Tidal variability of the motion in the Strait of Otranto

Various current data, collected in the Strait of Otranto during the period 1994–2007, have been analysed with the aim of describing the characteristics of the tidal motions and their contribution to the total flow variance. The principal tidal constituents in the area were the semi-diurnal (M2) and the diurnal (K1), with the latter one predominant. The total flow was, in general, more energetic along the flanks than in the middle of the strait. Specifically, it was most energetic over the western shelf and in the upper layer along the eastern flank. In spite of the generally low velocities (a few cm s⁻¹) of the principal tidal constituents, the tidal variance has a pattern similar to that of the total flow variance, that is, it was large over the western shelf and low in the middle. The proportion of non-tidal (comprising the inertial and sub-inertial low-frequency bands) to tidal flow variances was quite variable in both time and space. The low-frequency motions dominated over the tidal and inertial ones in the eastern portion of the strait during the major part of the year, particularly in the upper and intermediate layers. In the deep, near-bottom layer the variance was evenly distributed between the low frequency, diurnal and semi-diurnal bands. An exception was observed near the western shelf break during the summer season when the contribution of the tidal signal to the total variance reached 77%. This high contribution was mainly due to the intensification of the diurnal signal at that location at both upper and bottom current records (velocities of about 10 cm s⁻¹). Local wind and sea level data were analysed and compared with the flow to find the possible origin of this diurnal intensification. Having excluded the sea-breeze impact on the intensification of the diurnal tidal signal, the most likely cause remains the generation of the topographically trapped internal waves and the diurnal resonance in the tidal response. These waves were sometimes generated by the barotropic tidal signal in the presence of summer stratification and the strong bottom slope. This phenomenon may stimulate diapycnal mixing during the stratified season and enhance ventilation of the near-bottom layers

Multiple Myeloma Index for Risk of Infection

Based on our earlier research into the main characteristics and risk factors for infections in hospitalized patients with multiple myeloma, we created the numerical Multiple Myeloma Index for Risk of Infection (MMIRI) to predict infection in myeloma patients. The included factors that could influence the pathogenesis and incidence of infections were sex, perform ance status, Durie Salmon stage of disease, International Staging System, serum creatinine level, immune paresis, neutropenia, serum ferritin level, the presence of any catheters, disease duration, stable/progressive disease, and type of therapy. For each of these parameters, the strength of association with infection was statistically estimated and specific number of points was assigned to each of these parameters, proportional to the strength of the association. When designing the MMIRI, we included only those parameters that we determined were pathophysiologically associated with the infection. After further statistical analysis, we identified an optimal cutoff score of 6 or above as indicating a significant risk for infection, with a sensitivity of 93.2% and specificity of 80.2%. The scoring system in the retrospective receiver operating characteristic analysis showed an area under the curve of 0.918. The potential value of the MMIRI is the possibility of identifying those patients who would benefit from the prophylactic administration of antibiotics and other anti -infective measures while minimizing the contribution to antibiotic resistance related to the overuse of these drugs. As far as we know, this index represents the first attempt to create such an instrument for predicting the occurrence of infections in myeloma patients

Application of sos/umuc assay in eco/genotoxicology

Introduction. The SOS/umuC assay is used for assessment of water genotoxicity. Salmonella typhimurium TA1535/pSK1002 is used in this test, but the results can be extrapolated on higher eukaryotic organisms with the introduction of enzymatic S9 fraction in experimental procedure. The test is standardised for the determination of the genotoxic potential of water and wastewater (ISO/DIS 13829, 2000). Aim. Sensitivity of the assay was challenged by using parallel in situ and in vitro approach in evaluation of the genotoxic potential in the basins of significant tributaries of the Danube River: the Sava River and the Velika Morava River. Materials and methods. Within in vitro testing, native water samples were analysed by SOS/umuC test. DNA damage in situ was assessed in bleak (Alburnus alburnus) erythrocytes by the comet and micronucleus assays. The concentration of heavy metals in fish tissue and the data of the physico-chemical parameters measured in water were used as a measure of the pollution pressure at the sites. Results. Results showed that applied in vitro tests with native water samples are less sensitive in comparison with in situ tests. None of 20 investigated samples showed genotoxic potential in SOS/umuC assay while in situ analyses indicated variation of genotoxic potential among the investigated sites. Conclusions. The results of our study point towards low sensitivity of the SOS/umuC test when processing un-concentrated (native) water samples; the results of in vitro tests should be taken with precaution when making predictions on the status of the ecosystem

