6
$\begingroup$

I'm currently trying to worldbuild a tidally locked planet and I had a question regarding plants and how they might impact atmospheric composition.

Would a tidally locked planet, all other things being equal, have a higher or lower amount of photosynthesis (and inversely carbon dioxide) in its atmosphere compared to a non tidally locked planet like Earth?

Since all the plants are permanently illuminated by a sun that never moves in the sky they should have a higher level of photosynthesis meaning the atmosphere should have an oxygen-CO2 ratio similar to that of Earth or potentially even more oxygen. Despite the fact that only half the planet is covered in photosynthetic organisms.

However if only half the planet is covered in photosynthetic organisms instead of having complete coverage like on Earth that would reduce the total oxygen production capacity of the planet.

Not to mention only the plants in the area directly under the star would be well illuminated, the rest would have to deal with potentially far less light. Leading to an atmosphere with higher carbon dioxide levels than on Earth.

What would the correct answer be?

$\endgroup$
3
  • $\begingroup$ the amount of available sunlight is identical for both. $\endgroup$ Commented yesterday
  • $\begingroup$ I leave it as a comment as I have not enought deep knowledge about it and the resulting answer would be boring or unusable. I wonder if photosynthesis like we know could evolve on such a planet. Photosynthesis suits two purposes, one is to collect carbon to be able to grow, the other is to store energy for the night and winter. But there is no need to collect energy when there is a constant access to sunlight. It might be that there isn't even the requirement to grow if not mainly to be able to collect and store more energy to survive longer. $\endgroup$ Commented 16 hours ago
  • $\begingroup$ Will you say why tidal locking might change anything in your exposition? $\endgroup$ Commented 12 hours ago

4 Answers 4

11
$\begingroup$

It would most likely have less. (I say most likely because until we get better data on tidally locked planets we can only make predictions on how their climate might act.) There would be less photosynthesis not just because half the planet is in darkness, but because much of the daylight side is probably uninhabitable.

Simply put, the areas receiving the maximum amount of light would become so hot that they'd become vast deserts where little or no plant life could survive. The only habitable zones would be a ring bounded on the inside by the hottest areas and bounded on the outside by the night side. Oceans could help mitigate the harsh daylight side but even with them it's unlikely that the brightest areas would develop the same level of biodiversity as the habitable ring.

enter image description here

As an interesting side note, any plants that did manage to survive in the bright areas would probably evolve white leaves to reflect as much light as possible to avoid being scorched.

$\endgroup$
5
  • 2
    $\begingroup$ Re: "the areas receiving the maximum amount of light would become so hot that they'd become vast deserts where little or no plant life could survive" —couldn't you fix that by moving the planet farther out? Then again, that would probably mean less photosynthesis anyway, since less solar energy would be hitting the planet. $\endgroup$ Commented yesterday
  • 2
    $\begingroup$ It could, as could putting the planet around a dimmer star. However, OP stated "all other things being equal" so I assumed earth sized planet at a 1AU orbit around a sun like star. $\endgroup$ Commented yesterday
  • $\begingroup$ Thanks for your answer! What would happen if the "max light area" was over the ocean instead of a landmass? Would that make things more habitable, especially with the potential cloud cover and rain generated? $\endgroup$ Commented 21 hours ago
  • $\begingroup$ @MJ713, Your question poses an interesting conundrum. What would happen as a tide-locked atmosphere bearing plant were moved further from the star? One of the unavoidable results of tide-locking with an atmosphere is the winds pushing the air around the planet. If you moved the planet far enough away to prevent that, then the atmosphere would freeze on the dark side, leaving the planet airless. It's only the constant winds that prevent it from doing so. $\endgroup$ Commented 19 hours ago
  • 1
    $\begingroup$ @BlackCat42 possibly, however I'd imagine the storms rolling off such a large area of high pressure would be of hurricane intensity. Though again this purely speculative as climate modeling is difficult to do, especially for a type of planet that we have no observational data on. $\endgroup$ Commented 2 hours ago
8
$\begingroup$

The availability of sunlight is not the main factor limiting photosynthetic production.

The main number one limitation of photosynthetic production on Earth in the current geological age is the extremely low amount of carbon dioxide in the air. Basically, plants ate it all in the Carboniferous period which ended 300 million years ago.

The number two limitation is the high concentration of oxygen; oxygen is poisonous to the enzymes which work in the photosynthesis process.

The number three limitation is the scarcity of water in a large part of the planet's surface.

The number four limitation is the scarcity of phosphates in the soil in most parts of the world. That's why phosphate fertilizers work so well to increase agricultural production.

The availability of sunlight is only the number five limitation.

