Ediacaran paleoenvironmental changes recorded in the mixed carbonate-siliciclastic Bambui Basin, Brazil
Autor(a) principal: | |
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Data de Publicação: | 2019 |
Outros Autores: | , , , , , |
Tipo de documento: | Artigo |
Idioma: | eng |
Título da fonte: | Repositório Institucional da UNESP |
Texto Completo: | http://dx.doi.org/10.1016/j.palaeo.2018.12.022 http://hdl.handle.net/11449/185405 |
Resumo: | Significant Ediacaran paleoenvironmental changes recorded in the mixed carbonate-siliciclastic Bambui Basin, east-central Brazil, outcrop in one of the best-preserved sites, the Januaria paleo-high. From a detailed strati graphic and chemostratigraphic approach (carbon and oxygen isotopes, total organic carbon, total sulfur and selected elements abundances), we identified transgressive-regressive intervals and depositional settings within the Barnhill Group stratigraphy and developed a new model for the origin of the extremely positive Middle Bambui Excursion (MIBE) present in the middle section of the basin. A post-Marinoan cap carbonate interval is recorded in the first similar to 10 m, preserving aragonite pseudomorph fans, barite-rich layers and negative delta C-13 anomaly. A hiatus separates the cap carbonate from the late Ediacaran succession that makes up the remaining Bambui Group. The younger intervals preserve both siliciclastic (middle Serra de Santa Helena Formation) and carbonate (middle/upper Sete Lagoas and Lagoa do Jacare formations) shallow-water depositional settings, requiring tectonic influence or climatic changes in source areas. The MIBE yields delta C-13 values as high as +14 parts per thousand and extends for about 350 m, from the upper Sete Lagoas Formation to the lower Serra da Saudade Formation. We suggest a model of a restricted basin setting that favored local carbon isotopic signals in the delta C-13 record of sedimentary carbonates through preferential weathering of ancient carbonate platforms on the continent and higher burial rate of authigenic carbonate. This scenario caused the global delta C-13 budget to be affected by an offset of, at least, + 4 parts per thousand in sedimentary carbonates deposited on the Sao Francisco craton and along its margin during the terminal Ediacaran. Many previous studies suggested a restricted nature for the middle Bambui Basin, which probably resulted from the central position of the Sao Francisco paleocontinent within the mosaic of collisional blocks during the SW Gondwana amalgamation. |
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Ediacaran paleoenvironmental changes recorded in the mixed carbonate-siliciclastic Bambui Basin, BrazilWest GondwanaPaleogeographyDepositional settingsChemostratigraphyCarbon isotope excursionCarbon burialSignificant Ediacaran paleoenvironmental changes recorded in the mixed carbonate-siliciclastic Bambui Basin, east-central Brazil, outcrop in one of the best-preserved sites, the Januaria paleo-high. From a detailed strati graphic and chemostratigraphic approach (carbon and oxygen isotopes, total organic carbon, total sulfur and selected elements abundances), we identified transgressive-regressive intervals and depositional settings within the Barnhill Group stratigraphy and developed a new model for the origin of the extremely positive Middle Bambui Excursion (MIBE) present in the middle section of the basin. A post-Marinoan cap carbonate interval is recorded in the first similar to 10 m, preserving aragonite pseudomorph fans, barite-rich layers and negative delta C-13 anomaly. A hiatus separates the cap carbonate from the late Ediacaran succession that makes up the remaining Bambui Group. The younger intervals preserve both siliciclastic (middle Serra de Santa Helena Formation) and carbonate (middle/upper Sete Lagoas and Lagoa do Jacare formations) shallow-water depositional settings, requiring tectonic influence or climatic changes in source areas. The MIBE yields delta C-13 values as high as +14 parts per thousand and extends for about 350 m, from the upper Sete Lagoas Formation to the lower Serra da Saudade Formation. We suggest a model of a restricted basin setting that favored local carbon