INFLUENCE OF HIGH SUMMER TEMPERATURES ON REDUCED FISH PRODUCTION IN FISH PONDS OF EASTERN CROATIA

Problem nedovoljnih količina vode i visoke temperature vode u ljetnim mjesecima u ribnjacima istočne Hrvatske (od 1. 7. do 1. 9. 1998.), utjecao je na smanjenu proizvodnju (prirast) riba u ribnjačarstvima. Temperature zraka od preko 30°C, te povećano zagrijavanje vode bili su uzrokom povećanog potroška hrane, a manjeg prirasta, kao i povećanih troškova crpnih postaja, troškova vezanih za oplemenjivanje vodenih površina s kisikom, te uzrokom manjeg ili većeg pomora ribe, kao i pogoršana zdravstvenog stanja nasada. Sve je ovo uzrokovalo smanjeni prirast kod riba u ribnjacima. Na 825 ha površina pod jednogodišnjim mlađem u ribnjačarstvima u istočnoj Hrvatskoj, kao i na 1.208 ha dvogodišnjeg mlađa i 2.637 ha ribnjaka s konzumnom ribom, smanjena je prosječno proizvodnja, i to: za jednogodišnji mlađ 36,0%, za dvogodišnji mlađ 30,0% i za konzumnu ribu 27,50%. Na osnovi ukupne procjene smanjenja prirasta i manjega broja kilograma proizvedene ribe, a na temelju prosječnih prodajnih vrijednosti ribe, ribnjačarstva su imala smanjenu realizaciju pretvorenu u kune za 24.230.079,00 kuna. Na osnovi ovih pokazatelja zaključuje se da je utjecaj visokih ljetnih temperatura prouzročio elementarnu nepogodu za proizvođače ribe istočne Hrvatske, te se može postaviti opravdani zahtjev za nadoknadu učinjene štete.The problem of insufficient quantities and high temperature of water during the summer months (1st July to 1st September 1998) in the fish ponds of Eastern Croatia had as a consequence a reduced production (growth) of fish in the fish ponds. Air temperatures higher than 30 °C and warming up of water were the causes of a larger food consumption and smaller growth, as well as of an increase in expenses connected with pump stations and with aeration of the water, and they have also caused a higher or lower death-rate of fish and a deterioration of the health condition of the fry setting. All this has resulted in a smaller growth of fish in fishponds. On the 825 ha of fish ponds with one year old fingerlings in Eastern Croatia, as well as on the 1,208 ha of fish ponds with two year old fingerlings and 2,637 ha of fish ponds with fish for the market the production was on the average reduced as follows: in one year old fingerlings it was reduced by 36,0%, in two year old fish by 30,0% and in the fish for the market by 27,5%. On the basis of the total assessment of the reduction of growth and of a smaller number of kilograms of produced fish founded on the average sale value of fish the fish ponds recorded a drop in realization which - converted into money - was reduced by 24,230.079,00 kn. These indicators lead to the conclusion that the influence of high summer temperatures had the effect of natural disaster for fish producers in Eastern Croatia and therefore they have a justified right to demand compensation for the damage they have suffered

