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Because, Earth is a huge recycling machine, and there are 3 different types of rock, with different ways of forming and changing.

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Describe many paths a carbon molecule can take through the carbon cycle?

Carbon molecules can enter the carbon cycle through various processes including photosynthesis by plants, respiration by organisms, decomposition of organic matter, combustion of fossil fuels, and diffusion between the atmosphere and ocean. Once in the cycle, carbon can be stored in plants, soils, oceans, and rocks, circulate through food chains, be released back into the atmosphere as carbon dioxide, or become trapped in long-term carbon sinks like fossil fuels or deep ocean sediments.


Who invented the rock cycle?

The concept of the rock cycle was not invented by a single individual, but was developed through the work of many geologists over time. James Hutton, a Scottish geologist, is often credited with laying the foundation for the understanding of rock cycles and earth processes in his work "Theory of the Earth" published in 1788.


If an organism is able to convert the sodium citrate in simmons citrate agar to pyruvate what are some possible reasons why an organism might ferment rather than metabolize it oxidatively in the Krebs?

Citrate, a Krebs cycle (i.e., TCA cycle or citric acid cycle) intermediate, is generated by many bacteria; however, utilization of exogenous citrate requires the presence of citrate transport proteins (permeases). Upon uptake by the cell, citrate is cleaved by citrate lyase to oxaloacetate and acetate. The oxaloacetate is then metabolized to pyruvate and CO2.


How many carbon dioxide molecules are produced in the Krebs cycle?

two :]


What rock cycle process causes many sedimentary rocks to have visible layers?

The rock cycle process that causes many sedimentary rocks to have visible layers is called sedimentation. This process involves the accumulation of sediments, such as sand, silt, and clay, in layers over time. As more and more sediments are deposited and compacted, the layers become more distinct, creating the visible stratification seen in sedimentary rocks.

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