The subthalamic nucleus : Part I: Development, cytology, topography and connections

This monograph on the subthalamic nucleus accentuates in Part I the gap between experimental animal and human information concerning subthalamic development, cytology, topography and connections. The light and electron microscopical cytology concerns the open nucleus concept and the neuronal types present in the STN. The cytochemistry encompasses: enzymes, NO, GRAP, calcium binding proteins, and receptors (dopamine, cannabinoid, piod, glutamate, GABA, serotonin, cholinergic, and calcium channels). The ontogeny of the subthalamic cell cord is reviewed. The topography concerns the rat, cat, baboon and human STN. The descriptions of the connections are also given from a historial point of view. Recent tracer studies on the rat nigro-subthalamic connection revealed contralateral projections

Sediment - animal - water interaction, Buzzards Bay, Massachusetts

Four stations in the northwestern part of Buzzards Bay, Massachusetts, were monitored from October, 1971 to November, 1972. Nitrogen, non-carbonate carbon, total organics and carbonate of the sediment were examined. Dissolved oxygen, salinity, temperature and pH of the bottom water were determined concurrently...

Edaphophyllum Irregularum, a New Middle Devonian Digonophyllid Coral from the Lower Arkona Formation, Ontario, Canada

Author Institution: Department of Geology, Wayne State University, Detroit, Michigan 48202Edaphophyllum irregularum n. sp., a digonophyllid coral, is described from limestone fragments in glacial drift inferred to represent the Middle Devonian (Traverse Group) Lower Arkona Formation of Ontario, Canada. The species is characterized by the development of a massive sequence of septal cones. This is the first occurrence of Edaphophyllum Simpson in the Michigan Basin

The retroflection of part of the East Greenland Current at Cape Farewell

The East Greenland Current (EGC) and the smaller East Greenland Coastal Current (EGCC) provide the major conduit for cold fresh polar water to enter the lower latitudes of the North Atlantic. They flow equatorward through the western Irminger Basin and around Cape Farewell into the Labrador Sea. The surface circulation and transport of the Cape Farewell boundary current region in summer 2005 is described. The EGCC merges with Arctic waters of the EGC to the south of Cape Farewell, forming the West Greenland Current. The EGC transport decreases from 15.5 Sv south of Cape Farewell to 11.7 Sv in the eastern Labrador Sea (where the water becomes known as Irminger Sea Water). The decrease in EGC transport is balanced by the retroflection of a substantial proportion of the boundary current (5.1 Sv) into the central Irminger Basin; a new pathway for fresh water into the interior of the subpolar gyre

Simulation of Micro-Electronic FlowFET Systems

A microelectronic fluidic system has been investigated by modeling and 3D simulation of fluid flow controlled by an applied gate voltage. The simulations have helped to characterize a novel FlowFET (a fluidic Field Effect Transistor) device under fault-free conditions. The FlowFET operates by applying a voltage field from a gate electrode in the insulated side wall of a microchannel to modulate the ␣-potential at the shear plane [1]. The change in ␣-potential can be used to control both the magnitude and direction of the electroosmotic flow in the microchannel