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Placentation in the rock cavy, Kerodon rupestris (Wied)

dc.contributor.authorOliveira, M. F.
dc.contributor.authorCarter, A. M.
dc.contributor.authorBonatelli, M.
dc.contributor.authorAmbrosio, C. E.
dc.contributor.authorMiglino, M. A.
dc.contributor.institutionUniversidade de São Paulo (USP)
dc.contributor.institutionMossoro Super Sch Agr
dc.contributor.institutionUniv So Denmark
dc.contributor.institutionUniversidade Estadual Paulista (Unesp)
dc.date.accessioned2014-05-20T15:23:07Z
dc.date.available2014-05-20T15:23:07Z
dc.date.issued2006-01-01
dc.description.abstractRock cavies are rodents found in the semi-arid caatinga of Brazil. We studied the structure of the rock cavy placenta by light and transmission electron microscopy. The exchange area of the labyrinth was organized in lobes separated by interlobular areas. The interhaemal barrier was syncytial haemomonochorial. The syncytiotrophoblast had recesses in the basal membrane and some invaginations of the apical membrane, but transtrophoblastic channels could not be found. The interlobular regions comprised syncytiotrophoblast, enclosing maternal venous blood channels, and cytotrophoblast. There was a prominent subplacenta composed of cytotrophoblast and syncytiotrophoblast. Microvilli projected into spaces between the cytotrophoblasts and into lacunae within the syncytiotrophoblast. The yolk sac epithelium exhibited coated pits, endocytotic vesicles and larger vacuoles, consistent with a role in protein uptake from the uterine lumen. Tight junctions between these cells provided a barrier to diffusion by the intercellular route. The reproductive biology of the rock cavy differs from other members of the family, including the guinea pig, but the architecture of the placenta remains remarkably constant. (c) 2004 Elsevier Ltd. All rights reserved.en
dc.description.affiliationUniv São Paulo, Sch Vet Med, Dept Surg, São Paulo, Brazil
dc.description.affiliationMossoro Super Sch Agr, Rio Grande do Norte, Brazil
dc.description.affiliationUniv So Denmark, Dept Physiol & Pharmacol, Odense, Denmark
dc.description.affiliationPaulista State Univ, São Paulo, Brazil
dc.description.affiliationUnespPaulista State Univ, São Paulo, Brazil
dc.format.extent87-97
dc.identifierhttp://dx.doi.org/10.1016/j.placenta.2004.11.012
dc.identifier.citationPlacenta. London: W B Saunders Co Ltd, v. 27, n. 1, p. 87-97, 2006.
dc.identifier.doi10.1016/j.placenta.2004.11.012
dc.identifier.issn0143-4004
dc.identifier.urihttp://hdl.handle.net/11449/33965
dc.identifier.wosWOS:000233996200011
dc.language.isoeng
dc.publisherW B Saunders Co Ltd
dc.relation.ispartofPlacenta
dc.relation.ispartofjcr2.434
dc.relation.ispartofsjr1,223
dc.rights.accessRightsAcesso restrito
dc.sourceWeb of Science
dc.subjecthystricomorphpt
dc.subjecthystricognathpt
dc.subjectrock cavypt
dc.subjectplacentapt
dc.subjectsubplacentapt
dc.subjectyolk sacpt
dc.subjectfetal membranespt
dc.subjectultrastructurept
dc.titlePlacentation in the rock cavy, Kerodon rupestris (Wied)en
dc.typeArtigo
dcterms.licensehttp://www.elsevier.com/about/open-access/open-access-policies/article-posting-policy
dcterms.rightsHolderW B Saunders Co Ltd
dspace.entity.typePublication

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