Literature DB >> 23615613

Long-term sedimentary recycling of rare sulphur isotope anomalies.

Christopher T Reinhard1, Noah J Planavsky, Timothy W Lyons.   

Abstract

The accumulation of substantial quantities of O2 in the atmosphere has come to control the chemistry and ecological structure of Earth's surface. Non-mass-dependent (NMD) sulphur isotope anomalies in the rock record are the central tool used to reconstruct the redox history of the early atmosphere. The generation and initial delivery of these anomalies to marine sediments requires low partial pressures of atmospheric O2 (p(O2); refs 2, 3), and the disappearance of NMD anomalies from the rock record 2.32 billion years ago is thought to have signalled a departure from persistently low atmospheric oxygen levels (less than about 10(-5) times the present atmospheric level) during approximately the first two billion years of Earth's history. Here we present a model study designed to describe the long-term surface recycling of crustal NMD anomalies, and show that the record of this geochemical signal is likely to display a 'crustal memory effect' following increases in atmospheric p(O2) above this threshold. Once NMD anomalies have been buried in the upper crust they are extremely resistant to removal, and can be erased only through successive cycles of weathering, dilution and burial on an oxygenated Earth surface. This recycling results in the residual incorporation of NMD anomalies into the sedimentary record long after synchronous atmospheric generation of the isotopic signal has ceased, with dynamic and measurable signals probably surviving for as long as 10-100 million years subsequent to an increase in atmospheric p(O2) to more than 10(-5) times the present atmospheric level. Our results can reconcile geochemical evidence for oxygen production and transient accumulation with the maintenance of NMD anomalies on the early Earth, and suggest that future work should investigate the notion that temporally continuous generation of new NMD sulphur isotope anomalies in the atmosphere was likely to have ceased long before their ultimate disappearance from the rock record.

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Year:  2013        PMID: 23615613     DOI: 10.1038/nature12021

Source DB:  PubMed          Journal:  Nature        ISSN: 0028-0836            Impact factor:   49.962


  22 in total

1.  Mass-independent sulfur of inclusions in diamond and sulfur recycling on early Earth.

Authors:  J Farquhar; B A Wing; K D McKeegan; J W Harris; P Cartigny; M H Thiemens
Journal:  Science       Date:  2002-12-20       Impact factor: 47.728

2.  The diversification of Paleozoic fire systems and fluctuations in atmospheric oxygen concentration.

Authors:  Andrew C Scott; Ian J Glasspool
Journal:  Proc Natl Acad Sci U S A       Date:  2006-07-10       Impact factor: 11.205

3.  Animal evolution, bioturbation, and the sulfate concentration of the oceans.

Authors:  Donald E Canfield; James Farquhar
Journal:  Proc Natl Acad Sci U S A       Date:  2009-05-18       Impact factor: 11.205

4.  A late Archean sulfidic sea stimulated by early oxidative weathering of the continents.

Authors:  Christopher T Reinhard; Rob Raiswell; Clint Scott; Ariel D Anbar; Timothy W Lyons
Journal:  Science       Date:  2009-10-30       Impact factor: 47.728

Review 5.  Iron and sulfur in the pre-biologic ocean.

Authors:  J C Walker; P Brimblecombe
Journal:  Precambrian Res       Date:  1985       Impact factor: 4.725

6.  A new model for atmospheric oxygen over Phanerozoic time.

Authors:  R A Berner; D E Canfield
Journal:  Am J Sci       Date:  1989-04       Impact factor: 5.772

7.  Atmospheric sulfur in Archean komatiite-hosted nickel deposits.

Authors:  Andrey Bekker; Mark E Barley; Marco L Fiorentini; Olivier J Rouxel; Douglas Rumble; Stephen W Beresford
Journal:  Science       Date:  2009-11-20       Impact factor: 47.728

8.  Climate sensitivity constrained by CO2 concentrations over the past 420 million years.

Authors:  Dana L Royer; Robert A Berner; Jeffrey Park
Journal:  Nature       Date:  2007-03-29       Impact factor: 49.962

