Redox variations in Mauna Kea lavas, the oxygen fugacity of the Hawaiian plume, and the role of volcanic gases in Earth’s oxygenation
Abstract
The behavior of C, H, and S in the solid Earth depends on their oxidation states, which are related to oxygen fugacity (fO2). Volcanic degassing is a source of these elements to Earth’s surface; therefore, variations in mantle fO2 may influence the fO2 at Earth’s surface. However, degassing can impact magmatic fO2 before or during eruption, potentially obscuring relationships between the fO2 of the solid Earth and of emitted gases and their impact on surface fO2. We show that low-pressure degassing resulted in reduction of the fO2 of Mauna Kea magmas by more than an order of magnitude. The least degassed magmas from Mauna Kea are more oxidized than midocean ridge basalt (MORB) magmas, suggesting that the upper mantle sources of Hawaiian magmas have higher fO2 than MORB sources. One explanation for this difference is recycling of material from the oxidized surface to the deep mantle, which is then returned to the surface as a component of buoyant plumes. It has been proposed that a decreasing pressure of volcanic eruptions led to the oxygenation of the atmosphere. Extension of our findings via modeling of degassing trends suggests that a decrease in eruption pressure would not produce this effect. If degassingmore »
- Authors:
- Publication Date:
- Research Org.:
- Argonne National Lab. (ANL), Argonne, IL (United States). Advanced Photon Source (APS)
- Sponsoring Org.:
- USDOE Office of Science (SC)
- OSTI Identifier:
- 1376255
- Resource Type:
- Journal Article
- Journal Name:
- Proceedings of the National Academy of Sciences of the United States of America
- Additional Journal Information:
- Journal Volume: 114; Journal Issue: 34; Journal ID: ISSN 0027-8424
- Publisher:
- National Academy of Sciences, Washington, DC (United States)
- Country of Publication:
- United States
- Language:
- ENGLISH
- Subject:
- 58 GEOSCIENCES
Citation Formats
Brounce, Maryjo, Stolper, Edward, and Eiler, John. Redox variations in Mauna Kea lavas, the oxygen fugacity of the Hawaiian plume, and the role of volcanic gases in Earth’s oxygenation. United States: N. p., 2017.
Web. doi:10.1073/pnas.1619527114.
Brounce, Maryjo, Stolper, Edward, & Eiler, John. Redox variations in Mauna Kea lavas, the oxygen fugacity of the Hawaiian plume, and the role of volcanic gases in Earth’s oxygenation. United States. doi:10.1073/pnas.1619527114.
Brounce, Maryjo, Stolper, Edward, and Eiler, John. Mon .
"Redox variations in Mauna Kea lavas, the oxygen fugacity of the Hawaiian plume, and the role of volcanic gases in Earth’s oxygenation". United States. doi:10.1073/pnas.1619527114.
@article{osti_1376255,
title = {Redox variations in Mauna Kea lavas, the oxygen fugacity of the Hawaiian plume, and the role of volcanic gases in Earth’s oxygenation},
author = {Brounce, Maryjo and Stolper, Edward and Eiler, John},
abstractNote = {The behavior of C, H, and S in the solid Earth depends on their oxidation states, which are related to oxygen fugacity (fO2). Volcanic degassing is a source of these elements to Earth’s surface; therefore, variations in mantle fO2 may influence the fO2 at Earth’s surface. However, degassing can impact magmatic fO2 before or during eruption, potentially obscuring relationships between the fO2 of the solid Earth and of emitted gases and their impact on surface fO2. We show that low-pressure degassing resulted in reduction of the fO2 of Mauna Kea magmas by more than an order of magnitude. The least degassed magmas from Mauna Kea are more oxidized than midocean ridge basalt (MORB) magmas, suggesting that the upper mantle sources of Hawaiian magmas have higher fO2 than MORB sources. One explanation for this difference is recycling of material from the oxidized surface to the deep mantle, which is then returned to the surface as a component of buoyant plumes. It has been proposed that a decreasing pressure of volcanic eruptions led to the oxygenation of the atmosphere. Extension of our findings via modeling of degassing trends suggests that a decrease in eruption pressure would not produce this effect. If degassing of basalts were responsible for the rise in oxygen, it requires that Archean magmas had at least two orders of magnitude lower fO2 than modern magmas. Estimates of fO2 of Archean magmas are not this low, arguing for alternative explanations for the oxygenation of the atmosphere.},
doi = {10.1073/pnas.1619527114},
journal = {Proceedings of the National Academy of Sciences of the United States of America},
issn = {0027-8424},
number = 34,
volume = 114,
place = {United States},
year = {2017},
month = {8}
}
Works referenced in this record:
The nature and distribution of carbon in submarine basalts and peridotite nodules
journal, December 1981
- Mathez, E. A.; Delaney, J. R.
- Earth and Planetary Science Letters, Vol. 56
The redox states of basic and silicic magmas: a reflection of their source regions?
journal, January 1991
- Carmichael, Ian S. E.
