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Delvig [45]
2 years ago
13

When the influenza virus enters into an epithelial cell within the respiratory tract, the infected cell responds by

Biology
1 answer:
Lena [83]2 years ago
8 0

When the influenza virus enters an epithelial cell, the infected cell responds by posting antigens and acting as a flag for cytotoxic T cells.

<h3>What is the cell-mediated response?</h3>

The cell-mediated response is a type of immune response where the organism is able to respond to pathogens by immune cells.

Macrophages (as well as other immune cells ) can act during cell-mediated immune responses.

In conclusion, when the influenza virus enters an epithelial cell, the infected cell responds by posting antigens and acting as a flag for cytotoxic T cells.

Learn more about cell mediated responses here:

brainly.com/question/24378503

#SPJ1

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Answer:

Hydrogen

Explanation:

Hydrogen is the only nonmetal in group 1, therefore it is the only element in group 1 that forms a covalent bond.

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What are convergent boundaries?
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Answer:

Explanation:

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Plate tectonics is driven by convection cells in the mantle. Convection cells are the result of heat generated by radioactive decay of elements in the mantle escaping to the surface and the return of cool materials from the surface to the mantle.[2] These convection cells bring hot mantle material to the surface along spreading centers creating new crust. As this new crust is pushed away from the spreading center by the formation of newer crust, it cools, thins, and becomes denser. Subduction begins when this dense crust converges with less dense crust. The force of gravity helps drive the subducting slab into the mantle.[3] As the relatively cool subducting slab sinks deeper into the mantle, it is heated, causing hydrous minerals to break down. This releases water into the hotter asthenosphere, which leads to partial melting of asthenosphere and volcanism. Both dehydration and partial melting occurs along the 1,000 °C (1,830 °F) isotherm, generally at depths of 65 to 130 km (40 to 81 mi).[4][5]

Some lithospheric plates consist of both continental and oceanic lithosphere. In some instances, initial convergence with another plate will destroy oceanic lithosphere, leading to convergence of two continental plates. Neither continental plate will subduct. It is likely that the plate may break along the boundary of continental and oceanic crust. Seismic tomography reveals pieces of lithosphere that have broken off during convergence

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Answer:

Here are several things you can do!↓

Explanation:

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Here are some of the differences I find  

Explanation:

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The red arrows in the diagrams below point to these structures in animal and plant cells.

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