Goldilocks at the dawn of complex life: mountains might have damaged Ediacaran–Cambrian ecosystems and prompted an early Cambrian greenhouse world
Autor(a) principal: | |
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Data de Publicação: | 2021 |
Outros Autores: | , , , , , , , , , , |
Tipo de documento: | Artigo |
Idioma: | eng |
Título da fonte: | Repositório Institucional da UNESP |
Texto Completo: | http://dx.doi.org/10.1038/s41598-021-99526-z http://hdl.handle.net/11449/222607 |
Resumo: | We combine U–Pb in-situ carbonate dating, elemental and isotope constraints to calibrate the synergy of integrated mountain-basin evolution in western Gondwana. We show that deposition of the Bambuí Group coincides with closure of the Goiás-Pharusian (630–600 Ma) and Adamastor (585–530 Ma) oceans. Metazoans thrived for a brief moment of balanced redox and nutrient conditions. This was followed, however, by closure of the Clymene ocean (540–500 Ma), eventually landlocking the basin. This hindered seawater renewal and led to uncontrolled nutrient input, shallowing of the redoxcline and anoxic incursions, fueling positive productivity feedbacks and preventing the development of typical Ediacaran–Cambrian ecosystems. Thus, mountains provide the conditions, such as oxygen and nutrients, but may also preclude life development if basins become too restricted, characterizing a Goldilocks or optimal level effect. During the late Neoproterozoic-Cambrian fan-like transition from Rodinia to Gondwana, the newborn marginal basins of Laurentia, Baltica and Siberia remained open to the global sea, while intracontinental basins of Gondwana became progressively landlocked. The extent to which basin restriction might have affected the global carbon cycle and climate, e.g. through the input of gases such as methane that could eventually have collaborated to an early Cambrian greenhouse world, needs to be further considered. |
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Goldilocks at the dawn of complex life: mountains might have damaged Ediacaran–Cambrian ecosystems and prompted an early Cambrian greenhouse worldWe combine U–Pb in-situ carbonate dating, elemental and isotope constraints to calibrate the synergy of integrated mountain-basin evolution in western Gondwana. We show that deposition of the Bambuí Group coincides with closure of the Goiás-Pharusian (630–600 Ma) and Adamastor (585–530 Ma) oceans. Metazoans thrived for a brief moment of balanced redox and nutrient conditions. This was followed, however, by closure of the Clymene ocean (540–500 Ma), eventually landlocking the basin. This hindered seawater renewal and led to uncontrolled nutrient input, shallowing of the redoxcline and anoxic incursions, fueling positive productivity feedbacks and preventing the development of typical Ediacaran–Cambrian ecosystems. Thus, mountains provide the conditions, such as oxygen and nutrients, but may also preclude life development if basins become too restricted, characterizing a Goldilocks or optimal level effect. During the late Neoproterozoic-Cambrian fan-like transition from Rodinia to Gondwana, the newborn marginal basins of Laurentia, Baltica and Siberia remained open to the global sea, while intracontinental basins of Gondwana became progressively landlocked. The extent to which basin restriction might have affected the global carbon cycle and climate, e.g. through the input of gases such as methane that could eventually have collaborated to an early Cambrian greenhouse world, needs to be further considered.Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)Fundação de Amparo à Pesquisa do Estado de Minas Gerais (FAPEMIG)Instituto SerrapilheiraCPMTC Research Center Universidade Federal de Minas GeraisDepartamento de Geologia Universidade Federal de Ouro PretoDepartment of Geoscience and Natural Resource Management University of Copenhagen, Øster Voldgade 10NEG-LABISE Universidade Federal de PernambucoLaboratório de Estudos Geodinâmicos Geocronológicos E Ambientais Universidade de BrasíliaDepartment of Geology São Paulo State UniversityGeological Survey of Brazil – CPRMDepartment of Geology São Paulo State UniversityFAPESP: 2018/26230-6CNPq: 303566/2019-1FAPEMIG: PPM-00618-18Instituto Serrapilheira: Serra-1912-31510Universidade Federal de Minas Gerais (UFMG)Universidade Federal de Ouro PretoUniversity of CopenhagenUniversidade Federal de Pernambuco (UFPE)Universidade de Brasília (UnB)Universidade Estadual Paulista (UNESP)Geological Survey of Brazil – CPRMCaxito, FabricioLana, CristianoFrei, RobertUhlein, Gabriel J.Sial, Alcides N.Dantas, Elton L.Pinto, André G.Campos, Filippe C.Galvão, PauloWarren, Lucas V. [UNESP]Okubo, Juliana [UNESP]Ganade, Carlos E.2022-04-28T19:45:46Z2022-04-28T19:45:46Z2021-12-01info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articlehttp://dx.doi.org/10.1038/s41598-021-99526-zScientific Reports, v. 11, n. 1, 2021.2045-2322http://hdl.handle.net/11449/22260710.1038/s41598-021-99526-z2-s2.0-85116814342Scopusreponame:Repositório Institucional da UNESPinstname:Universidade Estadual Paulista (UNESP)instacron:UNESPengScientific Reportsinfo:eu-repo/semantics/openAccess2022-04-28T19:45:46Zoai:repositorio.unesp.br:11449/222607Repositório InstitucionalPUBhttp://repositorio.unesp.br/oai/requestopendoar:29462024-08-05T21:08:36.355425Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)false |
