Effects of simulated serpentine soil conditions (elevated Mg:Ca ratio and N
i concentration) on seedlings from populations of Virginia pine (Pinus virg
iniana Mill.) from serpentine and non-serpentine sites were evaluated in sa
nd culture. We determined (1) how seedlings are affected by elevated Mg:Ca
ratio and Ni concentrations, (2) if there are interactive effects between M
g:Ca ratio and Ni concentrations on seedling growth, needle pigment concent
rations, and nutrition, and (3) if Virginia pine populations from serpentin
e areas are edaphic ecotypes. A Mg:Ca ratio of 5 and 50 mu M Ni both reduce
d seedling growth compared with control seedlings grown in the presence of
the standard Mg:Ca ratio of 0.5 and no Ni. Interactive effects between Mg:C
a ratio and Ni concentrations were highly significant for growth, foliar pi
gments, and needle and root elemental concentrations. Nickel-mediated reduc
tions in growth and foliar pigment concentrations were less at the serpenti
ne Mg:Ca ratio of 5 than at the standard (non-serpentine) Mg:Ca ratio of 0.
5. Foliar N was reduced by Ni concentrations as low as 10 mu M, and foliar
and root K, Ca and P concentrations were significantly reduced by Ni concen
trations above 25 mu M, with greater reductions at a Mg:Ca ratio of 0.5 tha
n at a Mg:Ca ratio of 5. There were no population x serpentine soil factor
interactions for seedling growth, foliar pigment concentrations, or nutriti
on, suggesting that seedlings from trees growing on serpentine soils are no
t edaphic ecotypes. We conclude that serpentine conditions present at the s
ite of seed collection have not resulted in the selection of edaphic ecotyp
es of Virginia pine with respect to Mg:Ca ratio and Ni concentration.