How long can a planet sustain life?

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Discussion Overview

The discussion centers around the sustainability of life on a planet, particularly focusing on the long-term performance of the biosphere as a system. Participants explore concepts related to resource depletion, recycling of life forms, and the impact of various cycles such as carbon and oxygen on the viability of life over time.

Discussion Character

  • Exploratory
  • Conceptual clarification
  • Debate/contested

Main Points Raised

  • One participant questions how the biosphere performs over the long term, specifically regarding resource depletion and recycling efficiency.
  • Another participant emphasizes the importance of cycles, particularly the carbon cycle, and raises concerns about potential leaks in these cycles affecting biomass sustainability.
  • There is a suggestion that the carbon cycle may not completely balance, leading to questions about future biomass levels and the ability to sustain life.
  • A different perspective notes that focusing solely on cycles may be too limiting, citing historical examples of life adapting to significant environmental changes.
  • One participant speculates that life on Earth has lasted for about three and a half billion years, but acknowledges that future conditions, such as increasing solar luminosity, could render the planet uninhabitable in about a billion years.
  • Another participant humorously references a specific date as a turning point for life sustainability, indicating a light-hearted approach to the topic.
  • There is curiosity about the potential for new organisms to evolve that could enhance recycling processes, though this is presented as speculative.

Areas of Agreement / Disagreement

Participants express a range of views on the sustainability of life, with no clear consensus on the long-term outcomes or the mechanisms that will govern them. Some ideas are speculative, and the discussion remains unresolved regarding the future of life on Earth.

Contextual Notes

Participants acknowledge the complexity of the topic, including the limitations of current understanding and the speculative nature of modeling life sustainability. There are references to historical events and future predictions that remain uncertain.

stargazer3
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Dear Physics Forums community,

This question has been bothering me for a few days, and I must apologize for the ambiguity of it. I'll try to explain it a little bit. I am not asking when the Sun will expand or the Earth cool down via radiative processes. So what I asked myself was: if you treat all organisms on a planet as a single system, how well does it perform "in the long run"? How fast the biosphere is depleting planet's natural resources? How efficiently all sorts of life are being recycled? If you exclude extintion events caused by asteroid impacts or radiation butsts, how the total biomass vs. time function can look like?

I do realize that these questions aren't very clear, but I don't really expect definite answers. I don't have a good biology background, so it's hard for me to put it all together.
 
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Obviously this is arm chair philosophizing and things are impossible to quantify. Essentialy it's all about cycles and recycling, water cycles, oxygen cycles, carbon cycles. The big question is if all cycles balance or if there are leaks.

Interesting is the big carbon cycle, since the amount if carbon in the biosphere is likely the limiting factor for the total possible biomass. Interesting are the very long cycles, coal forming, rock weathering, but especially oceanic micro organism making carbonate shells, remains of which we see in the white cliffs around the world.

So this seems a leak in the carbon cycle, when carbon reacts with calcium and oxygen forming limestone, calcite etc.

It's not a complete leak as volcanism returns some of that as CO2. So the question is, if this balances and if not, at what (much?) lower level will the cycle eventually balance? Enough to sustain life? Nobody's guess. Even if we could quantify the carbon loss today exactly, we have no idea about future mass flows. But I don't think we have to worry about that for our species.

Just two cents, it may be totally different.
 
Last edited:
Thank you Andre! I was afraid that my question was a total dead-end, but your reply is just what I needed!
 
:smile: You're welcome, I like collecting thank you's :rolleyes:
 
One more thing, burning fossil fuels also implies that we are indeed recycling old and lost carbon for the moment, bringing it back into the biomass carbon cycle.
 
Thinking only in terms of "cycles" is too restrictive. For example, consider what happened to life on Earth when some pesky organism mutated and started doing photosynthesis for the first time.

Most of the previously existing species were poisoned by the free oxygen that was released, but the ecosystem as a whole evolved and carried on just fine in a very different environment.
 
To answer the OP the only thing we can say with reasonable confidence is "about three and a half billion years, at least". We have only educated guesses as to whether life even exists anywhere else, so all the modelling we do - no matter how elegantly constructed - is highly speculative.

My own speculation would be that if it were not for increases in solar luminosity that will render the Earth uninhabitable in about a billion years that we could continue until internal heat stopped powering plate tectonics and the cycling Andre referred to ground to a halt. Still, that should take at least another billion years to prove fatal.
 
It should last until December 21, 2012. After that, all bets are off! :biggrin:
 
It is an interesting thought about burning fossil fuels. I wonder if there could be another pesky organism mutation (hats off to AlphZero) which allows rapid fossil recycling. Or what if we are *interrupts himself* But then again, I plunge into chair philosophizing even deeper. Thanks again.
 

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