Scientists have made a groundbreaking discovery in Antarctica, uncovering an air sample trapped within the oldest known ice core dating back approximately 6 million years. This ancient find has provided researchers with a unique opportunity to reconstruct Earth's atmosphere millions of years ago.
The team behind the study, led by geophysicist Sarah Shackleton at Woods Hole Oceanographic Institution, utilized advanced techniques such as detailed measurements of isotopes and laser spectroscopy to analyze the air bubbles trapped in three new ice cores collected from the Allan Hills. These ice sheets in southeastern Antarctica are home to some of the oldest known ice on Earth.
The findings reveal that the area corresponding to today's Allan Hills experienced a gradual, long-term decrease in temperatures of about 22 degrees Fahrenheit over millions of years, providing scientists with valuable insight into past climate conditions. However, one sample of dirty basal ice proved difficult to date due to its lack of gas, leading researchers to speculate about its significance and potential to shed light on the region's ancient history.
The team's research demonstrates the vast potential of ice cores in investigating and reconstructing climates long past, particularly for warmer periods. As Shackleton notes, "we think we've just scratched the surface of what's possible," with much more data still forthcoming from new measurements and further discoveries.
In fact, Shackleton hints that there may be even older ice out there to uncover, sparking excitement among researchers about the ongoing possibilities of this extraordinary discovery.
The team behind the study, led by geophysicist Sarah Shackleton at Woods Hole Oceanographic Institution, utilized advanced techniques such as detailed measurements of isotopes and laser spectroscopy to analyze the air bubbles trapped in three new ice cores collected from the Allan Hills. These ice sheets in southeastern Antarctica are home to some of the oldest known ice on Earth.
The findings reveal that the area corresponding to today's Allan Hills experienced a gradual, long-term decrease in temperatures of about 22 degrees Fahrenheit over millions of years, providing scientists with valuable insight into past climate conditions. However, one sample of dirty basal ice proved difficult to date due to its lack of gas, leading researchers to speculate about its significance and potential to shed light on the region's ancient history.
The team's research demonstrates the vast potential of ice cores in investigating and reconstructing climates long past, particularly for warmer periods. As Shackleton notes, "we think we've just scratched the surface of what's possible," with much more data still forthcoming from new measurements and further discoveries.
In fact, Shackleton hints that there may be even older ice out there to uncover, sparking excitement among researchers about the ongoing possibilities of this extraordinary discovery.