isotopic signals in the delta C-13 record of sedimentary carbonates through preferential weathering of ancient carbonate platforms on the continent and higher burial rate of authigenic carbonate. This scenario caused the global delta C-13 budget to be affected by an offset of, at least, + 4 parts per thousand in sedimentary carbonates deposited on the Sao Francisco craton and along its margin during the terminal Ediacaran. Many previous studies suggested a restricted nature for the middle Bambui Basin, which probably resulted from the central position of the Sao Francisco paleocontinent within the mosaic of collisional blocks during the SW Gondwana amalgamation.Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)Fundação de Amparo à Pesquisa do Estado de Minas Gerais (FAPEMIG)Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)Univ Fed Minas Gerais, Inst Geociencias, Ctr Pesquisas Manoel Teixeira Costa, Campus Pampulha,Av Antonio Carlos 6627, BR-31270901 Belo Horizonte, MG, BrazilUniv Estado Rio De Janeiro, Fac Geol, Dept Paleontol & Estratig, Av Sao Francisco Xavier 524, BR-20550013 Rio De Janeiro, RJ, BrazilUniv Estadual Paulista, Dept Geol Aplicada, Inst Geociencias & Ciencias Exatas, Ave 24A,1515, BR-13506900 Rio Claro, SP, BrazilUniv Fed Pernambuco, NEG LABISE, Dept Geol, Av Arquitetura S-N, BR-50670901 Recife, PE, BrazilUniv Estadual Paulista, Dept Geol Aplicada, Inst Geociencias & Ciencias Exatas, Ave 24A,1515, BR-13506900 Rio Claro, SP, BrazilCNPq: 447449/2014-1CNPq: 444070/2014-1FAPEMIG: APQ-01711-14FAPEMIG: APQ-00914-14FAPEMIG: PPM-00539-15FAPESP: 2015/07391-0Elsevier B.V.Universidade Federal de Minas Gerais (UFMG)Universidade do Estado do Rio de Janeiro (UERJ)Universidade Estadual Paulista (Unesp)Universidade Federal de Pernambuco (UFPE)Uhlein, Gabriel J.Uhlein, AlexandrePereira, EgbertoCaxito, Fabricio A.Okubo, Juliana [UNESP]Warren, Lucas V. [UNESP]Sial, Alcides N.2019-10-04T12:35:14Z2019-10-04T12:35:14Z2019-03-01info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/article39-51http://dx.doi.org/10.1016/j.palaeo.2018.12.022Palaeogeography Palaeoclimatology Palaeoecology. Amsterdam: Elsevier Science Bv, v. 517, p. 39-51, 2019.0031-0182http://hdl.handle.net/11449/18540510.1016/j.palaeo.2018.12.022WOS:000457815500004Web of Sciencereponame:Repositório Institucional da UNESPinstname:Universidade Estadual Paulista (UNESP)instacron:UNESPengPalaeogeography Palaeoclimatology Palaeoecologyinfo:eu-repo/semantics/openAccess2021-10-23T12:24:10Zoai:repositorio.unesp.br:11449/185405Repositório InstitucionalPUBhttp://repositorio.unesp.br/oai/requestopendoar:29462024-08-05T18:20:38.417186Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)false |
dc.title.none.fl_str_mv |
Ediacaran paleoenvironmental changes recorded in the mixed carbonate-siliciclastic Bambui Basin, Brazil |
title |
Ediacaran paleoenvironmental changes recorded in the mixed carbonate-siliciclastic Bambui Basin, Brazil |
spellingShingle |
Ediacaran paleoenvironmental changes recorded in the mixed carbonate-siliciclastic Bambui Basin, Brazil Uhlein, Gabriel J. West Gondwana Paleogeography Depositional settings Chemostratigraphy Carbon isotope excursion Carbon burial |
title_short |
Ediacaran paleoenvironmental changes recorded in the mixed carbonate-siliciclastic Bambui Basin, Brazil |
title_full |
Ediacaran paleoenvironmental changes recorded in the mixed carbonate-siliciclastic Bambui Basin, Brazil |
title_fullStr |
Ediacaran paleoenvironmental changes recorded in the mixed carbonate-siliciclastic Bambui Basin, Brazil |
title_full_unstemmed |
Ediacaran paleoenvironmental changes recorded in the mixed carbonate-siliciclastic Bambui Basin, Brazil |
title_sort |
Ediacaran paleoenvironmental changes recorded in the mixed carbonate-siliciclastic Bambui Basin, Brazil |
author |
Uhlein, Gabriel J. |
author_facet |
Uhlein, Gabriel J. Uhlein, Alexandre Pereira, Egberto Caxito, Fabricio A. Okubo, Juliana [UNESP] Warren, Lucas V. [UNESP] Sial, Alcides N. |
author_role |
author |
author2 |
Uhlein, Alexandre Pereira, Egberto Caxito, Fabricio A. Okubo, Juliana [UNESP] Warren, Lucas V. [UNESP] Sial, Alcides N. |
author2_role |
author author author author author author |
dc.contributor.none.fl_str_mv |