9.  A whiff of oxygen before the great oxidation event?

Authors:  Ariel D Anbar; Yun Duan; Timothy W Lyons; Gail L Arnold; Brian Kendall; Robert A Creaser; Alan J Kaufman; Gwyneth W Gordon; Clinton Scott; Jessica Garvin; Roger Buick
Journal:  Science       Date:  2007-09-28       Impact factor: 47.728

10.  Fluctuations in Precambrian atmospheric oxygenation recorded by chromium isotopes.

Authors:  Robert Frei; Claudio Gaucher; Simon W Poulton; Don E Canfield
Journal:  Nature       Date:  2009-09-10       Impact factor: 49.962

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  15 in total

1.  A productivity collapse to end Earth's Great Oxidation.

Authors:  Malcolm S W Hodgskiss; Peter W Crockford; Yongbo Peng; Boswell A Wing; Tristan J Horner
Journal:  Proc Natl Acad Sci U S A       Date:  2019-08-12       Impact factor: 11.205

2.  False Negatives for Remote Life Detection on Ocean-Bearing Planets: Lessons from the Early Earth.

Authors:  Christopher T Reinhard; Stephanie L Olson; Edward W Schwieterman; Timothy W Lyons
Journal:  Astrobiology       Date:  2017-04       Impact factor: 4.335

Review 3.  The rise of oxygen in Earth's early ocean and atmosphere.

Authors:  Timothy W Lyons; Christopher T Reinhard; Noah J Planavsky
Journal:  Nature       Date:  2014-02-20       Impact factor: 49.962

Review 4.  Life: the first two billion years.

Authors:  Andrew H Knoll; Kristin D Bergmann; Justin V Strauss
Journal:  Philos Trans R Soc Lond B Biol Sci       Date:  2016-11-05       Impact factor: 6.237

5.  Microbial helpers allow cyanobacteria to thrive in ferruginous waters.

Authors:  Nadia Szeinbaum; Yael J Toporek; Christopher T Reinhard; Jennifer B Glass
Journal:  Geobiology       Date:  2021-04-19       Impact factor: 4.216

6.  A 200-million-year delay in permanent atmospheric oxygenation.

Authors:  Simon W Poulton; Andrey Bekker; Vivien M Cumming; Aubrey L Zerkle; Donald E Canfield; David T Johnston
Journal:  Nature       Date:  2021-03-29       Impact factor: 69.504

7.  Globally asynchronous sulphur isotope signals require re-definition of the Great Oxidation Event.

Authors:  Pascal Philippot; Janaína N Ávila; Bryan A Killingsworth; Svetlana Tessalina; Franck Baton; Tom Caquineau; Elodie Muller; Ernesto Pecoits; Pierre Cartigny; Stefan V Lalonde; Trevor R Ireland; Christophe Thomazo; Martin J van Kranendonk; Vincent Busigny
Journal:  Nat Commun       Date:  2018-06-08       Impact factor: 14.919

8.  Transient episodes of mild environmental oxygenation and oxidative continental weathering during the late Archean.

Authors:  Brian Kendall; Robert A Creaser; Christopher T Reinhard; Timothy W Lyons; Ariel D Anbar
Journal:  Sci Adv       Date:  2015-11-20       Impact factor: 14.136

9.  Rapid oxygenation of Earth's atmosphere 2.33 billion years ago.

Authors:  Genming Luo; Shuhei Ono; Nicolas J Beukes; David T Wang; Shucheng Xie; Roger E Summons
Journal:  Sci Adv       Date:  2016-05-13       Impact factor: 14.136

10.  The Great Oxidation Event preceded a Paleoproterozoic "snowball Earth".

Authors:  Matthew R Warke; Tommaso Di Rocco; Aubrey L Zerkle; Aivo Lepland; Anthony R Prave; Adam P Martin; Yuichiro Ueno; Daniel J Condon; Mark W Claire
Journal:  Proc Natl Acad Sci U S A       Date:  2020-06-01       Impact factor: 11.205

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