Dating stalagmite from Caverna do Diabo (Devil´S Cave) by TL and EPR techniques

Detalhes bibliográficos
Autor(a) principal: WATANABE,SHIGUEO
Data de Publicação: 2016
Outros Autores: CANO,NILO F., RAO,T.K. GUNDU, SILVA-CARRERA,BETZABEL N., CARMO,LUCAS S., QUINA,ANTONIO J.A., GENNARI,ROSELI F., MUNITA,CASIMIRO S., AYALA-ARENAS,JORGE S., FERNANDES,BRUNO G.
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Anais da Academia Brasileira de Ciências (Online)
Texto Completo: http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652016000602137
Resumo: ABSTRACT A cylindrical fragment of stalagmite from Caverna do Diabo, State of São Paulo, Brazil, has been studied and dated by thermoluminescence and electron paramagnetic resonance techniques. The thermoluminescence glow curves of stalagmite samples and subsequently gamma irradiated, have shown rise of three peaks at 135, 180 and 265 °C. From electron paramagnetic resonance spectra of stalagmite was possible to clearly identify three paramagnetic centers in the g = 2.0 region: Centers I, II and III are due to , and , respectively. The additive method was applied to calculate the accumulated dose using thermoluminescence peak at 265 °C and the electron paramagnetic resonance signal at g = 1.9973 of CO- 2 radical. The ages of the different slices of stalagmite were determined from the Dac- values and Dan- value, obtaining an average of 86410 for central slice, 53421 for second slice, 31490 for third slice and 46390 years B.P. for the central region of upper end.
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spelling Dating stalagmite from Caverna do Diabo (Devil´S Cave) by TL and EPR techniquesstalagmiteCaverna do DiabodatingTLEPRABSTRACT A cylindrical fragment of stalagmite from Caverna do Diabo, State of São Paulo, Brazil, has been studied and dated by thermoluminescence and electron paramagnetic resonance techniques. The thermoluminescence glow curves of stalagmite samples and subsequently gamma irradiated, have shown rise of three peaks at 135, 180 and 265 °C. From electron paramagnetic resonance spectra of stalagmite was possible to clearly identify three paramagnetic centers in the g = 2.0 region: Centers I, II and III are due to , and , respectively. The additive method was applied to calculate the accumulated dose using thermoluminescence peak at 265 °C and the electron paramagnetic resonance signal at g = 1.9973 of CO- 2 radical. The ages of the different slices of stalagmite were determined from the Dac- values and Dan- value, obtaining an average of 86410 for central slice, 53421 for second slice, 31490 for third slice and 46390 years B.P. for the central region of upper end.Academia Brasileira de Ciências2016-12-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersiontext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652016000602137Anais da Academia Brasileira de Ciências v.88 n.4 2016reponame:Anais da Academia Brasileira de Ciências (Online)instname:Academia Brasileira de Ciências (ABC)instacron:ABC10.1590/0001-3765201620150755info:eu-repo/semantics/openAccessWATANABE,SHIGUEOCANO,NILO F.RAO,T.K. GUNDUSILVA-CARRERA,BETZABEL N.CARMO,LUCAS S.QUINA,ANTONIO J.A.GENNARI,ROSELI F.MUNITA,CASIMIRO S.AYALA-ARENAS,JORGE S.FERNANDES,BRUNO G.eng2017-06-12T00:00:00Zoai:scielo:S0001-37652016000602137Revistahttp://www.scielo.br/aabchttps://old.scielo.br/oai/scielo-oai.php||aabc@abc.org.br1678-26900001-3765opendoar:2017-06-12T00:00Anais da Academia Brasileira de Ciências (Online) - Academia Brasileira de Ciências (ABC)false
dc.title.none.fl_str_mv Dating stalagmite from Caverna do Diabo (Devil´S Cave) by TL and EPR techniques
title Dating stalagmite from Caverna do Diabo (Devil´S Cave) by TL and EPR techniques
spellingShingle Dating stalagmite from Caverna do Diabo (Devil´S Cave) by TL and EPR techniques
WATANABE,SHIGUEO
stalagmite
Caverna do Diabo
dating
TL
EPR
title_short Dating stalagmite from Caverna do Diabo (Devil´S Cave) by TL and EPR techniques
title_full Dating stalagmite from Caverna do Diabo (Devil´S Cave) by TL and EPR techniques
title_fullStr Dating stalagmite from Caverna do Diabo (Devil´S Cave) by TL and EPR techniques
title_full_unstemmed Dating stalagmite from Caverna do Diabo (Devil´S Cave) by TL and EPR techniques
title_sort Dating stalagmite from Caverna do Diabo (Devil´S Cave) by TL and EPR techniques
author WATANABE,SHIGUEO
author_facet WATANABE,SHIGUEO
CANO,NILO F.
