Scientists resurrect ancient enzyme to study origins of life on Earth

Researchers have reconstructed a nitrogen-fixing enzyme from more than three billion years ago using synthetic biology. The work offers new insights into how life evolved on early Earth and could inform searches for life elsewhere in the universe.

Scientists at Utah State University and the University of Wisconsin-Madison rebuilt ancestral versions of nitrogenases, enzymes that convert atmospheric nitrogen into a form usable by living organisms. The study, published in Nature Communications, examined how these enzymes may have functioned billions of years ago.

Lance Seefeldt, a biochemist at Utah State University, noted that all living organisms need nitrogen to survive yet cannot access it directly. "Enzymes called nitrogenases enable nitrogen fixation," he said. The team measured nitrogen isotope fractionation in engineered strains to compare ancient and modern versions.

Betül Kaçar, who leads the NASA-funded MUSE project, said the findings help explain conditions on early Earth before oxygen-dependent life emerged. She added that understanding the planet's past is essential for identifying life on other worlds.

The research may also support efforts to improve agriculture in drought-prone areas and to grow food in space.

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Scientist in lab studying bacterial production of HDAC inhibitor cancer drug variants through molecular mix-and-match mechanism.
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Scientists map a ‘mix-and-match’ bacterial mechanism behind variants of a cancer drug family

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Researchers at the University of Warwick report they have identified how bacteria can reliably produce multiple versions of certain histone deacetylase (HDAC) inhibitor compounds, a finding they say could help scientists engineer new drug candidates inspired by these natural products.

Two researchers have identified a new organelle that allows a type of algae to fix nitrogen from the air. The discovery challenges a long-standing rule of biology. It could offer insights for future agricultural innovations.

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New computer models indicate that ancient asteroid strikes created vast underground hydrothermal systems on early Earth. These environments could have supported the chemical processes needed for life to begin. Researchers from the Southwest Research Institute led the study.

Computer simulations have identified a previously unknown manganese-rich oxide that may have contributed to Earth's Great Oxygenation Event around 2 billion years ago.

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