Plasma Inhibin Levels in Relation to Steroids and Gonadotrophins during Oestrous Cycle in Buffalo

The study was conducted on six Murrah buffalo synchronized and induced to oestrus. An indwelling catheter was placed in the jugular vein of each buffalo 4 days before the expected onset of the oestrus following the induced oestrus and blood samples were collected at 8 h intervals from each animal throughout the oestrous cycle. Plasma immunoreactive inhibin, follicle-stimulating hormone (FSH), luteinizing hormone (LH), estradiol-17β and progesterone were estimated by radioimmunoassay to study the variations in the peripheral levels of these hormones and their inter-relationships in order to elucidate the feedback systems controlling them during the oestrous cycle of buffalo. Plasma inhibin levels ranged between 391.25 and 631.97 pg/ml during various phases of the oestrous cycle and were found to be higher than reported in cows. Peak LH and FSH levels during oestrus were 38.40 ± 9.21 and 24.04 ± 4.75 ng/ml, respectively and estradiol-17β and progesterone were 19.50 ± 5.51 pg/ml and 0.61 ± 0.25 ng/ml, respectively. The mean plasma inhibin concentration on the day of oestrus was 562.5 ± 18.9 pg/ml. Levels of FSH in the plasma showed three mid-cycle elevations which corresponded to comparatively lower inhibin and elevated estradiol-17β levels during the same period. From this observation it was deduced that both inhibin and estradiol-17β have a feed-back regulatory effect on FSH secretion in buffalo.     

Implications of the VEGA Balloon Results for Venus Atmospheric Dynamics

Both VEGA balloons encountered vertical winds with typical velocities of 1 to 2 meters per second. These values are consistent with those estimated from mixing length theory of thermal convection. However, small-scale temperature fluctuations for each balloon were sometimes larger than predicted. The approximate 6.5-kelvin difference in temperature consistently seen between VEGA-1 and VEGA-2 is probably due to synoptic or planetary-scale nonaxisymmetric disturbances that propagate westward with respect to the planet. There is also evidence from Doppler data for the existence of solar-fixed nonaxisymmetric motions that may be thermal tides. Surface topography may influence atmospheric motions experienced by the VEGA-2 balloon.     

Subsurface radar sounding of the south polar layered deposits of Mars

The ice-rich south polar layered deposits of Mars were probed with the Mars Advanced Radar for Subsurface and Ionospheric Sounding on the Mars Express orbiter. The radar signals penetrate deep into the deposits (more than 3.7 kilometers). For most of the area, a reflection is detected at a time delay that is consistent with an interface between the deposits and the substrate. The reflected power from this interface indicates minimal attenuation of the signal, suggesting a composition of nearly pure water ice. Maps were generated of the topography of the basal interface and the thickness of the layered deposits. A set of buried depressions is seen within 300 kilometers of the pole. The thickness map shows an asymmetric distribution of the deposits and regions of anomalous thickness. The total volume is estimated to be 1.6 x 10(6) cubic kilometers, which is equivalent to a global water layer approximately 11 meters thick.     

Physical, chemical, and mineralogical characteristics of steppe paleosols of the ural region

Investigation of paleosols with different ages of burial mounds and the unique fortified city of Arkhaim in the steppe zone of the Southern Trans-Urals (Chelyabinsk region) is carried out. They are located on the remnants of the Big Karaganka River valley. The time of construction of archaeological monuments dates back to the Early Iron Age (Sarmatian Culture, 2300–2200 years ago) and Middle Bronze Age (Sintashta culture, 3800–4100 years ago). The soils are of medium and light loamy granulometric composition. Morphological, chemical, and mineralogical investigations of paleosols and background soils indicate that, in the Sarmatian time, the climatic conditions in the region were drier than currently, while during the Sintashta cultural development, the climate of the region was similar to the present one.     

Investigation of hematological indices of female rabbit blood with addition of an antioxidant preparation to the ration

Homeostasis constants of female rabbits of the Soviet Chinchilla breed aged from 2 to 6 months with addition of the antioxidant preparation Eurotiox Plus Dry to the ration were studied under normal ontogenetic conditions. Age-related changes in the cell composition of female rabbits of different age groups, including the quantitative composition and differential white blood cell count, are shown. The data obtained are analyzed in connection with ontogenetic characteristics of metabolism of the animals.     

RAPD marker evaluation of phylogenetic relationships in species of genus Beta L.

RAPD markers are used for establishing phylogenetic relationships between and within various beet species. On the basis of the electrophoretic profiles obtained, phylogenetic trees are constructed by the unweighted pair group with arithmetic mean (UPGMA) method and relationships between wild and cultivated beet accessions stored in the world collection at the Vavilov Plant Industry Research Institute (VIR)are determined.     

Assessment of soil erosion rate trends in two agricultural regions of European Russia for the last 60 years

Purpose

Forest–steppe and the southern forest ecotones of European Russia (ER) are the most productive agricultural areas in Russia. Both climate and land use changes have occurred within the ER during last 30 years. These changes can lead to changes in the timing, magnitude, and spatial distribution of soil erosion rates on cultivated lands. The objective of this research was to assess the trends in soil erosion rates since the 1960s for two agricultural regions of ER.

Materials and methods

Rates of soil erosion were estimated for two time windows (1963–1986 and 1986–2015) within the two agricultural regions. Both regions are characterized by a high proportion of cropland (>?60%), and within each region, one river basin and one 1st–3rd-order agricultural catchment were selected for a detailed assessment of soil erosion rates. Erosion models and visual interpretation of satellite images were used for the evaluation of the erosion rates for the river basins. Sediment budget assessments, ¹³⁷Cs dating, geomorphologic mapping, and erosion models were used for the evaluation of the sediment redistribution for the two time windows in agricultural catchments.

Results and discussion

At the river basin scale, the mean annual erosion rate did not change in the western part of forest–steppe ecotone; however, there was a weak negative trend in the mean annual erosion rate for the eastern part of the southern forest ecotone. A large negative trend in the erosion rate was found for both small agricultural catchments. In all cases, the reduction in the erosion rates was mainly associated with a decrease of surface runoff during snowmelt, as a result of an increase in both the air and soil temperatures during winter season. The soil loss reduction during snowmelt was counteracted by an equal increase in rainfall erosion due to increase of rainfall intensity in western part of forest–steppe ecotone.

Conclusions

Reduction of surface runoff during spring snowmelt was the main reason the erosion rates declined on cultivated lands within the forest–steppe and southern forest ecotones of ER. Evaluation of ephemeral gully erosion rate was not incorporated into State Hydrological Institute erosion model used for the evaluation of the soil losses during snowmelt. This has led to an underestimation of the total soil losses for the 1963–1986 time window for all study sites.