10 Truth About Life On Earth From Shallow Soda Lake

25th Janurary By James Smith

Scientists from the University of Washington discovered a shallow "soda lake" in western Canada resembling Darwin's "warm little ponds," theorized as the birthplaces of life on Earth.

The soda lake's unique chemistry and conditions align with the prerequisites for the spontaneous synthesis of complex molecules crucial for the emergence of life around 4 billion years ago. 

Soda lakes, characterized by high levels of dissolved carbonates and sodium, mimic conditions similar to having baking soda dumped into them, with the elevated levels caused by reactions between water and volcanic rocks. 

The findings from this research may provide insights into how life emerged on Earth and could be applicable to understanding the potential for life on other planets, such as Mars and Venus. 

The study addresses the "phosphate problem," a challenge in explaining the emergence of life, suggesting that soda lakes could hold the key to the formation of RNA and DNA, crucial molecules for life. 

The concentrations of phosphates needed for biomolecule formation in traditional bodies of water are up to 1 million times lower than required in laboratory settings, making soda lakes a potential solution. 

Soda lakes, like Last Chance Lake in British Columbia, Canada, contain large amounts of phosphates, with concentrations up to 1 million times greater than typical bodies of water, making them ideal for the emergence of key life molecules. 

Last Chance Lake was chosen for examination due to its high phosphate levels, volcanic basalt rock at its bottom, and a dry, windy climate that keeps water levels low and compounds concentrated. 

– The research team visited Last Chance Lake multiple times between 2021 and 2022, studying it in both summer and winter to understand the lake's chemistry under different conditions.

– The team found that Last Chance Lake's unique conditions, where calcium combines with carbonate and magnesium to form dolomite, could have allowed for the existence of the necessary high concentrations of key life ingredients around 4 billion years ago.