$\endgroup$
4
  • $\begingroup$ This leads to the conclusion that a tidally locked planet will have less photosynthesis doesn't it? The depletion of phosphates in photosynthesis on a tidally locked planet would cause it to stall, whereas in a rotating planet, the phosphates and other nutrient minerals rotate in and out of the sunlit zone. This happens on earth, with tropical waters becoming nutrient poor and massive booms in productivity in polar regions in spring as nutrient rich water/land is hit by sun. $\endgroup$ Commented yesterday
  • $\begingroup$ This assumes that this planet would have evolved enzymes that are as easily oxidized as they are on Earth and that phosphates are as scarce on this planet as they are on Earth $\endgroup$ Commented 18 hours ago
  • 1
    $\begingroup$ Take out the Coriolis force, and you lose the mechanism that moves air and water vapor around the world for free. I suspect the tidally-locked planet has no water flowing on the bright side. $\endgroup$ Commented 18 hours ago
  • $\begingroup$ @MindwinRememberMonica: The mechanism which moves air and water vapor around the planet is differential heating. What the Coriolis force does is bend the path of the stuff which is already flowing. (To the right in the northen hemisphere, and to the left in the southern hemisphere.) The Coriolis force is not experienced at all by stuff which is not already moving. $\endgroup$ Commented 6 hours ago
4
$\begingroup$

Probably less photosynthesis (but not necessarily less CO$_{2}$)

Mandatory disclaimer: We know a fair bit about exactly one life-bearing world (Earth) and that world is not tidally locked. So this answer could be significantly wrong.

A problem with a tidally locked world is that while atmospheric action will cause some variation, each area maintains basically the same temperature all of the time. Let's take Earth as an example. If it magically stopped spinning (with everything magically slowed down at the same rate to avoid Earth-scouring winds destroying everything) and became tidally locked to the sun with the Democratic Republic of Congo experiencing permanent midday, then the DRC would attain a temperature close to the boiling point of water and become uninhabitable. Temperatures in Tripoli and Capetown would probably still be above human habitability, but some plants might be able to survive. The survivable land areas for most life as we know it would be parts of Europe, Iran and Iraq. The eastern tip of Brazil, much of India and northern Europe would have a permanent climate equivalent to summer within the polar regions today. (Everyone in the opposite hemisphere - Australia, the rest of the Americas etc - has frozen to death, obviously.) Big chunks of the Atlantic Ocean will have survivable temperatures, but there is unlikely to be much photosynthesis occurring there.

Alternatively, if a spot in the middle of the southern Indian Ocean became the spot with permanent midday, then there is far more land in the mid-to-high latitudes where temperatures are tolerable. This assumes that the vaporised Indian Ocean eventually recondenses and freezes on the cold side of the planet...

A third alternative - the Earth is tidally locked and either is moved into a more distant orbit or a dimmer sun is used. In this case the "permanent midday" area could be inhabitable but it gets much colder as you move further away. Taking the first example - Africa could be entirely inhabitable but southern Europe etc are really cold and eastern Brazil/western India etc are permanently sitting at -40ish temperatures. (Note that tidal locking is pretty unlikely with distant orbits, so a dim-but-massive sun is probably a good idea, though outside the scope of this question.)

Finally, none of this necessarily implies certain O$_{2}$ or CO$_{2}$ percentages. Even if there is lots of area for plants, they do not need to be as efficient in their use of sunlight when it is always "on". On the flip-side, if there are few animals then the O₂ levels could get really high to the point where thunderstorms cause massive fires. The equilibrium has been different at various times in Earth's existence, resulting in e.g. the massive insects that could exist in the Cretaceous with higher oxygen levels.

$\endgroup$
1
$\begingroup$

In my estimation, a tidally-locked earth-like planet would have as much, if not more photosynthesis than Earth itself.

Why would this be, when half of the planet would be in permanent daylight, and the other half would be perpetually dark?

If we were dealing with Earth itself, with its large amount of surface water, we would expect much of that water to evaporate from the daylight side and eventually be deposited on the night-time side, where it would freeze. However, ice is not static, it flows under the impetus of gravity as glaciers, so we could expect melting and evaporation of the glaciers around the twilight edge. While much of that water would eventually end up on the night-time side again, we can expect that some of it will temporarily end up falling as rain on the sunlit side.

Given that the seas on Earth are very deep, we could expect that some of them may reach around the sunlit side, and be deep enough that they don't boil dry, but remain filled with glacial meltwater from the night side and twilight zones.

Then, we can expect that photosynthetic organisms will evolve to be able to live on the daylight side. Why would they not, when there's all that light, all the time? They would have adaptations that would allow them to live in such a hot, low rainfall, permanently sunlit area. Every possible part of the sunlit surface would likely have some photosynthetic organism on it, and seas on the sunlit side would be a soup of photosynthetic organisms

However, the night-time side would be covered in ice. We would not expect much life in that area, and the little that existed would lead long, slow, low-metabolism lives, most certainly with no significant photosynthesis. We might expect under-ice black smokers with chemosynthetic organisms clustering around them, living at a faster rate than the ice-bound organisms on the ice.

So, while only half the planet would have photosynthesizing organisms on it, they would be photosynthesizing all the time, not just half the day.

$\endgroup$

You must log in to answer this question.

Start asking to get answers

Find the answer to your question by asking.

Ask question

Explore related questions

See similar questions with these tags.