Earth's atmosphere has undergone dramatic changes over time, yet the gas bubbles trapped in polar ice cores can only preserve atmospheric compositions from the past six million years—less than 0.2% of Earth's history. To explore even earlier atmospheric conditions, scientists typically analyze chemical traces of metals and minerals in ancient rocks. Now, researchers at Rensselaer Polytechnic Institute (RPI) in the United States are taking a more direct approach: extracting and analyzing tiny liquid and gas inclusions trapped in salts, quartz veins, and crystallized magma.
These samples date back more than three billion years and contain direct records of rare gases, oxygen, nitrogen, and carbon dioxide. This breakthrough offers a new perspective on Earth's atmospheric history. While many findings remain preliminary, the research has already confirmed some longstanding hypotheses while challenging others. For example, studies indicate that oxygen levels were sufficient to support animal respiration as early as 800 million years ago—before animals emerged.
To extract these ancient gases, researchers gradually crush rock samples in a vacuum-sealed press, releasing the trapped gases for analysis using mass spectrometry. This process requires analyzing large quantities of rock—about 10 grams per sample—to obtain sufficient gas for measurement.
Additionally, by studying gas inclusions in rock salt deposits, such as those in Death Valley, scientists have traced nitrogen and oxygen, which are crucial for life. Although some gases dissolve in water over time, potentially affecting measurements, researchers have developed correction methods to enhance data accuracy.
This innovative approach marks a significant step forward in reconstructing Earth's atmospheric evolution, providing deeper insights into the planet's environmental conditions over billions of years.