Palynology is the science that studies contemporary and fossil palynomorphs , including pollen, spores, dinoflagellate cysts, acritarchs, chitinozoans and scolecodonts , together with particulate organic matter (POM) and kerogen found in sedimentary rocks and sediments.

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, and 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).

Palynology is an interdisiplinary 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 Palaeontology and micropalaeontology which studies fossil palynomorphs from the Holocene to Precambrian.

Contents

1 Methods of study 2 Applications 3 References 4 External links

Methods of study

Palynomorphs (usually between 5 and 500 micrometres in size) are extracted from rocks and sediments physically, by wet sieving, often after ultrasonic treatment, and chemically, by using chemical digestion to remove the non-organic fraction (e.g. using hydrochloric acid (HCl) is used to digest carbonate minerals, and hydrofluoric acid (HF) is used to digest silicate minerals in suitable fume cupboards in specialist laboratories).

Samples are then mounted on microscope slides and examined using light microscopy or scanning electron microscopy.

Palynology uses many techniques from other related fields such as geology, botany, paleontology, archaeology, pedology, and geography.

Applications

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

• Biostratigraphy and geochronology. Geologists use palynological studies in biostratigraphy to correlate strata and determine the relative age of a given bed, horizon, formation or stratigraphical sequence.
• Palaeoecology and climate change. Palynology can be used to reconstruct past vegetation (land plants) and marine and freshwater phytoplankton communities, and so infer past environmental (palaeoenvironmental ) and palaeoclimatic conditions.
• Organic palynofacies studies, which examine the preservation of the particulate organic matter and palynomorphs provides information on the depositional environment of sediments and depositional palaeoenvironments of sedimentary rocks.
• Geothermal alteration studies examine the colour of palynomorphs extracted from rocks to give the thermal alteration and maturation of sedimentary sequences, which provides estimates of maximum palaeotemperatures .
• Limnology studies. Freshwater palynomorphs and animal and plant fragments, including the prasinophytes and desmids (green algae) can be used to study past lake levels and long term climate change.
• Taxonomy and evolutionary studies.
• Forensic palynology- the study of pollen and other palynomorphs for evidence at a crime scene.
• Allergy studies. Studies of the geographic distribution and seasonal production of pollen, can help sufferers of allergies such as hay fever.
• Melissopalynology - the study of pollen and spores found in honey.

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.

References

• Moore, P.D., et al. (1991), Pollen Analysis (Second Edition). Blackwell Scientific Publications. ISBN 0632021764
• Thanikaimoni, G., 1980 ("1978"). Complexities of aperture, columella and tectum. Proc. IVth Intern. Palynol. Conf., I: 228-239.
• Thanikaimoni, G., (1984). Omniaperturate Euphorbiaceae pollen with striate spines. Bull. Jard. Bot. Nat. Belge, 54: 305-325.
• Thanikaimoni, K., et al. (1999). Eighth bibliographic index to the pollen morphology of angiosperms (EN). Huitieme index Bibliographique sur la Morphologie Des Pollens d'Angiospermes (FR). 346p. Paper. Institut Francais de Pondichery ISSN 0971-3107
• Traverse, A. (1988), Paleopalynology. Unwin Hyman ISBN 0045610010

External links

• International Federation of Palynological Societies
• American Association of Stratigraphic Palynologists, Inc. (AASP)
• Centre for Palynology, University of Sheffield, UK
• 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.
• CIMP Subcommission on Acritarchs
• CIMP Chitinozoan Subcommission
• Linnean Society Palynology Specialist Group (LSPSG)
• Canadian Association of Palynologists
• Pollen and Spore Identification Literature