You are interested in building a fully functional, bionic mitochondrion. In order to replicate the function of the F0 subunit of the ATP synthase in the normal mitochondrion, the F0 subunit in your bionic ATP synthase:. a. should undergo a mechanical rotation induced by passage of protons from the matrix to the intermembrane space that would result in ATP synthesis.
b. should include a series of smaller subunits within the F0 subunit that can bind ADP.
c. should have a structural connection or "bridge" that couples movements of the multiple subunits in the bionic F0 to conformational changes in F1.
d. should undergo a conformational change like that induced by uncoupling proteins in thermogenic brown fat that block proton gradients between the matrix and the intermembrane space.
e. should have enough rotating subunits to account for transfer of three ATP molecules from F1 directly into the intermembrane space in the bionic mitochondrion.

Bidk

Mantle convection  is the slow  creepingmotion of earth's solid silicate  mantle  caused by  convection  currents carrying  heat from the interior  to the planet's surface.[1][2]  the earth's surface  lithosphere, which rides atop the  asthenosphere  (the two components of the  upper mantle), is divided into a number of  plates  that are continuously being created and consumed at their opposite  plate boundaries. accretion occurs as mantle is added to the growing edges of a plate, associated with  seafloor spreading. this hot added material cools down by  conduction  and  convection  of heat. at the consumption edges of the plate, the material has thermally contracted to become dense, and it sinks under its own weight in the process of  subduction  usually at an  ocean trench.[3]this subducted material sinks through the earth's interior. some subducted material appears to reach the lower mantle,[4]  while in other regions, this material is impeded from sinking further, possibly due to a phase transition from  spinel  to  silicate perovskiteand  magnesiowustite, an  endothermic reaction.[5]the subducted oceanic crust triggers  volcanism, although the basic mechanisms are varied. volcanism may occur due to processes that add buoyancy to partially melted mantle causing an upward flow due to a decrease in density of the partial melt.secondary forms of convection that may result in surface volcanism are postulated to occur as a consequence of intraplate extension[6]  and  mantle plumes.[7]it is because the mantle can convect that the  tectonic plates  are able to move around the earth's surface.[8]mantle convection seems to have been much more active during the  hadean  period, resulting in gravitational sorting of heavier molten  iron, and  nickel  elements and  sulphides  in the core, and lighter  silicate minerals  in the  mantle.