@CowperKettle Seaweed grows in the sea, far far away from the center of a continent.
The ocean is a thousand miles away from me here.
This is very different from growing up half an hour to the west of the coast of Lake Michigan, with its access to world shipping. And seaweed. :)
Plus the western part of the state is delimited by the great river of our continent down which countless barges move inexorably towards the Gulf of Mexico.
It is a wetter place than here in the landlocked intermountain west.
> Denver appears to be leading a heartland trend toward creating ersatz oceans. About 400,000 people, or 1 of 5 residents of greater Denver, are expected to swim, sun and play this summer at Water World, which calls its latest attraction the Colorado Wave, ''the world's first dual ocean wave surfing simulator.''
We have a beach, just no waves: it's called Great Sand Dunes National Park. :)
But every lake and river and reservoir provides ample shoreline for a "beach".
You just can't get around the area by travelling anywhere and everywhere by canoe the way the early French explorers did in the Great Lakes region.
Yekaterinburg is also high on a dry steppe, just as Denver is. It receives only 23 annual inches of rain, although that's more than Denver or Boulder by a several inches.
@DannyuNDos Little seaweed is to be had high on the dry steppe a thousand miles from the sea.
You might as well ask a dweller in the Gobi desert of Mongolia about their seaweed experiences. :)
That being said, seaweed is technically an alga. I believe many surprising microörganisms lurk within the drylands' cryptobiotic crust or as "desert varnish".
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Biological soil crusts are communities of living organisms on the soil surface in arid and semi-arid ecosystems. They are found throughout the world with varying species composition and cover depending on topography, soil characteristics, climate, plant community, microhabitats, and disturbance regimes. Biological soil crusts perform important ecological roles including carbon fixation, nitrogen fixation and soil stabilization; they alter soil albedo and water relations and affect germination and nutrient levels in vascular plants. They can be damaged by fire, recreational activity, grazing and...
It looks dead. It is not. But if you step upon it your murderous footprint lasts a century before it has restored itself.
> Cyanobacteria are the main photosynthetic component of biological soil crusts,[2] in addition to other photosynthetic taxa such as mosses, lichens, and green algae. The most common cyanobacteria found in soil crusts belong to large filamentous species such as those in the genus Microcoleus.
Cyanobacteria being the microörganism sometimes referred to as blue-green algae.
So yes, green algae do grow there as well. It's not especially noticeable to the casual observer.
> Green algae in soil crusts are present just below the soil surface where they are partially protected from UV radiation. They become inactive when dry and reactivate when moistened. They can photosynthesize to fix carbon from the atmosphere.
That's the closest we get to seaweed around here. :)
> Biological soil crusts are also known as biocrusts or as cryptogamic, microbiotic, microphytic, or cryptobiotic soils.
"Hidden life" for the ungreekly version.
Why does science love Greek so much?
> Biocrust is poikilohydric and does not have the ability to maintain or regulate its own water retention.
Adjective: poikilohydric (not comparable)
- (biology, of a plant) Having no mechanism to prevent desiccation
"Desiccation" not drying out. "Mechanism" not way. "Prevent" not stop or forestall.
Stripped of its Classical words, English would be a much shorter language to write in. :)
This must be so hard for non-Indoeuropeans trying to learn English. They can't see the double layering.