Using the diagram completed on the reverse side of this page, answer the questions regarding ingredients and products of photosynthesis using the list on the right.
B 1. Oxidized in the light reactions
2. Reduced in the Calvin Cycle (CC)
3. Carries H and electrons from the light reactions to the CC
4. Food produced by photosynthesis
A. Carbon Dioxide (CO2)
5. Source of O atoms that ends up in glucose
B. Water (H20)
6. Where the O atoms from water end up
C. Glucose (C6H1206)
7. Oxidized in the in CC
D. Oxygen (O2)
E. ADP +P
8. Reduced in the light reactions
F. ATP
9. Supplies energy to the CC
G. NADP
H. NADPH
10. Recycled from the CC to make ATP
1. Light
11. Supplies energy to the light dependent reactions
12. Gas produced by reactions in the thylakoids
13. Gas consumed by the reactions in the stroma
14. Source of carbon for carbon fixation
15. Picks up energized electrons from the light reactions

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.

Atissue is a group of connected cells that have a similar function within an organism.

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