This scarcity presents a major question for researchers: how could life have emerged in an environment lacking sufficient phosphorus? Laboratory studies suggest that prebiotic chemistry, the set of reactions that precedes life, requires phosphorus concentrations around 10,000 times higher than what is typically found in natural waters.
Earth scientist Craig Walton, a researcher affiliated with ETH Zurich's Centre for Origin and Prevalence of Life (COPL), proposes a compelling explanation. He suggests that large soda lakes, which lack natural outlets and only lose water through evaporation, could have provided the necessary high-phosphorus environment for life to originate. His findings, recently published in *Science Advances*, explore the geochemical dynamics that could have supported this process.
In closed-basin soda lakes, phosphorus doesn't escape through flowing water but instead accumulates as water evaporates. Over time, this leads to exceptionally high phosphorus levels. Such conditions could persist even after life begins to consume the available phosphorus, offering a stable chemical environment conducive to early biological activity.
While earlier research from the University of Washington in 2020 hinted at soda lakes as potential cradles of life, Walton's study builds on that concept by focusing on lake size and inflow dynamics. According to Walton, small soda lakes would rapidly deplete their phosphorus reserves once life emerged, stalling further biochemical development. In contrast, large lakes with significant river inflow and no outflow retain phosphorus effectively, allowing concentrations to remain high enough to support life over extended periods.
Mono Lake in California serves as a modern analog. Roughly twice the size of Lake Zurich, it maintains consistently high phosphorus levels that support diverse microbial life. This stability is due to the continuous influx of phosphorus-rich water and the lack of any natural outlet, which prevents nutrient loss.
Walton and his team argue that such large, closed-basin lakes could have served as optimal environments for the origin of life on early Earth. These lakes not only provided abundant phosphorus but also maintained it at levels suitable for both prebiotic chemistry and the development of living organisms. The new hypothesis challenges earlier ideas, such as Charles Darwin's concept of life beginning in small, shallow pools.
"This new theory helps to solve another piece of the puzzle of the origin of life on Earth," says Walton.
Research Report:Large closed-basin lakes sustainably supplied phosphate during the origins of life
Related Links
ETH Zurich's Centre for Origin and Prevalence of Life (COPL)
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