when Earth was hit my carbonic acids, rocks eroded, and granite, carried by rivers, was released into oceans, at some point CO2 was released into the oceans, and stromatolites formed in shallow seas and absorbed the CO2, eventually it spit out oxygen and after oxygen become to much in the sea it moved into an area of lower concentration outside of the ocean and into the atmosphere
The formation of the oxygen atmosphere on Earth occurred about 2.4 billion years ago during the Great Oxidation Event in the Proterozoic Eon. This period marked a significant increase in atmospheric oxygen levels due to the photosynthetic activity of early cyanobacteria.
formation of ozone
oxygen
Ozone (O3) could not have been present in an early Earth atmosphere because it is a product of oxygen reacting with ultraviolet radiation. Early Earth's atmosphere lacked the high levels of oxygen needed for ozone formation.
21% of the atmosphere is oxygen.
The atmosphere is 79.9% oxygen.
Rising oxygen levels in the atmosphere contributed to the evolution of larger and more complex organisms, as oxygen is essential for aerobic respiration. Additionally, increased oxygen levels also played a role in the formation of the ozone layer, which helped shield Earth's surface from harmful ultraviolet radiation.
Ozone is formed at the top because UV radaitions have converted oxygen into ozone over there. Ozone formation is a chemical process. When oxygen is treated with UV radiations oxygen gets converted into ozone.
Contrary to popular secular belief, tree's don't actually produce the majority of the worlds oxygen, in fact, approximately 91.6% of the worlds oxygen is produced by phytoplankton blooms in the northern hemisphere of the ocean.
cyanobacteria also called blue-green algae is thought to be one of the first ever photosynthetic organism...prior to the evolution of photosynthetic organisms theoxygen percentage of the atmosphere was 0% and as we all know without oxygen (O2), ozone(O3) cannot form, and without ozone there can be no atmosphere. Photosynthetic organisms allowed for the formation of oxygen and brought oxygen levels to the percentage it is today (20% a significant increase from 0%) as a result ozone was able to form and ultimately the atmosphere emerged.
Oxygen in the atmosphere is essential for life on Earth, as it is necessary for cellular respiration in most living organisms. It supports combustion and helps maintain the balance of ecosystems by participating in various biochemical cycles. Additionally, oxygen contributes to the formation of the ozone layer, which protects the planet from harmful ultraviolet radiation.
The natural formation of atmospheric ozone requires presence of oxygen, sunlight, and the presence of pollutants or precursor gases such as nitrogen oxides and volatile organic compounds. These factors initiate chemical reactions leading to the formation of ozone in the atmosphere.