- Jul 2024
-
-
Global industrialized world is doing today on the planet is that it's just so far out of equilibrium and so beyond um the Al operation of the 00:50:27 carbon cycle that it's just completely it's impossible that it will that it will persist um very far into the future
for - climate crisis - reflections - perspectives - human vs deep time
adjacency - between - climate crisis - different perspectives - human vs - deep time - adjacency relationship - Our global industrialized world is perturbing the carbon cycle so far out of equilibrium that the status quo civilization cannot persist very far into the future<br /> - the earth system has been through many such perturbations and it ALWAYS self corrects - Even the most extreme climate events earth has ever experienced are called transient because they are still relatively short in geological time - In the long term, the planet will restore equilibrium no matter how much extreme the perturbations human civilization creates in the next few centuries - In the long term, the earth is going to be fine - Homo sapien is just one of millions of species, most of which have gone extinct - We should NOT feel we are exceptional - We are comparing different timescales: - human lifetimes are measured in a hundred years - earth system time scales are measured in millions of years - even if there were another mass extinction event, on a geological time scale of tens of million years a new biosphere will regenerate and the ocean chemistry will be restored - Here we have an interesting intersectionality of different timescales. - paleontologists provide a deep time perspective - while we humans live in a timescale of no greater than 100 years - our bodies cannot directly sense change in deep time - therefore, any scientific information about deep time will need to go through our cognitive system - Our body is not evolutionarily designed to biologically respond to information on a deep-time timescale - It may be beneficial to help us see from a deep-time perspective to appreciate the geological-scale changes we are responsible for
-