What does the existence of a weak intrinsic magnetic field on the much smaller planet Mercury suggest about Venus's core state?

Answer

Mercury's core is likely still at least partially molten and convecting.

The contrast between Mercury and Venus presents a significant paradox regarding internal thermal evolution. Mercury is significantly smaller than Venus, and generally, smaller bodies are expected to cool and solidify their cores faster than larger ones. However, Mercury possesses at least a weak intrinsic magnetic field, which requires a liquid, convecting, conductive core. Since Venus is larger, thermal models suggest it should have retained internal heat longer than Mercury. Therefore, the fact that Venus lacks a field while the smaller Mercury exhibits one implies that Venus's core situation, whether solidified or convectively stagnant, is unexpected based purely on size and cooling rates.

What does the existence of a weak intrinsic magnetic field on the much smaller planet Mercury suggest about Venus's core state?
Venüsplanetsolar windmagnetic fieldatmosphere