Phosphorus transformations along a soil/vegetation series of fire-prone, dolomitic, semi-arid shrublands of southern Spain Soil P and Mediterranean shrubland dynamic

Models of P transformations duringpedogenesis and with succession have developed fromstudies in temperate humid regions with neutral toacidic soils. Little is known about P biogeochemistryand P availability in semi-arid Mediterranean-typeshrublands with alkaline soils. We studied Ptransformations in a series of semi-arid, dolomiticshrublands in southeastern Spain, ranging from afrequently-burned, open gorse-scrubland on erodedTypic Xerorthents to a long-unburned, mature garrigueon Entic Haploxerolls. In contrast to the commonpattern of decreasing total P concentrations in thesoil profile with soil development due to leaching,total P increased markedly in this system. This is dueto concentration increases of relatively insolubleelements (P, Al, Fe, Ti) as karstification of parentmaterial (dolomitic marbles with up to 94% Ca-Mgcarbonate) during pedogenesis released bicarbonateand, subsequently, Ca and Mg leached from the profileat a higher rate. The total element to Ti ratiosindicated that the relative ion weathering losssequence, from easily weathered to resistant ions, wasCa>Mg > > > Fe>=Al>Ti, showing that P islost from these shrublands at an intermediate rate. Inone extreme of the series (the open gorse-scrubland),most soil P was Ca bound and organic P concentrations,organic matter content and phosphatase activity werevery low, as predicted by the model of Walker andSyers for the initial stages of soil development.However, this site showed the highest inorganic soilsolution P concentration, low soil P fixation capacityand the lowest foliar N:P ratios. Soils from theintermediate stages of the series showed the highestlabile inorganic and labile organic P concentrations.At the other extreme of the series (the maturegarrigue), a high proportion of soil P was in occludedinorganic and organic forms as predicted by the Walkerand Syers'; model. However, Ca bound P still accountedfor the largest single P fraction. Soils showed veryhigh sorption capacity (and high extractable Fe and Alconcentrations) and released very little P tosolution. Increasing values for NaOH extractable Po,organic matter and phosphatase activity indicate thatcycling of P through organic matter is increasinglyimportant with ecosystem development through theseries.     

Expression and activity of 3-hydroxy-3-methylglutaryl-CoA synthase and reductase in the fat body of ovariectomized and allatectomized Blattella germanica

Abstract. . 3-Hydroxy-3-methylglutaryl-CoA (HMG-CoA) synthase and HMG-CoA reductase show coordinated regulation in the fat body of Blattella germanica females. Since the profile of activity is parallel to the cycle of vitellogenin production, we postulated a link between the mevalonate pathway and vitellogenesis. Here we have studied both enzymes in females of B.germanica modified by ovariectomy (which leads to a saturable accumulation of vitellogenin) and allatectomy (which supresses vitellogenesis). Protein levels and enzymatic activity for both enzymes in ovariectomized specimens rose early in the first days of imaginal life and remained high until the end of the period studied, whereas controls showed cyclic profiles. In allatectomized specimens the same parameters were measured on day 4 of adult life and values were much lower with respect to controls. The parallelism between the patterns of HMG-CoA synthase and reductase, and that of vitellogenin, suggests a functional relationship between the mevalonate pathway and the glycosylation of vitellogenin through dolichol intermediates.