Did global tectonics drive early biosphere evolution? Carbon isotope record from 2.6 to 1.9 Ga carbonates of Western Australian basins.

The δ13Ccarb record of well preserved carbonates in outcrop and core is here examined from the 2.6 to 1.9 Ga old basins of Western Australia. These data, which are constrained by a well defined stratigraphic and tectonic framework, and by U-Pb zircon age

Bibliographic Details
Published in:Precambrian Research
Main Authors: Lindsay, John, Brasier, Martin
Format: Article in Journal/Newspaper
Language:unknown
Published: Elsevier
Subjects:
Keywords: carbon
carbonic acid derivative
gallium
lead
oxygen
uranium
zirconium
biosphere
carbon isotope
carbonate
early Earth
paleoatmosphere
Precambrian
tectonic evolution
archaean
article
asthenospheric upwelling
atmosphere
Australia
biosphere Archean
Carbon isotopes
Hamersley basin
Palaeoproterozoic
Pilbara
Carbonic acid
Online Access:http://hdl.handle.net/1885/64925
https://doi.org/10.1016/S0301-9268(01)00219-4
https://openresearch-repository.anu.edu.au/bitstream/1885/64925/7/MigratedxPub1022_2002.pdf.jpg
https://openresearch-repository.anu.edu.au/bitstream/1885/64925/9/MigratedxPub1022_RSD_2002.pdf.jpg
https://openresearch-repository.anu.edu.au/bitstream/1885/64925/11/01_Lindsay_Did_global_tectonics_drive_2002.pdf.jpg
https://openresearch-repository.anu.edu.au/bitstream/1885/64925/13/02_Lindsay_Did_global_tectonics_drive_2002.pdf.jpg
Description
Summary:The δ13Ccarb record of well preserved carbonates in outcrop and core is here examined from the 2.6 to 1.9 Ga old basins of Western Australia. These data, which are constrained by a well defined stratigraphic and tectonic framework, and by U-Pb zircon age

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