It has been recognized for a decade that stellar models which account
for the microscopic diffusion of lithium are not compatible with the n
early uniform lithium abundance, as a function of temperature, found i
n metal-poor halo dwarfs (the Spite plateau). The recent observations
of Thorburn (1994) extend the Spite plateau by about 200 degrees (to h
igher temperatures) and thus significantly exacerbate the problem. Her
ein it is shown that microscopic diffusion can be compatible with the
lithium observations if mild main-sequence mass loss occurs throughout
the evolution of these halo dwarfs. Mass-loss rates of approximately
- 1 x 10(-12) M(.) yr-1 are required. These models suggest that halo s
tars have depleted their initial lithium uniformly by a factor of appr
oximately 1.6 or 0.2 dex. These models should also provide agreement w
ith globular cluster color-magnitude diagrams superior to that of diff
usion models without mass loss.