Fertilidade em garanhões avaliada através do exame andrológico Fertility in stallions as accessed by the breeding soundness examination

O presente trabalho teve por objetivo discutir aspectos da fertilidade de garanhões e sua relação com o exame andrológico. Numa primeira análise, 10 garanhões usados em monta natural exclusivamente, tiveram seus índices reprodutivos relacionados a qualidade do seu sêmen. Num segundo grupo, foram considerados 14 garanhões cujos acasalamentos eram, alternadamente, inseminação artificial e/ou monta natural. No terceiro estudo, foram relacionados garanhões específicos, pertencentes aos dois grupos anteriores, sabidamente subférteis em que os índices de fertilidade foram relacionados a características do sêmen ou manejo. Quando os garanhões são submetidos a monta natural dentro de um programa de manejo racional existe uma significativa relação entre qualidade de sêmen e fertilidade (P <0,01). O mesmo não se verifica quando há interferência de manejo (homem), usando inseminação artificial e modificando condições naturais (inseminação artificial inadequadamente empregada reduzindo a fertilidade e. adequadamente empregada, melhorando a fertilidade de garanhões subférteis). A análise de exames andrológicos individuais evidencia falares intrínsecos e extrínsecos (manejo) afetando a fertilidade.<br>This paper discuss certain aspects of the fertility in stallions and its relationship to the Breeding Soundness Examination. In afirst analysis, 10 stallions that were bred only naturally had their reproductive standards correlated to the sêmen quality. In a second step, we consider 14 stallions that were bred either by artificial insemination and for naturally. In a third study, certain subfertile stallions, belonging to the previous two groups, had their fertility standards correlated to sêmen quality and management procedures. A significam association (P<0.01) was observed between sêmen quality (sperm morphology) and fertility, when stallions were bred naturally under appropriate management procedures. This relationship was not observed when artificial insemination was included in the management, because it can improve the fertility of subfertile stallions or be detrimental to normal stallions when misused used. The individual analysis of the subfertile stallions allowed to determine if the cause the infertility can befrom intrinsic or extrinsic (management) factors

Neoproterozoic cap carbonates: a critical appraisal of existing models and the plumeworld hypothesis

Evidence for glaciation during the mid-late Neoproterozoic is widespread on Earth, reflecting three or more ice ages between 730 Ma and 580 Ma. Of these, the late Neoproterozoic Marinoan glaciation of approximately 635 Ma stands out because of its ubiquitous association with a characteristic, microcrystalline cap dolostone that drapes glacially influenced rock units worldwide. The Marinoan glaciation is also peculiar in that evidence for low altitude glaciation at equatorial latitudes is compelling. Three models have been proposed linking abrupt deglaciation with this global carbonate precipitation event: (i) overturn of an anoxic deep ocean; (ii) catastrophically accelerated rates of chemical weathering because of supergreenhouse conditions following global glaciation (Snowball Earth Hypothesis); and (iii) massive release of carbonate alkalinity from destabilized methane clathrates. All three models invoke extreme alkalinity fluxes into seawater during deglaciation but none explains how such alkalinity excess from point sources could be distributed homogeneously around the globe. In addition, none explains the consistent sequence of precipitation events observed within cap carbonate successions, specifically: (i) the global blanketing of carbonate powder in shallow marine environments during deglaciation; (ii) widespread and disruptive precipitation of dolomite cement; followed by (iii) localized barite precipitation and seafloor cementation by aragonite. The conceptual model presented here proposes that low latitude deglaciation was so massive and abrupt that the resultant meltwater plume could extend worldwide, physically separating the surface and deep ocean reservoirs for ≥103 years. It is proposed that cap dolostones formed primarily by microbially mediated precipitation of carbonate whitings during algal blooms within this low salinity plumeworld rather than by abiotic precipitation from normal salinity seawater. Many of the disruption features that are characteristic of cap dolostones can be explained by microbially mediated, early diagenetic dolomitization and cementation. The re-initiation of whole ocean circulation degassed CO2 into the atmosphere in areas of upwelling, triggering localized, abiotic CaCO3 precipitation in the form of aragonite fans that overlie cap dolostones in NW Canada and Namibia. The highly oxygenated shallow marine environments of the glacial and post-glacial Neoproterozoic world provided consistently favourable conditions for the evolutionary development of animals and other oxygenophiles