Der Carrier DcuB als zweiter Sensor des Zweikomponentensystems DcuSR in Escherichia coli

Escherichia coli kann C4-Dicarboxylate und andere Carbonsäuren als Substrate für den aeroben und anaeroben Stoffwechsel nutzen. Die Anwesenheit von C4-Dicarboxylaten im Außenmedium wird über das Zweikomponentensystem DcuSR, bestehend aus der membranständigen Sensorkinase DcuS und dem cytoplasmatischen Responseregulator DcuR, erkannt. Die Bindung von C4-Dicarboxylaten an die periplasmatische Domäne von DcuS führt zu einer Induktion der Zielgene. Hierzu zählen die Gene für den anaeroben Fumarat/Succinat-Antiporter DcuB (dcuB), die anaerobe Fumarase (fumB) und die Fumaratreduktase (frdABCD). Unter aeroben Bedingungen stimuliert DcuSR die Expression des dctA Gens, das für den aeroben C4-Dicarboxylat-Carrier DctA kodiert. Für den Carrier DcuB konnte eine regulatorische Funktion bei der Expression der DcuSR-regulierten Gene gezeigt werden. Die Inaktivierung des dcuB Gens führte bereits ohne Fumarat zu einer maximalen Expression einer dcuB´-´lacZ Reportergenfusion und anderer DcuSR-abhängiger Gene. Diese Stimulierung erfolgte nur in einem dcuS-positiven Hintergrund. DcuB unterscheidet sich damit von den alternativen Carriern DcuA und DcuC, die diesen Effekt nicht zeigten. Mithilfe ungerichteter Mutagenese wurden DcuB-Punktmutanten hergestellt (Thr394Ile und Asp398Asn), die eine Geninduktion verursachten, aber eine intakte Transportfunktion besaßen. Dies zeigt, dass der regulatorische Effekt von DcuB unabhängig von dessen Transportfunktion ist. Durch gerichtete Mutagenese wurde die Funktion einer Punktmutation (Thr394) näher charakterisiert. Es werden zwei Modelle zur Membrantopologie von DcuB und der Lage der Punktmutationen im Protein vorgestellt. Da DcuB seine regulatorische Funktion über eine Interaktion mit DcuS vermitteln könnte, wurden mögliche Wechselwirkungen zwischen DcuB und DcuS als auch DcuR mithilfe von Two-Hybrid-Systemen untersucht. Für biochemische Untersuchungen von DcuB wurde außerdem die Expression des Proteins in vivo und in vitro versucht. Unter aeroben Bedingungen beeinflusst der C4-Dicarboxylat-Carrier DctA die Expression der DcuSR-abhängigen Gene. Eine Mutation des dctA Gens bewirkte eine stärkere Expression einer dctA´-´lacZ Reportergenfusion im Vergleich zum Wildtyp. Diese Expression nahm in einem dcuS-negativen Hintergrund ab, die Succinat-abhängige Induktion blieb jedoch erhalten. Unter anaeroben Bedingungen kann das dctA Gen auch durch Inaktivierung von DcuB induziert werden. Es wird ein Modell vorgestellt, das die Beteiligung beider Carrier an der DcuSR-abhängigen Regulation erklärt.

The vacuolar-ATPase B1 subunit in distal tubular acidosis: novel mutations and mechanisms for dysfunction

Mutations in the B1 subunit of the multisubunit vacuolar ATPase cause autosomal-recessive distal renal tubular acidosis and sensorineural deafness. Here, we report a novel frameshift mutation that truncates the C-terminus of the human B1 subunit. This mutant protein failed to assemble with other subunits in the cytosol to form the complex that can be targeted to vesicular structures in mammalian cells. Loss of proton pump activity was demonstrated in a functional complementation assay in B-subunit null yeast. The mutation caused loss of a discreet C-terminal region critical for subunit interaction not related to the C-terminal PDZ motif. Co-expression studies failed to demonstrate dominant negative effects of this truncated mutant over wild-type B1. Analysis of 12 reported B1 subunit missense mutations showed one polymorphic allele had intact pump function, two point mutants had intact assembly but defective proton pumping, and the remaining nine had disrupted assembly with no pump function. One presumed polymorphic allele was actually an inactivating mutation. Our study shows that multiple mechanisms of pump dysfunction result from B1 subunit mutations with a common outcome being defective assembly. Polymorphisms of the B1 subunit in the general population may affect renal acidification and urinary chemistry.

