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Una nueva especie de Neuryurus Ameghino (Mammalia, Glyptodontidae) en el Pleistoceno tardío de la Mesopotamia de Argentina

Identifieur interne : 000257 ( PascalFrancis/Corpus ); précédent : 000256; suivant : 000258

Una nueva especie de Neuryurus Ameghino (Mammalia, Glyptodontidae) en el Pleistoceno tardío de la Mesopotamia de Argentina

Auteurs : Alfredo Eduardo Zurita ; Brenda Soledad Ferrero

Source :

RBID : Pascal:09-0450878

Descripteurs français

English descriptors

Abstract

Among the South American Pleistocene Glyptodontidae (Xenarthra, Cingulata), one of the most scarcely represented genus in the fossil record is Neuryurus Ameghino, in which the only well characterized species, until now, is Neuryurus rudis (Gervais), coming from the Ensenadan (early-middle Pleistocene) of the Pampean region, Argentina. In this contribution, we report and describe a new species of Neuryurus, coming from the Arroyo Feliciano Formation (early Lujanian; ca. 130 ka), Entre Rios province, Argentina, in a particular palaebiogeographic context, more associated with the western sector of Uruguay and southern Brazil than the Pampean region. From a morphological perspective, this new taxon is characterized by: (a) the remarkable development of the foramina at the exposed surface of the osteoderms of the dorsal carapace, showing un aspect almost spongy; (b) the large diameter of the perforations observed in the ventral surface of the osteoderms, resembling to those present in the dorsal surface of the osteoderms of the Glyptodontidae Doedicurinae; (c) the evident thickness of the osteoderms, as in Glyptodon Owen; (d) area of contact and articulation of adjacent osteoderms very denticulate, with deep osseous interdigitating projections, as in Glyptodon and Glyptotherium Osborn, but here more evident; (e) larger osteoderms of the dorsal carapace showing, in the dorsal surface, many little conical tubercles, having some resemblance to Panochthus tuberculatus Burmeister. The presence of this new species in the early late Pleistocene of the Mesopotamic region is another element that adds to the biogeographical characterization of this particular area, especially evident during the warm and humid pulses of the late Pleistocene. In turn, this species represents the most complete record of the genus outside the Pampean region and partially complete the stratigraphic and geographic distribution of the genus.

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Pour connaître la documentation sur le format Inist Standard.

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C01 01    ENG  @0 Among the South American Pleistocene Glyptodontidae (Xenarthra, Cingulata), one of the most scarcely represented genus in the fossil record is Neuryurus Ameghino, in which the only well characterized species, until now, is Neuryurus rudis (Gervais), coming from the Ensenadan (early-middle Pleistocene) of the Pampean region, Argentina. In this contribution, we report and describe a new species of Neuryurus, coming from the Arroyo Feliciano Formation (early Lujanian; ca. 130 ka), Entre Rios province, Argentina, in a particular palaebiogeographic context, more associated with the western sector of Uruguay and southern Brazil than the Pampean region. From a morphological perspective, this new taxon is characterized by: (a) the remarkable development of the foramina at the exposed surface of the osteoderms of the dorsal carapace, showing un aspect almost spongy; (b) the large diameter of the perforations observed in the ventral surface of the osteoderms, resembling to those present in the dorsal surface of the osteoderms of the Glyptodontidae Doedicurinae; (c) the evident thickness of the osteoderms, as in Glyptodon Owen; (d) area of contact and articulation of adjacent osteoderms very denticulate, with deep osseous interdigitating projections, as in Glyptodon and Glyptotherium Osborn, but here more evident; (e) larger osteoderms of the dorsal carapace showing, in the dorsal surface, many little conical tubercles, having some resemblance to Panochthus tuberculatus Burmeister. The presence of this new species in the early late Pleistocene of the Mesopotamic region is another element that adds to the biogeographical characterization of this particular area, especially evident during the warm and humid pulses of the late Pleistocene. In turn, this species represents the most complete record of the genus outside the Pampean region and partially complete the stratigraphic and geographic distribution of the genus.
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Format Inist (serveur)

