Large Impacts onto the Early Earth: Planetary Sterilization and Iron Delivery
Late accretion onto the Hadean Earth included large impacts that could have influenced early habitability, either by sterilizing the planet or alternatively catalyzing the origin of life by delivering iron required to create a reducing environment/atmosphere. We present 3D numerical simulations of 1...
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IOP Publishing
2022-01-01
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| Series: | The Planetary Science Journal |
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| Online Access: | https://doi.org/10.3847/PSJ/ac66e8 |
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| author | Robert I. Citron Sarah T. Stewart |
| author_facet | Robert I. Citron Sarah T. Stewart |
| author_sort | Robert I. Citron |
| collection | DOAJ |
| description | Late accretion onto the Hadean Earth included large impacts that could have influenced early habitability, either by sterilizing the planet or alternatively catalyzing the origin of life by delivering iron required to create a reducing environment/atmosphere. We present 3D numerical simulations of 1500–3400 km diameter impacts on the early Earth in order to quantify their effects on planetary habitability. We find sterilizing impact events require larger projectiles than previously assumed, with a 2000–2700 km diameter impactor required to completely melt Earth’s surface and an extrapolated >700 km diameter impactor required for ocean vaporization. We also find that reducing environments are less likely to arise following large impacts than previously suggested, because >70% of the projectile iron is deposited in the crust and upper mantle where it is not immediately available to reduce surface water and contribute to forming a reducing atmosphere. Although the largest expected late-accretion impacts (∼1 lunar mass) delivered sufficient iron to the atmosphere to have reduced an entire ocean mass of water, such impacts would also have melted the entire surface, potentially sequestering condensing iron that is not oxidized quickly. The hypothesis that life emerged in the aftermath of large impacts requires an efficient mechanism of harnessing the reducing power of iron sequestered in the crust/mantle, or an origin-of-life pathway that operates in more weakly reducing post-impact environments that require smaller quantities of impact-delivered iron. |
| format | Article |
| id | doaj-art-69f687f80a67488382e02e88b09fcdf9 |
| institution | OA Journals |
| issn | 2632-3338 |
| language | English |
| publishDate | 2022-01-01 |
| publisher | IOP Publishing |
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| series | The Planetary Science Journal |
| spelling | doaj-art-69f687f80a67488382e02e88b09fcdf92025-08-20T02:27:42ZengIOP PublishingThe Planetary Science Journal2632-33382022-01-013511610.3847/PSJ/ac66e8Large Impacts onto the Early Earth: Planetary Sterilization and Iron DeliveryRobert I. Citron0https://orcid.org/0000-0001-8920-0356Sarah T. Stewart1https://orcid.org/0000-0001-9606-1593Department of Earth and Planetary Science, University of California Davis , Davis, CA 95616, USADepartment of Earth and Planetary Science, University of California Davis , Davis, CA 95616, USALate accretion onto the Hadean Earth included large impacts that could have influenced early habitability, either by sterilizing the planet or alternatively catalyzing the origin of life by delivering iron required to create a reducing environment/atmosphere. We present 3D numerical simulations of 1500–3400 km diameter impacts on the early Earth in order to quantify their effects on planetary habitability. We find sterilizing impact events require larger projectiles than previously assumed, with a 2000–2700 km diameter impactor required to completely melt Earth’s surface and an extrapolated >700 km diameter impactor required for ocean vaporization. We also find that reducing environments are less likely to arise following large impacts than previously suggested, because >70% of the projectile iron is deposited in the crust and upper mantle where it is not immediately available to reduce surface water and contribute to forming a reducing atmosphere. Although the largest expected late-accretion impacts (∼1 lunar mass) delivered sufficient iron to the atmosphere to have reduced an entire ocean mass of water, such impacts would also have melted the entire surface, potentially sequestering condensing iron that is not oxidized quickly. The hypothesis that life emerged in the aftermath of large impacts requires an efficient mechanism of harnessing the reducing power of iron sequestered in the crust/mantle, or an origin-of-life pathway that operates in more weakly reducing post-impact environments that require smaller quantities of impact-delivered iron.https://doi.org/10.3847/PSJ/ac66e8Planetary scienceEarth (planet)Impact phenomenaHabitable planetsAstrobiology |
| spellingShingle | Robert I. Citron Sarah T. Stewart Large Impacts onto the Early Earth: Planetary Sterilization and Iron Delivery The Planetary Science Journal Planetary science Earth (planet) Impact phenomena Habitable planets Astrobiology |
| title | Large Impacts onto the Early Earth: Planetary Sterilization and Iron Delivery |
| title_full | Large Impacts onto the Early Earth: Planetary Sterilization and Iron Delivery |
| title_fullStr | Large Impacts onto the Early Earth: Planetary Sterilization and Iron Delivery |
| title_full_unstemmed | Large Impacts onto the Early Earth: Planetary Sterilization and Iron Delivery |
| title_short | Large Impacts onto the Early Earth: Planetary Sterilization and Iron Delivery |
| title_sort | large impacts onto the early earth planetary sterilization and iron delivery |
| topic | Planetary science Earth (planet) Impact phenomena Habitable planets Astrobiology |
| url | https://doi.org/10.3847/PSJ/ac66e8 |
| work_keys_str_mv | AT roberticitron largeimpactsontotheearlyearthplanetarysterilizationandirondelivery AT sarahtstewart largeimpactsontotheearlyearthplanetarysterilizationandirondelivery |