Incidence of hypo- and hyper-capnia in a cross-sectional European cohort of ventilated newborn infants

OBJECTIVE To determine the incidence of hypo- and hyper-capnia in a European cohort of ventilated newborn infants. DESIGN AND SETTING Two-point cross-sectional prospective study in 173 European neonatal intensive care units. PATIENTS AND METHODS Patient characteristics, ventilator settings and measurements, and blood gas analyses were collected for endotracheally ventilated newborn infants on two separate dates. RESULTS A total of 1569 blood gas analyses were performed in 508 included patients with a mean±SD Pco2 of 48±12 mm Hg or 6.4±1.6 kPa (range 17-104 mm Hg or 2.3-13.9 kPa). Hypocapnia (Pco2<30 mm Hg or 4 kPa) and hypercapnia (Pco2>52 mm Hg or 7 kPa) was present in, respectively, 69 (4%) and 492 (31%) of the blood gases. Hypocapnia was most common in the first 3 days of life (7.3%) and hypercapnia after the first week of life (42.6%). Pco2 was significantly higher in preterm infants (49 mm Hg or 6.5 kPa) than term infants (43 mm Hg or 5.7 kPa) and significantly lower during pressure-limited ventilation (47 mm Hg or 6.3±1.6 kPa) compared with volume-targeted ventilation (51 mm Hg or 6.8±1.7 kPa) and high-frequency ventilation (50 mm Hg or 6.7±1.7 kPa). CONCLUSIONS This study shows that hypocapnia is a relatively uncommon finding during neonatal ventilation. The higher incidence of hypercapnia may suggest that permissive hypercapnia has found its way into daily clinical practice.

Biogeochemical investigation of cold seep sediments in the Eastern Mediterranean Sea

Cold seep ecosystems are highly productive, fragmented ecosystems of the deep-sea floor. They form worldwide where methane reaches the surface seafloor, and are characterized by rich chemosynthetic communities fueled by the microbial utilization of hydrocarbons. Here we investigated with in situ (benthic chamber, microprofiler) and ex situ (pore water constituents, turnover rates of sulfate and methane, prokaryote abundance) techniques reduced sites from three different seep ecosystems in the Eastern Mediterranean deep-sea. At all three cold seep systems, the Amon Mud Volcano, Amsterdam Mud Volcano and the Nile Deep Sea Fan Pockmark area, we observed and sampled patches of highly reduced, methane-seeping sulfidic sediments which were separated by tens to hundreds of (kilo)meters with non-reduced oxygenated seafloor areas. All investigated seep sites were characterized by gassy, sulfidic sediments of blackish color, of which some were overgrown with thiotrophic bacterial mats. Fluxes of methane and oxygen, as well as sulfate reduction rates varied between the different sites.

Pore water geochemistry of Håkon Mosby mud volcano sediments measured at station PS74/169-1_PUC-15 (Z1-S1, new flow surface)

Pore water and turnover rates were determined for surface sediment cores obtained in 2009 and 2010. The pore water was extracted with Rhizons (Rhizon CSS: length 5 cm, pore diameter 0.15 µm; Rhizosphere Research Products, Wageningen, Netherlands) in 1 cm-resolution and immediately fixed in 5% zinc acetate (ZnAc) solution for sulfate, and sulfide analyses. The samples were diluted, filtered and the concentrations measured with non-suppressed anion exchange chromatography (Waters IC-Pak anion exchange column, waters 430 conductivity detector). The total sulfide concentrations (H2S + HS- + S**2-) were determined using the diamine complexation method (doi:10.4319/lo.1969.14.3.0454). Samples for dissolved inorganic carbon (DIC) and alkalinity measurements were preserved by adding 2 µl saturated mercury chloride (HgCl2) solution and stored headspace-free in gas-tight glass vials. DIC and alkalinity were measured using the flow injection method (detector VWR scientific model 1054) (doi:10.4319/lo.1992.37.5.1113). Dissolved sulfide was eliminated prior to the DIC measurement by adding 0.5 M molybdate solution (doi:10.4319/lo.1995.40.5.1011). Nutrient subsamples (10 - 15 ml) were stored at - 20 °C prior to concentration measurements with a Skalar Continuous-Flow Analyzer (doi:10.1002/9783527613984).