Unraveling abiotic organic synthesis pathways in the mafic crust of mid-ocean ridges

The aqueous alteration of the oceanic lithosphere provides significant energy that impacts the synthesis and diversity of organic compounds, which are crucial for the deep carbon cycle and may have provided the first building blocks for life. Although abiotic organic synthesis has been documented in mantle-derived rocks, the formation mechanisms and complexity of organic compounds in crustal rocks remain largely unknown. Here, we show the specific association of aliphatic carbonaceous matter with Fe oxyhydroxides in mafic crustal rocks of the Southwest Indian Ridge (SWIR). We determine potential Fe-based pathways for abiotic organic synthesis from CO<sub>2</sub> and H<sub>2</sub> using multimodal and molecular nano-geochemical tools. Quantum mechanical modeling is further employed to constrain the catalytical activity of Fe oxyhydroxides, revealing that the catalytic cycle of hydrogen may play a key role in carbon-carbon bond formation. This approach offers the possibility of interpreting physicochemical organic formation and condensation mechanisms at an atomic scale. The findings expand our knowledge of the existence of abiotic organic carbon in the oceanic crustal rocks and emphasize the mafic oceanic crust of the SWIR as a potential site for low-temperature abiotic organic synthesis.

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Publication Details

Journal
Proceedings of the National Academy of Sciences
Published
2024-10-10
DOI
https://doi.org/10.1073/pnas.2308684121
Citations
3
Primary Topic
Catalysis and Oxidation Reactions
Type
article
Field-Weighted Citation Impact
0.32

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article

Unraveling abiotic organic synthesis pathways in the mafic crust of mid-ocean ridges

Renbiao Tao, Weiqi Yao, Martina Preiner, Yongxiang Luo et al.
3 citations
Proceedings of the National Academy of Sciences
Catalysis and Oxidation Reactions
0.32
article

Unraveling abiotic organic synthesis pathways in the mafic crust of mid-ocean ridges

Renbiao Tao, Weiqi Yao, Martina Preiner, Yongxiang Luo, Jing‐Guang Lu, Iris C. ten Have, Jingbo Nan, Qian-Bao Liu, Oliver Plümper, Xiaotong Peng, Yu Liu, Zhen Shen, Shaolin Li, Yingjie Hu
article en
3 citations

Abstract

The aqueous alteration of the oceanic lithosphere provides significant energy that impacts the synthesis and diversity of organic compounds, which are crucial for the deep carbon cycle and may have provided the first building blocks for life. Although abiotic organic synthesis has been documented in mantle-derived rocks, the formation mechanisms and complexity of organic compounds in crustal rocks remain largely unknown. Here, we show the specific association of aliphatic carbonaceous matter with Fe oxyhydroxides in mafic crustal rocks of the Southwest Indian Ridge (SWIR). We determine potential Fe-based pathways for abiotic organic synthesis from CO<sub>2</sub> and H<sub>2</sub> using multimodal and molecular nano-geochemical tools. Quantum mechanical modeling is further employed to constrain the catalytical activity of Fe oxyhydroxides, revealing that the catalytic cycle of hydrogen may play a key role in carbon-carbon bond formation. This approach offers the possibility of interpreting physicochemical organic formation and condensation mechanisms at an atomic scale. The findings expand our knowledge of the existence of abiotic organic carbon in the oceanic crustal rocks and emphasize the mafic oceanic crust of the SWIR as a potential site for low-temperature abiotic organic synthesis.

Proceedings of the National Academy of SciencesVol. 121(43)
Macau University of Science and Technology (MO), Philipps University of Marburg (DE), Utrecht University (NL), Chinese Academy of Sciences (CN), China University of Mining and Technology (CN), Southern University of Science and Technology (CN), Nanjing Institute of Geology and Paleontology (CN), Nanjing Xiaozhuang University (CN), Center for High Pressure Science and Technology Advanced Research (CN), Loewe Center for Synthetic Microbiology (DE), Institute of Deep-Sea Science and Engineering (CN), Max Planck Institute for Terrestrial Microbiology (DE)
National Natural Science Foundation of China, Universiteit Utrecht, Chinese Academy of Sciences, Nederlandse Organisatie voor Wetenschappelijk Onderzoek, China University of Mining and Technology, Hokkaido University, Max-Planck-Institut für Terrestrische Mikrobiologie, Peking University, Nanjing Xiaozhuang University, Southern University of Science and Technology, Macau University of Science and Technology, Sorbonne Université, Zentrum für Synthetische Mikrobiologie, Nationaal Regieorgaan Onderwijsonderzoek, National Key Research and Development Program of China
Life below water
Openalex Percentile: Top 53%
Catalysis and Oxidation Reactions
0.32
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