RAO,T.K. GUNDU
SILVA-CARRERA,BETZABEL N.
CARMO,LUCAS S.
QUINA,ANTONIO J.A.
GENNARI,ROSELI F.
MUNITA,CASIMIRO S.
AYALA-ARENAS,JORGE S.
FERNANDES,BRUNO G.
author_role author
author2 CANO,NILO F.
RAO,T.K. GUNDU
SILVA-CARRERA,BETZABEL N.
CARMO,LUCAS S.
QUINA,ANTONIO J.A.
GENNARI,ROSELI F.
MUNITA,CASIMIRO S.
AYALA-ARENAS,JORGE S.
FERNANDES,BRUNO G.
author2_role author
author
author
author
author
author
author
author
author
dc.contributor.author.fl_str_mv WATANABE,SHIGUEO
CANO,NILO F.
RAO,T.K. GUNDU
SILVA-CARRERA,BETZABEL N.
CARMO,LUCAS S.
QUINA,ANTONIO J.A.
GENNARI,ROSELI F.
MUNITA,CASIMIRO S.
AYALA-ARENAS,JORGE S.
FERNANDES,BRUNO G.
dc.subject.por.fl_str_mv stalagmite
Caverna do Diabo
dating
TL
EPR
topic stalagmite
Caverna do Diabo
dating
TL
EPR
description ABSTRACT A cylindrical fragment of stalagmite from Caverna do Diabo, State of São Paulo, Brazil, has been studied and dated by thermoluminescence and electron paramagnetic resonance techniques. The thermoluminescence glow curves of stalagmite samples and subsequently gamma irradiated, have shown rise of three peaks at 135, 180 and 265 °C. From electron paramagnetic resonance spectra of stalagmite was possible to clearly identify three paramagnetic centers in the g = 2.0 region: Centers I, II and III are due to , and , respectively. The additive method was applied to calculate the accumulated dose using thermoluminescence peak at 265 °C and the electron paramagnetic resonance signal at g = 1.9973 of CO- 2 radical. The ages of the different slices of stalagmite were determined from the Dac- values and Dan- value, obtaining an average of 86410 for central slice, 53421 for second slice, 31490 for third slice and 46390 years B.P. for the central region of upper end.
publishDate 2016
dc.date.none.fl_str_mv 2016-12-01
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652016000602137
url http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652016000602137
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv 10.1590/0001-3765201620150755
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv text/html
dc.publisher.none.fl_str_mv Academia Brasileira de Ciências
publisher.none.fl_str_mv Academia Brasileira de Ciências
dc.source.none.fl_str_mv Anais da Academia Brasileira de Ciências v.88 n.4 2016
reponame:Anais da Academia Brasileira de Ciências (Online)
instname:Academia Brasileira de Ciências (ABC)
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instname_str Academia Brasileira de Ciências (ABC)
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institution ABC
reponame_str Anais da Academia Brasileira de Ciências (Online)
collection Anais da Academia Brasileira de Ciências (Online)
repository.name.fl_str_mv Anais da Academia Brasileira de Ciências (Online) - Academia Brasileira de Ciências (ABC)
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