Implications of a long-lived basal magma ocean in generating Earth's ancient magnetic field

Illustration of three phases of geodynamo generation:

Illustration of three phases of geodynamo generation:

TitleImplications of a long-lived basal magma ocean in generating Earth's ancient magnetic field
Publication TypeJournal Article
Year of Publication2013
AuthorsZiegler L.B, Stegman DR
JournalGeochemistry Geophysics Geosystems
Volume14
Pagination4735-4742
Date Published2013/11
Type of ArticleArticle
ISBN Number1525-2027
Accession NumberWOS:000330531900001
Keywordsbillion years ago; core conditions; electrical-conductivity; evolution; high-pressure; Iron; Magma Ocean; mantle conductivity; metallization; models; paleomagnetism; Thermal; thermal evolution of Earth
Abstract

Observations of Earth's magnetic field extending back to 3.45 billion years ago indicate that generation by a core dynamo must be sustained over most of Earth's history. However, recent estimates of thermal and electrical conductivity of liquid iron at core conditions from mineral physics experiments indicate that adiabatic heat flux is approximately 15 TW, nearly three times larger than previously thought, exacerbating difficulties for driving a core dynamo throughout Earth history by convective core cooling alone. Here, we explore the geomagnetic consequences of a basal magma ocean layer in the lowermost mantle, hypothesized to exist in the early Earth and perhaps surviving until well after the Archean. While the modern, solid lower mantle is an electromagnetic insulator, electrical conductivities of silicate melts are known to be higher, though as yet they are unconstrained for lowermost mantle conditions. We consider a range of possible electrical conductivities and find that for the highest electrical conductivities considered, a long-lived basal magma ocean could be a primary dynamo source region. This would suggest the proposed three magnetic eras observed in paleomagnetic data originate from distinct sources for dynamo generation: from 4.5 to 2.45 Ga within a basal magma ocean, from 2.25 to 0.4 Ga within a superadiabatically cooled liquid core, and from 0.4 Ga to present within a quasi-adiabatic core that includes a solidifying inner core.

DOI10.1002/2013gc005001
Short TitleGeochem. Geophys. Geosyst.
Impact: 

The hypothesized existence of a basal magma ocean, a liquid rather than solid core for the ancient Earth, and new views of the insulating capabilities of the mantle, imply that the mechanism for generating Earth's magnetic field has changed over time. This also suggests there may have been transitional periods during which the Earth's magnetic shield was absent or reduced.

Integrated Research Themes: 
Student Publication: 
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