Temporal Scaling of Age-Dependent Mortality: Dynamics of Aging in Caenorhabditis elegans Is Easy to Speed Up or Slow Down, but Its Overall Trajectory Is Stable.

The dynamics of aging is often described by survival curves that show the proportion of individuals surviving to a given age. The shape of the survival curve reflects the dependence of mortality on age, and it varies greatly for different organisms. In a recently published paper, Stroustrup and coauthors ((2016) Nature, 530, 103-107) showed that many factors affecting the lifespan of Caenorhabditis elegans do not change the shape of the survival curve, but only stretch or compress it in time. Apparently, this means that aging is a programmed process whose trajectory is difficult to change, although it is possible to speed it up or slow it down. More research is needed to clarify whether the "rule of temporal scaling" is applicable to other organisms. A good indicator of temporal scaling is the coefficient of lifespan variation: similar values of this coefficient for two samples indicate similar shape of the survival curves. Preliminary results of experiments on adaptation of Drosophila melanogaster to unfavorable food show that temporal scalability of survival curves is sometimes present in more complex organisms, although this is not a universal rule. Both evolutionary and environmental changes sometimes affect only the average lifespan without changing the coefficient of variation (in this case, temporal scaling is present), but often both parameters (i.e. both scale and shape of the survival curve) change simultaneously. In addition to the relative stability of the coefficient of variation, another possible argument in favor of genetic determination of the aging process is relatively low variability of the time of death, which is sometimes of the same order of magnitude as the variability of timing of other ontogenetic events, such as the onset of sexual maturation.

Adaptation of Drosophila melanogaster to Unfavorable Growth Medium Affects Lifespan and Age-Related Fecundity.

Experimental adaptation of Drosophila melanogaster to nutrient-deficient starch-based (S) medium resulted in lifespan shortening, increased early-life fecundity, accelerated reproductive aging, and sexually dimorphic survival curves. The direction of all these evolutionary changes coincide with the direction of phenotypic plasticity observed in non-adapted flies cultured on S medium. High adult mortality rate caused by unfavorable growth medium apparently was the main factor of selection during the evolutionary experiment. The results are partially compatible with Williams' hypothesis, which states that increased mortality rate should result in relaxed selection against mutations that decrease fitness late in life, and thus promote the evolution of shorter lifespan and earlier reproduction. However, our results do not confirm Williams' prediction that the sex with higher mortality rate should undergo more rapid aging: lifespan shortening by S medium is more pronounced in naïve males than females, but it was female lifespan that decreased more in the course of adaptation. These data, as well as the results of testing of F1 hybrids between adapted and control lineages, are compatible with the idea that the genetic basis of longevity is different in the two sexes, and that evolutionary response to increased mortality rate depends on the degree to which the mortality is selective. Selective mortality can result in the development of longer (rather than shorter) lifespan in the course of evolution. The results also imply that antagonistic pleiotropy of alleles, which increase early-life fecundity at the cost of accelerated aging, played an important role in the evolutionary changes of females in the experimental lineage, while accumulation of deleterious mutations with late-life effects due to drift was more important in the evolution of male traits.

[Maternal effect obscures adaptation to adverse environments and hinders divergence in Drosophila melanogaster].

Adaptation to contrasting environments can facilitate ecological divergence and sympatric speciation. Factors that influence the probability and tempo of these processes are poorly known. We performed an evolutionary experiment on Drosophila melanogaster in order to attain better understanding of adaptation dynamics and to model the initial steps of sympatric speciation. In our experiment, several populations are being cultured either on standard rich medium (RM) or on nutrient-deficient starch-based medium (SM). After 10 generations, experimental populations demonstrated unexpected changes in their fitness: on the starch medium, flies grown on RM (FRM) outcompeted those that were cultured on SM (FSM), while on the rich medium, FRM were outcompeted by FSM. That is, experimental populations demonstrated higher fitness on the foreign medium, but were outcompeted by the aliens on the one they had been accustomed to. To explain the paradox, we hypothesize that the observed low fitness of FSM on SM was due to maternal effect, or the "effect of starving mother". The FSM flies are probably better adapted to SM, but the phenotypic outcome of their adaptations is obscured because the females grown on the poor medium invest less in their offspring (for instance, they may produce nutrient-deficient eggs). Larvae hatched from such eggs develop successfully on the rich medium RM, but experience delayed growth and/or lower survival rate on the nutrient-deficient medium SM. To test the hypothesis, we measured the fitness of the flies FSM after culturing them for one generation on RM, in order to remove the assumed maternal effect. As expected, this time FSM demonstrated higher fitness on SM compared to control flies (FRM) and to FSM before the removal of the maternal effect. The results support the idea that non-adaptive phenotypic plasticity and maternal effects can mask adaptation to adverse environments and prohibit ecological divergence and speciation by allowing the migrants from favourable habitats to outcompete resident individuals in adverse ecotopes despite the possible presence of specific adaptations in the latter.

[Northward shift in faunal diversity is a general pattern of evolution of the phanerozoic marine biota].

The analysis of two global databases on spatio-temporal distribution of fossil marine animal genera (Sepkoski's compendium and The Paleobiology Database) has revealed the presence of the latitudinal diversity gradient (LDG) in the marine realm throughout the Phanerozoic. Within each time interval, LDG is characterized by two parameters: the latitudinal position of peak diversity and the steepness of monotonous decline of diversity with increasing distance from the zone of the highest diversity. During the Phanerozoic, peak diversity has drifted gradually from the tropics and subtropics of the Southern hemisphere into northern midlatitudes. The shift in peak diversity is not likely to be an artifact of incompleteness of the fossil record or uneven sampling of different regions. The shift proceeded in a stepwise manner, with periods of relatively fast changes separated by longer periods of little or no change. The latitudinal shift in peak diversity was probably due to a combination of several causes: tectonic (northward shift in the latitudinal distribution of continental shelf area), climatic (as demonstrated by the fact that peak diversity tended to occur near equator during the cold epochs and in midlatitudes during the warm epochs), and historical ("evolutionary inertia" of local faunas).

[Interaction of clay minerals with microorganisms: a review of experimental data].

A review of publications containing results of experiments on the interaction of microorganisms with clay minerals is presented. Bacteria are shown to be involved in all processes related to the transformation of clay minerals: formation of clays from metamorphic and sedimentary rocks, formation of clays from solutions, reversible transitions of different types of clay minerals, and consolidation of clay minerals into sedimentary rocks. Integration of these results allows to conclude that bacteria reproduced all possible abiotic reactions associated with the clay minerals, these reactions proceed much faster with the bacteria being involved. Thus, bacteria act as a living catalyst in the geochemical cycle of clay minerals. The ecological role of bacteria can be considered as a repetition of a chemical process of the abiotic world, but with the use of organic catalytic innovation.