The degrading processes can, under special conditions, slow to a minimum. Environments which are waterlogged, such as lakes, seas, clay soils, and where the water-table is high, often become near-anaerobic and the activity of aggressive wood-decomposing microorganisms decreases dramatically. This is why, under these conditions, we can still find wooden objects which give us new information about the past. If we look 30 years back in time, we see that wood conservators and scientists concentrated for a long period on the hypothesis that the decomposition of waterlogged wooden material was of a chemical nature with hydrolytic reactions. It was in 1988, at the American Chemical Society congress in Los Angeles, that wood biologists first established that the degradation of waterlogged archaeological wood was caused mainly by microorganisms. In 1983, Holt and Nilsson made the first detailed description of wood attack by a bacterium [1]. By using a combination of light microscopy and transmission electron microscopy (TEM) it was possible to investigate and verify a new group of wood-decaying organisms, the tunnelling bacteria [2]. In the years which followed, two other wood-decaying bacteria were found: the cavitation bacteria and the erosion bacteria [3]. The use of new techniques like TEM and scanning electron microscopy (SEM), where the magnification is extremely high, was essential for these new discoveries. Since 1988 a number of archaeological wooden objects have been investigated under the microscope, and microbial attack has been observed in most cases. In dry wood, for example from the Pyramids, attack has mainly been due to fungi [4]. In waterlogged material, soft rot, tunnelling and erosion bacteria dominate [4-8]. The environmental history of wooden objects can be inferred from the results of microscopic observations. Basidiomycete fungi, like white rot and brown rot, require relatively high levels of oxygen for their wood-decaying activities, while soft rot, belonging to the group of ascomycetes and fungi imperfecti, can be active at lower concentrations. Some bacteria require only minimal amounts of oxygen. 'Bulverket' was a peculiar construction in the lake of Tingstdide Trask, Gotland, Sweden, from the early mediaeval period. Houses of wood were built on a construction of poles. Finds of dark-coloured poles led archaeologists to believe that the whole construction had been burned. However, microscopic examination showed that the dark colour was due to attack by soft rot fungi. It was also demonstrated that the house building material showed terrestrial decay forms associated with white and brown rot. Therefore the likely cause of destruction was rot and not fire. The foremast from the ship Vasa was broken, presumably during the wreck, and microscopic examination of wood samples taken next to the fracture revealed a special type of white rot. This white rot fungus grows in living trees and does not occur in aquatic environments. Therefore the wood used for the mast must have come from a tree attacked by white rot when being felled. The use of inferior wood indicates either that the shipwrights were poorly qualified, or that the building project was running out of time or money. In the current project, a great number of wood samples will be studied by light and electron microscopy and the microbial results will be related to environment, age and wood species to see if there is some relationship between the rate and type of decay. A large number of stratified wood fragments were obtained from different archaeological sites in Sweden through the cooperation of field archaeologists. The wood samples were from terrestrial and aquatic sites, including bogs, lake, sea, clay, sand and 'mediaeval deposits'. The age of the samples varies from 7000 BC to AD 1676 and different wood species are represented (mostly pine and oak). The wood samples were sectioned by hand with a razor blade, and stained with safranin or methylene blue in lactic acid. The sections were studied using polarized light. The use of light microscopy made it possible to identify different forms of attack (bacterial or fungal) and to assess the severity of attack. Earlier results [5-8] and preliminary results from this study show that erosion bacteria are responsible for most of the decay in waterlogged archaeological wood. A knowledge of the role of microbial decay in archaeological wood and the different forms of decay must be fundamental for the choice of conservation method.