Goldilocks at the dawn of complex life: mountains might have damaged Ediacaran–Cambrian ecosystems and prompted an early Cambrian greenhouse world

Abstract 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)...

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Autores principales: Fabricio Caxito, Cristiano Lana, Robert Frei, Gabriel J. Uhlein, Alcides N. Sial, Elton L. Dantas, André G. Pinto, Filippe C. Campos, Paulo Galvão, Lucas V. Warren, Juliana Okubo, Carlos E. Ganade
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Publicado: Nature Portfolio 2021
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spelling oai:doaj.org-article:34b267a34b9f4faa8c4825288af8dad62021-12-02T18:37:08ZGoldilocks at the dawn of complex life: mountains might have damaged Ediacaran–Cambrian ecosystems and prompted an early Cambrian greenhouse world10.1038/s41598-021-99526-z2045-2322https://doaj.org/article/34b267a34b9f4faa8c4825288af8dad62021-10-01T00:00:00Zhttps://doi.org/10.1038/s41598-021-99526-zhttps://doaj.org/toc/2045-2322Abstract 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.Fabricio CaxitoCristiano LanaRobert FreiGabriel J. UhleinAlcides N. SialElton L. DantasAndré G. PintoFilippe C. CamposPaulo GalvãoLucas V. WarrenJuliana OkuboCarlos E. GanadeNature PortfolioarticleMedicineRScienceQENScientific Reports, Vol 11, Iss 1, Pp 1-15 (2021)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Fabricio Caxito
Cristiano Lana
Robert Frei
Gabriel J. Uhlein
Alcides N. Sial
Elton L. Dantas
André G. Pinto
Filippe C. Campos
Paulo Galvão
Lucas V. Warren
Juliana Okubo
Carlos E. Ganade
Goldilocks at the dawn of complex life: mountains might have damaged Ediacaran–Cambrian ecosystems and prompted an early Cambrian greenhouse world
description Abstract 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.
format article
author Fabricio Caxito
Cristiano Lana
Robert Frei
Gabriel J. Uhlein
Alcides N. Sial
Elton L. Dantas
André G. Pinto
Filippe C. Campos
Paulo Galvão
Lucas V. Warren
Juliana Okubo
Carlos E. Ganade
author_facet Fabricio Caxito
Cristiano Lana
Robert Frei
Gabriel J. Uhlein
Alcides N. Sial
Elton L. Dantas
André G. Pinto
Filippe C. Campos
Paulo Galvão
Lucas V. Warren
Juliana Okubo
Carlos E. Ganade
author_sort Fabricio Caxito
title Goldilocks at the dawn of complex life: mountains might have damaged Ediacaran–Cambrian ecosystems and prompted an early Cambrian greenhouse world
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
publisher Nature Portfolio
publishDate 2021
url https://doaj.org/article/34b267a34b9f4faa8c4825288af8dad6
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