Close

1. Identity statement
Reference TypeJournal Article
Siteplutao.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP3W/3FCL46Q
Repositorysid.inpe.br/plutao/2013/12.12.15.22.52   (restricted access)
Last Update2014:03.27.12.40.13 (UTC) administrator
Metadata Repositorysid.inpe.br/plutao/2013/12.12.15.22.53
Metadata Last Update2018:06.04.23.39.14 (UTC) administrator
DOI10.1007/s00024-013-0726-2
ISSN0033-4553
Labellattes: 9831996893882845 5 PrestesRNEVSWG:2013:EvSoAc
Citation KeyPrestesRNEVEWG:2013:EvSoAc
TitleImprint of climate variability on mesozoic fossil tree rings: evidences of solar activity signals on environmental records around 200 million years ago?
ProjectFAPESP (2009/02907-8); CNPq (309092/2010-8); CNPq (APQ 470605/2012-0; 303368/2012- 8); CNPq (304368/2013-0); CNPQ/PQ (301233/2011-0); FAPESP (2012/066734).
Year2013
MonthNov.
Access Date2024, May 16
Type of Workjournal article
Secondary TypePRE PI
Number of Files1
Size424 KiB
2. Context
Author1 Prestes, Alan
2 Rigozo, Nivaor Rodolfo
3 Nordemann, Daniel Jean R.
4 Echer, Ezequiel
5 Vieira, Luis Eduardo Antunes
6 Echer, Mariza Pereira de Souza
7 Wrasse, Cristiano Max
8 Guarnieri, F. L.
Resume Identifier1
2
3
4 8JMKD3MGP5W/3C9JH3D
Group1
2 DGE-CEA-INPE-MCTI-GOV-BR
3
4 DGE-CEA-INPE-MCTI-GOV-BR
5 DGE-CEA-INPE-MCTI-GOV-BR
6 DGE-CEA-INPE-MCTI-GOV-BR
7 DAE-CEA-INPE-MCTI-GOV-BR
Affiliation1 Universidade do Vale do Paraíba
2 Instituto Nacional de Pesquisas Espaciais (INPE)
3
4 Instituto Nacional de Pesquisas Espaciais (INPE)
5 Instituto Nacional de Pesquisas Espaciais (INPE)
6 Instituto Nacional de Pesquisas Espaciais (INPE)
7 Instituto Nacional de Pesquisas Espaciais (INPE)
8 Vale Soluções em Energia
Author e-Mail Address1 aprestes@gmail.com
2 rodolfo@dge.inpe.br
3
4 eecher@dge.inpe.br
5 luis.vieira@inpe.br
6 mariza.echer@inpe.br
7 cristiano.wrasse@inpe.br
e-Mail Addressluis.vieira71@googlemail.com
JournalPure and Applied Geophysics
Volume.
Pages.
Secondary MarkA2
History (UTC)2013-12-12 18:00:28 :: lattes -> administrator :: 2013
2013-12-12 18:16:15 :: administrator -> lattes :: 2013
2013-12-12 18:23:25 :: lattes -> administrator :: 2013
2018-06-04 23:39:14 :: administrator -> marcelo.pazos@inpe.br :: 2013
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
Keywordssolar–planetary relationships
tree-ring data
fossil (Mesozoic)
time series
spectral analysis
solar evolution
AbstractEvidence of the solar activity modulation of the Earths climate has been observed on several parameters, from decadal to millennial time scales. Several proxies have been used to reconstruct the paleoclimate as well as the solar activity. The paleoclimate reconstructions are based on direct and/or indirect effects of global and regional climate conditions. The solar activity reconstructions are based on the production of the 14C isotope due to the interaction of cosmic ray flux and the Earths atmosphere. Because trees respond to climate conditions and store 14 C, they have been used as proxies for both for climate and solar activity reconstructions. The imprints of solar activity cycles dating back to 10,000 years ago have been observed on tree-ring samples using 14 C data, and those dating back to 20 million years ago have been analyzed using fossil tree-growth rings. All this corresponds to the Cenozoic era. However, solar activity imprints on tree rings from earlier than that era have not been investigated yet. In this work, we showed that tree rings from the Mesozoic Era (of ~ 200 million years ago) recorded 11- and 22-year cycles, which may be related to solar activity cycles, and that were statistically significant at the 95 % confidence level. The fossil wood was collected in the southern region of Brazil. Our analysis of the fossils tree-ring width series power spectra showed characteristics similar to the modern araucaria tree, with a noticeable decadal periodicity. Assuming that the Earths climate responds to solar variability and that responses did not vary significantly over the last ~ 200 million years, we conclude that the solarclimate connection was likely present during the Mesozoic era.
AreaCEA
Arrangement 1urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDAE > Imprint of climate...
Arrangement 2urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDGE > Imprint of climate...
doc Directory Contentaccess
source Directory Contentthere are no files
agreement Directory Contentthere are no files
4. Conditions of access and use
Languageen
Target Filemata-publicado.pdf
User Grouplattes
marcelo.pazos@inpe.br
self-uploading-INPE-MCTI-GOV-BR
Reader Groupadministrator
marcelo.pazos@inpe.br
Visibilityshown
Archiving Policydenypublisher denyfinaldraft12
Read Permissiondeny from all and allow from 150.163
Update Permissionnot transferred
5. Allied materials
Mirror Repositoryiconet.com.br/banon/2006/11.26.21.31
Next Higher Units8JMKD3MGPCW/3ETL868
8JMKD3MGPCW/3EU29DP
Citing Item Listsid.inpe.br/bibdigital/2013/09.29.20.43 1
sid.inpe.br/mtc-m21/2012/07.13.14.45.47 1
DisseminationWEBSCI; PORTALCAPES; COMPENDEX; SCOPUS.
Host Collectiondpi.inpe.br/plutao@80/2008/08.19.15.01
6. Notes
Empty Fieldsalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel format isbn lineage mark nextedition notes number orcid parameterlist parentrepositories previousedition previouslowerunit progress rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype url
7. Description control
e-Mail (login)marcelo.pazos@inpe.br
update 


Close