Dokument: The role of nitrogen in the onset of metabolism
Titel: | The role of nitrogen in the onset of metabolism | |||||||
URL für Lesezeichen: | https://docserv.uni-duesseldorf.de/servlets/DocumentServlet?id=61516 | |||||||
URN (NBN): | urn:nbn:de:hbz:061-20230130-092125-3 | |||||||
Kollektion: | Dissertationen | |||||||
Sprache: | Englisch | |||||||
Dokumententyp: | Wissenschaftliche Abschlussarbeiten » Dissertation | |||||||
Medientyp: | Text | |||||||
Autor: | do Nascimento Vieira, Andrey [Autor] | |||||||
Dateien: |
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Beitragende: | Prof. Dr. Martin, William F. [Gutachter] Preiner, Martina [Gutachter] | |||||||
Dewey Dezimal-Klassifikation: | 500 Naturwissenschaften und Mathematik » 570 Biowissenschaften; Biologie | |||||||
Beschreibung: | Life is a set of chemical reactions that unfolded shortly after the planet's formation 4.5 billion years ago. Although direct geochemical evidence of metabolic origins is scarce, phylogenetic reconstructions of the last universal common ancestor (LUCA) shed some light on what conditions took place before and during the time of origins some 4.2 billion years ago. These reconstructions point toward aqueous, metal-bearing, serpentinizing environments such as those found in modern-day alkaline hydrothermal vents.
The mechanisms of nitrogen assimilation at origins have been under intense debate for the last century due to its low geologic abundance and reactivity. Despite its relative availability, the Redfield ratio, a hypothetical formula for life, indicates the ubiquitous importance of nitrogen to cellular life. As such, a question remains. How did nitrogen get available in substantial amounts to feed early autocatalytic networks? Given the high partial pressure of dinitrogen in the atmosphere, it is plausible that this gas was the starting point to a series of reactions that would result in the formation of highly soluble and reactive nitrogen-bearing species. In this work, the mechanisms of nitrogen assimilation into prebiotically relevant organics were tested under alkaline hydrothermal conditions. The synthesis of formamide and acetamide from ammonia was attained overnight in the presence of suitable catalysts in the liquid phase, as demonstrated by 1H-NMR at 70 °C. Alanine and glycine, two proteinogenic amino acids, were also observed, but efforts to increase yields and facilitate detection are yet to be optimized. These results indicate that when given the right conditions, a simple mixture of dinitrogen (N2), carbon dioxide (CO2), ammonia (NH3), molecular hydrogen (H2), and suitable catalysts can yield the formation of organic acids and C-N-bearing molecules. These 16-hour reactions give us a glimpse of what could unfold in geologic timescales. | |||||||
Lizenz: | ![]() Dieses Werk ist lizenziert unter einer Creative Commons Namensnennung 4.0 International Lizenz | |||||||
Fachbereich / Einrichtung: | Mathematisch- Naturwissenschaftliche Fakultät | |||||||
Dokument erstellt am: | 30.01.2023 | |||||||
Dateien geändert am: | 30.01.2023 | |||||||
Promotionsantrag am: | 19.05.2022 | |||||||
Datum der Promotion: | 28.10.2022 |