The environmental fate of insecticidal Cry proteins,
including
time-dependent conservation of biological properties, results from
their structural stability in soils. The complex cascade of reactions
involved in biological action requires Cry proteins to be in solution.
However, the pH-dependent changes in conformational stability and
the adsorption–desorption mechanisms of Cry protein on soil
minerals remain unclear. We used Derjaguin–Landau–Verwey–Overbeek
(DLVO) calculation and differential scanning calorimetry to interpret
the driving forces and structural stabilities of Cry1Ac and two contrasting
model proteins adsorbed by montmorillonite. The structural stability
of Cry1Ac is closer to that of the “hard” protein, α-chymotrypsin,
than that of the “soft” bovine serum albumin (BSA).
The pH-dependent adsorption of Cry1Ac and α-chymotrypsin could
be explained by DLVO theory, whereas the BSA adsorption deviated from
it. Patch-controlled electrostatic attraction, hydrophobic effects,
and entropy changes following protein unfolding on a mineral surface
could contribute to Cry1Ac adsorption. Cry1Ac, like chymotrypsin,
was partly denatured on montmorillonite, and its structural stability
decreased with an increase in pH. Moreover, small changes in the conformational
heterogeneity of both Cry1Ac and chymotrypsin were observed following
adsorption. Conversely, adsorbed BSA was completely denatured regardless
of the solution pH. The moderate conformational rearrangement of adsorbed
Cry1Ac may partially explain why the insecticidal activity of Bt toxin
appears to be conserved in soils, albeit for a relatively short time
period.