100x larger hydrogen-rich hydrothermal system beneath western Pacific seafloor discovered.
Researchers revealed that the Kunlun hydrothermal field—a tectonically active site roughly 80 kilometers west of the Mussau Trench on the Caroline Plate—comprises 20 large seafloor depressions (some exceeding one kilometer in diameter) clustered together like a pipe swarm, a group of vertical or steeply inclined cylindrical rock structures that funnel liquid or gas from Earth’s interior.
The total area is 11.1 square kilometers, i.e., over a hundred times larger than the Lost City, a unique deep-sea hydrothermal field located on the Atlantis Massif, a section of the Mid-Atlantic Ridge.
“The Kunlun system stands out for its exceptionally high hydrogen flux, scale, and unique geological setting,” said Prof. SUN Weidong, the study’s corresponding author. “It shows that serpentinization-driven hydrogen generation can occur far from mid-ocean ridges, challenging long-held assumptions.”