Publications by authors named "Grosso O"

Iron is an essential nutrient that regulates productivity in ~30% of the ocean. Compared with deep (>2000 meter) hydrothermal activity at mid-ocean ridges that provide iron to the ocean's interior, shallow (<500 meter) hydrothermal fluids are likely to influence the surface's ecosystem. However, their effect is unknown.

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Diazotrophs are widespread microorganisms that alleviate nitrogen limitation in 60% of our oceans, thereby regulating marine productivity. Yet, the group-specific contribution of diazotrophs to organic matter export has not been quantified, which so far has impeded an accurate assessment of their impact on the biological carbon pump. Here, we examine the fate of five groups of globally-distributed diazotrophs by using an original combination of mesopelagic particle sampling devices across the subtropical South Pacific Ocean.

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Article Synopsis
  • Trichodesmium, a cyanobacterium found in low latitude oceans, is known for fixing nitrogen (N) and contributing to primary productivity, raising questions about its abilities in deeper, darker ocean layers.
  • Recent findings show that Trichodesmium colonies that sink to depths of 170 to 1000 meters can fix nitrogen at rates similar to those observed in surface waters, comprising a significant portion of overall nitrogen fixation in those layers.
  • Experiments indicate that while high pressure and low temperatures in the dark ocean reduce Trichodesmium's nitrogen fixation, it can still function by using stored carbon from photosynthesis, thus providing essential nutrients to other organisms in the mesopelagic zone.
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The unicellular diazotrophic cyanobacterium Crocosphaera contributes significantly to fixed nitrogen inputs in the oligotrophic ocean. In the western tropical South Pacific Ocean (WTSP), these diazotrophs abound thanks to the phosphorus-rich waters provided by the South Equatorial Current, and iron provided aeolian and subsurface volcanic activity. East of the WTSP, the South Pacific Gyre (SPG) harbors the most oligotrophic and transparent waters of the world's oceans, where only heterotrophic diazotrophs have been reported before.

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Background: The vaginal microenvironment, regulated by an immune system, can be protected or altered by many factors, including contraceptive methods.

Objective: The objective of this study is to evaluate the impact of contraceptive methods on the basic vaginal states (BVSs) and to identify culturable vaginal Lactobacillus species.

Methods: This is a prospective, consecutive, longitudinal, and descriptive study.

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Ocean acidification is posing a threat to calcifying organisms due to the increased energy requirements of calcification under high CO conditions. The ability of scleractinian corals to cope with future ocean conditions will thus depend on their ability to fulfil their carbon requirement. However, the primary productivity of coral holobionts is limited by low nitrogen (N) availability in coral reef waters.

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  • Coral reefs face threats from global warming, leading to coral bleaching due to disrupted relationships with their symbiotic algae, primarily Symbiodiniaceae.
  • Research shows that bleached corals, when incubated with nitrogen-fixing plankton, significantly increased nitrogen absorption rates compared to untreated corals.
  • Additionally, bleached corals preferred consuming nitrogen-rich Synechococcus over other types of phytoplankton, providing a potential means for recovery in nutrient-poor conditions.
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  • Diatoms are crucial primary producers in oceans, contributing to about 20% of Earth’s photosynthetically fixed carbon, but many small species are often overlooked.
  • Large diatoms are typically represented in marine models, while the smaller nanophytoplankton and picoplanktonic diatoms are underrepresented due to their minuscule size and detection difficulties.
  • A recent discovery of a spring bloom of the small diatom species Minidiscus in the northwestern Mediterranean Sea suggests the need to reassess their ecological roles, indicating they can contribute significantly to marine food webs and carbon cycling.
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Corals are mixotrophs: they are able to fix inorganic carbon through the activity of their symbiotic dinoflagellates and to gain nitrogen from predation on plankton and uptake of dissolved organic and inorganic nutrients. They also live in close association with diverse diazotrophic communities, inhabiting their skeleton, tissue and mucus layer, which are able to fix dinitrogen (N2). The quantity of fixed N2 transferred to the corals and its distribution within coral compartments as well as the quantity of nitrogen assimilated through the ingestion of planktonic diazotrophs are still unknown.

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Dinitrogen (N2) fixation was investigated together with organic matter composition in the mesopelagic zone of the Bismarck (Transect 1) and Solomon (Transect 2) Seas (Southwest Pacific). Transparent exopolymer particles (TEP) and the presence of compounds sharing molecular formulae with saturated fatty acids and sugars, as well as dissolved organic matter (DOM) compounds containing nitrogen (N) and phosphorus (P) were higher on Transect 1 than on Transect 2, while oxygen concentrations showed an opposite pattern. N2 fixation rates (up to ~1 nmol N L-1 d-1) were higher in Transect 1 than in Transect 2, and correlated positively with TEP, suggesting a dependence of diazotroph activity on organic matter.

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We examined rates of N2 fixation from the surface to 2000 m depth in the Eastern Tropical South Pacific (ETSP) during El Niño (2010) and La Niña (2011). Replicated vertical profiles performed under oxygen-free conditions show that N2 fixation takes place both in euphotic and aphotic waters, with rates reaching 155 to 509 µmol N m(-2) d(-1) in 2010 and 24±14 to 118±87 µmol N m(-2) d(-1) in 2011. In the aphotic layers, volumetric N2 fixation rates were relatively low (<1.

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Meglumine antimonate is the active of Glucantime® used for the treatment of leishmaniasis, a tropical disease caused by parasitic protozoa, and it is estimated that 12 million people worldwide are affected. This drug mainly contains Sb(V) under the form of an organic complex with N-methylglucamine (NMG). During the synthesis of this molecule, traces of Sb(III) may be present, also probably complexed.

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The ribosome is the central effector of protein synthesis, and its synthesis is intimately coordinated with that of proteins. At present, the most documented way to modulate ribosome biogenesis involves control of rDNA transcription by RNA polymerase I (RNA Pol I). Here we show that after infection of human cells with herpes simplex virus type 1 (HSV-1) the rate of ribosome biogenesis is modulated independently of RNA Pol I activity by a dramatic change in the rRNA maturation pathway.

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Chronic hypertension induces changes in the structure of the left ventricle, atrium, and aortic root. However, the effects of transient hypertension are unclear. Pregnancy-induced hypertension (PIH) offers a natural and spontaneous model of this condition.

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The changes induced by transient hypertension on cardiac structure and function are unclear. Pregnancy-induced hypertension offers a natural and spontaneous model of this condition. To assess the potential of echocardiographic Doppler to unmask left ventricular function impairment, we studied 28 women aged 26.

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The changes induced by transient hypertension upon cardiac geometry (G) are unclear. Pregnancy-induced hypertension (PIH) offers a natural and spontaneous model of this condition. To assess geometric changes according to two-dimensionally guided M-mode echocardiography, we compared patients with PIH with normal pregnant women (NPW).

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