A metamorphic origin for Europa's ocean

Date
2021
Journal Title
Journal ISSN
Volume Title
Publisher
John Wiley & Sons, Inc
Abstract
Europa likely contains an iron-rich metal core. For it to have formed, temperatures within Europa reached urn:x-wiley:00948276:media:grl62926:grl62926-math-00011250 K. Going up to that temperature, accreted chondritic minerals — for example, carbonates and phyllosilicates — would partially devolatilize. Here, we compute the amounts and compositions of exsolved volatiles. We find that volatiles released from the interior would have carried solutes, redox-sensitive species, and could have generated a carbonic ocean in excess of Europa's present-day hydrosphere, and potentially an early urn:x-wiley:00948276:media:grl62926:grl62926-math-0002 atmosphere. No late delivery of cometary water was necessary. Contrasting with prior work, urn:x-wiley:00948276:media:grl62926:grl62926-math-0003 could be the most abundant solute in the ocean, followed by urn:x-wiley:00948276:media:grl62926:grl62926-math-0004, urn:x-wiley:00948276:media:grl62926:grl62926-math-0005, and urn:x-wiley:00948276:media:grl62926:grl62926-math-0006. However, gypsum precipitation going from the seafloor to the ice shell decreases the dissolved S/Cl ratio, such that Clurn:x-wiley:00948276:media:grl62926:grl62926-math-0007S at the shallowest depths, consistent with recently inferred endogenous chlorides at Europa's surface. Gypsum would form a 3–10 km thick sedimentary layer at the seafloor.
Description
CITATION: Melwani Daswani, M., Vance, S. D., Mayne, M. J., & Glein, C. R. (2021). A metamorphic origin for Europa's Ocean. Geophysical Research Letters, 48, e2021GL094143. doi.10.1029/2021GL094143
The original publication is available at: wiley.com
Keywords
Metamorphic -- Europa, Carbon cycle (Biogeochemistry), Metamorphism (Geology) -- Europa's ocean, Water temperature -- Europa, Carbonate minerals
Citation
Melwani Daswani, M., Vance, S. D., Mayne, M. J., & Glein, C. R. (2021). A metamorphic origin for Europa's Ocean. Geophysical Research Letters, 48, e2021GL094143. doi.10.1029/2021GL094143