The Role of Maturation Drying in the Transition from Seed Development to Germination: I. ACQUISITION OF DESICCATION-TOLERANCE AND GERMINABILITY DURING DEVELOPMENT OF Ricinus communis L. SEEDS

Kermode, A. R. and Bewley, J. D. 1985. The role of maturationdrying in the transition from seed development to germination.1. Acquisition of desiccation–tolerance and germinabilityduring development of Ricinus communis L. seeds.—J. exp.Bot. 36: 1906–1915. Seeds of Ricinus communis L. cv. Hale(castor bean) undergo a transition from desiccation–intoleranceto desiccation–tolerance approximately midway throughtheir development. Tolerance of slow desiccation is gained overonly a few days of development (between 20 and 25 d) and isachieved well before the completion of major developmental events,such as reserve deposition and the onset of normal maturationdrying. A tolerance of very rapid water loss brought about bydrying over silica gel is not acquired by this seed until nearmaturity. Coincident with the acquisition of tolerance to slowdesiccation the seeds gain the capacity to germinate upon subsequentrehydration. Germinability and capacity for normal post–germinativegrowth during the tolerant phase are not fully expressed unlessthe seed is dried at an optimal rate, which is dependent uponthe developmental stage of the seed. Drying presumably actsto terminate developmental processes and to initiate those metabolicprocesses necessary to prepare the seed for germination andgrowth. Key words: Desiccation-tolerance, germinability, seed development, castor bean     

Costs and benefits of cervical screening. III. Cost/benefit analysis of a call of previously unscreened women

A population‐based cervical screening programme issued invitations to women with no record of a previous smear. This call was very good value, at £5780 per life saved or £159 per life‐year saved at 1991 prices. The first priority for the cervical screening service should be comprehensive coverage.     

A long-term record of carbon exchange in a boreal black spruce forest: means, responses to interannual variability, and decadal trends

We present a decadal (1994–2004) record of carbon dioxide flux in a 160‐year‐old black spruce forest/veneer bog complex in central Manitoba, Canada. The ecosystem shifted from a source (+41 g C m⁻², 1995) to a sink (−21 g C m⁻², 2004) of CO₂ over the decade, with an average net carbon balance near zero. Annual mean temperatures increased 1–2° during the period, consistent with the decadal trend across the North American boreal biome. We found that ecosystem carbon exchange responded strongly to air temperature, moisture status, potential evapotranspiration, and summertime solar radiation. The seasonal cycle of ecosystem respiration significantly lagged that of photosynthesis, limited by the rate of soil thaw and the slow drainage of the soil column. Factors acting over long time scales, especially water table depth, strongly influenced the carbon budget on annual time scales. Net uptake was enhanced and respiration inhibited by multiple years of rainfall in excess of evaporative demand. Contrary to expectations, we observed no correlation between longer growing seasons and net uptake, possibly because of offsetting increases in ecosystem respiration. The results indicate that the interactions between soil thaw and water table depth provide critical controls on carbon exchange in boreal forests underlain by peat, on seasonal to decadal time scales, and these factors must be simulated in terrestrial biosphere models to predict response of these regions to future climate.     

Intercellular communication in Chara: factors affecting transnodal electrical resistance and solute fluxes

The permeability of plasmodesmata in the nodal complex of branch cells of Chara corallina was examined by measuring both the transnodal electrical resistance and transnodal fluxes of ³⁶CI and ¹⁴C-buty-rate. Under normal circumstances, the resistance across the node was low, but increased rapidly in response to metabolic inhibition, pressure gradients across the node or excision of one of the cells. For each of these treatments, there was a substantial reduction in solute transport between the cells. Acidification of the cytoplasm by weak acids or alkalinization by amines did not affect either the electrical resistance or the flux of solutes through the node between whorl cells. The transnodal resistance was significantly higher in older cell pairs, but was unaffected by large transnodal voltage differences or by the passage of action potentials. There was no evidence that short-term increases in cytoplasmic calcium have any effect on plasmodesmatal permeability.     

Phosphatized soft-bodied squids from the Jurassic Oxford Clay

A diagenetic case study of phosphatized soft-bodied squids from the lower part of the Oxford Clay of Christian Malford, Wiltshire, has dated mineralization in relation to burial history. Complete squids with mantle tissues were examined under the SEM as uncoated specimens at low KV. A simple stage attachment designed for this purpose is described. Soft-parts are preserved in three dimensions and must therefore have been mineralized prior to decay-induced tissue collapse. Such mineralization occurred near to the anoxic/oxic boundary in the 'soupy' upper layer of organic-rich sediment. In acrobic conditions, phosphates were liberated to pore-water solution from decomposing organic matter and became adsorbed to ferric hydroxides within sediment. The reduction of these ferric hydroxides at the anoxic-oxic interface liberated phosphates to solutions which were conccntrated in the decomposing carcasses of the squids. This mineral concentration was favoured by the development of a high pH reducing environment around the carcass and possibly by complexing with protcolipids liberated by decomposition of animal matter. ▭ Soft-part preservation, phosphatization, SEM techniques, cephatopod. Oxford Clay, Wiltshire, England.