Application of sos/umuc assay in eco/genotoxicology

Introduction. The SOS/umuC assay is used for assessment of water genotoxicity. Salmonella typhimurium TA1535/pSK1002 is used in this test, but the results can be extrapolated on higher eukaryotic organisms with the introduction of enzymatic S9 fraction in experimental procedure. The test is standardised for the determination of the genotoxic potential of water and wastewater (ISO/DIS 13829, 2000). Aim. Sensitivity of the assay was challenged by using parallel in situ and in vitro approach in evaluation of the genotoxic potential in the basins of significant tributaries of the Danube River: the Sava River and the Velika Morava River. Materials and methods. Within in vitro testing, native water samples were analysed by SOS/umuC test. DNA damage in situ was assessed in bleak (Alburnus alburnus) erythrocytes by the comet and micronucleus assays. The concentration of heavy metals in fish tissue and the data of the physico-chemical parameters measured in water were used as a measure of the pollution pressure at the sites. Results. Results showed that applied in vitro tests with native water samples are less sensitive in comparison with in situ tests. None of 20 investigated samples showed genotoxic potential in SOS/umuC assay while in situ analyses indicated variation of genotoxic potential among the investigated sites. Conclusions. The results of our study point towards low sensitivity of the SOS/umuC test when processing un-concentrated (native) water samples; the results of in vitro tests should be taken with precaution when making predictions on the status of the ecosystem

Linking mixing processes and climate variability to the heat content distribution of the Eastern Mediterranean abyss

The heat contained in the ocean (OHC) dominates the Earth’s energy budget and hence represents a fundamental parameter for understanding climate changes. However, paucity of observational data hampers our knowledge on OHC variability, particularly in abyssal areas. Here, we analyze water characteristics, observed during the last three decades in the abyssal Ionian Sea (Eastern Mediterranean), where two competing convective sources of bottom water exist. We find a heat storage of ~1.6 W/m2– twice that assessed globally in the same period – exceptionally well-spread throughout the local abyssal layers. Such an OHC accumulation stems from progressive warming and salinification of the Eastern Mediterranean, producing warmer near-bottom waters. We analyze a new process that involves convectively-generated waters reaching the abyss as well as the triggering of a diapycnal mixing due to rough bathymetry, which brings to a warming and thickening of the bottom layer, also influencing water-column potential vorticity. This may affect the prevailing circulation, altering the local cyclonic/anticyclonic long-term variability and hence precondition future water-masses formation and the redistribution of heat along the entire water-column

Genetic Differentiation of the Western Capercaillie Highlights the Importance of South-Eastern Europe for Understanding the Species Phylogeography

The Western Capercaillie (Tetrao urogallus L.) is a grouse species of open boreal or high altitude forests of Eurasia. It is endangered throughout most mountain range habitat areas in Europe. Two major genetically identifiable lineages of Western Capercaillie have been described to date: the southern lineage at the species' southernmost range of distribution in Europe, and the boreal lineage. We address the question of genetic differentiation of capercaillie populations from the Rhodope and Rila Mountains in Bulgaria, across the Dinaric Mountains to the Slovenian Alps. The two lineages' contact zone and resulting conservation strategies in this so-far understudied area of distribution have not been previously determined. The results of analysis of mitochondrial DNA control region sequences of 319 samples from the studied populations show that Alpine populations were composed exclusively of boreal lineage; Dinaric populations of both, but predominantly (96%) of boreal lineage; and Rhodope-Rila populations predominantly (>90%) of southern lineage individuals. The Bulgarian mountains were identified as the core area of the southern lineage, and the Dinaric Mountains as the western contact zone between both lineages in the Balkans. Bulgarian populations appeared genetically distinct from Alpine and Dinaric populations and exhibited characteristics of a long-term stationary population, suggesting that they should be considered as a glacial relict and probably a distinct subspecies. Although all of the studied populations suffered a decline in the past, the significantly lower level of genetic diversity when compared with the neighbouring Alpine and Bulgarian populations suggests that the isolated Dinaric capercaillie is particularly vulnerable to continuing population decline. The results are discussed in the context of conservation of the species in the Balkans, its principal threats and legal protection status. Potential conservation strategies should consider the existence of the two lineages and their vulnerable Dinaric contact zone and support the specificities of the populations