NO : PASCAL 09-0450878 INIST
ET : (A new species of Neuryurus Ameghino (Mammalia, Glyptodontidae) from the late Pleistocene of the Mesopotamic region of Argentina)
ST : Una nueva especie de Neuryurus Ameghino (Mammalia, Glyptodontidae) en el Pleistoceno tardío de la Mesopotamia de Argentina
AU : EDUARDO ZURITA (Alfredo); SOLEDAD FERRERO (Brenda)
AF : Centro de Ecología Aplicada del Litoral (CECOAL-CONICET), Universidad Nacional del Nordeste (UNNE), Ruta 5, km 2,5 CC/128 (3400) Corrientes/Argentine (1 aut.); Laboratorio de Paleontología de Vertebrados, CICYTTP-COMCEI Materi y España, (3105) Diamante, Entre Ríos/Argentine (2 aut.)
DT : Publication en série; Niveau analytique
SO : Geobios : (Lyon); ISSN 0016-6995; France; Da. 2009; Vol. 42; No. 5; Pp. 663-673; Abs. anglais/français; Bibl. 1 p.3/4
LA : Espagnol
EA : Among the South American Pleistocene Glyptodontidae (Xenarthra, Cingulata), one of the most scarcely represented genus in the fossil record is Neuryurus Ameghino, in which the only well characterized species, until now, is Neuryurus rudis (Gervais), coming from the Ensenadan (early-middle Pleistocene) of the Pampean region, Argentina. In this contribution, we report and describe a new species of Neuryurus, coming from the Arroyo Feliciano Formation (early Lujanian; ca. 130 ka), Entre Rios province, Argentina, in a particular palaebiogeographic context, more associated with the western sector of Uruguay and southern Brazil than the Pampean region. From a morphological perspective, this new taxon is characterized by: (a) the remarkable development of the foramina at the exposed surface of the osteoderms of the dorsal carapace, showing un aspect almost spongy; (b) the large diameter of the perforations observed in the ventral surface of the osteoderms, resembling to those present in the dorsal surface of the osteoderms of the Glyptodontidae Doedicurinae; (c) the evident thickness of the osteoderms, as in Glyptodon Owen; (d) area of contact and articulation of adjacent osteoderms very denticulate, with deep osseous interdigitating projections, as in Glyptodon and Glyptotherium Osborn, but here more evident; (e) larger osteoderms of the dorsal carapace showing, in the dorsal surface, many little conical tubercles, having some resemblance to Panochthus tuberculatus Burmeister. The presence of this new species in the early late Pleistocene of the Mesopotamic region is another element that adds to the biogeographical characterization of this particular area, especially evident during the warm and humid pulses of the late Pleistocene. In turn, this species represents the most complete record of the genus outside the Pampean region and partially complete the stratigraphic and geographic distribution of the genus.
CC : 001E01Q04; 001E01P02; 227A04; 226C02
FD : Mammalia; Biostratigraphie; Xenarthra; Taxon nouveau; Taxinomie; Biogéographie; Pléistocène sup; Paléobiogéographie; Province Entre Rios; Formation Arroyo Feliciano; Cingulata; Neuryurini; Argentine
FG : Tetrapoda; Vertebrata; Chordata; Edentata; Eutheria; Theria; Pléistocène; Quaternaire; Cénozoïque; Phanérozoïque; Amérique du Sud
ED : Mammalia; biostratigraphy; Xenarthra; new taxa; taxonomy; biogeography; upper Pleistocene; paleobiogeography; Argentina
EG : Tetrapoda; Vertebrata; Chordata; Edentata; Eutheria; Theria; Pleistocene; Quaternary; Cenozoic; Phanerozoic; South America
SD : Mammalia; Bioestratigrafía; Xenarthra; Nuevo taxón; Taxonomía; Biogeografía; Argentina
LO : INIST-14199.354000171136070090
ID : 09-0450878

