Phosphofructokinase-1 (pfk-1) is a large enzyme that catalyzes the phosphorylation of fructose 6-phosphate during glycolysis. in fungi, the pfk-1 enzyme is composed of four alpha subunits and four beta subunits. how would you describe the quaternary structure of pfk-1?

Explanation:

The quaternary structure of proteins describes the arrangement of two or more polypeptide subunits in the space. According to the given information, the enzyme phosphofructokinase-1 (PFK-1) has two different types of subunits namely alpha and beta subunits. A protein with two or more different types of the subunit is said to be hetero-polymer.

There are four alpha subunits and four beta subunits in the protein PFK-1 making a total of 8 subunits. A protein with eight subunits is said to be an octamer. Therefore, the quaternary structure of PFK-1 would include an arrangement of 4 alpha and 4 beta subunits in space.

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]