Two ways that carbon can get from the ocean to the lithosphere

1. Burning of fossil fuels.

Under natural conditions the release of carbon from fossil fuels occurs slowly, as they are sub ducted into the mantle, and CO2 is released through volcanic activity. However, humans are heavily reliant on fossil fuels, and extract it from the lithosphere in great quantities. Put in to fire a coal, oil, natural gas, and other fossil fuels – for industrial movement and power generation for example, neglect the carbon from the fossil fuels and emits it as CO2 into the atmosphere.

2. Land use and land cover change (e.g. deforestation)

Big part of carbon are stored in living plants. Then, land use changes, most importantly the clearance of forests (which are very densely inhabited by plants, and therefore contain a large amount of carbon), can influence the carbon cycle in two ways. Firstly, removing of vegetation will let the plants die which would otherwise be capturing carbon from the atmosphere through photosynthesis. And as dense forests are change by crops/pasture land/built environments, there is usually a net decrease in the carbon store, as smaller plants (and worse still, concrete) store far less carbon than large trees. Deforestation also make much more soil to be eroded, and carbon stored in the soil is rapidly taken into rivers.

Because the nature is in cycle of the carbon cycle, humans are affected and cause the lead to a number of amplifications and feedbacks. Thereby releasing more CO2 to the atmosphere. Increases in global temperature also affect ocean temperatures, modifying oceanic ecosystems and having the potential to disrupt the oceanic carbon cycle, limiting the ocean’s capability to absorb and store carbon.

answer; i believe that the correct answer is (light);

interphase

the period of cell growth when the cell synthesizes new molecules and organelles. the cell is not dividing and it constitutes the majority of the time spent in the cell cycle

prophase

changes occur in the nucleus and cytoplasm. the chromatin condenses to form structures (sister chromatids) visible with a light microscope and the mitotic spindle begins to form, but the nucleus is still in tact

prometaphase

the nuclear envelope fragments and the spindle microtubules attach to the kinetochores of the sister chromatids

metaphase

all the cell's duplicated chromosomes are lined up at an imaginary plane equidistant between the poles of the mitotic spindle

anaphase

begins when sister chromatids separate from each other and ending when a complete set of daughter chromosomes arrives at each of the two poles of the cell

telophase

the daughter nuclei form at the two poles of a cell

cytokinesis

the division of a cytoplasm to form two separate daughter cells. usually occurs during telophase during mitosis. this and mitosis make up to mitotic (m) phase of the cell cycle