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Le document en format XML

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<div type="abstract" xml:lang="en">Among the South American Pleistocene Glyptodontidae (Xenarthra, Cingulata), one of the most scarcely represented genus in the fossil record is Neuryurus Ameghino, in which the only well characterized species, until now, is Neuryurus rudis (Gervais), coming from the Ensenadan (early-middle Pleistocene) of the Pampean region, Argentina. In this contribution, we report and describe a new species of Neuryurus, coming from the Arroyo Feliciano Formation (early Lujanian; ca. 130 ka), Entre Rios province, Argentina, in a particular palaebiogeographic context, more associated with the western sector of Uruguay and southern Brazil than the Pampean region. From a morphological perspective, this new taxon is characterized by: (a) the remarkable development of the foramina at the exposed surface of the osteoderms of the dorsal carapace, showing un aspect almost spongy; (b) the large diameter of the perforations observed in the ventral surface of the osteoderms, resembling to those present in the dorsal surface of the osteoderms of the Glyptodontidae Doedicurinae; (c) the evident thickness of the osteoderms, as in Glyptodon Owen; (d) area of contact and articulation of adjacent osteoderms very denticulate, with deep osseous interdigitating projections, as in Glyptodon and Glyptotherium Osborn, but here more evident; (e) larger osteoderms of the dorsal carapace showing, in the dorsal surface, many little conical tubercles, having some resemblance to Panochthus tuberculatus Burmeister. The presence of this new species in the early late Pleistocene of the Mesopotamic region is another element that adds to the biogeographical characterization of this particular area, especially evident during the warm and humid pulses of the late Pleistocene. In turn, this species represents the most complete record of the genus outside the Pampean region and partially complete the stratigraphic and geographic distribution of the genus.</div>
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<s0>Mammalia</s0>
<s2>NY</s2>
<s5>01</s5>
</fC03>
<fC03 i1="02" i2="2" l="FRE">
<s0>Biostratigraphie</s0>
<s5>03</s5>
</fC03>
<fC03 i1="02" i2="2" l="ENG">
<s0>biostratigraphy</s0>
<s5>03</s5>
</fC03>
<fC03 i1="02" i2="2" l="SPA">
<s0>Bioestratigrafía</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="2" l="FRE">
<s0>Xenarthra</s0>
<s2>NY</s2>
<s5>04</s5>
</fC03>
<fC03 i1="03" i2="2" l="ENG">
<s0>Xenarthra</s0>
<s2>NY</s2>
<s5>04</s5>
</fC03>
<fC03 i1="03" i2="2" l="SPA">
<s0>Xenarthra</s0>
<s2>NY</s2>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="FRE">
<s0>Taxon nouveau</s0>
<s5>06</s5>
</fC03>
<fC03 i1="04" i2="2" l="ENG">
<s0>new taxa</s0>
<s5>06</s5>
</fC03>
<fC03 i1="04" i2="2" l="SPA">
<s0>Nuevo taxón</s0>
<s5>06</s5>
</fC03>
<fC03 i1="05" i2="2" l="FRE">
<s0>Taxinomie</s0>
<s5>07</s5>
</fC03>
<fC03 i1="05" i2="2" l="ENG">
<s0>taxonomy</s0>
<s5>07</s5>
</fC03>
<fC03 i1="05" i2="2" l="SPA">
<s0>Taxonomía</s0>
<s5>07</s5>
</fC03>
<fC03 i1="06" i2="2" l="FRE">
<s0>Biogéographie</s0>
<s5>08</s5>
</fC03>
<fC03 i1="06" i2="2" l="ENG">
<s0>biogeography</s0>
<s5>08</s5>
</fC03>
<fC03 i1="06" i2="2" l="SPA">
<s0>Biogeografía</s0>
<s5>08</s5>
</fC03>
<fC03 i1="07" i2="2" l="FRE">
<s0>Pléistocène sup</s0>
<s2>NX</s2>
<s5>09</s5>
</fC03>
<fC03 i1="07" i2="2" l="ENG">
<s0>upper Pleistocene</s0>
<s2>NX</s2>
<s5>09</s5>
</fC03>
<fC03 i1="08" i2="2" l="FRE">
<s0>Paléobiogéographie</s0>
<s5>10</s5>
</fC03>
<fC03 i1="08" i2="2" l="ENG">
<s0>paleobiogeography</s0>
<s5>10</s5>
</fC03>
<fC03 i1="09" i2="2" l="FRE">
<s0>Province Entre Rios</s0>
<s4>INC</s4>
<s5>52</s5>
</fC03>
<fC03 i1="10" i2="2" l="FRE">
<s0>Formation Arroyo Feliciano</s0>
<s4>INC</s4>
<s5>53</s5>
</fC03>
<fC03 i1="11" i2="2" l="FRE">
<s0>Cingulata</s0>
<s4>INC</s4>
<s5>54</s5>
</fC03>
<fC03 i1="12" i2="2" l="FRE">
<s0>Neuryurini</s0>
<s4>INC</s4>
<s5>55</s5>
</fC03>
<fC03 i1="13" i2="2" l="FRE">
<s0>Argentine</s0>
<s2>NG</s2>
<s5>62</s5>
</fC03>
<fC03 i1="13" i2="2" l="ENG">
<s0>Argentina</s0>
<s2>NG</s2>
<s5>62</s5>
</fC03>
<fC03 i1="13" i2="2" l="SPA">
<s0>Argentina</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>Pléistocène</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="07" i2="2" l="ENG">
