[Amino acid and lipid metabolism in embryos of flesh fowl with different yolk mass].

It has been proposed that variations in relative yolk mass in a population of flesh fowl be used as a model of development of nidicolous and nidifugous birds. During development of the eggs with a high proportion of yolk, an excess of lipids is cleaved at a higher rate and oxidized until day 17 of incubation, while in the embryos developing from the eggs with a low relative yolk mass, amino acids are intensely cleaved during the period preceding the hatching. Significant differences in the body content of cystine were found in 17-day embryos and upon hatching, thus suggesting a delayed activity of the genes encoding keratins in the group corresponding to the seminidicolous type according to the egg content of lipids. These biochemical differences question the widespread concept on the occurrence of dichotomy by the end of embryogenesis and beginning of neonatal growth of nidifugous and nidicolous birds.

[Altricial and precocial developmental features in modern meat-type chicks].

Variability of egg weight, egg yolk content, neonatal growth rate and relationships of these parameters were studied in meat-type chicks. As it had been established the level of variability in neonatal growth traits was greater than variability of the egg morphology parameters. Egg weight had stronger influence on the chicks' neonatal growth rate than egg yolk content did. Low egg size was associated with limited neonatal growth rate variability, declined chick weight at hatching and increased relative growth rate throughout four days post hatch. Comparison of egg morphological parameters in two species having the same female definitive body weight--meat-type domestic fowl (precocial type) and brown pelican (altricial type) has shown, that, in contrary to predicted on the basis of avian developmental typology, egg weight to female body ratio was greater in brown pelican, egg yolk content was equal in both species.

[Eggs fertilizability in domestic hens Gallus gallus domesticus as a function of the yolk surface area]. / Zavisimost' oplodotvoriaemosti iaitz domashnikh kur Gallus gallus domesticus ot ploshchadi poverkhnosti zheltka.

The increase of egg mass and reliable decrease of egg fertilizability were observed when the mass surface area of yolk (egg) increased. The results obtained suggest that, in addition to the number of viable spermatozoa penetrating across the perivitelline membrane within 15-20 min after ovulation, the probability of fertilization depends on the area of egg surface, which approximately corresponds to the area of perivitelline membrane. Apparently, the ratio of receptors' numbers and spermatozoa, which contact with them on the germ disc surface, to their number on the rest part of perivitelline membrane decreases with the increase of yolk size. The decreased egg fertilizability concomitant with the increased area of perivitelline membrane suggests that the egg size is one of the factors of fertility of the female gametes as concerns both variability of the egg composition and age.

Physical, chemical and biological processes in Lake Vostok and other Antarctic subglacial lakes.

Over 70 lakes have now been identified beneath the Antarctic ice sheet. Although water from none of the lakes has been sampled directly, analysis of lake ice frozen (accreted) to the underside of the ice sheet above Lake Vostok, the largest of these lakes, has allowed inferences to be made on lake water chemistry and has revealed small quantities of microbes. These findings suggest that Lake Vostok is an extreme, yet viable, environment for life. All subglacial lakes are subject to high pressure (approximately 350 atmospheres), low temperatures (about -3 degrees C) and permanent darkness. Any microbes present must therefore use chemical sources to power biological processes. Importantly, dissolved oxygen is available at least at the lake surface, from equilibration with air hydrates released from melting basal glacier ice. Microbes found in Lake Vostok's accreted ice are relatively modern, but the probability of ancient lake-floor sediments leads to a possibility of a very old biota at the base of subglacial lakes.