A new study reveals that the aerobic nitrogen cycle in the ocean may have occurred about 100 million years before oxygen began to significantly accumulate in the atmosphere, based on nitrogen isotope analysis from ancient South African rock cores. These findings not only refine the timeline of Earth’s oxygenation but also highlight a critical evolutionary shift, where life began adapting to oxygen-rich conditions — paving the way for the emergence of complex, multicellular organisms like humans.



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