User Tools

Site Tools


spores_pollen

Differences

This shows you the differences between two versions of the page.

Link to this comparison view

Next revision
Previous revision
spores_pollen [20/03/2023 13:00] – created mike_gssspores_pollen [05/05/2023 15:18] (current) mike_gss
Line 6: Line 6:
  
 //Assorted spores and pollen.// //Assorted spores and pollen.//
 +
 +{{:spores_pollen02.jpg?nolink|}}
  
 **Spores** **Spores**
Line 18: Line 20:
   * geologic range: Late Devonian – Recent (for Gymnosperm pollen); Cretaceous – Recent (for Angiosperm pollen)   * geologic range: Late Devonian – Recent (for Gymnosperm pollen); Cretaceous – Recent (for Angiosperm pollen)
  
 +Spores and pollen grains, because of their extremely small size and weight, have the potential to be transported by wind and water over very large distances (as intended!). It is not uncommon to find terrestrial pollen grains in samples from deep-water, offshore sediments. Whilst clearly not originally from that environment, their presence can still aid in age-determination and also in paleoclimate and environmental evaluations as they can indicate conditions in the hinterland at the time of deposition.
spores_pollen.1679317232.txt.gz · Last modified: 20/03/2023 13:00 by mike_gss

Donate Powered by PHP Valid HTML5 Valid CSS Driven by DokuWiki