- Contributions to Mineralogy and Petrology, Vol. 106, Issue 2
Sulfur in basaltic magmas
journal, May 1992
- Wallace, Paul; Carmichael, Ian S. E.
- Geochimica et Cosmochimica Acta, Vol. 56, Issue 5
Sulfur K-edge XANES analysis of natural and synthetic basaltic glasses: Implications for S speciation and S content as function of oxygen fugacity
journal, October 2010
- Jugo, Pedro J.; Wilke, Max; Botcharnikov, Roman E.
- Geochimica et Cosmochimica Acta, Vol. 74, Issue 20
Rise of atmospheric oxygen and the “upside-down” Archean mantle: RESEARCH LETTER
journal, January 2001
- Kump, Lee R.; Kasting, James F.; Barley, Mark E.
- Geochemistry, Geophysics, Geosystems, Vol. 2, Issue 1
Sulfur speciation, oxidation state, and sulfur concentration in backarc magmas
journal, August 1993
- Nilsson, Kristen; Peach, Cheryl L.
- Geochimica et Cosmochimica Acta, Vol. 57, Issue 15
Temporal evolution of mantle wedge oxygen fugacity during subduction initiation
journal, July 2015
- Brounce, Maryjo; Kelley, Katherine A.; Cottrell, Elizabeth
- Geology, Vol. 43, Issue 9
The oxidation state of sulfur in synthetic and natural glasses determined by X-ray absorption spectroscopy
journal, April 2009
- Métrich, Nicole; Berry, Andrew J.; O’Neill, Hugh St. C.
- Geochimica et Cosmochimica Acta, Vol. 73, Issue 8
Increased subaerial volcanism and the rise of atmospheric oxygen 2.5 billion years ago
journal, August 2007
- Kump, Lee R.; Barley, Mark E.
- Nature, Vol. 448, Issue 7157
The redox state of subduction zones: insights from arc-peridotites
journal, September 1999
- Parkinson, Ian J.; Arculus, Richard J.
- Chemical Geology, Vol. 160, Issue 4
The constancy of upper mantle fO2 through time inferred from V/Sc ratios in basalts
journal, December 2004
- Anser Li, Zheng-Xue; Aeolus Lee, Cin-Ty
- Earth and Planetary Science Letters, Vol. 228, Issue 3-4
Redox reactions in seafloor basalts: possible insights into silicic hydrothermal systems
journal, October 2004
- Holloway, John R.
- Chemical Geology, Vol. 210, Issue 1-4
Variations in Fe3+/∑Fe of Mariana Arc Basalts and Mantle Wedge fO2
journal, December 2014
- Brounce, M. N.; Kelley, K. A.; Cottrell, E.
- Journal of Petrology, Vol. 55, Issue 12
Long-term fluxes and budget of ferric iron: implication for the redox states of the Earth's mantle and atmosphere
journal, January 1999
- Lécuyer, C.
- Earth and Planetary Science Letters, Vol. 165, Issue 2
Role of oxygen pressure in the crystallization and differentiation of basaltic magma
journal, November 1959
- Osborn, E. F.
- American Journal of Science, Vol. 257, Issue 9
Mantle Oxidation State and Its Relationship to Tectonic Environment and Fluid Speciation
journal, April 1990
- Wood, B. J.; Bryndzia, L. T.; Johnson, K. E.
- Science, Vol. 248, Issue 4953
The impact of degassing on the oxidation state of basaltic magmas: A case study of Kīlauea volcano
journal, September 2016
- Moussallam, Yves; Edmonds, Marie; Scaillet, Bruno
- Earth and Planetary Science Letters, Vol. 450
Volcanic gases, black smokers, and the great oxidation event
journal, November 2002
- Holland, Heinrich D.
- Geochimica et Cosmochimica Acta, Vol. 66, Issue 21
Mantle Redox Evolution and the Oxidation State of the Archean Atmosphere
journal, March 1993
- Kasting, James F.; Eggler, David H.; Raeburn, Stuart P.
- The Journal of Geology, Vol. 101, Issue 2
The compressibility of silicate liquids containing Fe2O3 and the effect of composition, temperature, oxygen fugacity and pressure on their redox states
journal, July 1991
- Kress, Victor C.; Carmichael, Ian S. E.
- Contributions to Mineralogy and Petrology, Vol. 108, Issue 1-2
The influence of magmatic differentiation on the oxidation state of Fe in a basaltic arc magma
journal, May 2012
- Kelley, Katherine A.; Cottrell, Elizabeth
- Earth and Planetary Science Letters, Vol. 329-330
The oxidation state of Fe in MORB glasses and the oxygen fugacity of the upper mantle
journal, May 2011
- Cottrell, Elizabeth; Kelley, Katherine A.
- Earth and Planetary Science Letters, Vol. 305, Issue 3-4
Oxidation-reduction relations in basic magma: a case for homogeneous equilibria
journal, June 1986
- Carmichael, Ian S. E.; Ghiorso, Mark S.
- Earth and Planetary Science Letters, Vol. 78, Issue 2-3