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Palynology is the study of microorganisms and microscopic fragments of mega-organisms that are composed of acid-resistant organic material and occur in sediments, sedimentary rocks, and even some metasedimentary rocks.
Fusulinid from the Plattsmouth Chert, Red Oak, Iowa ().Micropaleontology can be roughly divided into four areas of study on the basis of microfossil composition: (a) calcareous, as in coccoliths and foraminifera, (b) phosphatic, as in the study of some vertebrates, (c) siliceous, as in diatoms and radiolaria, or (d) organic, as in the pollen and spores studied in palynology.
Organic microfossils: The study of organic microfossils is called palynology. Organic microfossils include pollen, spores, chitinozoans (thought to be the egg cases of marine invertebrates), scolecodonts (worm jaws), acritarchs, dinoflagellate cysts, and fungal remains.
Acritarchs are organic microfossils, known from approximately 1800 million years ago to the present. [inconsistent] The classification is a catch all term used to refer to any organic microfossils that cannot be assigned to other groups.
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Palynology (3 C, 25 P) Pages in category "Microfossils" The following 11 pages are in this category, out of 11 total. This list may not reflect recent changes. C.
The society is organised into six specialist groups, namely Foraminifera, Microvertebrates, Calcareous Nannofossils, Ostracods, Palynology and Silicofossils. The groups hold separate meetings, including field trips, throughout the year; these were traditionally meetings for UK-based members but have become more international in their scope.
Paleoclimatology uses a variety of proxy methods from Earth and life sciences to obtain data previously preserved within rocks, sediments, boreholes, ice sheets, tree rings, corals, shells, and microfossils. Combined with techniques to date the proxies, the paleoclimate records are used to determine the past states of Earth's atmosphere.