Glycogen reserves can release glucose for cellular respiration. glycogen reserves are typically found in the muscles and liver.
- The liver and muscles contain the body's "quick" source of energy, known as glycogen stores.
- They go through further metabolism after being converted to glucose.
- After that, glucose can be further digested to release energy both aerobically and anaerobically.
<h3>Glycogen reserves: what are they?</h3>
- When the body doesn't need to consume the glucose for energy, the liver and muscles store it.
- This kind of stored glucose, which is made up of many connected glucose molecules, is known as glycogen.
<h3>How long are glycogen reserves good for?</h3>
- Utilizing the form, you can learn more about nutrition and glycogen.
- But it's helpful to know that once glycogen stores are exhausted, it will take at least 48 hours to fully refill them.
- This necessitates rest throughout the recovery period and a high-carbohydrate diet (60–70% of the energy must come from carbohydrates).
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They form an organ
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Answer:
Dodos were flightless birds that have been extinct for about 300 years. Imagine that biologists found two surviving dodos and mated this pair of birds. What would you expect of the resulting dodo population after three generations?
The maximum number of alleles present for any gene in the new population is two
Explanation:
As a result of this mating, in the third generation the maximum number of alleles present for any gene in the new population will be two.
In ecology<span>, a </span>niche<span> (</span>CanE<span>, </span><span><span>UK:</span> <span>/<span>ˈniːʃ</span>/</span></span><span> or </span><span><span>US:</span> <span>/<span>ˈnɪtʃ</span>/</span></span>)[1] is the fit of a species living under specific environmental conditions.
<span>https://en.wikipedia.org/wiki/Ecological_niche</span>
Answer:
Both physical and chemical weathering, along with erosion, can change Earth's surface as physical weathering allows breakdown of rock into smaller pieces, these pieces can be move from one place to another through water, wind or ice (erosion), and when the smaller pieces will settle down at a place, rain water can react with the soil or smaller rock pieces to form rock minerals.
For example: Running water, wind, and rapid heating/cooling allows the rocks to break down into smaller pieces or grains (physical weathering), then the small grains are transported and settled away from the source area through wind or river (erosion), and at the end the surface area exposed to air for chemical weathering.
