In the last stage of cellular respiration, oxidative phosphorylation, all of the reduced electron carriers produced in the previous stages are oxidized by oxygen via the electron transport chain. the energy from this oxidation is stored in a form that is used by most other energy-requiring reactions in cells. from the following compounds involved in cellular respiration, choose those that are the net inputs and net outputs of oxidative phosphorylation. drag each compound to the appropriate bin. if a compound is not involved in oxidative phosphorylation, drag it to the "not input or output" bin. (note that not all of the inputs and outputs of oxidative phosphorylation are listed.)

(glucose, co2, o2, atp, adp, had, hadh, h2o, coenzyme a, pyruvate, acetly coa )

The correct answer is:  

Net Input: NADH, ADP, O₂

Net Output: NAD⁺, ATP, and H2O

Not Input or Output: Pyruvate, Glucose, Acetyl CoA, Coenzyme A and CO₂.

NADH together with FADH2 are reduced electron carriers that transfer their electrons and turn back into NAD+ and FAD.

Electrons are transferred to O2 and H2O is produced.  

ADP can be described as precursor for ATP synthesis, since it receives phosphate group for the formation of ATP. This process is possible thanks to H ions gradient and enzyme ATP synthase.

1. desertification

2. captive breeding

3. black rhinoceros

4. renewable resources

explanation:

mark brainliest!

d concave shape of wave rock

explanation:

the concave shape of wave rock is a very good evidence that supports the evolution of earth due to chemical weathering. if we talk about structure of   wave rock, studies have estimated that it is around 2.7 billion years old. it also serves as the foundation of evidence that it was the place where australian continent began to form.

how the structure of wave rock was created?

studies suggest that structure of wave rock was created when the surrounded area was started to weather due to which deposition of material started on the part of land which now contains wave rock.

the structure of wave rock is considered to be one of the best-known landforms in australia. at the height of around 15 cm, there can be found flared slopes which formulate the margins of hyden rock. it is now assumed by geologists that wave rock was created by subsurface water-induced weathering and not by glaciers, waves or wind.

due to deposition of material over the period of long time, the wave rock became tougher and tougher due to weathering from surrounding terrain. this makes it a physical evidence that supports   the evolution of earth due to chemical weathering.

hope it !