  Because of the roughly linear correlation between Be/H and Fe/H in low
metallicity halo stars, it has been argued that a ``primary'' component in the
nucleosynthesis of Be must be present in addition to the ``secondary''
component from standard Galactic cosmic ray nucleosynthesis. In this paper we
critically re-evaluate the evidence for the primary versus secondary character
of Li, Be, and B evolution, analyzing both in the observations and in Galactic
chemical evolution models. While it appears that [Be/H] versus [Fe/H] has a
logarithmic slope near 1, it is rather the Be-O trend that directly arises from
the physics of spallation production. Using new abundances for oxygen in halo
stars based on UV OH lines, we find that the Be-O slope has a large uncertainty
due to systematic effects, rendering it difficult to distinguish from the data
between the secondary slope of 2 and the primary slope of 1. The possible
difference between the Be-Fe and Be-O slopes is a consequence of the variation
in O/Fe versus Fe: recent data suggests a negative slope rather than zero
(i.e., Fe $\propto$ O) as is often assumed. In addition to a phenomenological
analysis of Be and B evolution, we have also examined the predicted LiBeB, O,
and Fe trends in Galactic chemical evolution models which include outflow.
Based on our results, it is possible that a good fit to the LiBeB evolution
requires only traditional the Galactic cosmic ray spallation, and the (primary)
neutrino-process contribution to B11. We thus suggest that these two processes
might be sufficient to explain Li6, Be, and B evolution in the Galaxy, without
the need for an additional primary source of Be and B.
