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ATMOSPHERE EVOLUTION

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Parts of the all atmosphere evolution. Complete this phrases.

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PABLO CANDEL GALIANO
PABLO CANDEL GALIANO
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ATMOSPHERE EVOLUTION

Parts of the all atmosphere evolution. Complete this phrases.

PABLO CANDEL GALIANO
1

20% 1%

Atmosphere and how it evolved to be what it is today with a composition of about 80% nitrogen oxygen and all the other gases like carbon dioxide water vapor and the noble gases making up less than .

2

seabed oceans

As the water vapor condensed into liquid water though it formed the and it allowed lots of the carbon dioxide from the atmosphere to dissolve in them where it could go on to form carbon precipitates and then finally become sediments in the .

3

seabed sediment

When they died though they fell to the and became buried in layers of .

4

oxygen photosynthesis

Then a couple of billion years later , algae and green plants evolved and because of all the that they did they decreased atmospheric carbon dioxide levels and increased levels .

5

condensed oceans

Then as the water vapor in the atmosphere if formed the which the carbon dioxide was then able to dissolve in .

6

gasses dioxide billion volcanic

So to quickly recap all of this for the first years , there was loads of activity which produced lots of carbon and a few other .

7

oxygen atmosphere nitrogen

So overall , we now have an made mostly of and .

8

co2 atmosphere atmosphere oxygen carbon plants

To do this we'll take a look at the ball that volcanic activity played to create the early dioxide rich and how algae in then reduced that abundance of and increased the amount of in the .

9

billion theory First years

though we need to say that this is only a theory supported by lots of evidence the fact that has taken place over the past 4 . 6 means that there's not as much as we might like , so he's still considered a .

10

Slowly 2 billion plants 7

The next major change started about . billion years ago . at first as algae began to appear but becoming more rapid as green evolved over the following years .

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