Methods:

The flowering vegetation produces pollen (fig.1). This pollen dust is dispersed over long distances by wind, insects, birds etc.
The inner core of the pollen grain is protected by a durable outer shell made up of sporopollenin. Sporopollenin is an extremely resilient substance, which resists a large number of chemical processes. In this way, under the right conditions (mainly anaerobic milieu), pollen grains can be preserved over thousands of years.

To be able to carry out palynological work, first a suitable location for sampling has to be found. In general, the pollen's richest and best records can be gathered from peat or lake deposits. In this kind of environment an anaerobic milieu prevails. This prevents bacterial growth and subsequent feeding, as well as oxidation, which both would destroy the pollen grains (fig.2).

Normally a 'peat sampler' is used to extract the sediment sequences that are usually of a few meters in length. Afterwards, the sediment cores are sampled for pollen analyses. In most cases an amount of only 0.3 cm³ sediment is enough material (fig.3).
Before the analysis can start, however, the sediment samples have to undergo chemical treatment, during which most 'non-pollen' material is dissolved.
Pollen grains have a size from only a few microns (µm) to about 100 µm (= 0.1 mm), which means that they cannot be detected with the naked eye, but can only be examined under the microscope (fig.4).
Different plant taxa produce pollen grains of different shapes. Using these morphological characteristics, they can be identified in most cases to family level, sometimes even to species level.
In this manner, the vegetation, that grew when the sediment was deposited, can be inferred.
From longer records the vegetation cover of a landscape and its changes over thousands of years can be reconstructed.

Although, it seemed impossible to retrieve pollen bearing material from the semiarid Syrian steppe, during the course of the current project, a number of pollen sequences could be extracted. These are currently analysed in the J. - W. Goethe University in Frankfurt/Main.

For more detailed information on pollen analyses refer for example to:
FAEGRI, K. UND IVERSEN, J.:- (1989) Textbook of Pollenanalysis. 4. edition.; Chichester (John Wiley & Sons).
MOORE, P.H., WEBB, J.A. & COLLINSON, M.E. (1991) Pollen Analysis; Oxford (Blackwell Scientific Publications).

 

 

 

Fig.1: Pollen grains are microscopically, small plants, that can be differentiated by their morphology.
Fig.2: The picture shows a core retrieval with a peat sampler at a swamp site in Syria.
Fig.3: After the core retrieval the sediment is sampled for pollen analysis.
Fig.4: After chemical treatment of the sediment sample, the finished pollen sample is analysed under the microscope.