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A palynofacies is the complete assemblage of organic matter and palynomorphs in a fossil deposit.The term was introduced by the French geologist André Combaz in 1964.
It is the science that studies contemporary and fossil palynomorphs, including pollen, spores, orbicules, dinocysts, acritarchs, chitinozoans and scolecodonts, together with particulate organic matter (POM) and kerogen found in sedimentary rocks and sediments.
This was the introduction of pollen analysis in North America; pollen diagrams today still often remain in the same format with depth on the y-axis and abundances of species on the x-axis.
Pollen analysis advanced rapidly in this period due to advances in optics and computers.
Palynology does not include diatoms, foraminiferans or other organisms with siliceous or calcareous exoskeletons. A classic palynologist analyses particulate samples collected from the air, from water, or from deposits including sediments of any age.
Palynology does not include diatoms, foraminiferans or other organisms with siliceous or calcareous exoskeletons.
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