In a survivorship curve, a type i species, like a human or elephant, is a species that has

I chose to discuss the life history of the cheetahs on the Serengeti plains of Tanzania.

In the Serengeti National Park in Tanzania, female cheetahs occupy larger areas and the males are usually found in small territories. A trait in the life history of the male cheetahs is that they compete fiercely for their territories. However, the males do not survive as long as the females. Cheetah cubs have a high mortality rate because most of them fall prey to predator lions. During their life span, adolescent cheetahs live in temporary sibling groups. These cheetahs survive longer than the ones that are single offspring. After leaving their mother, adolescent male and female cheetahs stay in a group for about six months. After a period of six months, the females leave the group, and the males stay together. Female cheetahs prefer to live alone or with their cubs. The males prefer to live alone or with two or three other cheetahs.

Based on the life history of cheetahs, I think they would have a type II life history curve. They are not type I like humans because many cheetah cubs are killed and don’t survive to adulthood. They are not type III like sea turtles and oysters, because cheetah cubs are protected by their mothers, and adolescent cheetahs live in groups for protection, so more than a tiny fraction of cheetahs survive to adulthood.

Explanation:

answer: like 2%?

explanation:

a fossil fuel is a fuel formed by natural processes, such as anaerobic decomposition of buried dead organisms, containing energy originating in ancient photosynthesis.[1] the age of the organisms and their resulting fossil fuels is typically millions of years, and sometimes exceeds 650 million years.[2] fossil fuels contain high percentages of carbon and include petroleum, coal, and natural gas.[3] other commonly used derivatives include kerosene and propane. fossil fuels range from volatile materials with low carbon to hydrogen ratios like methane, to liquids like petroleum, to nonvolatile materials composed of almost pure carbon, like anthracite coal. methane can be found in hydrocarbon fields either alone, associated with oil, or in the form of methane clathrates.

the theory that fossil fuels formed from the fossilized remains of dead plants by exposure to heat and pressure in the earth's crust over millions of years was first introduced by andreas libavius "in his 1597 alchemia [alchymia]" and later by mikhail lomonosov "as early as 1757 and certainly by 1763".[4] the first use of the term "fossil fuel" was by the german chemist caspar neumann, in english translation in 1759.[5]

in 2017 the world's primary energy sources consisted of petroleum (34%), coal (28%), natural gas (23%), amounting to an 85% share for fossil fuels in primary energy consumption in the world.[6] non-fossil sources in 2006 included nuclear (8.5%), hydroelectric (6.3%), and others (geothermal, solar, tidal, wind, wood, waste) amounting to 0.9%.[7] world energy consumption was growing at about 2.3% per year. in 2015 about 18% of worldwide consumption was from renewable sources.[8]