Exoplanets, -moons, -comets

The Role Of Tectonic Luck in Long-Term Habitability of Abiotic Earth-like Planets

By Keith Cowing
Status Report
astro-ph.EP
August 1, 2025
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The Role Of Tectonic Luck in Long-Term Habitability of Abiotic Earth-like Planets
Modern-day Earth estimates of reservoirs and fluxes of the slow carbon system considered in our model, in units of gigatonnes of carbon (GtC, 1012 kgC) from C.-T. Lee et al. (2019). There is significant uncertainty in modern-day flux values. Carbon in continental crust (∼ 42 × 106 GtC), continental lithospheric mantle (≲ 48 × 106 GtC), and oceanic crust/lithospheric mantle (∼ 14 × 106 GtC) are not tracked in our simulations, as they are much larger than surface reservoirs and are treated as functionally inexhaustible. — astro-ph.EP

Carbonate-silicate weathering feedback is thought to stabilize Earth’s climate on geologic timescales.

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If climate warms, faster mineral dissolution and increased rainfall speed up weathering, increasing CO2 drawdown and opposing the initial warming.

Limits to where this feedback might operate on terrestrial exoplanets with N2-O2-CO2-H2O atmospheres are used to define the ‘habitable zone’-the range of orbits around a star where liquid water can be stable on a planet’s surface. However, the impacts on long-term habitability of randomly varying volcanic outgassing, tectonic collisions, and tectonic parameters (e.g., number of continental plates, size of plates, plate velocity) remain poorly understood.

In this work, we present an idealized and broadly-applicable quasi-2D model of the long-term climate stability of abiotic Earth-twins. The model tracks atmospheric CO2 as ‘disks’ collide, promoting uplift and supplying new weatherable minerals through erosion.

Without resupply, soils become less weatherable and the feedback’s strength wanes, making a planet susceptible to catastrophic warming events or hard snowballs where the surface becomes frozen over.

We find that tectonic uplift spurred by continental collisions cannot be the sole supplier of weatherable minerals within our model framework, as such climates either become uninhabitably hot (for complex life) as soils become leached of weatherable minerals or experience extreme swings in temperature over short timescales. This conclusion is strengthened when taking into account the destabilizing effects of outgassing variability and increasing stellar luminosity.

In addition to frequent collisions, other resupply mechanisms for weatherable minerals, such as wind-driven dust transport, glacial erosion, and/or seafloor weathering, are likely required for long-term stability on Earth-like terrestrial exoplanets.

Brandon Park Coy, Edwin S. Kite, R.J. Graham

Comments: 38 pages, 24 figures, Accepted for publication in PSJ
Subjects: Earth and Planetary Astrophysics (astro-ph.EP)
Cite as: arXiv:2507.23124 [astro-ph.EP] (or arXiv:2507.23124v1 [astro-ph.EP] for this version)
https://doi.org/10.48550/arXiv.2507.23124
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Submission history
From: Brandon Park Coy
[v1] Wed, 30 Jul 2025 21:57:07 UTC (13,129 KB)
https://arxiv.org/abs/2507.23124
astrobiology

Explorers Club Fellow, ex-NASA Space Station Payload manager/space biologist, Away Teams, Journalist, Lapsed climber, Synaesthete, Na’Vi-Jedi-Freman-Buddhist-mix, ASL, Devon Island and Everest Base Camp veteran, (he/him) 🖖🏻