dc.title.none.fl_str_mv |
Goldilocks at the dawn of complex life: mountains might have damaged Ediacaran–Cambrian ecosystems and prompted an early Cambrian greenhouse world |
title |
Goldilocks at the dawn of complex life: mountains might have damaged Ediacaran–Cambrian ecosystems and prompted an early Cambrian greenhouse world |
spellingShingle |
Goldilocks at the dawn of complex life: mountains might have damaged Ediacaran–Cambrian ecosystems and prompted an early Cambrian greenhouse world Caxito, Fabricio |
title_short |
Goldilocks at the dawn of complex life: mountains might have damaged Ediacaran–Cambrian ecosystems and prompted an early Cambrian greenhouse world |
title_full |
Goldilocks at the dawn of complex life: mountains might have damaged Ediacaran–Cambrian ecosystems and prompted an early Cambrian greenhouse world |
title_fullStr |
Goldilocks at the dawn of complex life: mountains might have damaged Ediacaran–Cambrian ecosystems and prompted an early Cambrian greenhouse world |
title_full_unstemmed |
Goldilocks at the dawn of complex life: mountains might have damaged Ediacaran–Cambrian ecosystems and prompted an early Cambrian greenhouse world |
title_sort |
Goldilocks at the dawn of complex life: mountains might have damaged Ediacaran–Cambrian ecosystems and prompted an early Cambrian greenhouse world |
author |
Caxito, Fabricio |
author_facet |
Caxito, Fabricio Lana, Cristiano Frei, Robert Uhlein, Gabriel J. Sial, Alcides N. Dantas, Elton L. Pinto, André G. Campos, Filippe C. Galvão, Paulo Warren, Lucas V. [UNESP] Okubo, Juliana [UNESP] Ganade, Carlos E. |
author_role |
author |
author2 |
Lana, Cristiano Frei, Robert Uhlein, Gabriel J. Sial, Alcides N. Dantas, Elton L. Pinto, André G. Campos, Filippe C. Galvão, Paulo Warren, Lucas V. [UNESP] Okubo, Juliana [UNESP] Ganade, Carlos E. |
author2_role |
author author author author author author author author author author author |
dc.contributor.none.fl_str_mv |
Universidade Federal de Minas Gerais (UFMG) Universidade Federal de Ouro Preto University of Copenhagen Universidade Federal de Pernambuco (UFPE) Universidade de Brasília (UnB) Universidade Estadual Paulista (UNESP) Geological Survey of Brazil – CPRM |
dc.contributor.author.fl_str_mv |
Caxito, Fabricio Lana, Cristiano Frei, Robert Uhlein, Gabriel J. Sial, Alcides N. Dantas, Elton L. Pinto, André G. Campos, Filippe C. Galvão, Paulo Warren, Lucas V. [UNESP] Okubo, Juliana [UNESP] Ganade, Carlos E. |
description |
We combine U–Pb in-situ carbonate dating, elemental and isotope constraints to calibrate the synergy of integrated mountain-basin evolution in western Gondwana. We show that deposition of the Bambuí Group coincides with closure of the Goiás-Pharusian (630–600 Ma) and Adamastor (585–530 Ma) oceans. Metazoans thrived for a brief moment of balanced redox and nutrient conditions. This was followed, however, by closure of the Clymene ocean (540–500 Ma), eventually landlocking the basin. This hindered seawater renewal and led to uncontrolled nutrient input, shallowing of the redoxcline and anoxic incursions, fueling positive productivity feedbacks and preventing the development of typical Ediacaran–Cambrian ecosystems. Thus, mountains provide the conditions, such as oxygen and nutrients, but may also preclude life development if basins become too restricted, characterizing a Goldilocks or optimal level effect. During the late Neoproterozoic-Cambrian fan-like transition from Rodinia to Gondwana, the newborn marginal basins of Laurentia, Baltica and Siberia remained open to the global sea, while intracontinental basins of Gondwana became progressively landlocked. The extent to which basin restriction might have affected the global carbon cycle and climate, e.g. through the input of gases such as methane that could eventually have collaborated to an early Cambrian greenhouse world, needs to be further considered. |
publishDate |
2021 |
dc.date.none.fl_str_mv |
2021-12-01 2022-04-28T19:45:46Z 2022-04-28T19:45:46Z |
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/10.1038/s41598-021-99526-z Scientific Reports, v. 11, n. 1, 2021. 2045-2322 http://hdl.handle.net/11449/222607 10.1038/s41598-021-99526-z 2-s2.0-85116814342 |
url |
http://dx.doi.org/10.1038/s41598-021-99526-z http://hdl.handle.net/11449/222607 |
identifier_str_mv |
Scientific Reports, v. 11, n. 1, 2021. 2045-2322 10.1038/s41598-021-99526-z 2-s2.0-85116814342 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
Scientific Reports |
dc.rights.driver.fl_str_mv |
info:eu-repo/semantics/openAccess |
eu_rights_str_mv |
openAccess |
dc.source.none.fl_str_mv |
Scopus 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 |
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1808129291156717568 |