A few years ago, I attended a 1-day symposium on long distance transport at a national meeting in a country abroad. Towards the end of the day, as the participants became tired and no general agreement was in sight, one observer from an allied discipline remarked, "Why can't you translocation workers make any progress, you still discuss the same miserable old models that were proposed 40 The 19th century produced innumerable theories of sap ascent. The "climbing theory," which originated with Malpighi and was advocated as late as 1910 by LeClerc, visualized the water as moving up the xylem in steps and being held in place by the ridges of the vessels in a valvelike manner. Another obscure concept is that of the "Jamin's chains," chains of bubbles in vessels that were said to somehow propel the water up the stem into the leaves while in fact they were a mere artifact of preparation. There were many others. The main problem was the difficulty of seeing water in the conducting elements. Water in vessels is usually under tension, and when a preparation is made for observation, air is drawn into the vessels. This gave rise to the notion that vessels are not normally water filled, an opinion held by the well known plant physiologist, Sachs, and maintained by some workers until quite recently on the basis of sophisticated reasoning. Sachs also maintained that diffusion is the mechanism by which photosynthetic products are distributed throughout the plant. Because of his great influence, Sachs' effect upon translocation research was rather negative, although he was undoubtedly an outstanding scientist in other respects.The turn of the century brought significant progress. It was recognized that the ascent of sap in the xylem is a physical phenomenon and does not depend on living cells (42), although this concept was challenged repeatedly until relatively recent times. A significant discovery was the observation that twigs (4) and models involving evaporation of water from clay cups (1,14) could raise water above barometric height. These experiments gradually gave rise to Dixon's cohesion theory (11). Dixon was a sort of radical among many respected scholars who still maintained a variety of "vital" theories, including the idea that root pressure provides the necessary force to push water into the top of trees. However, evidence in support of the cohesion theory accumulated gradually. Friedrich (18), who in 1897 invented the dendrograph to record tree growth, found diurnal shrinkage of trees which obviously was not a result of growth but of a fluctuating water content of the stem. This was later followed up in more detail by MacDougal et al. (30).Renner was able to demonstrate tensile water in fern sporangia (37) and Dixon made the first attempt to measure tensions in plants directly (1 1).During the first quarter of the 20th century little progress was made in phloem-transport research. It is very likely that interest which had been so keen during the second part of the preceding century turned to other problems. Plant...