Dharma/Bozozok (Dha/Boz) is a homeodomain protein containing an Engrailed homology (Eh) 1 repressor motif. It is important in zebrafish dorsal organizer formation. Dha/Boz interacted with a co-repressor Groucho through the Eh1 motif. Expression of a Dha/Boz fused to the transcriptional activator VP16 repressed dorsal axis formation and the expression of organizer genes but led to the dorsal exp...

Hydrothermal vent fluids are highly enriched in iron (Fe) compared to ambient seawater, and organic ligands may play a role in facilitating the transport of some hydrothermal Fe into the open ocean. This is important since Fe is a limiting micronutrient for primary production in large parts of the world’s surface ocean. We have investigated the concentration and speciation of Fe in several vent...

Vent vacuum relief valves (VRVs) are used to limit the negative pressure at the ventricular vent catheter tip as well as prevent reversal of blood flow and prevention of air embolism. The purpose of this study was to evaluate the performance of three commercially available ventricular vent valves. The negative pressure at which the vent valve opened was measured at the valve inlet using high-fi...

Reduced inorganic compounds of geothermal-origin hydrogen sulfide (H2S), iron (Fe[II]), and methane (CH4) were common but not ubiquitous components of hydrothermal vent fluids of Yellowstone Lake at concentrations capable of supporting chemolithoautotrophic (geochemical-oxidizing, carbon dioxide (CO2)-fixing) bacterial growth. Closely linked to the presence of reduced geochemicals was abundance...

The papers in the " Hydrothermal Vent " research topic cover a range of microbiological research in deep and shallow hydrothermal environments, from high temperature " black smokers, " to diffuse flow habitats and episodically discharging subsurface fluids, to the hydrothermal plumes. Together they provide a snapshot of current research interests in a field that has evolved rapidly since the di...

Vent opening hazard models are routinely used as inputs for assessing distal volcanic hazards (lava flows, tephra fallout) in distributed fields. These vent have traditionally relied on the location of mapped vents; seldom they taken into account how vents linked space and time. We show that needed to appropriately model fundamentally different than thoses required near-vent (ground deformation...

Many calderas show remarkable unrest, which often does not culminate in eruptions (non-eruptive unrest). In this context the interpretation of the geophysical data collected by the monitoring networks is difficult. When the unrest is eruptive, a vent opening process occurs, which leads to an eruption. In calderas, vent locations typically are scattered over a large area and monogenic cones form...