Please use this identifier to cite or link to this item: http://repositorio.unicamp.br/jspui/handle/REPOSIP/92748
Type: Artigo de periódico
Title: Double Aneuploidy (48,xxy,+21) Of Maternal Origin In A Child Born To A 13-year-old Mother: Evaluation Of The Maternal Folate Metabolism
Author: Biselli J.M.
Machado F.B.
Zampieri B.L.
Alves Da Silva A.F.
Goloni-Bertollo E.M.
Haddad R.
Eberlin M.N.
Vannucchi H.
Carvalho V.M.
Medina-Acosta E.
Pavarino-Bertelli E.C.
Abstract: The occurrence of non-mosaic double trisomy is exceptional in newborns. In this paper, a 48,XXY,+21 child, the parental origin of the extra chromosomes and the evaluation of the maternal folate metabolism are presented. The infant was born to a 13-year-old mother and presented with the typical clinical features of Down syndrome (DS). The origin of the additional chromosomes was maternal and most likely resulted from errors during the first meiotic division. Molecular analysis of 12 genetic polymorphisms involved in the folate metabolism revealed that the mother is heterozygous for the MTHFR C677T and TC2 A67G polymorphisms, and homozygous for the mutant MTRR A66G polymorphism. The maternal homocysteine concentration was 4.7 μmol/L, a value close to the one considered as a risk factor for DS in our previous study. Plasma methylmalonic acid and serum folate concentrations were 0.17 μmol/L and 18.4 ng/mL, respectively. It is possible that the presence of allelic variants for the folate metabolism and Hcy concentration might have favored errors in chromosomal disjunction during gametogenesis in this young mother. To our knowledge, this is the first patient with non-mosaic Down-Klinefelter born to a teenage mother, resulting from a rare fertilization event combining an abnormal 25,XX,+21 oocyte and a 23,Y spermatozoon.
Editor: 
Rights: fechado
Identifier DOI: 
Address: http://www.scopus.com/inward/record.url?eid=2-s2.0-70350180124&partnerID=40&md5=68753f33fb8b7ef9aa6aaa760db0c55b
Date Issue: 2009
Appears in Collections:Unicamp - Artigos e Outros Documentos

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