Timeline Flashcards
Maunder Minimum
The Maunder Minimum, also known as the “prolonged sunspot minimum”- 1645-1715
1965?
James Lovelock works at Nasa as part of the Viking mission to Mars to try and find life = he think its unnecessary because of the composition of the atmosphere (different atmospheres absorb carbon on different wavelengths.
1968 ?
The apollo moon shots
1979?
he Gaia hypothesis, a multitude of closed feedback loops that effect each other.
1981?
Climate Regulation – 1981- that a negative feedback loop could counteract with the sun and therefore keeping the earth warm.
The age of the earth?
The age of the earth is 1/3 of the universe- Earth formed – 4.54 Ba by acceretion from Solar Nebula
Brief Earth History
4.5 billion years of history = the sun was 30% less luminous than it is today= the earth was 33* cooler than it is today = oceans would have been frozen= life would not have been possible at that time= scientist were working out whether or not it was Amino in the atmsphere or a thick carbon blancket like other countries.
= eventually the carbon would have been transported to the earths crust= why did the sun get brighter as there was less carbon in the atmosphere so that life could exist.
4500 mya ?
Earth’s core and crust formed
4400 mya ?
The Earth’s first oceans formed
4.0 BA ?
Hadean earth = didn’t have life on earth – before ffosil proof
3BA ?
Archaean- most primitive life forms + earliest evidence of ff= earleiest evidence of evolution= the imergence of prokaryote cells
3 billion years ago?
emergence of ff by cyanobacteria (blue green algae) – co2 and light to create sugars leading to oxygen= changes the gas content of the atmosphere
2.5 billion years ago ?
fusion of bacterium and archean = eukareotic cell = nucleas and mitochondria
2BA?
Proterozoic , atmosphere is starting to become rich
1500 mya ?
Oxygen began to accumulate in the Earth’s atmosphere.
750-635 MA?
two snowball earths
700 mya ?
Animals started to exist
720 million to approximately 635 million years ago?
Cryogenian Period, second of three periods of the Neoproterozoic Era of geologic time, extending from approximately