A semimartingale is the sum of a local martingale and an adapted finite-variation process. This is the broad class of integrators for which the Itô stochastic integral is defined.
A continuous semimartingale is a continuous adapted process admitting a decomposition , with a zero-starting continuous local martingale and continuous adapted finite variation. The decomposition is unique because a continuous finite-variation local martingale starting at zero vanishes. Its quadratic variation is .
If is a semimartingale under and , then it is a semimartingale under . The Bichteler-Dellacherie theorem gives a short proof: terminal elementary integrals associated with uniformly small elementary predictable processes with stopping-time intervals converge to zero in -probability. Uniform convergence on compacts in probability under an absolutely continuous measure change, or its single-random-variable proof, transfers convergence to . The same good-integrator characterization now applies under . Adaptedness and càdlàg paths are preserved because -null sets remain -null; if necessary use the usual -completion of the same filtration. If the integrands are bounded only outside -null sets, clip their coefficients to the specified deterministic bounds before applying the -criterion; this preserves their -versions. Completion adds only equivalent versions of measurable coefficients. This theorem does not preserve the local martingale property.
If and is a semimartingale under both measures, the two integrals of any locally bounded predictable against agree up to -indistinguishability. Elementary integrals are the same increment sums. Bounded pointwise convergence of integrands, stochastic dominated convergence, and transfer of probability convergence from to extend equality by the monotone-class theorem. Localize to remove boundedness.
// Target: probability-and-statistics.bigb
An adapted càdlàg process is a semimartingale exactly when it is a good integrator: on each finite horizon, for every sequence of bounded elementary predictable processes with stopping-time intervals whose deterministic uniform bounds tend to zero, the elementary terminal integrals tend to zero in probability. The elementary integral is a finite sum of measurable coefficients times subsequent increments; the characterization says precisely when this operation extends continuously to stochastic integration. The theorem is used here as a standard characterization, not proved from first principles.
A process has finite variation on compact intervals when every sample path has finite total variation of a function there. Such a process can be integrated pathwise by the Lebesgue-Stieltjes integral.
For a path of finite variation, its total-variation process iswhere the supremum is over every partition of an interval of . It is an increasing process, and the signed measure satisfies .
If a càdlàg function has finite variation on compact intervals, its total-variation process is finite, nondecreasing, and càdlàg. Left limits follow from monotonicity. For right continuity, approximate the variation on by one finite partition. Changing its first endpoint from to changes the sum by at most , which tends to zero. Additivity of variation then bounds by an arbitrarily small error. Its jump is the absolute jump of . Without locally finite variation, right continuity can fail even as an extended-valued assertion: with has infinite variation on every interval starting at zero.
A semimartingale has a decomposition into a local martingale and an adapted finite-variation process . Under standard normalizations the decomposition is unique.
A continuous semimartingale has a decomposition in which both the local-martingale and finite-variation parts are continuous.
With the local martingale definition requiring each stopped process itself to be a martingale, the initial value is integrable. A normalized continuous semimartingale decomposition with can therefore have a local-martingale part only if is integrable. A smooth transformation need not preserve this condition: take , for an initially known standard normal random variable, and . Then is finite almost surely but has infinite expectation. The always-valid decomposition is instead with a zero-starting continuous local martingale and a continuous finite-variation process starting at zero.
Articles by others on the same topic
There are currently no matching articles.