a2.1 origins of cells Flashcards

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1
Q

how was earth formed?

A

earth formed around 4.5 billion years ago when gravity pulled in swirling gas and dust. the earth was compressed by gravity, causing an increase in temperature which caused the proto-earth to become a hot molten mass

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2
Q

what was the atmosphere like on early earth?

A

‘reducing atmosphere’ with higher proportion of reactive gases such as ammonia and hydrogen. there was very little oxygen

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3
Q

what was the temperature like on early earth?

A

it was significantly warmer than today due to heat from asteroid collisions and the formation of the planet

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4
Q

what was the UV radiation like on early earth?

A

no ozone layer to block radiation from the sun so intense UV radiation reached the surface

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5
Q

what was volcanic activity like on early earth?

A

volcanic eruptions released gases (H2O and CO2) into the atmosphere

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6
Q

how did carbon compounds form?

A

various carbon compounds may have formed in hot springs and hydrothermal vents. compounds may have formed in water droplets in the atmosphere, creating an organic aerosol haze. these compounds were then deposited in the ocean by rainfall.
in such a reducing atmosphere, energy from volcanic eruptions and lightning can catalyse the creation of certain basic small molecules of life, like amino acids. once formed, small organic molecules may have been able to spontaneously form polymers on early earth

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7
Q

what does cell theory say?

A
  1. cells are the smallest unit of life
  2. cells come from other/pre-existing cells
  3. all living things are composed of cells
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8
Q

how was spontaneous generation disproved?

A

louis pasteur heated broth in a swan neck flask to kill any microbes. the swan neck flask allowed airflow but prevented microbes from entering. no microbial growth occurred in the broth, which meant spontaneous generation didn’t happen.

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9
Q

why is it difficult to test hypotheses about the origins of cells?

A

it is difficult to test hypotheses about the origins of cells because it happened billions of years ago. well preserved fossils are rare, the methods used to estimate the dates of the first living cells have ranges of uncertainty

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10
Q

what is the evidence for the formation of organic carbon compounds?

A

in 1929, haldane described the pre-biotic ocean as a ‘hot dilute soup’ in which a variety of carbon compounds formed. he assumed that the atmosphere contained water vapour, carbon dioxide and ammonia. he claimed that when UV light acts on this mixture, a vast variety of organic substances are made, including sugars and amino acids

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11
Q

what did miller & urey do?

A

miller & urey tested haldane’s hypothesis about the origin of carbon compounds in the 1950s. they passed steam through a mixture of methane, hydrogen and ammonia. the mixture was thought to be representative of the early earth. electrical discharges were used to simulate lightning. analysis showed a variety of carbon compounds had been produced, including more than 20 amino acids. this showed that it was possible for carbon compounds to form spontaneously on earth before life had evolved.

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12
Q

what are vesicles?

A

vesicles are small droplets of fluid enclosed in a membrane. they are very common structures inside cells and some cells produce extracellular ones called exosomes. vesicles probably played a part in the early evolution of cells because of their non-polar membrane core (phospholipids). the movement of polar molecules into and out of them would be difficult, so they could have developed their own internal chemistry

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13
Q

why is RNA considered the first genetic material?

A

to replicate DNA and pass on genes, enzymes are needed but to make enzymes, genes are needed. at an earlier phase in evolution, RNA may have been the genetic material. it can store info in the same way as DNA but it is self-replicating and can act as a catalyst. some viruses (which are non living) use RNA which supports the theory that RNA could have been used before DNA evolved.

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14
Q

what is the evidence for having a last universal common ancestor?

A

organisms store information in a genetic code made up codons (a sequence of 3 bases). each codon has a specific meaning - an amino acid, a ‘start’ signal or a ‘stop’ signal. different species could use different codes but they don’t - the code is universal. the obvious explanation is that they inherited it from a common ancestor.
similar structures can evolve in organisms that do not have a recent common ancestor (like fish and whales) which is called convergent evolution. however, this is not thought to be the reason for the universal code. the most recent common ancestor to have existed is called LUCA.

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15
Q

what is a stromatolite?

A

a stromatolite is formed when mats of cyanobacteria in shallow sea water trap sediments and secrete calcium carbonate, slowly building rocky mounds over thousands of years

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16
Q

how can we estimate when LUCA was around?

A

palaeontology has provided evidence on evolutionary pathways, so it is an obvious approach for dating the first cells and LUCA. there are relatively well-preserved rocks dating from 3 billion years ago which contain fossil-like structures with isotope ratios that suggest they are the remains of living organisms. the earliest uncontested evidence of life comes from rocks in western australia in which large structures resembling fossilised stromatolites have been discovered

17
Q

what is the evidence for LUCA evolving near hydrothermal vents?

A

although LUCA lived billions of years ago, it’s genetic makeup can be investigated using organisms living today. if an evolutionary tree for a shared gene matches that of bacteria & archaea, we can deduce that a gene has been inherited from a common ancestor of both. using this technique, 355 protein families that are likely to have been in LUCA’s genome have been identified. they are genes needed for anaerobic metabolism and for fixing carbon dioxide & nitrogen. from this, it can be deduced that LUCA live in an environment with high concentrations of hydrogen, iron and carbon dioxide - for example, in and around hydrothermal vents in the oceans.