Hypothesis--a chemical mechanism for the biosynthesis of ATP involving ion-exchange reactions

Dissociation constants for Mg . ATP were determined by displacing ATP from Dowex-1 resin with magnesium. These constants were then used to analyze the kinetics of yeast mitochondrial ATPase, in terms of the concentrations of free magnesium and free ATP, at a series of pH values. Both Mg . ATP and hydroxide ions were found to compete with the binding of ATP to the enzyme. These results were interpreted, in terms of an ion-exchange model, to mean that the synthesis of ATP may require the utilization of both magnesium and hydroxide ions for the dissociation of ATP from the enzyme as Mg . ATP. The concentrations of Mg and hydroxide required to compete with ATP were both found to be about three orders of magnitude greater than those required to form products, indicating that magnesium and hydroxide ions can contribute about 8 kcal of energy when ATP is synthesized.     

Nile water as a cause of Eastern Mediterranean sapropel formation: Evidence for and against

During the late Pleistocene, sapropels (layers of organic-carbon rich sediment) formed throughout the entire Eastern Mediterranean Basin in close association with glacial/interglacial transitions. The current theory for the mechanism of sapropel formation involves a density stratification of the water column, due to the invasion of a large quantity of low-saline water, which resulted in oxygen depletion of the bottom waters. Most workers believe that this low-salinity water was glacial meltwater that entered the Mediterranean via the Black Sea and a series of interconnected glacial lakes, but the suggestion also has been made that the freshwater originated from the Nile River. In this study the oxygen isotope values of planktonic foraminifera,Globigerinoides ruber, have been examined in six gravity cores and one piston core from the southern Levantine Basin, and compared with the oxygen isotope records ofG. ruber from other areas of the Eastern Mediterranean. This study deals mainly with the latest sapropel which was deposited approximately 7000 to 9000 years ago. Results indicate that Nile discharge probably does reduce salinities somewhat in the immediate area surrounding the mouth of the Nile, but this water is rapidly mixed with the highly saline waters of the easternmost Mediterranean.Using a mixing equation and surface water salinity limitations, an approximate oxygen isotope balance of surface waters was calculated for the time of latest sapropel deposition. This calculation shows that neither Nile River discharge nor Black Sea input (nor both together) are large enough to account for the large-scale oxygen isotope depletion associated with latest sapropel deposition in the Eastern Mediterranean. This suggests that part of the isotopic change at Termination I is probably due to increased surface water salinities during the last glacial maximum. In addition, evidence from the timing of sapropel 1 deposition and the dissolved oxygen balance indicates that deposition of the latest sapropel is associated with increased surface water production of biogenic material, as much as three times higher than that of present day.     

Variation in response to cytotoxicity of cigarette smoke.

The cytotoxic effect of cigarette smoke condensate on human polymorphs was investigated in vitro by the method of vital dye exclusion. Exposure to 1/800 of the smoke from one high-tar cigarette killed a detectable proportion of a population of 10(6) cells. The response among the cells from 40 healthy people varied widely, the percentage of dead cells ranging from 3% to 66% and from 17% to 87% at exposure levels of 125 micrograms and 250 micrograms cigarette smoke condensate respectively. Differences in individuals'' responses were reproducible and unrelated to age or sex or smoking habit. The cells from 10 patients with irreversible obstructive airways disease and probable emphysema were significantly more sensitive than those from 10 patients with no respiratory disability matched for age and smoking habits. Genetically influenced variation in cellular response to cytotoxicity may be an important determinant of the risk of developing emphysema among smokers.     

Red cell enzyme polymorphisms in the Yoruba.

In this study are presented the results of an investigation of variation in 17 red cell enzyme systems in the Yoruba, a Negro population of western Nigeria. Nine of the systems were found not to be polymorphic. The other eight systems revealed a close resemblance to the Negroes of Southern Africa, and a marked contrast with the San ('Bushmen'). The Yoruba have a history of many centuries of urbanization, while the Southern African Negroes have only recently begun to inhabit large towns. It would appear not only that the polymorphisms investigated are irrelevant to adaptation to urban conditions, but also that no selective forces, and very little drift, has operated on them since the remote ancestral separation of the populations. These results also suggest that the Khoisan contribution to the Southern African Negro gene pool might not be as uniform or as considerable as might be supposed.     

Psychosocial modifiers of response to stress

The impact of stress upon an organism is far more complex than the simple design of most stress research implies. We offer an expanded model for studying the relation of stressors to pathological outcomes, which takes into account both the adaptive capacity of the organism before the stressor occurs and the defenses marshalled in response to the stressor. The model also distinguishes among the initial responses of alarm, sustained defensive behaviors, and the relatively irreversible endstates which remain after resistance has ended. Realizing that only a multidiscomplinary approach can begin to capture the wholeness of human experience, this research paradigm anticipates that stressors, adaptive capacities, defenses, alarm reactions, and pathologial end-states will take place at the biological, psychological, interpersonal and sociocultural levels simultaneously and successively. Data on life change stress and psychological health outcomes gathered as part of the Air Traffic Controller Health Change Study are analyzed to illustrate the use of the model in identifying psychosocial and biological modifiers of response to stress.     

The postcranial skeletons of the Triassic mammals Eozostrodon, Megazostrodon and Erythrotherium.

The purposes of this monograph are to describe the postcranial skeletons of the earliest known mammals, and to probe, in so far as possible by osteological study, biological questions concerning the habits and adaptations of these late Triassic forms. In this context, information on the background of this investigation is useful. Studies of Mesozoic mammals, begun some 150 years ago, are based on rare and fragmentary fossils, principally jaws and teeth. These investigations have yielded a bare outline of some 120 million years of mammalian evolution-about two-thirds of mammalian history. No assessment of the important biological changes occurring during this time can ever be complete, but major advances are possible as new discoveries provide material that is more complete or that represents a previously unknown evolutionary stage. So tenuous is the evidence that at least some concepts are re-evaluated with each discovery. Postcranial anatomy offers especially intriguing prospects for investigation because associated material (that can be positively assigned to a taxon below subclass) has been for the most part unknown, and indeed even dissociated bones are a rarity. Since G.G. Simpson's monographs of 1928 and 1929, progress in the study of Mesozoic mammals has been largely dependent on new finds. A major impetus to renewed investigation came from the discoveries of Mesozoic mammals by Walter Kühne in 1939 and during the immediate post-war years. Kühne first worked on fissures in the Carboniferous limestone quarries at Frome, Somerset, in southwest England where he collected a series of teeth of the problematical form Haramiya and two triconodont teeth which were placed in the genus Eozostrodon (Parrington 1941, 1946). The fissure faunas are generally thought to be of Upper Triassic (Rhaetic) age (Kühne 1946), although Kermack, Musset & Rigney (1973) believe that the evidence is insufficient to determine whether the deposits are Rhaetic or Lower Liassic. After the war Kühne carried his explorations farther west, eventually reaching the quarries at Bridgend in Glamorgan, Wales, where he not only found more triconodont teeth in some quantity (Kühne 1958) but also a symmetrodont tooth (Kühne 1950). Shortly after making these discoveries, Kühne returned to Germany and the work was continued by a team from University College, London, under the leadership of Dr K.A. Kermack.