The solar wind flows around Earth’s magnetic field. A new NASA study suggests that the amount of oxygen in the atmosphere and strength of the magnetic field have been correlated for more than half a billion years.
Credit: NASA’s Goddard Space Flight Center/Conceptual Image Laboratory
Earth’s magnetic field and atmospheric oxygen appear to have moved in sync for half a billion years, pointing to a surprising connection between the planet’s deep interior and life-supporting conditions above ground.
Magnetic Field and Oxygen Move Together Over Deep Time
A new analysis by NASA scientists finds that changes in Earth’s magnetic field strength have closely tracked shifts in atmospheric oxygen for roughly 540 million years. The results point to a possible connection between processes occurring deep inside the planet and the conditions that allow life to thrive at the surface.
The finding suggests that Earth’s habitability may not be shaped only by surface or atmospheric processes, but also by long-term activity within the planet itself.
How Earth Generates Its Magnetic Shield
Earth’s magnetic field is created by the movement of molten material inside the planet’s interior, which functions much like a massive electromagnet. This internal flow is not perfectly steady, causing the strength of the magnetic field to rise and fall over geological time.
Many researchers believe this magnetic shield helps protect Earth’s atmosphere from erosion by high-energy particles emitted by the Sun. However, as the authors of the study published in Science Advances note, the exact role magnetic fields play in preserving atmospheres is still being actively studied. Rather than attempting to untangle complex cause-and-effect relationships right away, the researchers first asked a more basic question: do changes in Earth’s magnetic field and atmospheric oxygen show matching patterns over time?
Earth’s magnetic field is created by the movement of molten material inside the planet’s interior, which functions much like a massive electromagnet. This internal flow is not perfectly steady, causing the strength of the magnetic field to rise and fall over geological time.
Many researchers believe this magnetic shield helps protect Earth’s atmosphere from erosion by high-energy particles emitted by the Sun. However, as the authors of the study published in Science Advances note, the exact role magnetic fields play in preserving atmospheres is still being actively studied. Rather than attempting to untangle complex cause-and-effect relationships right away, the researchers first asked a more basic question: do changes in Earth’s magnetic field and atmospheric oxygen show matching patterns over time?
Clues Locked Inside Ancient Rocks
Evidence of Earth’s past magnetic fields is preserved in magnetized minerals. When molten rock rises at boundaries between spreading tectonic plates and begins to cool, minerals within the magma can capture a record of the surrounding magnetic field. That record remains intact as long as the minerals are not later reheated to extreme temperatures.
Scientists are also able to estimate ancient oxygen levels by studying the chemistry of old rocks and minerals, since their composition depends on how much oxygen was present when they formed. Extensive databases containing magnetic and chemical records have been compiled by geophysicists and geochemists over many years. According to the study’s authors, no previous research had closely compared these two long-term records in detail.
“These two datasets are very similar,” said coauthor Weijia Kuang, a geophysicist at NASA’s Goddard Space Flight Center in Greenbelt, Maryland. “Earth is the only known planet that supports complex life. The correlations we’ve found could help us to understand how life evolves and how it’s connected to the interior processes of the planet.”
Evidence of Earth’s past magnetic fields is preserved in magnetized minerals. When molten rock rises at boundaries between spreading tectonic plates and begins to cool, minerals within the magma can capture a record of the surrounding magnetic field. That record remains intact as long as the minerals are not later reheated to extreme temperatures.
Scientists are also able to estimate ancient oxygen levels by studying the chemistry of old rocks and minerals, since their composition depends on how much oxygen was present when they formed. Extensive databases containing magnetic and chemical records have been compiled by geophysicists and geochemists over many years. According to the study’s authors, no previous research had closely compared these two long-term records in detail.
“These two datasets are very similar,” said coauthor Weijia Kuang, a geophysicist at NASA’s Goddard Space Flight Center in Greenbelt, Maryland. “Earth is the only known planet that supports complex life. The correlations we’ve found could help us to understand how life evolves and how it’s connected to the interior processes of the planet.”
A Pattern Reaching Back to the Rise of Complex Life
By analyzing the magnetic and oxygen records side by side, Kuang and his colleagues found that both followed comparable ups and downs for nearly half a billion years. The pattern extends back to the Cambrian explosion, the period when complex life first became widespread on Earth.
“This correlation raises the possibility that both the magnetic field strength and the atmospheric oxygen level are responding to a single underlying process, such as the movement of Earth’s continents,” said study coauthor Benjamin Mills, a biogeochemist at the University of Leeds.
By analyzing the magnetic and oxygen records side by side, Kuang and his colleagues found that both followed comparable ups and downs for nearly half a billion years. The pattern extends back to the Cambrian explosion, the period when complex life first became widespread on Earth.
“This correlation raises the possibility that both the magnetic field strength and the atmospheric oxygen level are responding to a single underlying process, such as the movement of Earth’s continents,” said study coauthor Benjamin Mills, a biogeochemist at the University of Leeds.
Looking Deeper Into Earth’s Life-Supporting Systems
The research team plans to examine even older datasets to determine whether the relationship holds further back in Earth’s history. They also aim to study the past levels of other elements essential for life as we know it, including nitrogen, to see if similar patterns emerge.
As for identifying the exact mechanisms that link Earth’s deep interior to conditions at the surface, Kopparapu emphasized that more investigation is needed, saying: “There’s more work to be done to figure that out.”
The research team plans to examine even older datasets to determine whether the relationship holds further back in Earth’s history. They also aim to study the past levels of other elements essential for life as we know it, including nitrogen, to see if similar patterns emerge.
As for identifying the exact mechanisms that link Earth’s deep interior to conditions at the surface, Kopparapu emphasized that more investigation is needed, saying: “There’s more work to be done to figure that out.”
The Life of Earth
https://chuckincardinal.blogspot.com/
No comments:
Post a Comment
Stick to the subject, NO religion, or Party politics