Applications of Pollen Data
Palynological Richness = Number of pollen taxa observed
Anthropogenic Indicators
- Hunter gatherers create small burning and some record
- Slash and burn agriculture is a clear impact, causing changes in natural fire regime and thus vegetation and pollen and charcoal records
- Decrease in Picea and Pinus pollen and increase in Populus, Betula, Epilobium and Pteridium are indicators in the pollen record.
- Increase in open and bare soil (Plantagor major pollen is often thought of as a human/agriculture footprint)
- These aren't definite human impact markers, but some things are almost certain human indicators like:
- Rye pollen (Secale cereale) (easy to identify from other pollen taxa)
- Cornflower (Centaurea cyanys) (also easy to identify)
- Plus a decrease in forest taxa, then you can be sure
- First pollen records in FInland from 4500 - 3000 cal yr BP
- Mostly barley (Hordeum)
- some finds of buckwheat (Fagopyrum) from 7200, 6200 cal yr BP which are debated and only from one site
- Reconstruction of vegetation openness
- Studied all non-tree species except sedges (Cyperaceae) pollen and measured changes over time
- Sedges are excluded since they grow abundantly in the bogs and fens where the samples came from
- Examples showing the land use history of Helsinki and the British Isles based on pollen samples
- Increase in population correlates with opnening of vegetation
Landscape Reconstruction Algorithm
- Model of percentage cover of vegetation
Patterns of modern pollen and plant richess in Europe
- While we might only find a fraction of pollen taxa preserved in the paleo data, the trends in diversity will reflect the diversity of plants seen generally
- Correlation between pollen richness and plant richness in Europe were confirmed, best with wind-pollinated taxa (especially trees), while grasses and herbs are less represented
Montane area bias
- In one study from a montane area in Spain, the pollen record showed more tree species thanactual observed vegetation - this is because the tree pollen travelled further
Rate of Change of vegetation during Late Glacial and Holocene
- This study can tell us which periods had the fastest change in vegetation - this lets us compare changing climate events and whicheffect of vegetation
Plant Functional Trait Composition in paleorecord
- Study from Estonia that looked at functional trait composition in woody and herbaceous taxa from a certain fen
- Can see trends such as increased height, seed number increase, seed leaf area increases since holocene
- This assumes that plant phenotype has not changed over this time (no evolution)
Sedimentary Ancient DNA (SedaDNA) and pollen data
- This can reveal more diverse taxa that aren't captured in the pollen record such as animals, mammals etc
- Can also give more precise identification of pollen, such as identifying to species rather than to family in the case of pollen (example from northern Norway)
- Study from Northern Finland showing terrestrial species richness from sedaDNA and from pollen record, where sedaDNA shows more diversity
- Sedimentary DNA also shows more species such as aquatic and bryophyte species which don't produce as much pollen