Photosynthesis is responsible for lowering the levels of atmospheric CO2 since it is a requirement to make glucose. Cellular respiration produces CO2 as a by-product, so it is responsible for some atmospheric CO2.
Carbon dioxide (CO2) is the atmospheric gas that enables green plants to carry on the process of photosynthesis. Plants absorb carbon dioxide from the air and convert it into sugars and oxygen through the process of photosynthesis.
Respiration, photosynthesis, and decay are key processes in the carbon cycle that regulate atmospheric carbon dioxide (CO2) levels. Photosynthesis by plants and other organisms absorbs CO2, converting it into organic matter and releasing oxygen, which helps lower atmospheric CO2. In contrast, respiration by animals and plants, along with the decay of organic matter, releases CO2 back into the atmosphere. Together, these processes create a dynamic balance, with photosynthesis generally offsetting the CO2 produced by respiration and decay under stable ecological conditions.
The process responsible for removing most of the CO2 from the atmosphere is photosynthesis. During this process, plants, algae, and some bacteria absorb carbon dioxide and sunlight to produce glucose and oxygen. Additionally, oceanic processes, such as the absorption of CO2 by seawater and its conversion by marine organisms, also play a significant role in regulating atmospheric CO2 levels. Together, these processes help mitigate the greenhouse effect and stabilize the climate.
The process of feeding in carbon dioxide, such as through photosynthesis in plants, plays a crucial role in regulating atmospheric CO2 levels. During photosynthesis, plants absorb CO2 from the atmosphere and convert it into glucose, effectively reducing the concentration of CO2 in the air. This natural process helps mitigate climate change by acting as a carbon sink, thus balancing the carbon cycle. Additionally, when carbon is stored in biomass and soils, it further controls CO2 levels by sequestering carbon for long periods.
Plants use water and dissolved minerals from the soil but the majority of the organic material comes from the carbon they fix by photosynthesis from atmospheric CO2
CO2 or CarbonDiOxide
the increased CO2 levels since the destruction of forests will be fixed by photosynthesis
Atmospheric carbon dioxide concentrations fluctuate seasonally due to the natural processes of photosynthesis and respiration in plants. During the growing season, plants take in carbon dioxide for photosynthesis, which reduces the amount of CO2 in the atmosphere. In the winter, when plants are dormant, there is less photosynthesis and more respiration, leading to an increase in atmospheric CO2 levels.
Carbon dioxide (CO2) is the atmospheric gas that enables green plants to carry on the process of photosynthesis. Plants absorb carbon dioxide from the air and convert it into sugars and oxygen through the process of photosynthesis.
Carbon dioxide (CO2) is the atmospheric gas that most directly influences the rate of photosynthesis under optimum light intensity, as it is needed as a substrate for the Calvin cycle, one of the key reactions in photosynthesis. Increasing the concentration of CO2 can usually lead to an increase in the rate of photosynthesis up to a certain point.
Respiration, photosynthesis, and decay are key processes in the carbon cycle that regulate atmospheric carbon dioxide (CO2) levels. Photosynthesis by plants and other organisms absorbs CO2, converting it into organic matter and releasing oxygen, which helps lower atmospheric CO2. In contrast, respiration by animals and plants, along with the decay of organic matter, releases CO2 back into the atmosphere. Together, these processes create a dynamic balance, with photosynthesis generally offsetting the CO2 produced by respiration and decay under stable ecological conditions.
The process responsible for removing most of the CO2 from the atmosphere is photosynthesis. During this process, plants, algae, and some bacteria absorb carbon dioxide and sunlight to produce glucose and oxygen. Additionally, oceanic processes, such as the absorption of CO2 by seawater and its conversion by marine organisms, also play a significant role in regulating atmospheric CO2 levels. Together, these processes help mitigate the greenhouse effect and stabilize the climate.
There would be significantly more CO2 in the atmosphere because plants take in CO2 during photosynthesis and fix the carbon into glucose.
The process most responsible for the increase in early Earth's atmospheric oxygen levels is photosynthesis. This is the process by which plants, algae, and some bacteria convert carbon dioxide and sunlight into oxygen and energy. Over time, the accumulation of oxygen from photosynthesis led to the rise in atmospheric oxygen levels.
The fluctuation in atmospheric CO2 levels throughout the year is primarily caused by the seasonal cycle of plant growth and decay. During the growing season, plants absorb CO2 through photosynthesis, reducing the levels in the atmosphere. In the winter, when plants are dormant and decomposing, CO2 is released back into the atmosphere, leading to an increase in levels.
Oxygen is the atmospheric component chiefly produced by life processes, such as photosynthesis by plants and algae. It is essential for the survival of most living organisms on Earth.
When more than 200ppm of CO2 is added, the rate of oxygen production during photosynthesis may decrease. This is because high levels of CO2 can inhibit the enzymes responsible for photosynthesis in plants, leading to a decrease in oxygen production.