Universidade Federal de Minas Gerais (UFMG) Universidade do Estado do Rio de Janeiro (UERJ) Universidade Estadual Paulista (Unesp) Universidade Federal de Pernambuco (UFPE) |
dc.contributor.author.fl_str_mv |
Uhlein, Gabriel J. Uhlein, Alexandre Pereira, Egberto Caxito, Fabricio A. Okubo, Juliana [UNESP] Warren, Lucas V. [UNESP] Sial, Alcides N. |
dc.subject.por.fl_str_mv |
West Gondwana Paleogeography Depositional settings Chemostratigraphy Carbon isotope excursion Carbon burial |
topic |
West Gondwana Paleogeography Depositional settings Chemostratigraphy Carbon isotope excursion Carbon burial |
description |
Significant Ediacaran paleoenvironmental changes recorded in the mixed carbonate-siliciclastic Bambui Basin, east-central Brazil, outcrop in one of the best-preserved sites, the Januaria paleo-high. From a detailed strati graphic and chemostratigraphic approach (carbon and oxygen isotopes, total organic carbon, total sulfur and selected elements abundances), we identified transgressive-regressive intervals and depositional settings within the Barnhill Group stratigraphy and developed a new model for the origin of the extremely positive Middle Bambui Excursion (MIBE) present in the middle section of the basin. A post-Marinoan cap carbonate interval is recorded in the first similar to 10 m, preserving aragonite pseudomorph fans, barite-rich layers and negative delta C-13 anomaly. A hiatus separates the cap carbonate from the late Ediacaran succession that makes up the remaining Bambui Group. The younger intervals preserve both siliciclastic (middle Serra de Santa Helena Formation) and carbonate (middle/upper Sete Lagoas and Lagoa do Jacare formations) shallow-water depositional settings, requiring tectonic influence or climatic changes in source areas. The MIBE yields delta C-13 values as high as +14 parts per thousand and extends for about 350 m, from the upper Sete Lagoas Formation to the lower Serra da Saudade Formation. We suggest a model of a restricted basin setting that favored local carbon isotopic signals in the delta C-13 record of sedimentary carbonates through preferential weathering of ancient carbonate platforms on the continent and higher burial rate of authigenic carbonate. This scenario caused the global delta C-13 budget to be affected by an offset of, at least, + 4 parts per thousand in sedimentary carbonates deposited on the Sao Francisco craton and along its margin during the terminal Ediacaran. Many previous studies suggested a restricted nature for the middle Bambui Basin, which probably resulted from the central position of the Sao Francisco paleocontinent within the mosaic of collisional blocks during the SW Gondwana amalgamation. |
publishDate |
2019 |
dc.date.none.fl_str_mv |
2019-10-04T12:35:14Z 2019-10-04T12:35:14Z 2019-03-01 |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
http://dx.doi.org/10.1016/j.palaeo.2018.12.022 Palaeogeography Palaeoclimatology Palaeoecology. Amsterdam: Elsevier Science Bv, v. 517, p. 39-51, 2019. 0031-0182 http://hdl.handle.net/11449/185405 10.1016/j.palaeo.2018.12.022 WOS:000457815500004 |
url |
http://dx.doi.org/10.1016/j.palaeo.2018.12.022 http://hdl.handle.net/11449/185405 |
identifier_str_mv |
Palaeogeography Palaeoclimatology Palaeoecology. Amsterdam: Elsevier Science Bv, v. 517, p. 39-51, 2019. 0031-0182 10.1016/j.palaeo.2018.12.022 WOS:000457815500004 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
Palaeogeography Palaeoclimatology Palaeoecology |
dc.rights.driver.fl_str_mv |
info:eu-repo/semantics/openAccess |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
39-51 |
dc.publisher.none.fl_str_mv |
Elsevier B.V. |
publisher.none.fl_str_mv |
Elsevier B.V. |
dc.source.none.fl_str_mv |
Web of Science reponame:Repositório Institucional da UNESP instname:Universidade Estadual Paulista (UNESP) instacron:UNESP |
instname_str |
Universidade Estadual Paulista (UNESP) |
instacron_str |
UNESP |
institution |
UNESP |
reponame_str |
Repositório Institucional da UNESP |
collection |
Repositório Institucional da UNESP |
repository.name.fl_str_mv |
Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP) |
repository.mail.fl_str_mv |
|
_version_ |
1808128922594836480 |