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Notes: Widespread bleaching (chlorosis) of patches of the dominant desert moss Syntrichia caninervis was observed across the northern Mojave Desert in the winter of 2002–03 following an extended period of drought interrupted by small rain events. These rain events were more frequent during the warmer months just prior to the appearance of chlorosis. We hypothesized that the patches were experiencing physiological stress due to partial hydration/rapid dehydration cycling during the warmer months. Compared to unbleached (green) shoots, chlorotic shoots exhibited significantly reduced photochemical performance, photosynthetic pigments, regenerational potential, sex expression, and lower rates of growth and productivity. However, age-specific analyses revealed older leaves from chlorotic shoots did not show the typical decline in vigour, suggesting that stress may primarily affect younger tissues. It is concluded that this chlorosis phenomenon is indicative of physiological stress presently occurring in the Mojave Desert, and is likely due to exposure to a higher than normal frequency of light rain events (〈 3.5 mm), which serve to partially hydrate moss patches that then rapidly desiccate.

Notes: Soils from seven sites on the island of Jamaica were assayed for the symbiotic diazotrophs Frankia and Rhizobium using serial dilutions. Most probable number and least squares regression methods were used to estimate each soil's capacity to nodulate native Myrica cerifera, exotic Leucaena leucocephala and exotic Casuarina cunninghamiana. The sample sites included a montane forest, a slash-and-burn agricultural site, reclaimed bauxite mining areas, abandoned sugar cane fields, and a garden plot. None of the host plants used in the bioassay were present on the sites sampled except for scattered L. leucocephala on one site. Frankia capable of nodulating M. cerifera, which is native to Jamaican highlands, occurred at all sites sampled. No C. cunninghamiana-infective Frankia was detected in soils sampled. Only soils from one site on the tropical coastal plain harbored rhizobia able to nodulate L. leucocephala (37 nodulation units cm−3 of soil). A subset of nodulated M. cerifera and L. leucocephala reduced acetylene to ethylene indicating nitrogenase activity. The slash-and-burn agricultural site, which was situated at an elevation of 200 m and possessed both high natural fertility and high soil moisture-supplying capacity, had significantly greater Myrica infectious capacity (1 000 nodulation units cm−3 of soil) than the other sites (7−207 nodulation units cm−3 of soil). A planned, paired comparison revealed that a recently cultivated sugar cane field and a recently reclaimed bauxite mining site together had significantly less Myrica-infective Frankia (4 nodulation units cm−3 of soil) than a corresponding pair of sites consisting of a sugar cane field abandoned for 25 years and a bauxite mining site reclaimed 20 years before sampling (118 nodulation units cm−3 of soil). Results indicate that Myrica-infective Frankia is widespread in Jamaica, that the number of Myrica-infective Frankia units vary from site to site in accordance with soil type and soil history, that Jamaican sites sampled lack soil Frankia populations capable of nodulating a casuarina host, that rhizobial symbionts capable of nodulating L. leucocephala may be geographically restricted to lowlands in Jamaica, and that the occurrence of Frankia in these soils is independent of host plant presence.