On Mon, 01 Jun 2015 17:36:11 -0400, jillery <
69jp...@gmail.com>
wrote:
So you're claiming proof through obscurity ?
Well now ... the earth has been "nice" for about 3 billion
years ... not too hot, not too cold, but with little pockets
of extremes that could spawn all sorts of interesting
chemistry.
So who says those alternative threads of life had to take
shape right around the same time ours did ? Seems
like ANY time would be a good time ... 3 billion OR 3
million years ago. If life is something even vaguely
"likely" to take shape then it should have been doing
so quite often - and, as I mentioned, the more 'alternate'
the less competition issues with our thread-o-life.
But, alas, nada.
>> Also, on the question of alternate lifeforms being out-
>> competed .... being 'alternate', ie of significantly
>> different biochemistry, how much competiton would
>> there BE for resources ? Line 'A' and line 'B' could
>> be only partial competitors ... each mostly keen on
>> the kinds of chemicals IT uses.
>
>
>It's not really a question of being out-competed. Lots of systems
>start out with initial diversity, then just by random chance converge
>to one over time, like genetic drift, or the loss of surnames in small
>towns.
I think you're talking about "99% compatible" lines-o-life. Sure,
they COULD merge.
But DNA/RNA isn't the only thing that can be used to store
genetic info, our kinds of proteins aren't the only kinds of
proteins (and proteins aren't the only thing you can make
structure and enzymes from), our phospholipid membranes
aren't the only way to make membranes, chlorophyl isn't the
only molecule that can harvest solar energy ... there's more
than enough "stuff" on this planet to assemble a number of
VERY different threads-o-life ... very incompatible ones.
But, alas, nada.
>But there's also the advantage of CHNOPS chemistry. These are among
>the most abundant elements on Earth. Any life using those elements is
>going to have access to more building blocks in more locations than
>other alternate chemistries. Even where there were local patches
>where some other elements dominated which might have supported some
>other chemical life, that alternate life would simply be outnumbered
>everywhere else. Sooner or later, some CHNOPS mutation would use that
>alternate chemistry and simply overwhelm any previously evolved life
>with its superior numbers.
"Overwhelming" only works well when there's competiton for
the same resources. By your logic there should be only ONE
kind of bacteria in the world ... the fastest-breeding kind ...
which would have overwhelmed all the others aeons ago.
>> Life proliferates, it adapts, it evolves. There are vast
>> numbers of species of OUR kind of life - and over
>> time some DO get out-competed or their ideal
>> environment goes away, but there are always a
>> lot more OTHER species that persist. Your proposed
>> 'alternate' must have been pretty wimpy ....
>
>My understanding is extinction is more a matter of bad luck than bad
>genes.
Typically yes ... although it's hard to tell what genes are "bad"
until you arrive at a particular environmental situation. The
proposed "global warming" is likely to happen faster than
some species can adapt or spawn new species - therefore
they'll die out, some of their genes which were "good"
yesterday suddenly became "bad".
>> It's not impossible that we'd find an 'alternate' thread
>> of life *somewhere* eventually ... perhaps some of
>> the deepest darkest hottest cracks in the crust. There
>> has been a fair amount of sampling and drilling and
>> such however and, so far, nothing found. Maybe they
>> haven't been looking for the right thing ? After all, what
>> does an 'alternate' line look like ? What does it
>> consume ? What does it excrete ? If it's not DNA and
>> a bunch of OUR favorite proteins/sugars/fats then
>> what might they be ?
>
>
>It would be a whole lot easier to reasonably speculate about
>life-as-we-don't-know-it if science had a more complete understanding
>of how life-as-we-know-it got started.
Well, they're working on that ...
I don't expect an *exact* answer, you'd have to be
there to be sure, but just as physics can kind-of
run the universe backwards it's possible to run
genetics/biochemistry backwards to a degree.
That'll give more clues to the chemists who are
working on self-assembling life-like chemical
soups.
And hey, maybe the panspermia people were
accidently right ... earth may NEVER have been
good for the initial creation of life - just for its
subsequent sustenence. The Answer may be
on some other planet that DID have a better
chemical toolkit and environment.
>> There was one horrible horrible global disaster about
>> 600 million years ago ... an upstart multi-colony organism
>> called a "stromatalite" began producing a gawdawfully
>> toxic gas called "oxygen" ... and it killed almost *everything*.
>> Maybe it was worse on your 'alternate' than on our line ?
>
>
>AIUI was a global disaster 600 mya, and there was a geologically
>sudden release of biogenic oxygen into the atmosphere, but those are
>two entirely separate events.
Who says you can't have two disasters one right
after the other ? :-)
>The evidence is that 600 mya, and perhaps other times previously,
>Earth went through the ultimate global cooling, where glaciers formed
>from pole to equator, perhaps covering Earth's entire surface with
>ice. Some speculate this event led to the rise of multicellular life,
>as preserved in Ediacaran fossils
>
>The evidence is that the Great Oxygenation Event happened around 2.3
>bya, resulting from the evolution of photosynthesis in cyanobacteria.
I likely got my timeframe wrong with the oxygen. However
it was a terrible blow to the sulfide-suckin' community.
Lucky there was a LOT of dissolved iron to absorb the
evil oxygen ... slowed things down enough to allow SOME
adaptation/evolution.
>And it's likely there were other global life-threatening catastrophes
>that happened since life evolved almost 4 bya. For example, it's
>estimated that a meteor impact like the one which wiped out non-avian
>dinosaurs hits Earth about once every 100 million years. If so,
>plenty of equivalent-sized asteroids hit Earth since abiogenesis, but
>natural processes have erased any evidence of most of them.
Plenty of disasters ... and while asteroids are spectacular,
maybe the periodic giant-scale volcanic events were even
more disasterous for life - and they lasted a LONG time
compared to one little whack from above.
OTOH ... if you put ego aside, by far the dominant lifeform
on the planet is single-celled organisms - by number,
variety and metric tonnage. So some trees and dinosaurs
dying off *barely* rates a blip on the extinct-o-meter because
almost all life on the planet is microscopic specks in the
ocean :-)