Prebiotic RNA synthesis by montmorillonite catalysis
Sohan Jheeta1, Prakash C Joshi2
1NoR HGT&LUCA, 1 Scott Hall Crescent, Leeds LS7 3RB, UK. sohan7@ntlworld.com.
Life (Basel, Switzerland)
|November 6, 2014
Summary
Mineral salts and montmorillonite clay catalyze prebiotic RNA synthesis, simplifying its origin. This process facilitated homochiral selection, crucial for the Last Universal Common Ancestor (LUCA).
Area of Science:
- Astrobiology
- Origin of Life Studies
- Prebiotic Chemistry
Background:
- Understanding the origin of RNA is key to understanding the origin of life.
- Previous research suggests RNA played a central role in the Last Universal Common Ancestor (LUCA).
Purpose of the Study:
- To investigate the role of mineral salts in prebiotic RNA synthesis.
- To explore the catalytic capabilities of montmorillonite clay minerals in RNA formation.
- To demonstrate a simple mechanism for prebiotic RNA synthesis.
Main Methods:
- Utilized montmorillonite clay minerals as catalysts for RNA synthesis from monomers.
- Investigated the effect of various mineral salts (monovalent cations and anions) on RNA chain length using High-Performance Liquid Chromatography (HPLC).
- Examined the influence of hydrophobic and hydrophilic interactions on the reaction.
Main Results:
- Montmorillonite clay catalyzed RNA synthesis and facilitated homochiral selection.
- The addition of sodium chloride significantly enhanced RNA chain length compared to synthesis in water alone.
- Monovalent cations and anions influenced catalysis in specific orders (Li+ > Na+ > K+ and Cl- > Br- > I-, respectively).
Conclusions:
- Prebiotic RNA synthesis is a simple process achievable with abundant early Earth materials: clay minerals and mineral salts.
- Mineral salts play a crucial role in enhancing the efficiency and chain length of clay-catalyzed RNA synthesis.
- These findings support a plausible pathway for the emergence of functional RNA necessary for early life.
Related Concept Videos
Origin of Cellular Life
100
The origin of life on Earth is a complex and enigmatic event rooted in ancient biochemical processes and geological conditions. Experimental evidence supports the hypothesis that life began with the spontaneous formation of organic molecules such as RNA nucleotides, amino acids, and lipids under early Earth conditions. Factors like volcanic activity, intense UV radiation, and a reducing atmosphere without free oxygen likely facilitated these reactions. Hydrothermal vents on the ocean floor are...
100
Ribosomal RNA Synthesis
12.2K
Ribosome synthesis is a highly complex and coordinated process involving more than 200 assembly factors. The synthesis and processing of ribosomal components occurs not only in the nucleolus but also in the nucleoplasm and the cytoplasm of eukaryotic cells.
Ribosome biogenesis begins with the synthesis of 5S and 45S pre-rRNAs by distinct RNA polymerases. The primary transcripts are extensively processed and modified before they are bound and folded by ribosomal proteins and assembly factors,...
Ribosome biogenesis begins with the synthesis of 5S and 45S pre-rRNAs by distinct RNA polymerases. The primary transcripts are extensively processed and modified before they are bound and folded by ribosomal proteins and assembly factors,...
12.2K
Ribosomal RNA Synthesis
3.7K
3.7K
Bacterial RNA Polymerase
19.9K
Unlike eukaryotes, bacteria use a single RNA Polymerase (RNAP) to transcribe all genes. The different subunits of bacterial RNAPhave distinct functions. The multisubunit structure of the bacterial RNAP helps the enzyme to maintain catalytic function, facilitate assembly, interact with DNA and RNA, and self-regulate its activity.
In most genes, the transcription site is a single base present upstream of the coding sequence. Though RNAP is a catalytically efficient enzyme, it does not recognize...
In most genes, the transcription site is a single base present upstream of the coding sequence. Though RNAP is a catalytically efficient enzyme, it does not recognize...
19.9K
Bacterial RNA Polymerase
10.9K
10.9K
Conditions on Early Earth
66.8K
Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.
66.8K


