0000000000180007

AUTHOR

Lucia Pappalardo

0000-0002-4491-2082

showing 2 related works from this author

The NMR structure of the sensory domain of the membranous two-component fumarate sensor (histidine protein kinase) DcuS of Escherichia coli

2003

The structure of the water-soluble, periplasmic domain of the fumarate sensor DcuS (DcuS-pd) has been determined by NMR spectroscopy in solution. DcuS is a prototype for a sensory histidine kinase with transmembrane signal transfer. DcuS belongs to the CitA family of sensors that are specific for sensing di- and tricarboxylates. The periplasmic domain is folded autonomously and shows helices at the N and the C terminus, suggesting direct linking or connection to helices in the two transmembrane regions. The structure constitutes a novel fold. The nearest structural neighbor is the Per-Arnt-Sim domain of the photoactive yellow protein that binds small molecules covalently. Residues Arg107, H…

Models MolecularProtein FoldingMagnetic Resonance SpectroscopyProtein ConformationStereochemistryMolecular Sequence DataReceptors Cell SurfaceBiologyArginineBiochemistryProtein Structure SecondaryBacterial ProteinsFumaratesEscherichia coliTransferaseHistidineAmino Acid SequenceProtein kinase AMolecular BiologyHistidineBinding SitesEscherichia coli ProteinsC-terminusCell MembraneHistidine kinaseCell BiologyNuclear magnetic resonance spectroscopyPeriplasmic spaceChemoreceptor CellsTransmembrane proteinProtein Structure TertiaryCrystallographyMutationPeriplasmProtein KinasesSignal Transduction
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The geological CO2degassing history of a long-lived caldera

2015

The majority of the ~100 Holocene calderas on Earth host vigorously active hydrothermal systems, the heat and volatile budgets of which are sustained by degassing of deeply stored magma. Calderas may thus contribute a nontrivial, although poorly quantified, fraction of the global budget of magmatic volatiles such as CO2. Here we use original isotopic a d petrological results from Campi Flegrei volcano, Italy, to propose that hydrothermal calcites are natural mineral archives for the magmatic CO2 that reacted with reservoir rocks during the geological history of a caldera. We show that Campi Flegrei calcites, identified in core samples extracted from 3-km-deep geothermal wells, formed at iso…

Calcitegeographygeography.geographical_feature_categoryEarth scienceGeochemistryGeologyHydrothermal circulationFumarolechemistry.chemical_compoundVolcanochemistryMagmaCalderaGeothermal gradientHoloceneGeologyGeology
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