Oparin believed that there was one molecule lightning strike and then the gases developed
energy from the sun,lightening,earths heat triggered chemical reaction for the early gases of the earth combined
Early volcanoes discharged different combinations of gases into the Earth's atmosphere creating rain, which cooled the planet and formed solid land masses, and every other element discovered presently.
They look at the mineral composition of the rocks. There are some minerals that can only form in the presence of oxygen.
What happened to all the water vapour in the early atmosphere
Carbon doixide
Oparin's hypothesis suggested that early Earth's atmosphere lacked free oxygen. Instead, it consisted of gases like methane, ammonia, hydrogen, and water vapor.
Oxygen
( h2; ch4; nh3)
It is believed that the early Earth's atmosphere did not contain significant amounts of oxygen. Oxygen began to accumulate in the atmosphere around 2.4 billion years ago due to the emergence of photosynthetic organisms.
Oparin's hypothesis proposed that the early Earth's atmosphere consisted of gases such as ammonia, methane, water vapor, and hydrogen, with little to no oxygen. These gases were thought to have been involved in the synthesis of organic molecules that led to the origin of life.
oxygen
One thing that is true in the Oparin - Haldane theory is that the early earth used to consist of an atmosphere which carried ammonia and water vapor. This is true because that is a condition that allows biological polymers to thrive.
He thought that the early Earth's atmosphere contained ammonia, NH3; hydrogen gas, H2; water vapor, H2o; and compounds made of hydrogen and carbon, such as, CH4.
oxygen
nitrogen
Oxygen (O2) was not present in early Earth's reducing atmosphere. It only became abundant in the atmosphere due to the photosynthetic activity of cyanobacteria and other early organisms.
photosynthetic organisms, like cyanobacteria, which produced oxygen as a byproduct of photosynthesis. This led to the increase in atmospheric oxygen levels, changing the composition of Earth's early atmosphere.