<s0>Pleistocene</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="08" i2="2" l="FRE">
<s0>Quaternaire</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="08" i2="2" l="ENG">
<s0>Quaternary</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="08" i2="2" l="SPA">
<s0>Cuaternario</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>Amérique du Sud</s0>
<s2>564</s2>
</fC07>
<fC07 i1="11" i2="2" l="ENG">
<s0>South America</s0>
<s2>564</s2>
</fC07>
<fC07 i1="11" i2="2" l="SPA">
<s0>America del sur</s0>
<s2>564</s2>
</fC07>
<fN21>
<s1>327</s1>
</fN21>
</pA>
</standard>
<server>
<NO>PASCAL 09-0450878 INIST</NO>
<ET>(A new species of Neuryurus Ameghino (Mammalia, Glyptodontidae) from the late Pleistocene of the Mesopotamic region of Argentina)</ET>
<ST>Una nueva especie de Neuryurus Ameghino (Mammalia, Glyptodontidae) en el Pleistoceno tardío de la Mesopotamia de Argentina</ST>
<AU>EDUARDO ZURITA (Alfredo); SOLEDAD FERRERO (Brenda)</AU>
<AF>Centro de Ecología Aplicada del Litoral (CECOAL-CONICET), Universidad Nacional del Nordeste (UNNE), Ruta 5, km 2,5 CC/128 (3400) Corrientes/Argentine (1 aut.); Laboratorio de Paleontología de Vertebrados, CICYTTP-COMCEI Materi y España, (3105) Diamante, Entre Ríos/Argentine (2 aut.)</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>Geobios : (Lyon); ISSN 0016-6995; France; Da. 2009; Vol. 42; No. 5; Pp. 663-673; Abs. anglais/français; Bibl. 1 p.3/4</SO>
<LA>Espagnol</LA>
<EA>Among the South American Pleistocene Glyptodontidae (Xenarthra, Cingulata), one of the most scarcely represented genus in the fossil record is Neuryurus Ameghino, in which the only well characterized species, until now, is Neuryurus rudis (Gervais), coming from the Ensenadan (early-middle Pleistocene) of the Pampean region, Argentina. In this contribution, we report and describe a new species of Neuryurus, coming from the Arroyo Feliciano Formation (early Lujanian; ca. 130 ka), Entre Rios province, Argentina, in a particular palaebiogeographic context, more associated with the western sector of Uruguay and southern Brazil than the Pampean region. From a morphological perspective, this new taxon is characterized by: (a) the remarkable development of the foramina at the exposed surface of the osteoderms of the dorsal carapace, showing un aspect almost spongy; (b) the large diameter of the perforations observed in the ventral surface of the osteoderms, resembling to those present in the dorsal surface of the osteoderms of the Glyptodontidae Doedicurinae; (c) the evident thickness of the osteoderms, as in Glyptodon Owen; (d) area of contact and articulation of adjacent osteoderms very denticulate, with deep osseous interdigitating projections, as in Glyptodon and Glyptotherium Osborn, but here more evident; (e) larger osteoderms of the dorsal carapace showing, in the dorsal surface, many little conical tubercles, having some resemblance to Panochthus tuberculatus Burmeister. The presence of this new species in the early late Pleistocene of the Mesopotamic region is another element that adds to the biogeographical characterization of this particular area, especially evident during the warm and humid pulses of the late Pleistocene. In turn, this species represents the most complete record of the genus outside the Pampean region and partially complete the stratigraphic and geographic distribution of the genus.</EA>
<CC>001E01Q04; 001E01P02; 227A04; 226C02</CC>
<FD>Mammalia; Biostratigraphie; Xenarthra; Taxon nouveau; Taxinomie; Biogéographie; Pléistocène sup; Paléobiogéographie; Province Entre Rios; Formation Arroyo Feliciano; Cingulata; Neuryurini; Argentine</FD>
<FG>Tetrapoda; Vertebrata; Chordata; Edentata; Eutheria; Theria; Pléistocène; Quaternaire; Cénozoïque; Phanérozoïque; Amérique du Sud</FG>
<ED>Mammalia; biostratigraphy; Xenarthra; new taxa; taxonomy; biogeography; upper Pleistocene; paleobiogeography; Argentina</ED>
<EG>Tetrapoda; Vertebrata; Chordata; Edentata; Eutheria; Theria; Pleistocene; Quaternary; Cenozoic; Phanerozoic; South America</EG>
<SD>Mammalia; Bioestratigrafía; Xenarthra; Nuevo taxón; Taxonomía; Biogeografía; Argentina</SD>
<LO>INIST-14199.354000171136070090</LO>
<ID>09-0450878</ID>
</server>
</inist>
</record>

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