Oceanographic Considerations for Exoplanet Life Detection

TL;DR

This study investigates how ocean dynamics on exoplanets influence nutrient cycling and the potential for detectable life, highlighting the importance of planetary parameters like rotation and pressure in shaping habitable ocean environments.

Contribution

It uses climate modeling to explore how different planetary conditions affect ocean circulation and nutrient availability, informing strategies for exoplanet life detection.

Findings

Slower rotation and higher surface pressure enhance upwelling and nutrient supply.

High obliquity can increase nutrient mixing through seasonal deepening.

Ocean dynamics significantly impact biosignature production and detectability.

Abstract

Liquid water oceans are at the center of our search for life on exoplanets because water is a strict requirement for life as we know it. However, oceans are dynamic habitats---and some oceans may be better hosts for life than others. In Earth's ocean, circulation transports essential nutrients such as phosphate and is a first-order control on the distribution and productivity of life. Of particular importance is upward flow from the dark depths of the ocean in response to wind-driven divergence in surface layers. This `upwelling' returns essential nutrients that tend to accumulate at depth via sinking of organic particulates back to the sunlit regions where photosynthetic life thrives. Ocean dynamics are likely to impose constraints on the activity and atmospheric expression of photosynthetic life in exo-oceans as well, but we lack an understanding of how ocean dynamics may differ on other planets. We address this issue by exploring the sensitivity of ocean dynamics to a suite of planetary parameters using ROCKE-3D, a fully coupled ocean-atmosphere GCM. Our results suggest that planets that rotate slower and have higher surface pressure than Earth may be the most attractive targets for remote life detection because upwelling is enhanced under these conditions, resulting in greater nutrient supply to the surface biosphere. Seasonal deepening of the mixed layer on high obliquity planets may also enhance nutrient replenishment from depth into the surface mixed layer. Efficient nutrient recycling favors greater biological activity, more biosignature production, and thus more detectable life. More generally, our results demonstrate the importance of considering oceanographic phenomena for exoplanet life detection and motivate future interdisciplinary contributions to the emerging field of exo-oceanography.