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yo what's up in this video we're going
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to have a look at early Evolution so
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thank you for coming back so let's have
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a look at what happened shortly after
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abiogenesis which we met in the last
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video and let's look at a period when
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life was getting a foothold on Earth so
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if there's one thing I can tell you
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about this time period is that there are
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lots and lots of Fairly open questions
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that remain much like those questions
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that we saw when we were looking at a
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biogenesis and the different theories by
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which that may have originated so things
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that I can tell you for sure are the
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life nowaday uses RNA shown on the left
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hand side of this image here and DNA on
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the right hand side of this image as
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informational molecules these are long
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molecules and as I said they are
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generally informational they store
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information for living
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things what happened immediately after a
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biogenesis is still very poorly known
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but what we think may have happened is
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that longer and um increasing numbers of
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molecules were created through the
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evolution of early
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life now um we think that uh simpler
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molecules than RNA that's shown here may
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have been around first for example there
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is a thing called TNA this is uh 30's
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nucleic acid or PNA peptide nucle
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nucleic acid another form of long long
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molecule but with a different kind of
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backbone may have existed before
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rned the evidence for that is is lacking
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um we don't have rocks from this time
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period or indeed any remnants of uh the
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biochemistry of the things that were
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alive in this period to test that idea
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but it kind of as a first principle
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makes sense that we may want to start
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off with a simpler molecule than
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RNA after that however most people do
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agree that there was a period um in
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which life was all RNA based it used
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this molecule uh shown on the left here
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which was we call the RNA world so RNA
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is a kind of like an allinone molecule
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it's it's generally single stranded has
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one backbone as opposed to DNA which has
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two and as well as storing information
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it can catalyze reactions there are
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things called rymes that catalyze
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reactions and this means that rnas have
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the capacity to carry out a wide range
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of important biochemical functions and
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they would have been a very good
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candidate for the earlier informational
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molecules um before the Advent of DNA
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during this time um we think as well as
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having the evolution of RNA after the
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origin of life we would have seen the
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origin of cells to house and prot
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protect genetic
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molecules at some point or also there
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must have been a switch towards DNA as
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opposed to RNA and that kind of actually
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does make a bit again of first principal
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sense RNA is relatively unstable
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compared to DNA for example uh the M you
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know viruses tend to use RNA and there
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could even be a hangover of the RNA
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world one of the reasons you and I um
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get colds many years and indeed why
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covid is kind of moving across the world
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still going into new forms is because
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RNA is relatively unstable so viruses
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mutate relatively quickly that can help
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you uh survive if you're a virus that
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takes advantage I suppose of other um
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cells that do your application for you
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but if you want a
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longstore um repository of your genetic
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information maybe that's not so good and
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so DNA is actually a better solution to
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storing your genetic
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information so that must happened at
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some point after abiogenesis of
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course so by this uh point in kind of
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your your reading and your education you
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may well have come across this idea that
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all life is related and we can place it
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onto a evolutionary tree and this is one
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example of such an evolutionary tree
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otherwise known as a
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cladogram so this is a cogram that shows
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the relationship between all different
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forms of of life just arranged into a
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circle to make it a bit more compressed
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and make make it so I can fit it onto a
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single slide um this shows the
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relationships between all major groups
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of organisms that are alive on Earth
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today if you think about this um kind of
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idea of a tree and implication of that
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and the theory of evolution and
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hierarchical nesting and branching of
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forms is that at some point there must
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have been a population of organisms from
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which everything that is alive today
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descends that's marked by the star on
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this clayr here and this is a thing that
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is called the last Universal common
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ancestor which is often abbreviated to
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Luca as shown here I'm going to be
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saying Luca um for the rest of this
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video because it just makes life a lot
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easier we can tell by looking at what
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all life shares some elements of the bio
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biochemistry of Luca so for for example
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we can say that it must have had
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ribosomes to make protein it probably
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had DNA to store its genetic information
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and it had chromosome something that
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we'll get on to
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later other details such as what kind of
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organism it might have been and other
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elements of its physiology are slightly
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harder to get at but actually this is an
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area of really active research people
