i am not sure if it is but i think it it
Through Crebs' cycle in aerobic respiration
Two alternate carbon-fixing pathways used by plants in hot climates are the C4 pathway and the CAM (Crassulacean acid metabolism) pathway. In the C4 pathway, carbon fixation via PEP carboxylase occurs in mesophyll cells, and then the bundle sheath cells carry out the Calvin cycle. In the CAM pathway, plants open their stomata at night to take in CO2, which is stored in organic acids and used in the Calvin cycle during the day.
The Calvin cycle, also known as the light-independent reactions, is the metabolic pathway of photosynthesis in which carbon dioxide is converted into glucose using ATP. This process occurs in the stroma of the chloroplasts.
C3 carbon fixation or the Calvin cycle is a metabolic pathway for carbon fixation in photosynthesis. This process converts co2 and ribulose bisphosphate into 3-phosphoglycerate through the following reaction: 6 CO2 + 6 RuBP → 12 3-phosphoglycerate In C4 , carbon dioxide is drawn out of malate and into this reaction rather than directly from the air. Since every CO2 molecule has to be fixed twice, the C4 pathway is more energy-consuming than the C3 pathway. The C3 pathway requires 18 ATP for the synthesis of one molecule of glucose while the C4 pathway requires 30 ATP. But since otherwise tropical plants lose more than half of photosynthetic carbon in photorespiration, the C4 pathway is an adaptive mechanism for minimizing the loss.
The first stable intermediate in the C4 pathway is oxaloacetate. It is involved in capturing carbon dioxide in mesophyll cells to form a 4-carbon compound, which is then transported to bundle-sheath cells for further processing in the Calvin cycle.
Kreb's cycle
fossil fuels
The citric acid cycle is a cyclic pathway rather than a linear pathway because it is easier to remove electrons and produce CO2 from compounds with three or more carbon atoms that form a two-carbon compound such as acetyl CoA.
no because its online somewhere else
no because its online somewhere else
Through Crebs' cycle in aerobic respiration
Two alternate carbon-fixing pathways used by plants in hot climates are the C4 pathway and the CAM (Crassulacean acid metabolism) pathway. In the C4 pathway, carbon fixation via PEP carboxylase occurs in mesophyll cells, and then the bundle sheath cells carry out the Calvin cycle. In the CAM pathway, plants open their stomata at night to take in CO2, which is stored in organic acids and used in the Calvin cycle during the day.
The Calvin cycle, also known as the light-independent reactions, is the metabolic pathway of photosynthesis in which carbon dioxide is converted into glucose using ATP. This process occurs in the stroma of the chloroplasts.
C3 carbon fixation or the Calvin cycle is a metabolic pathway for carbon fixation in photosynthesis. This process converts co2 and ribulose bisphosphate into 3-phosphoglycerate through the following reaction: 6 CO2 + 6 RuBP → 12 3-phosphoglycerate In C4 , carbon dioxide is drawn out of malate and into this reaction rather than directly from the air. Since every CO2 molecule has to be fixed twice, the C4 pathway is more energy-consuming than the C3 pathway. The C3 pathway requires 18 ATP for the synthesis of one molecule of glucose while the C4 pathway requires 30 ATP. But since otherwise tropical plants lose more than half of photosynthetic carbon in photorespiration, the C4 pathway is an adaptive mechanism for minimizing the loss.
The first stable intermediate in the C4 pathway is oxaloacetate. It is involved in capturing carbon dioxide in mesophyll cells to form a 4-carbon compound, which is then transported to bundle-sheath cells for further processing in the Calvin cycle.
The Krebs cycle is an example of an aerobic metabolic pathway, as it requires oxygen to function efficiently.
The carbon cycle consists of slow and fast pathways for carbon movement in the environment. The fast pathway involves the rapid exchange of carbon between the atmosphere and living organisms through processes like photosynthesis and respiration, where carbon dioxide is absorbed and released within short time frames. In contrast, the slow pathway encompasses long-term processes, such as the weathering of rocks, sedimentation, and the formation of fossil fuels, which can take thousands to millions of years to cycle carbon through the Earth’s systems. Together, these pathways maintain the balance of carbon in the atmosphere and contribute to climate regulation.