2="2" l="FRE"><s0>Eutheria</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="02" i2="2" l="ENG"><s0>Eutheria</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="03" i2="2" l="FRE"><s0>Theria</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="03" i2="2" l="ENG"><s0>Theria</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="04" i2="2" l="FRE"><s0>Mammalia</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="04" i2="2" l="ENG"><s0>Mammalia</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="04" i2="2" l="SPA"><s0>Mammalia</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="05" i2="2" l="FRE"><s0>Tetrapoda</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="05" i2="2" l="ENG"><s0>Tetrapoda</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="05" i2="2" l="SPA"><s0>Tetrapoda</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="06" i2="2" l="FRE"><s0>Vertebrata</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="06" i2="2" l="ENG"><s0>Vertebrata</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="06" i2="2" l="SPA"><s0>Vertebrata</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="07" i2="2" l="FRE"><s0>Chordata</s0>
</fC07>
<fC07 i1="07" i2="2" l="ENG"><s0>Chordata</s0>
</fC07>
<fC07 i1="07" i2="2" l="SPA"><s0>Chordata</s0>
</fC07>
<fC07 i1="08" i2="2" l="FRE"><s0>Miocène</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="08" i2="2" l="ENG"><s0>Miocene</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="08" i2="2" l="SPA"><s0>Mioceno</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="09" i2="2" l="FRE"><s0>Néogène</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="09" i2="2" l="ENG"><s0>Neogene</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="09" i2="2" l="SPA"><s0>Neógeno</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="10" i2="2" l="FRE"><s0>Tertiaire sup</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="10" i2="2" l="ENG"><s0>upper Tertiary</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="11" i2="2" l="FRE"><s0>Tertiaire</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="11" i2="2" l="ENG"><s0>Tertiary</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="11" i2="2" l="SPA"><s0>Terciario</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="12" i2="2" l="FRE"><s0>Cénozoïque</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="12" i2="2" l="ENG"><s0>Cenozoic</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="12" i2="2" l="SPA"><s0>Cenozoico</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="13" i2="2" l="FRE"><s0>Phanérozoïque</s0>
</fC07>
<fC07 i1="13" i2="2" l="ENG"><s0>Phanerozoic</s0>
</fC07>
<fC07 i1="13" i2="2" l="SPA"><s0>Fanerozoico</s0>
</fC07>
<fC07 i1="14" i2="2" l="FRE"><s0>Amérique du Sud</s0>
</fC07>
<fC07 i1="14" i2="2" l="ENG"><s0>South America</s0>
</fC07>
<fC07 i1="14" i2="2" l="SPA"><s0>America del sur</s0>
</fC07>
<fN21><s1>199</s1>
</fN21>
</pA>
</standard>
<server><NO>PASCAL 05-0286905 INIST</NO>
<ET>Ossified meniscus and cyamo-fabella in some fossil sloths : a morpho-functional interpretation</ET>
<AU>SALAS (Rodolfo); PUJOS (Francois); DE MUIZON (Christian)</AU>
<AF>Museo de Historia Natural-UNMSM, Dpto. de Paleontología de Vertebrados, Apdo. 14-0434/Lima/Pérou (1 aut.); Instituto Froncés de Estudios Andinos, Casilla 18-1217, Contralmirante Montero 141/Lima/Pérou (1 aut., 2 aut.); UMR 8569 du CNRS, Département Histoire de la Terre, Muséum national d'Histoire naturelle, 8, rue Buffon/75005 Paris/France (2 aut., 3 aut.)</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>Geobios : (Lyon); ISSN 0016-6995; France; Da. 2005; Vol. 38; No. 3; Pp. 389-394; Abs. français/espagnol; Bibl. 22 ref.</SO>
<LA>Anglais</LA>
<EA>An articulated skeleton of Thalassocnus natans (Xenarthra : Nothrotheriidae) and a review of some other fossil sloths provide new information on sesamoid bones located at the knee joint. A sesamoid bone and an ossified meniscus have been identified at this joint. The cyanofabella (posterior sesamoid of the tibio-femoral articulation) of T. natans may act like a pulley through which the tendon of the m. gastrocnemius would have passed. The ossified meniscus, which is also present in Megatheriidae and Mylodontidae, could be related to the pedolateral stance and a large rotation of the knee joint during locomotion.</EA>
<CC>227A04; 224A; 001E01Q04; 001E01I</CC>
<FD>Interprétation; Squelette; Xenarthra; Ossement; Miocène sup; Locomotion; Anatomie; Biostratigraphie; Anatomie locomotion; Pliocène; Megatheriidae; Nothrotheriidae; Mylodontidae; Pérou</FD>
<FG>Edentata; Eutheria; Theria; Mammalia; Tetrapoda; Vertebrata; Chordata; Miocène; Néogène; Tertiaire sup; Tertiaire; Cénozoïque; Phanérozoïque; Amérique du Sud</FG>
<ED>interpretation; skeletons; Xenarthra; bones; upper Miocene; locomotion; anatomy; biostratigraphy; extremities; Pliocene; Peru</ED>
<EG>Edentata; Eutheria; Theria; Mammalia; Tetrapoda; Vertebrata; Chordata; Miocene; Neogene; upper Tertiary; Tertiary; Cenozoic; Phanerozoic; South America</EG>
<SD>Interpretación; Xenarthra; Osamenta; Mioceno sup; Locomoción; Anatomía; Bioestratigrafía; Anatomía locomoción; Plioceno; Perú</SD>
<LO>INIST-14199.354000124794660090</LO>
<ID>05-0286905</ID>
</server>
</inist>
</record>
Pour manipuler ce document sous Unix (Dilib)
EXPLOR_STEP=$WICRI_ROOT/Wicri/Santé/explor/EdenteV2/Data/PascalFrancis/Corpus
HfdSelect -h $EXPLOR_STEP/biblio.hfd -nk 000506 | SxmlIndent | more
Ou
HfdSelect -h $EXPLOR_AREA/Data/PascalFrancis/Corpus/biblio.hfd -nk 000506 | SxmlIndent | more
Pour mettre un lien sur cette page dans le réseau Wicri
{{Explor lien |wiki= Wicri/Santé |area= EdenteV2 |flux= PascalFrancis |étape= Corpus |type= RBID |clé= Pascal:05-0286905 |texte= Ossified meniscus and cyamo-fabella in some fossil sloths : a morpho-functional interpretation }}
This area was generated with Dilib version V0.6.32. |