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  1. Jul 2024
    1. 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