Evolution of the Earths atmosphere Flashcards
how did volcanic activity help develop the Earths atmosphere
- released gases like nitrogen, CO2, methane and ammonia
- released water vapour which, when the earth cooled, condensed to form oceans
what gases were present in Earth’s early atmosphere
- nitrogen
- carbon dioxide
- water vapour
- methane
- ammonia
what proportion of gases make up Earths atmosphere today
- 78% nitrogen
- 21% oxygen
- 1% argon
- 0.04% carbon dioxide and
How did oceans develop the Earths atmosphere
- when water vapour condensed, it formed the oceans
- lots of carbon dioxide was removed from the early atmosphere as some dissolved in the oceans to form a weak acid, and this reacted with minerals in the sea, to form precipitates,
- Over time, this formed sediments of carbonate rock on the sea bed
- some of the carbon dioxide in the sea was used to make corals and shells of organisms such as mussels
- when these died, they formed the sedimentary rock limestone, which also removed co2 from the air
how did fossil fuels and rocks help the development of earths atmosphere
- some of the carbon that algae and green plants took in from the atmosphere and oceans became locked in rocks and fossil fuels after the organisms died
examples of sedimentary rock
limestone
coal
how did oxygen increase
- algae producing oxygen by carrying out photosynthesis
- billions of years later, plants evolved and also started carrying out photosynthesis
- at some point, the level of oxygen reached a point where animals could evolve
when did algae evolve
2.7 billion years ago
impact of the increased level of oxygen
more complex life like animals could evolve
how are sedimentary rock formed
- when plants,plankton and marine animals die, they fall to the seabed and get buried in layers of sedimentary rock, oil and gas, which trap the carbon and help keep co2 levels in the atmosphere reduced
differences between the early atmosphere and atmosphere today
- early atmosphere contained large amounts of CO2, atmosphere today only contains a small amount
- early atmosphere contained very little oxygen, atmosphere today contains a lot
how did algae and plants increase the amount of oxygen in the atmosphere
- around 2.7 bil years ago, algae evolved in oceans, they then carried out photosynthesis, which produces oxygen, and entered the atmosphere
- over the following billion years, plants evolved, this increased the amount of oxygen in the atmosphere, and at some point the level of oxygen reached the point where animals could evolve
features of fossil fuels
- form over millions of years
- non renewable, will eventually run out
how is coal formed
- from the remains of ferns and trees
- if these die in marshy wetlands, they do not decompose, and this can be due to lack of oxygen or acidic conditions
-(These both prevent bacteria from carrying out decomposition) - over time the plant remains are covered with sediment and compressed
- high temperature and pressure create coal
how is crude oil formed
- from plankton which are tiny plants and animals found in the sea
- when these die, they settle in mud on the sea bed
- if oxygen is not present, they don’t decompose
- over time these are compressed by sediment
- heat and pressure then convert them into crude oul