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1. Identity statement
Reference TypeJournal Article
Sitemtc-m21b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP3W34P/3PP9FEP
Repositorysid.inpe.br/mtc-m21b/2017/10.06.11.50   (restricted access)
Last Update2017:10.06.11.50.54 (UTC) administrator
Metadata Repositorysid.inpe.br/mtc-m21b/2017/10.06.11.50.54
Metadata Last Update2018:06.04.02.27.55 (UTC) administrator
DOI10.1016/j.jsames.2017.08.007
ISSN0895-9811
Citation KeyGandiniRossGuimGoes:2017:MiWaEs
TitleA Miocene wave-dominated estuarine system in the Paraíba Basin, northeastern Brazil
Year2017
MonthNov.
Access Date2024, Apr. 20
Type of Workjournal article
Secondary TypePRE PI
Number of Files1
Size13436 KiB
2. Context
Author1 Gandini, Rosana
2 Rossetti, Dilce de Fátima
3 Guimaraes Netto, Renata
4 Goes, Ana Maria
Resume Identifier1
2 8JMKD3MGP5W/3C9JGTQ
Group1
2 DIDSR-CGOBT-INPE-MCTIC-GOV-BR
Affiliation1 Univesidade de São Paulo (USP)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
3 Universidade dos Sinos (UNISINOS)
4 Universidade de São Paulo (USP)
Author e-Mail Address1 gandini.rosana@usp.br
2 dilce.rossetti@inpe.br
3 nettorg@unisinos.br
4 goes@igc.usp.br
JournalJournal of South American Earth Sciences
Volume79
Pages267-280
Secondary MarkA1_INTERDISCIPLINAR A1_GEOGRAFIA A2_GEOCIÊNCIAS A2_ENGENHARIAS_III A2_CIÊNCIAS_AGRÁRIAS_I B1_ODONTOLOGIA B1_MEDICINA_II B1_CIÊNCIAS_AMBIENTAIS B1_BIODIVERSIDADE B1_ANTROPOLOGIA_/_ARQUEOLOGIA B2_QUÍMICA B2_MATERIAIS B2_CIÊNCIAS_BIOLÓGICAS_I B3_ASTRONOMIA_/_FÍSICA C_ENGENHARIAS_II
History (UTC)2017-10-06 11:50:54 :: simone -> administrator ::
2017-10-06 11:50:54 :: administrator -> simone :: 2017
2017-10-06 11:55:25 :: simone -> administrator :: 2017
2018-06-04 02:27:55 :: administrator -> simone :: 2017
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
KeywordsMioceneBarreiras FormationParaíba BasinEstuarySea level
AbstractA number of publications have documented the effect of the Miocene transgression on several coasts of the world. However, this event is incompletely documented along the Brazilian margin, despite the existence of an impressive record of Miocene deposits exposed mostly as several coastal cliffs along more than 5000 km of distance. The transgressive nature of Miocene deposits, so far recognized only in a few localities of northeastern Brazil, needs to be amplified in order to better characterize the impact of the Miocene transgression in eastern South America. In this work, we provide facies analysis of early/middle Miocene strata exposed in the Paraíba Basin, northeastern Brazil, aiming reconstruct the depositional paleoenvironments and analyze their evolution within the context of relative sea-level fluctuations data. The results revealed deposits characterized by several features that were related to the action of tidal currents, such as alternating thicker/thinner forest packages, abundant reactivation surfaces, mud drapes and oppositely-dipping (herringbone) cross sets. These sedimentary structures were associated with an ichnological assemblage indicative of marine-influenced and brackish water, best represented by Ophiomorpha, Planolites-Palaeophycus-Thalassinoides and Thallassinoides-Planolites-Palaeophycus ichnofabrics. Sedimentation occurred in environments consisting of estuarine channel, estuarine central basin, tidal inlet/tidal channel, tidal delta/washover, tidal flat/shoal and foreshore, which were related to an estuarine setting, at least in part of a wave-dominated type. Analysis of facies stratal patterns led to suggest that the estuarine deposits of the Paraíba Basin reflect a rise in relative sea level probably during the transgressive and/or highstand stage of a depositional sequence formed directly overlying Cretaceous rocks. This rise can be correlated with the worldwide early/mid Miocene marine transgression. However, while the eustatic sea level remained rising through the middle Miocene, the estuarine sedimentation in the study area was cut off, being replaced by a regional unconformity marked by lateritic paleosols. Thus, a relative sea-level fall is recorded in the Paraíba Basin while the eustatic sea level remained rising through the middle Miocene, before its fall in the Tortonian. It follows that other factors, such as tectonics, is proposed to explain the mid-Miocene fall in sea level along the Paraíba coast, while the eustatic sea level was rising.
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Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSR > A Miocene wave-dominated...
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4. Conditions of access and use
Languageen
Target Filegandini_miocene.pdf
User Groupsimone
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Visibilityshown
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5. Allied materials
Next Higher Units8JMKD3MGPCW/3ER446E
Citing Item Listsid.inpe.br/mtc-m21/2012/07.13.14.44.37 2
sid.inpe.br/bibdigital/2013/09.13.21.11 2
DisseminationWEBSCI; PORTALCAPES; COMPENDEX; SCOPUS.
Host Collectionsid.inpe.br/mtc-m21b/2013/09.26.14.25.20
6. Notes
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