In a lot of time-series analysis references I find (written by mathematicians or statisticians rather than engineers), I find the following signal decomposition for a stochastic process, termed the "Cramér representation" (e.g. eqn 8.11 of this reference): $$ X[n] = \int_{\langle 2\pi \rangle} e^{-j\omega n} d Z(\omega) $$
The factor $dZ(\omega)$ is referred to as a spectral increment. I found another reference (ref, eqn 77) that said that the spectral increments are orthogonal (w.r.t. the expectation operator) if the process is stationary.
Compare this to the inverse discrete-time Fourier Transform (IDTFT), non-normalized, angular frequency convention (eqn 4.2.28 of Proakis & Manolakis, Digital Signal Processing, 4th ed): $$ X[n] = \frac{1}{2\pi} \int_{\langle 2\pi \rangle} e^{j\omega n} X(\omega) d\omega $$
With the exception of trivial differences in convention (minus sign in the exponent, normalization factor), the two representations appear to be the same. Ignoring the minus sign convention on $\omega$ for now, I am tempted to just conclude: $$ dZ(\omega) = \frac{1}{2\pi} X(\omega) d\omega $$ but I suspect there is a deeper mathematical reason why this would be wrong and that the statistics literature uses spectral increments instead.
Why do statisticians prefer the Cramér representation? Are there any computational or theoretical advantages to using it?
Does it have something to do with the convergence (or existence) of some type of integral? Or some issue relating to the fact that $X[n]$ is explicitly a stochastic process in the Cramér representation whereas the DTFT might rely on the signal being deterministic.
I wonder this because engineering education (at least mine was this way) tends to abuse notation or gloss over certain mathematical difficulties because those nuances wouldn't matter for the situations in which an engineer would be using said mathematical tools. For instance, as an undergrad I never had to learn what a Lebesgue integral was, even though I was implicitly computing Lebesgue integrals in my probability course.