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...orphs as paleoclimate indicators and the methods by which sedimentation of palynomorph assemblages help infer depositional environments in both marine and nonmari ==Distribution of palynomorph types==

...al alteration index) are maturation indicators that measure the color of [[palynomorph]]s. Color changes as a function of [[Maturation|maturity]].

[[file:AlghufailyetalFigure5.jpg|thumb|300px|{{figure number|5}}Integrated palynomorph-AOM thermal alteration index (IPA-TAI).<ref name=Ertugetal_2019>Ertug, K., ...ermal alteration indexes and visual charts have been proposed which relate palynomorph color to thermal maturity (e.g., Staplin,<ref name=Staplin_1969>Staplin, F.

Ratios or percentages of in situ vs. reworked calcareous nannofossil or palynomorph species may differentiate among distinct sediment packages. * Ratios or percentages of in situ vs. reworked calcareous nannofossil or palynomorph species

...mistry, v. 2, Academic Press, London, p. 2.</ref>). Organic facies are not palynomorph facies, palynofacies, pollen facies, [[kerogen]] facies, organic matter fac