Palynology is the "study of dust" (from Greek παλύνω - palunō, "strew, sprinkle"[2] and -logy) or "particles that are strewn". A classic palynologist analyses particulate samples collected from the air, water, or from deposits including sediments of any age. The condition and identification of those particles, organic and inorganic, give the palynologist clues to the life, the environment, and energetic conditions that produced them.

The term is sometimes narrowly used to refer to a subset of the discipline, which is defined as "the study of microscopic objects of macromolecular organic composition (i.e. compounds of carbon, hydrogen, nitrogen and oxygen), not capable of dissolution in hydrochloric or hydrofluoric acids."[3] 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. Palynology does not include diatoms, foraminiferans or other organisms with siliceous or calcareous exoskeletons.

Palynology is an interdisciplinary science and is a branch of earth science (geology or geological science) and biological science (biology), particularly plant science (botany). Stratigraphical palynology is a branch of micropalaeontology and paleobotany which studies fossil palynomorphs from the Precambrian to the Holocene.

A history of palynology

Early history

The earliest reported observations of pollen under a microscope are likely to have been in the 1640s by the English botanist Nehemiah Grew[4] who described pollen, the stamen, and correctly predicted that pollen is required for sexual reproduction in flowering plants. As microscopes began to improve, further studies included work by Robert Kidston and P. Reinsch who examined the presence of spores in coal and compared them to modern spores.[5] The early pioneers also included Christian Gottfried Ehrenberg (radiolarians, diatoms and dinoflagellate cysts), Gideon Mantell (desmids) and Henry Hopley White (dinoflagellate cysts).

Modern palynology

The earliest quantitative analysis of pollen was published by Lennart von Post who laid out the foundations of modern pollen analysis in his Kristiania lecture of 1916.[6] Pollen analysis was initially confined to Nordic countries because many early publications were in Nordic languages.[7] This isolation ended with the publication of Gunnar Erdtman's thesis of 1921 when pollen analysis became widespread throughout Europe and North America for use in studies of Quaternary vegetation and climate change.[6]

The term palynology was introduced by Hyde and Williams in 1944, following correspondence with the Swedish geologist Antevs, in the pages of the Pollen Analysis Circular (one of the first journals devoted to pollen analysis, produced by Paul Sears in North America). Hyde and Williams chose palynology on the basis of the Greek words paluno meaning 'to sprinkle' and pale meaning 'dust' (and thus similar to the Latin word pollen).[8]

Methods of study


Palynomorphs are broadly defined as organic-walled microfossils between 5 and 500 micrometres in size. They are extracted from rocks and sediment cores both physically, by wet sieving, often after ultrasonic treatment, and chemically, by using chemical digestion to remove the non-organic fraction.

A palynomorph (from Greek, meaning "strewn or sprinkled forms") is a particle of a size between five and 500 micrometres, found in rock deposits (sedimentary rocks) and composed of organic material such as chitin, pseudochitin and sporopollenin. Described palynomorphs are sometimes referred to as palynotaxa.

Palynomorphs form a geological record of importance in determining the type of prehistoric life that existed at the time the sedimentary formation was laid down. As a result, these microfossils give important clues to the prevailing climatic conditions of the time. Their paleontological utility derives from an abundance numbering in millions of cells per gram in organic marine deposits, even when such deposits are generally not fossiliferous. Palynomorphs, however, generally have been destroyed in metamorphic or recrystallized rocks.

Typically, palynomorphs are dinoflagellate cysts, acritarchs, spores, pollen, fungi, scolecodonts (scleroprotein teeth, jaws and associated features of polychaete annelid) worms, arthropod organs (such as insect-mouth parts), chitinozoans and microforams. Palynomorphs microscopic structure that are abundant in most sediments ans resistant to routine pollen extraction including strong acid and bases and acetolysis,density separation

Chemical preparation

Chemical digestion follows a number of steps.[9] Initially the only chemical treatment used by researchers was treatment with KOH to remove humic substances; defloculation was accomplished through surface treatment or ultra-sonic treatment, although sonification may cause the pollen exine to rupture.[7] The use of hydrofluoric acid (HF) to digest silicate minerals was introduced by Assarson and Granlund in 1924, greatly reducing the amount of time required to scan slides for palynomorphs.[10] Palynological studies using peats presented a particular challenge because of the presence of well preserved organic material including fine rootlets, moss leaflets and organic litter. This was the last major challenge in the chemical preparation of materials for palynological study. Acetolysis was developed by Gunnar Erdtman and his brother to remove these fine cellulose materials by dissolving them.[11] In acetolysis the material is treated with acetic anhydride and sulfuric acid, dissolving cellulistic materials and providing better visibility for palynomorphs.

Some steps of the chemical treatments require special care for safety reason, in particular the use of HF which diffuses very fast through the skin and, causes severe chemical burns, and can be fatal.[12]

Other treatment include kerosene flotation for chitinous materials.


Once samples have been prepared chemically, they are mounted on microscope slides using silicon oil, glycerol or glycerol-jelly and examined using light microscopy or mounted on a stub for scanning electron microscopy.

Researchers will often study either modern samples from a number of unique sites within a given area, or samples from a single site with a record through time, such as samples obtained from peat or lake sediments. More recent studies have used the modern analog technique in which paleo-samples are compared to modern samples for which the parent vegetation is known[13]

When the slides are observed under a microscope, the researcher counts the number of grains of each pollen taxon. This record is next used to produce a pollen diagram. These data can be used to detect anthropogenic effects, such as logging,[14] traditional patterns of land use[15] or long term changes in regional climate[16]

Palynology can be applied to problems in many fields including geology, botany, paleontology, archaeology, pedology (soil study), and physical geography.


Palynology is used for a diverse range of applications, related to many scientific disciplines:

Because the distribution of acritarchs, chitinozoans, dinoflagellate cysts, pollen and spores provides evidence of stratigraphical correlation through biostratigraphy and palaeoenvironmental reconstruction, one common and lucrative application of palynology is in oil and gas exploration.

Palynology also allows scientists to infer the climatic conditions from the vegetation present in an area thousands or millions of years ago. This is a fundamental part of research into climate change.

See also


  • Moore, P.D., et al. (1991), Pollen Analysis (Second Edition). Blackwell Scientific Publications. ISBN 0-632-02176-4
  • Traverse, A. (1988), Paleopalynology. Unwin Hyman ISBN 0-04-561001-0
  • Roberts, N. (1998), The Holocene an environmental history, Blackwell Publishing. ISBN 0-631-18638-7

External links

  • International Federation of Palynological Societies
  • Palynology Laboratory, French Institute of Pondicherry, India
  • The Palynology Unit, Kew Gardens, UK
  • PalDat, palynological database hosted by the University of Vienna, Austria
  • The Micropalaeontological Society
  • The American Association of Stratigraphic Palynologists (AASP)
  • Commission Internationale de Microflore du Paléozoique (CIMP), international commission for Palaeozoic palynology.
  • Linnean Society Palynology Specialist Group (LSPSG)
  • Canadian Association of Palynologists
  • Pollen and Spore Identification Literature
  • Palynologische Kring, The Netherlands and Belgium
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