A common hypothesis is that helium isotopes in mantle-derived materials rep
resent two distinct populations. the midocean ridge (MORB) reservoir and th
e oceanic island (OIB) reservoir. We ask the question 'Can we disprove the
null hypothesis that OIB and MORB samples are drawn from the same populatio
n distribution function?' The answer is no, meaning that the datasets could
be drawn from the same population. Previous studies have reached the oppos
ite conclusion by comparing extreme values in one population with the mean
value, or range, of the other population after the extreme values are remov
ed, The variance of the He-3/He-4 distribution for various ridge segments d
ecreases with the spreading rate and the high variance of individual OIB da
tasets is consistent with slow spreading, small sampled volume, or low degr
ees of melting or degassing. (C) 2001 Elsevier Science B.V. All rights rese
rved.