Mass sufficiency of unmelted early NC planetesimals

Determine whether early-generation, small NC planetesimals that escaped melting and differentiation carried sufficient mass to serve as the precursors of the NC chondrites.

Background

The paper argues that efficient isolation of the NC reservoir from inward-drifting CC dust implies that the inner disk was not substantially replenished during late stages. This raises the problem of how enough primitive dust remained available to form the late-accreting NC chondrite parent bodies.

The authors consider an origin in secondary dust generated by collisions among earlier planetesimals, but regard this as unlikely because NC chondrites preserve presolar grains and isotopic heterogeneity. They therefore identify early, small planetesimals that escaped melting and differentiation as a possible source, while explicitly leaving unresolved whether such bodies contained enough mass.

References

Instead, this dust would have to derive from an early generation of planetesimals that owing to their small size escaped melting and differentiation. While such planetesimals may have existed, it is unclear if they carried sufficient mass to be the precursors of the NC chondrites.

Origin of nucleosynthetic isotope variability in the NC reservoir: Evidence from Ti, Cr, and Mo isotopes  (2608.19786 - Wölfer et al., 20 Aug 2026) in Section 4.4, pp. 21–22