Has anyone ever speculated on what type of vegetation you would have on a thin to very thin atmosphere world? I keep thinking something on the order of Tundra or edge of tree line.
Hadn't yet, so spitballing some ideas...
(All degrees in °C)
first off, a quick google to confirm my understanding that temperature seems to be the primary issue for trees:
Alpine Treelines: Functional Ecology of the Global High Elevation Tree Limits. This document notes that the growing season is primarily based upon soil temps being above freezing... it looks like the annual mean temperature for the treeline is about 6.5°
Also, remembering that water's boiling point correlates to pressure; lower pressure, lower boiling point. 273.16 K at a pressure of 611.2 Pa is the triple point; below that pressure, you only have solid and gaseous states. Standard pressure is 100kPa. Thin is 25 to 75 kPa, and very thin is 10-25 kPa, so we have a liquid water state.
For Very Thin, I find at Engineering Toolbox, roughly 50° to 64° boil, and 0° freeze.
For Thin, about 64° to 92° boil, and a 0° freeze point.
You've got competing size demands:
- minimum surface area for thermo-regulation
- maximum surface area for external respiration
- maximum surface area for solar absorption
- minimum cross-section for wind
If we assume the annual mean temp of 6.5° at 10cm below grade treeline...
We should see some trees or tree-like plants.
A
nasa paper notes that at 0.1 Atm (the lower bound for VThin) terran plants think they're in a drought, no matter how much water there is. So, VT is unlikely to support terran plants without modifications (nor Vland's native life, either. Probably not Zhdantl's, either.)
The Snowline on earth at the equator is about 5500m, so about 50 kPa. Firmly in the middle of the thin type. So we know that Terran plant life can thrive at 50 kPa if the temps are warm enough, even tho' 10 kPa makes them think they're dying.
So, we need plants that respond to daily freeze-thaw cycles, with mean root temps of about 6.5°, and not much above 30° to 45° (vs the 50° of central Australia, which I'm using to set my vertical plant maximum temperature as a ratio of the boiling point).
Which means we need plants that react. Which, itself, is an established fact. It's just not usually profound enough.
If in an area moderated by large bodies of water and/or large thermal mass of heatable stone, the average daily temperature variation can be quite mild. 3° or so.
In areas of dry sand desert, daily temps can range easily 50° at Standard Pressure (100 kPa).
Mars, at 6 kPa mean and up to 13 kPa transient in the depths of the Hellas (11.5 kPa mean) (Seasonal and weather dependent) is low enough to preclude life as we know it, since it's too close to the triple point.
I'm thinking Thin isn't going to be thin enough to matter all that much, except for the variability in temps.
Very Thin, well, my initial run with Grand Survey shows that a size 6 is either going to freeze a couple hours after dark or boil daily at the equator. Tidelocking may in fact be essential to having a stable plant zone in the 6° to 30° range. In which case, think "streamlined" - the winds should be pretty steady, and the tallest plants get more light and have a lower surface area ratio on the non-leaf areas... I think Saguaro Cactus and Palms... on the cold edge. On the hot edge, more updraft, less water, more vertical sun: barrel cacti, grassoids, and dry-mosses.
I'll need to think some more and punch in the formulae for figuring temps to make much sense of the numbers before I can say much more.