Carbon emissions along divergent plate boundaries modulate icehouse-greenhouse climates

Jan 1, 2026·
Dr. Ben Mather
Dr. Ben Mather
R. Dietmar Müller
R. Dietmar Müller
Adriana Dutkiewicz
Adriana Dutkiewicz
Sabin Zahirovic
Sabin Zahirovic
· 1 min read
Abstract
The exchange of carbon between oceanic plates, the deep Earth, and the atmosphere plays a significant role in modulating global climate. Icehouse-greenhouse climate fluctuations have been attributed to changes in palaeogeography and solid Earth degassing, particularly along continental arcs, to arc weathering and to the sequestration of carbon into oceanic carbonate-rich sediments. However, the proportions of these contributions and their effect on modulating global climate are poorly constrained. Here we show that the changing balance between volcanic outgassing and carbon sequestration into oceanic lithosphere is the key driver for major climate shifts. Combined volcanic arc, mid-ocean ridge and continental rift emissions exceed carbon sequestration during greenhouse climates. In contrast, oceanic plate sequestration exceeds emissions during icehouse climates. Our results challenge the long-held view that carbon degassing along volcanic arcs is the main contributor to atmospheric carbon, suggesting instead that mid-ocean ridge and rift degassing surpass arc emissions before 100 Ma.
Type
Publication
Communications Earth & Environment
publications

Plain Language Summary

Earth’s climate has alternated between warm “greenhouse” periods and cold “icehouse” periods over hundreds of millions of years. A major factor in these swings is the amount of carbon dioxide (CO₂) released by volcanic and tectonic activity versus the amount stored away in oceanic rocks and sediments. But which tectonic processes matter most has been debated for decades.

This study reveals that the balance between CO₂ emissions from all volcanic sources — including mid-ocean ridges, continental rifts, and volcanic arcs — and carbon being locked into the oceanic plates is what drives the big climate shifts. During greenhouse periods, total volcanic emissions outpace carbon sequestration; during icehouse periods, the oceans absorb and store more carbon than volcanoes release. Crucially, the study challenges the long-standing assumption that volcanic arcs above subduction zones are the dominant source of tectonic CO₂.

Before 100 million years ago, CO₂ emissions from mid-ocean ridges and continental rifts — where tectonic plates pull apart — actually exceeded arc emissions, making divergent plate boundaries the primary driver of atmospheric carbon. This finding fundamentally reshapes our understanding of how plate tectonics has regulated Earth’s climate through geological time and provides critical new constraints for models of the long-term carbon cycle.

Dr. Ben Mather
Authors
ARC Industry Research Fellow

I am an ARC Industry Research Fellow in the School of Geography, Earth and Atmospheric Sciences at The University of Melbourne. I am an expert in fusing Earth evolution models with data to understand how groundwater moves critical minerals through the landscape. Related research interests include the cycling of volatiles within the Earth, probabilistic thermal models of the lithosphere to unravel past tectonic and climatic events, and understanding the how enigmatic volcanoes form.

I am a vocal advocate for the integral role of geoscience in responding to challenges we face in transitioning to the carbon-neutral economy. As an expert in my field, I have been interviewed in national and international print media, TV, and radio on a wide variety of subjects including earthquakes, volcanoes, groundwater, and critical minerals.

R. Dietmar Müller
Authors
Professor of Geophysics
Dietmar Müller leads the EarthByte Group and is a Fellow of the Australian Academy of Science. His research focuses on plate tectonics, geodynamics, and the development of the GPlates software for producing open-access models of Earth’s dynamic history.
Adriana Dutkiewicz
Authors
Associate Professor
Adriana Dutkiewicz is a sedimentologist in the EarthByte Group who uses scientific ocean drilling data to understand deep-sea circulation and carbon reservoirs over geological time. She is the first woman to receive the Australian Academy of Science’s Mawson Medal.
Sabin Zahirovic
Authors
Lecturer and Robinson Fellow
Sabin Zahirovic is an Earth scientist focused on the deep-time evolution of our planet, specialising in global plate tectonic reconstructions, geodynamics, paleogeography, and the links between plate tectonics and the deep carbon cycle.