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are using the shared genetic Heritage of
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all life at the moment to rebuild a kind
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of a
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an idea of the repertoire of different
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genes Luca might have had and then you
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are using that to say something about
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how it metabolized and so that's a
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really interesting and exciting area at
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the moment and if you want to explore
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this um Tree of Life further you can do
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so at this URL here which I will link to
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um below this video so you can actually
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start explor the inter relationships
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between these groups
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so if we're thinking about life um in
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this tree likee framework and we're
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thinking about what happened after this
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last Universal common ancestor we can
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say that there are three fairly
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fundamental splits in the tree of life
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the pro cariot that's a word that I put
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on the the the bottom here the procar is
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a shorthand term for two of those three
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um uh spits those two two of those
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groups that um represent an early
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branching in the tree of life and those
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proc carats are members of the groups
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the bacteria and the archa these are
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organisms that look like what you can
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see give or take on this slide
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here um 10,000 species of pro cariot
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have been described and these are
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organisms that split by binary fish and
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they just kind of generally pop po a
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clone they are normally smaller than 10
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microns in size um this is a a kind of a
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very simplified diagram showing many of
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the um elements of the architecture of
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their cells that they share their cells
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lack a nucleus or any form of internal
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membrane bound structure those are
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things that we call organel in organisms
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that have them they the um Pro cariot
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these ARA and the bacteria um contain in
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their cytoplasm in the middle of their
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cell uh a single Loop of DNA
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and the differences between those two
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groups of proar the ARA and the bacteria
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um generally revolve around the
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chemistry of their cell wall that
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surrounds the cell and the methods by
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which they synthesize proteins from
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their DNA that process that I talked
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about a couple of videos back now the AR
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include the
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methanogenic um archan the those that
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metabolize methane in anoxic conditions
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and for example the bacteria include
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photosynthesizing cyano
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bacteria so that's a a very very brief
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overview of the pro carots for you so
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it's then um very likely that the
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earliest traces of life on Earth we will
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see in the fossil record probably
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represent a pro cariot grade of
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organization because the other group of
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organisms that includes fungi and
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animals for example we think uh results
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from uh Evolution based on Pro carots
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and of the different procar
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groups and there is a fair amount of
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debatable evidence for traces of life
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from early Earth so a lot of these will
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try and use uh geochemistry of rocks to
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unravel when life may have appeared for
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example that will often include um isot
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isotope ratios of carbon in early rocks
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that are carbon rich and there are even
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papers that kind of talk about potential
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fossils all the way back to 4.2 billion
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years ago I would say that all of those
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need to be very carefully considered and
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more um competing um potential pieces of
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evidence for early over life keep on
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appearing and in all of these there is a
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rich ongoing debate about the strengths
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and the weaknesses of the different
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forms of evidence for early life on
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Earth um I don't have time sadly in this
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lecture to give you chapter and verse on
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all of that so I thought I would finish
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this video by introducing um these
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3.4 billion year old um fossils from a
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place called strell pool in um in
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Australia which I think is arguably the
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best supported evidence fossil evidence
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we have for early life well you can see
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examples um photographs of the
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structures that are found in
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uh uh silicon dioxide Rock from early
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Earth at the top here and in this
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paper all the papers that I have
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reference the bottom here the authors
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even to conduct 3D reconstructions to
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allow us to understand the morphology of
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these structures slightly better and I
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believe that these teams of researchers
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make a convincing case based on both the
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morphology the shape of these structures
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and their chemistry to suggest that
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these May well be the uh reliable early
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traces of a pro cariot type organism and
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the arguments from chemistry surround
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not only chemistry that may reflect um
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their original makeup but help but also
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reflect arguments regarding how they may
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have been preserved in the environment
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in which they were
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living so those are if the um these
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authors are correct those are indigenous
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microfossils preserved within a beach
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rock um dripstone fabric so these could
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be traced the amongst the earliest
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traces of life on Earth that were
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actually preserved in situ from a really
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ancient Beach and I think that's really
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really cool and they're 3.4 billion
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years old so that's still quite old and
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a really nice example of potential
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fossils of early life on
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Earth and that brings me to the end of
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this video so I will see you very
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shortly in the next one take care