I was wondering: Given a variety over a finite field, say the projective plane or sphere over $\mathbb{F}_q$. Then I can try to define parallel transport along (geodesic) curves. In particular, I can compare the parallel transport along different paths and see if or if not they differ by an element in the point stabilizer, say $\mathrm{SO}_{2}(\mathbb{F}_q)$. This should somehow mean curvature. Any literature tips? I only found parallel transport for $p$-adic varieties.
More explicitly I have the following problem: I want to pick for every two elements (suitable) $x,y$ on a projective plane or sphere an element in $\mathrm{SO}_{3}(\mathbb{F}_q)$ sending $x\mapsto y$; say the rotation along the circle connecting $x,y$. Then I want to understand how much this assignment is non-multiplicative. My guess is that for composing $x\mapsto y \mapsto z$ I can get for different $y$ the same number of times each possible results (differing by the point stabilizer), and those giving the same result as directly $x \mapsto z$ come precisely for the $y$ laying on the circle through $x$, $z$. But I see no way to prove this for general $q$.
This seems like an elementary question about spheres over finite fields, but I am not successful in finding results on it. My intuition puts it in the corner of parallel transport, but maybe the right way to deal with it comes from a complete different direction.