Our solar system passed through a star-forming region in the direction of the Orion constellation around 14 million years ago.
During this passage, the solar system traversed the Radcliffe Wave, a gaseous structure in the Orion Arm of the Milky Way known for its stellar nurseries.
The journey coincided with the Middle Miocene Climate Transition, potentially impacting Earth's climate through interstellar dust influx.
The findings were published in Astronomy & Astrophysics on February 11, 2025, revealing the solar system's encounter with higher gas density.
Scientists used Gaia mission data to trace the solar system's path through the Orion region, passing star clusters like NGC 1977 and NGC 1981.
The compression of the heliosphere during the passage could have increased interstellar dust influx on Earth.
Traces of radioactive elements originating from supernovae may exist in Earth's geological record due to this event.
The passage through the Orion region roughly 14 million years ago coincided with a climate shift, though the exact impact is still under investigation.
While the contribution of interstellar dust to Earth's climate transition is being explored, it's noted that the current climate change differs significantly in timescales and causes.
This event highlights the potential influence of interstellar encounters on planetary climate over extended periods.