4.7 Article

Reactive oxygen species at the oxide/water interface: Formation mechanisms and implications for prebiotic chemistry and the origin of life

Journal

EARTH AND PLANETARY SCIENCE LETTERS
Volume 363, Issue -, Pages 156-167

Publisher

ELSEVIER
DOI: 10.1016/j.epsl.2012.12.008

Keywords

radical; titania; Fe2O3; mineral surface; prebiotic chemistry; origin of life

Funding

  1. NSF [EAR 0346689]
  2. NASA Astrobiology Institute Director's Discretionary Fund (NAI DDF)
  3. University of Akron
  4. Weeks Graduate Fellowship
  5. Department of Geoscience, the University of Wisconsin-Madison (UW)

Ask authors/readers for more resources

The goal of our study is to identify free radical formation pathways on mineral surfaces. Organic molecules on early Earth might have been modified or decomposed by such pathways, thus affecting the total organic inventory for prebiotic synthesis reactions. Specifically, we evaluated several common oxide minerals under a range of environmental conditions and combinations of conditions (pH, O-2 level, UV-wavelength, and particle loading), for formation of highly reactive oxygen species (ROS) at the oxide surfaces by quantifying the generated [OH center dot] and [H2O2]. We identified anatase/rutile (beta-TiO2/alpha-TiO2) and hematite (alpha-Fe2O3) as active in ROS production and, importantly, found different dominant pathways for ROS formation on anatase/rutile versus hematite. Hydroxyl radicals (OH center dot) in anatase and rutile suspensions were generated mainly through the oxidation of OH- by photo-generated holes and H2O2 was generated through the combination of an OH center dot radical with an OH- and a hole. This pathway for the TiO2 phases did not require the presence of O-2, and was not shut down under anaerobic conditions. In contrast, formation of H2O2 and OH center dot in hematite suspensions involved reduction of O-2 by electrons, which was inhibited under anaerobic conditions. The surface ROS as well as free radicals formed by reactions with other gases on early Earth atmosphere were capable of destroying molecules such as lipids and pre-RNA or RNA essential to assembly of protocells and survival of the earliest cells. At the same time, surface associated ROS and other free radicals may also have promoted aminoamide formation. Thus, the surface ROS would have affected prebiotic organic compound inventory and protocell/early life evolution. (C) 2012 Elsevier B.V. All rights reserved.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.7
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
Article Geochemistry & Geophysics

Eoarchean ultramafic rocks represent crustal cumulates: A case study of the Narssaq ultramafic body, southern West Greenland

Lingyu Zhang, Kristoffer Szilas

Summary: This study presents new petrological and geochemical data for the Narssaq Ultramafic Body (NUB) in the Itsaq Gneiss Complex of SW Greenland. The results indicate that the ultramafic rocks of NUB are not mantle residues, but instead represent crustal cumulates derived from high-Mg magmas.

EARTH AND PLANETARY SCIENCE LETTERS (2024)

Article Geochemistry & Geophysics

Iron isotope evidence in continental intraplate basalts for mantle lithosphere imprint on heterogenous asthenospheric melts

Rong Xu, Sarah Lambart, Oliver Nebel, Ming Li, Zhongjie Bai, Junbo Zhang, Ganglan Zhang, Jianfeng Gao, Hong Zhong, Yongsheng Liu

Summary: This study investigated the iron isotope compositions of Cenozoic basalts in Southeast China, finding significant variations related to different types of basalts and their respective sources.

EARTH AND PLANETARY SCIENCE LETTERS (2024)

Article Geochemistry & Geophysics

Shallow sources of upper mantle seismic anisotropy in East Africa

C. J. Ebinger, Miriam C. Reiss, Ian Bastow, Mary M. Karanja

Summary: The East African rift system is formed above mantle upwellings and the formation of rifts is related to lithospheric thinning and magmatic activity. The amount of splitting varies spatially and the fast axes are predominantly parallel to the orientation of the rifts. Thick lithospheric modules have less splitting and different orientations, which may indicate mantle plume flow. Splitting rotates and increases in strength as it enters the rift zones, suggesting that the anisotropy is mainly present at shallow depths.

EARTH AND PLANETARY SCIENCE LETTERS (2024)

Correction Geochemistry & Geophysics

Serpentinite fluids and slab-melting in the Aleutian arc: Evidence from molybdenum isotopes and boron systematics (vol 603, 117970, 2023)

Ekaterina Rojas-Kolomiets, Owen Jensen, Michael Bizimis, Gene Yogodzinski, Lukas Ackerman

EARTH AND PLANETARY SCIENCE LETTERS (2024)

Article Geochemistry & Geophysics

Concordance of V-in-olivine and Fe-XANES oxybarometry methods in mid-ocean ridge basalts

Robert W. Nicklas, Igor S. Puchtel, Ethan F. Baxter

Summary: Oxygen fugacity is a fundamental parameter for understanding redox processes in igneous systems. This study compares the Fe-XANES oxybarometry method with the V-in-olivine method for evaluating fO(2) in MORB lavas. The results show that the V-in-olivine method is not applicable to samples with low MgO content, and that the majority of Archean komatiite sources have lower fO(2) than modern MORB.

EARTH AND PLANETARY SCIENCE LETTERS (2024)

Article Geochemistry & Geophysics

Calcium isotopes track volatile components in the mantle sources of alkaline rocks and associated carbonatites

Chunfei Chen, Stephen F. Foley, Sebastian Tappe, Huange Ren, Lanping Feng, Yongsheng Liu

Summary: The volatile components CO2 and H2O play a major role in mantle melting and heterogeneity. In this study, Ca isotopes were used to trace the lithological heterogeneity in alkaline magmatic rocks. The results revealed the presence of K-richterite and carbonate components as the source of alkaline magmas with low delta 44/40Ca values. These findings highlight the importance of Ca isotopes as a robust tracer of lithological variation caused by volatiles in the Earth's upper mantle.

EARTH AND PLANETARY SCIENCE LETTERS (2024)

Article Geochemistry & Geophysics

Cosmogenic (un-)steadiness revealed by paired-nuclide catchment-wide denudation rates in the formerly half-glaciated Vosges Mountains (NE France)

Timothee Jautzy, Gilles Rixhon, Regis Braucher, Romain Delunel, Pierre G. Valla, Laurent Schmitt, Aster Team

Summary: Although the current approach to estimate catchment-wide denudation rates using only 10Be concentrations has made significant progress in geomorphology, this study argues for the inclusion of 26Al measurements and testing of steady-state assumptions in slow eroding, formerly glaciated landscapes. The study conducted measurements of both 10Be and 26Al in stream sediments from the Vosges Massif in France and found that elevation, slope, channel steepness, and precipitation were the primary factors controlling denudation rates. The study also revealed a significant relationship between the extent of past glaciation and the cosmogenic (un-)steadiness in the stream sediments.

EARTH AND PLANETARY SCIENCE LETTERS (2024)

Article Geochemistry & Geophysics

Linking rates of slab sinking to long-term lower mantle flow and mixing

Erik van der Wiel, Douwe J. J. van Hinsbergen, Cedric Thieulot, Wim Spakman

Summary: Numerical models of Earth's mantle dynamics can predict the vigour and mixing of mantle flow, and the average slab sinking rates are an unexplored parameter that can provide intrinsic information on these characteristics. Through numerical experiments, it has been found that slab sinking rates are strongly correlated with mantle convection and mixing, and may explain geochemical observations from hotspot volcanoes.

EARTH AND PLANETARY SCIENCE LETTERS (2024)