Geodynamic transition at 2.7 Ga in Earths largest craton
<div>The first ca. 2.2 billion years of Earth history saw significant change; from a water-world dominated by an anoxic atmosphere and tonalitic continents, to the exposed landmasses, oxygenated atmosphere, and granitic crust of the Paleoproterozoic. Precisely when, and how, these major changes occurred, remain some of the most important and controversial questions in modern geoscience. Here, we present an extensive new zircon U-Pb-Hf-O isotopic and trace element dataset from Earth’s largest preserved Archean continent, the Superior Craton, Canada. These data record a number of fundamental geochemical changes through time and indicate a major geological and geodynamic transition occurred toward the end of Archean, at ca. 2.7 Ga. Our data show that, at >2704–2695 Ma, the southern Superior Craton had juvenile εHf, light to mantle-like δ18O, low (Eu/Eu*)/Y (drier/shallower crust), reduced ΔFMQ, less continental initial-U (Ui)/Yb, and more mantle-like Ui/Nb. At ca. 2704–2695 Ma, there is a marked transition in multiple datasets, including increases in δ18O, (Eu/Eu*)/Y, ΔFMQ, Ui/Yb and Ui/Nb data, together with more distinct arc-like trace element trends. These data reveal that at 2.7 Ga there was an increase in: (1) continental surface weathering, supported by increased sedimentation at <2.68 Ga, (2) oxidized and hydrous magmatism, and (3) surface material in magma sources. Together, these observations suggest a major geodynamic transition from ‘vertical’ tectonics (sagduction, drips) to north-dipping subduction at 2.7 Ga. The increase in δ18O suggests that proximal continental crust, probably in the northern Superior Craton, became emergent at this time, an inference supported by detrital zircon geochronology. Hence, this dataset links major geodynamic change to the emergence of continental crust and the rise of more oxidized magmatism. These fundamental changes to the Earth’s surface environment, tectonics, and atmosphere at 2.7 Ga, provide evidence for an Earth systems turning-point at the end of the Neoarchean.</div>
This Abstract was submitted/presented to the 2022 Specialist Group in Geochemistry, Mineralogy and Petrology (SGGMP) Conference 7-11 November ( https://gsasggmp.wixsite.com/home/biennial-conference-2021)
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- Date (Creation)
- 2022-09-02T16:00:00
- Date (Publication)
- 2023-02-20T02:27:28
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- Geoscience Australia Persistent Identifier/https://pid.geoscience.gov.au/dataset/ga/147185
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Role Organisation / Individual Name Details Publisher Commonwealth of Australia (Geoscience Australia)
Voice Author Mole, D.
Internal Contact Author Thurston, P.C.
External Contact Author Marsh, J.H.
External Contact Author Stern, R.A.
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Specialist Group in Geochemistry, Mineralogy and Petrology (SGGMP) Conference 7-11 November 2022 Yallingup WA
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Abstract for the "Specialist Group in Geochemistry, Mineralogy and Petrology" conference in Yalingup, WA.
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Role Organisation / Individual Name Details Resource provider Minerals, Energy and Groundwater Division
External Contact Point of contact Commonwealth of Australia (Geoscience Australia)
Voice Point of contact Mole, D.
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Product data repository: Various Formats
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Data Store directory containing one or more files, possibly in a variety of formats, accessible to Geoscience Australia staff only for internal purposes
- Keywords
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zircon
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Geochemistry
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Archean
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- theme.ANZRC Fields of Research.rdf
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Isotope Geochemistry
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Published_External
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Creative Commons Attribution 4.0 International Licence
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CC-BY
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4.0
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© Commonwealth of Australia (Geoscience) 2022
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Australian Government Security Classification System
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- 2018-11-01T00:00:00
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Australian Government Security Classification System
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Link to Conference Webpage
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Link to GSWA Publications and maps (pdf)
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<div>This is external research conducted by D. Mole before commencing at GA. However, the work is closely aligned to GA goals and projects.</div>
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-
Australian Government Security Classification System
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- 2018-11-01T00:00:00
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- Unclassified
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Role Organisation / Individual Name Details Point of contact Commonwealth of Australia (Geoscience Australia)
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Conference Abstract
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Geoscience Australia - short identifier for metadata record with
uuid
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- Date info (Creation)
- 2023-02-20T01:24:08
- Date info (Revision)
- 2023-02-20T01:24:08
Metadata standard
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AU/NZS ISO 19115-1:2014
Metadata standard
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ISO 19115-1:2014
Metadata standard
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ISO 19115-3
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Geoscience Australia Community Metadata Profile of ISO 19115-1:2014
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Version 2.0, September 2018
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