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Molecular Biology of the Cell by Bruce Alberts, Alexander Johnson, Julian Lewis, David Morgan, Martin Raff, Keith Roberts, Peter Walter by by Bruce Alberts, Alexander Johnson, Julian Lewis, David Morg

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606 Chapter 11: Membrane Transport of Small Molecules and the Electrical Properties of Membranes

ions

or K + or Na + or Ca ++

small molecule

H + H + H +

H + H +

lipid

bilayer

CYTOSOL

P

ADP

ATP

ATP

ADP

+

P i

ATP

ADP +

P i

ATP

ADP +

P i

P i +

ADP

ATP

P-type pump

ABC transporter

V-type proton pump

F-type ATP synthase

There Are Three Classes of ATP-Driven Pumps

ATP-driven pumps are often called transport ATPases because they hydrolyze ATP

to ADP and phosphate and use the energy released to pump MBoC6 ions n11.100/11.12

or other solutes

across a membrane. There are three principal classes of ATP-driven pumps (Figure

11–12), and representatives of each are found in all prokaryotic and eukaryotic

cells.

1. P-type pumps are structurally and functionally related multipass transmembrane

proteins. They are called “P-type” because they phosphorylate

themselves during the pumping cycle. This class includes many of the ion

pumps that are responsible for setting up and maintaining gradients of

Na + , K + , H + , and Ca 2+ across cell membranes.

2. ABC transporters (ATP-Binding Cassette transporters) differ structurally

from P-type ATPases and primarily pump small molecules across cell

membranes.

3. V-type pumps are turbine-like protein machines, constructed from multiple

different subunits. The V-type proton pump transfers H + into organelles

such as lysosomes, synaptic vesicles, and plant or yeast vacuoles (V = vacuolar),

to acidify the interior of these organelles (see Figure 13–37).

Structurally related to the V-type pumps is a distinct family of F-type ATPases,

more commonly called ATP synthases because they normally work in reverse:

instead of using ATP hydrolysis to drive H + transport, they use the H + gradient

across the membrane to drive the synthesis of ATP from ADP and phosphate (see

Figure 14–30). ATP synthases are found in the plasma membrane of bacteria, the

inner membrane of mitochondria, and the thylakoid membrane of chloroplasts.

The H + gradient is generated either during the electron-transport steps of oxidative

phosphorylation (in aerobic bacteria and mitochondria), during photosynthesis

(in chloroplasts), or by the light-driven H + pump (bacteriorhodopsin) in

Halobacterium. We discuss some of these proteins in detail in Chapter 14.

For the remainder of this section, we focus on P-type pumps and ABC transporters.

Figure 11–12 Three types of ATP-driven

pumps. Like any enzyme, all ATP-driven

pumps can work in either direction,

depending on the electrochemical

gradients of their solutes and the ATP/ADP

ratio. When the ATP/ADP ratio is high, they

hydrolyze ATP; when the ATP/ADP ratio is

low, they can synthesize ATP. The F-type

ATPase in mitochondria normally works in

this “reverse” mode to make most of the

cell’s ATP.

A P-type ATPase Pumps Ca 2+ into the Sarcoplasmic Reticulum

in Muscle Cells

Eukaryotic cells maintain very low concentrations of free Ca 2+ in their cytosol

(~10 –7 M) in the face of a very much higher extracellular Ca 2+ concentration (~10 –3

M). Therefore, even a small influx of Ca 2+ significantly increases the concentration

of free Ca 2+ in the cytosol, and the flow of Ca 2+ down its steep concentration

gradient in response to extracellular signals is one means of transmitting these

signals rapidly across the plasma membrane (discussed in Chapter 15). It is thus

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