@ Omhra
tree rings, rocks, ice and such things, by far do not enable us to know the rather old Earths climate history in detail (less than ever does it include details of potential universal influences to weather and climate, still less understood than anything else). Our limited methods just cover minor local periods. If you take a local record somewhere, you can't say you have found out huge details about the Earths global climate history. Even one million years still wouldn't be enough.
Our few methods can't explain why the climate changes, and what causes ice ages, although politicians, scientists and other people feel able enough to make utterances like "our models are right, it's the real world that's wrong". That's typical human behaviour. Try to know and to control almost everything. But if there is the next hurricane, flooding, earthquake and so on, all we can do is to look a proper Charlie and try to hide like rats, if still possible. But that still does not scrape at our megalomania, which is to think to be the big boss, the center of almost everything around us.
And if we can't stop global warming because we don't like the ideas global warming generates in some people minds, well, then we simply will colonize the whole universe and escape sometime in the future. Because there is no doubt that we insignificant creatures can do everything...
Tree rings give you a very accurate year per year idea of short term 50-1000 years trend, depending on the length of the life of this tree and/or when the
remains were found.
Rocks and Ice and such things are not the same things...
Rocks are made under many different conditions... a basalt is not the same as sedimentary rock for instance. A basalt will under proper interrogation take you back to several hundred million years when it emerged from its parent volcano/lava flow.
IT and
where it is (what other "such things" surrounds
it) begins to tell the story of how
IT got there. A basalt in mud means it got carried there lets say.
Sedimentary rock is like a million little rocks all packed together with all this information. Like; what compounds and how much of them. What chemistry have these been exposed to... What reactions occurred... AND its Half life... How long have they been in this "present" form. Every atom has a half life... It obviously takes volumes to explain, so I will summarize to this: If you have a bunch of like atoms they will decay at very well established patterns. This decay, incidentally, keeps the mantle of the Earth molten Which in bulk resets the properties of individual compounds.
In other words (very succinct words) once a compound surfaces its half life clock begins to tick.
With this info we can tell when a geode was made. And what reactions it has undergone.
As this sediment accrues there will be pollutants that are not of "rock" origin...
such as shells, bones, aunt sally, and assorted biomass...
So its all
CORRELATION....
What is
where with
whom and for
how long?... That is the story told from Rocks and their "such".
NOW.
ICE... water evaporates, drifts and becomes to cold to remain air free and so it freezes and agregates... as it does this it traps in its blocky cells gas (and dust [little little rocks]) present at the time it froze. Gases and dust are elements/compunds and they
too suffer from half life... but that not being enough the ice behaves similar to all sedimentary formations... And it creates layers...
These two methods alone allowes us to see several million years back with very high presicion and 10s of millions years back with a
considerable (means you have to be careful not to over or under estimate) marign of error and100s of millions back with some worth of measure.
So I guess for some this means that we know NOTHING because we don't know EVERYTHING... but those two terms are impossible to equate...
NOTHING is not the same as EVERYTHING and that is why your argument falls apart Moon walker.