On the study of impact induced hydrothermal systems as potential environments for the origins of life on earth

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Authors
Herrero Perez, Maria Jesus
Issue Date
2025-12
Type
Electronic thesis
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en_US
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Geology
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Abstract
Understanding how life emerged on Earth requires exploring environments that couldpotentially have supported prebiotic chemistry reactions. Impact-induced hydrothermal systems offer a unique combination of energy, mineral composition, and organic material that may have fostered chemical evolution on the early Earth. This dissertation investigates the fate of simple organic compounds delivered by meteorites within these dynamic hydrothermal environments. First, the implementation of two analytical techniques will be presented for their ability to detect small organic molecules in complex, saline fluids representative of the early Earth oceans. These techniques, Direct Analysis in Real Time mass spectrometry (DART-MS) and nuclear magnetic resonance (NMR), will be discussed in detail for how effectively they can characterize organic mixtures with minimal sample processing. Building on this analytical foundation, a series of high-pressure, high-temperature experiments will be presented. These experiments simulate the chemical alteration of meteoritic soluble organic compounds within subaerial and submarine impact-induced hydrothermal systems. It will be shown how temperature, mineral composition, redox state, and salinity all play crucial roles in determining the direction and complexity of organic transformations. Finally, the design and implementation of a novel flow-through reactor system capable of simulating the dynamic, flowing conditions within impact craters will be shown. Ultimately, the research presented will offer new insights and fundamental aspects about how postimpact environments may have contributed to the emergence of life on the early Earth.
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December2025
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Rensselaer Polytechnic Institute, Troy, NY
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