370 likes | 627 Views
Quaternary Environments Pollen Analysis. Pollen Analysis. Millions of tons of organic material is dispersed into the atmosphere by flowering plants and cryptogams every year Sedimentation rate is important for fine resolution. Basis of Pollen Analysis. Distinct morphology of pollen grains
E N D
Pollen Analysis • Millions of tons of organic material is dispersed into the atmosphere by flowering plants and cryptogams every year • Sedimentation rate is important for fine resolution
Basis of Pollen Analysis • Distinct morphology of pollen grains • Produced in vast quantities by wind-pollinated plants • Extremely resistant to decay • Reflect natural vegetation
Pollen • 10 – 150 microns • Exine – Chemically resistant outer layer • Morphology • Shape • Size • Sculpturing • Number of apertures
Treatment • Hydrochloric Acid • Sulfuric Acid • Hydrofluoric Acid • Acetic Anhydride • Pollen Solution • Lycopodium Control
Catchment • Preservation sites • Lakes • Bogs • Estuaries • Alluvial deposits • Marine sediments • Glacial ice • Archaeological sites • Packrat middens • Coprolites
Scale • Basin size determines catchment area • Based on dispersal distance • Based on pollen productivity • Different spatial and temporal scales of pollen change are driven by different processes
Other Factors that Affect Pollen Dispersal • Fire • Insect infestation • Plant successional changes • Season of pollination • Interference by humans
Problems • Differential production • Wind versus insect or animal pollinated • Differential preservation • Populus pollen disintegrates easily • Number of pollen grains to count • Greater than 200 • Bioturbation
Biostratigraphic Zones • Biostratigraphic Zone: "A biostratigraphic zone is defined solely by the fossils it contains, without reference to lithology, inferred environment, or concepts of time." Code of Stratigraphic Nomenclature. Bull.Amer.Assoc.Petrol.Geol. 45(5):645-665.
Vegetation versus Modern Pollen Hickory Oak Ash Elm
Callibration • Compare pollen assemblages to known temperature and precipitation • Develop transfer functions to reconstruct past climate
Altitudinal Changes in vegetation zones in the Eastern Cordillera of Columbia