Download - Non-marine paleoclimate records
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Non-marine paleoclimate records
Pollen Data
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Basis for Pollen Studies
• Pollen grains can directly identify plant species.
• Pollen is widely present and abundantly produced.
• Pollen grains are resistant to decay.
Alnus
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Pollen Studies
• Palynology is the study of pollen
• Pollen grains can be found in caves, lake sediments, soils, peat deposits, marine sediments, glacial deposits.
• Pollen data provides information of changes in vegetation, climate, and human disturbance of terrestrial ecosystems.
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Pollen Production
• Pollen production is inversely proportional to the probability of fertilization. – Authogamous plants < Entomophilous < Anemophilous
(self-fertilizing) (insect-fertilizing) (wind-dispersed)
• Pollen can be produced during different seasons by different plants.
• How representative are pollen grains of species distribution and abundance?
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Genus Pollen Production
Grain/flower
Rate of Fall (cm/sec)
Pinus >15 million 2
Picea 200,000 9
Abies 100 40
Poacea 90,000 10
Betula 10,000 1
Quercus 9,000 5
Fagus 15 8
Acer 8,000 4
Tilia 20,000 18
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Pollen Production
• Pollen production is species-specific. Whereas some plants can produce 70,000 grains per anther, others produce up to 100 grains per anther.
• The pollen record is biased towards wind-pollinated plants (all gymnosperms and most angiosperms) because these plants need to produce vast quantities of pollen.
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Pollen Production
• Anemophilous plants (wind-pollinated) produce light, aerodynamically shaped pollen.
• Pollen deposition depends on grain shape and weight, wind velocity, wind direction, canopy cover
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Pollen dispersal
• Travel distance is inversely proportional to pollen-grain size.
• Pollen grains are filtered as they move through the canopy.
• Some light pollen grains can be transported long-distances in the upper atmosphere.
• In general, pollen from low-standing plants have low probability of dispersal.
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Pollen dispersal
• Meteorological conditions control pollen dispersal.
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Pollen and vegetation
Ponds: local vegetation Lakes: regional vegetation
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Pollen percentages in surface samples from eastern Canada.
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Pollen and Vegetation
• Surface pollen composition is different than vegetation composition and abundance.
• Pollen composition at a given point within an ecosystem is fairly consistent.
• But, pollen compositions at different sites within the same ecosystem are slightly different.
• However, the difference between pollen composition among sites in different ecosystems is far greater than the difference between sites within a single ecosystem.
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Pollen Analysis
• Sediments are collected • Pollen grains are isolated
from the sediment matrix via chemical treatments.
• Isolated pollen grains are mounted onto a glass slide, and they are identified and quantified under a microscope.
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Pollen Analysis
• Pollen counts in each slide are reported in percentages of the total pollen count (excluding wetland or rare species).
• Changes in the % of one species are interpreted to reflect a similar change in the composition of vegetation.
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Pollen Analysis
• Problem: % of pollen counts could give unrealistic information of vegetation composition if, for instance, a plant species is replaced by an abundantly pollen-producing plant.
X-axis: % pollen grains
Y-a
xis:
Tim
e
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Pollen Analysis
• To circumvent biases associated with pollen production, one could use pollen flux density values (pollen grain/yr-cm2).
• However, accurate and numerous dates are needed. Because this is rare, pollen fluxes are not used very often.
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Pollen Interpretation
• Pollen diagrams are usually divided into zones to facilitate interpretations.
• Changes in pollen composition are interpreted to indicate changes in climate or human disturbance.
St. Paul, MN (Matsch, 1976).
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Pollen Interpretation
• Two general interpretative approaches exist:– Individualistic Approach: Past environmental
conditions are reconstructed on the basis of present-day ecology and environmental tolerance and optima of a plant species.
– Assemblage Approach: Past environmental conditions are reconstructed on the basis modern plant associations in climate/ biogeographical regions.
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Pollen Interpretation
• Individualistic approach (Midwest):
• Decline in hardwood species (beech, maple, oak, hickory) and/or increase in conifer species (spruce, fir, pine) indicates cooling.
• Increase in ash and/or elm indicates wet environments.
• Decline in trees and increase in grasses indicates drier conditions.
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Pollen record for Money Creek and Pine Creek in southeastern Minnesota(Baker et al., 2002).
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Pollen Interpretation
• Assemblage Approach:• Modern Analog Technique (MAT): Central
assumption: If two assemblages contain a similar mixture of pollen grains, then the communities that produced those assemblages must also have been similar.
• Another assumption: Plant composition in an ecosystem is at equilibrium with the environment.
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Pollen Interpretation
• MAT: relies on the dissimilarities of modern and fossil assemblages.
• To determine if they are the same, the threshold of relatedness is based on statistical comparisons between paired populations within and between ecosystems.
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Pollen Interpretation
• Hierarchical Analog Approach: Based on functional analogs rather than on plant associations.
• First level of analyses: similar to MAT
• Second level: based on plant functional types.
• Third level: based on plant life forms.
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Williams, 2003.
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Williams, 2003.
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