Atmosphere, but can be composed of different elements.
Mars's atmosphere is composed of about 2.7% nitrogen.
The word is "atmosphere."
Ganymede has a extremely thin atmosphere mainly composed of oxygen however is extremely tenous so there it's almost no air
Yesm Mars has a very thin atmosphere mostly composed of carbon dioxide.
During the Precambrian time, the Earth's atmosphere lacked free oxygen, and the early atmosphere was likely composed of gases such as methane, ammonia, and carbon dioxide. Throughout the Precambrian, there were significant changes in atmospheric composition due to volcanic activity and the evolution of photosynthetic organisms that contributed oxygen to the atmosphere.
The Earth's Precambrian atmosphere was primarily composed of carbon dioxide, methane, ammonia, and water vapor. It lacked oxygen and had higher levels of greenhouse gases compared to the present atmosphere. This environment supported the evolution of early life forms such as bacteria and algae.
During the Precambrian era, the atmosphere was mostly composed of gases like carbon dioxide, methane, water vapor, and nitrogen. There were lower levels of oxygen compared to present-day levels. The lack of oxygen contributed to the different forms of life that existed during that time.
During the Precambrian period, significant changes occurred in the atmosphere. Early in the period, the atmosphere was primarily composed of gases like methane, ammonia, and carbon dioxide with little to no oxygen. But over time, due to the emergence of photosynthetic bacteria, oxygen levels began to rise, leading to the development of an oxygen-rich atmosphere by the end of the Precambrian. This rise in oxygen was a major milestone in Earth's history, paving the way for the evolution of complex multicellular life forms.
Gas was lacking from Earth's early atmosphere in the early Precambrian era because the primitive atmosphere was composed mainly of hydrogen and helium, which were lost over time. The formation of the Earth's magnetic field and the development of the ozone layer prevented the atmosphere from being stripped away by solar winds, leading to the accumulation of gases like carbon dioxide and water vapor over billions of years.
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During the Precambrian time, Earth's atmosphere was mostly composed of carbon dioxide, methane, ammonia, and water vapor. Over time, as cyanobacteria evolved and photosynthesis increased, oxygen began to accumulate in the atmosphere, leading to the Great Oxidation Event around 2.4 billion years ago. This rise in oxygen levels was a major shift that had profound effects on the evolution of life on Earth.
oxygen
About 21% of the Earth's atmosphere is composed of oxygen.
During the Precambrian time, the Earth's atmosphere underwent significant changes. Initially, the atmosphere was mostly composed of gases like carbon dioxide, water vapor, and nitrogen. As photosynthetic organisms evolved, they started producing oxygen as a byproduct, leading to the Great Oxidation Event around 2.4 billion years ago, which gradually increased oxygen levels in the atmosphere. This shift in atmospheric composition had a profound impact on the evolution of life on Earth.
The origin of free oxygen
Igneous rocks can be found in the mountains, which are partially composed of Precambrian plutonic rock.