“The Aleutian Islands tell a much older tectonic story than we had previously assumed,” said lead author Prof. Dr. Kaj Hoernle, head of the Petrology and Geochemistry Group at GEOMAR Helmholtz Centre for Ocean Research Kiel. “According to our findings, the onset of subduction represents a key event that marked the beginning of a major, approximately ten-million-year-long period of plate restructuring.” These tectonic and magmatic processes may also have contributed to global climate events in the late Paleocene and early Eocene.
Ancient Rocks from a Remote Island Arc
To reconstruct the early history of the Aleutian Arc, the team collected rock samples from key parts of the island chain and its submarine basement. These samples were collected during the research cruises KALMAR SO201 and BERING SO249, as well as an expedition to the Russian Komandorsky Islands of Medny and Bering. This enabled both the American and Russian parts of the Aleutian Islands to be systematically investigated for the first time.
The researchers then determined the age of the rocks using two independent dating methods: uranium–lead dating of zircon crystals and argon–argon dating of volcanic rocks and minerals. The result was clear: the oldest traces of subduction are at least 56 million years old. The process thus began much earlier than many previous models had suggested.
This earlier age is important because it places the birth of the Aleutian subduction zone at the start of a major chain of tectonic events and a reorganization of plate motions across the Pacific. During this interval, several subduction zones and volcanic arcs around the Pacific formed, a spreading center (mid-ocean ridge) was subducted, and a large igneous province collided with the North American margin. The Aleutian Arc therefore appears to represent one piece of a much larger tectonic puzzle.
A Possible Link to Ancient Global Warming
It is particularly interesting that the newly determined date coincides with the Paleocene–Eocene Thermal Maximum (PETM). At that time, the Earth experienced one of the most extreme natural warming events in its recent history, with global mean temperatures rising by more than five degrees Celsius over a geologically short period of about 10,000 to 15,000 years. It was not until around 150,000 years later that temperatures returned to levels similar to those before the start of the PETM.
The authors emphasized that a direct causal link with the formation of the Aleutian subduction zone cannot yet be proven. However, the timing is striking. The researchers discuss whether the formation of large subduction zones could have contributed to carbon release through volcanism, hydrothermal activity, or uplift of shallow marine basins. Such processes may have transferred large amounts of carbon into the ocean and atmosphere.
For now, this remains a scientific hypothesis that requires further investigation. Nevertheless, the study suggests that the birth of major subduction zones may deserve more attention as a possible trigger or amplifier of ancient global warming events.
