Millions of years ago, there was more oxygen in the atmosphere due to high levels of photosynthesis by ancient plants. These plants absorbed carbon dioxide and released oxygen as a byproduct, leading to higher oxygen concentrations in the air.
Around 2.2 billion years ago, Earth's atmosphere contained very little oxygen, at levels less than 1% of what we have today. This period is known as the "Great Oxidation Event," when early photosynthetic organisms started releasing oxygen as a byproduct, gradually changing the composition of the atmosphere over millions of years.
The Earth's early atmosphere did not contain oxygen until about 2.5 billion years ago. Oxygen was produced by photosynthetic bacteria and later by plants as a byproduct of their metabolic processes. Over time, this accumulation of oxygen led to the development of the oxygen-rich atmosphere that we have today.
Petroleum is a substance formed from the remains of tiny marine organisms that lived millions of years ago. The organisms died and were buried under layers of sediment, where high pressure and heat transformed them into the fossil fuel we use today.
The transition from anoxic to oxic conditions on Earth occurred around 2.4 billion years ago during the Great Oxidation Event. This event marked the significant increase in atmospheric oxygen levels, leading to the formation of an oxygen-rich environment on Earth.
Scientists use various methods to study the similarities and differences in the physical characteristics, genetic makeup, and evolutionary history of organisms that lived millions of years ago and those living today. By comparing fossils, DNA sequences, and other evidence, researchers can trace the evolutionary relationships between different species and determine how they are related to each other over time. This helps us understand the connections between ancient and modern organisms and how they have evolved and changed over millions of years.
About the same. About a half billion years ago it was significantly higher, and more than a billion years ago it was lower, much lower. Before 1.5 or 2 billion years ago there was no free oxygen in the atmosphere, before 3 billion years ago there wasn't any.
Lower .
Lower .
The current oxygen content in the atmosphere is about the same as it was millions of years ago. Oxygen levels on Earth have been relatively stable over long periods due to the balance between oxygen production and consumption by various processes such as photosynthesis and respiration.
There were no cities millions of years ago.
cycads
millions and millions of years ago
it would be around 650 millions of years ago
Ozone is a tri oxygen molecule. It is formed in a natural process by the action of UV light on oxygen molecule. It was formed millions of years ago.
Justin bieber
It took approximately 2.4 billion years for Earth's atmosphere to reach oxygen levels similar to what we see today. This increase in oxygen was primarily due to the photosynthetic activity of early cyanobacteria, which released oxygen as a byproduct.
Nothing. While limestone existed millions of years ago there were no people to give it a name.