Wednesday, March 03, 2010

Blood Falls

Atlas Obscura: This five-story, blood-red waterfall pours very slowly out of the Taylor Glacier in Antarctica's McMurdo Dry Valleys. When geologists first discovered the frozen waterfall in 1911, they thought the red color came from algae, but its true nature turned out to be much more spectacular. Roughly 2 million years ago, the Taylor Glacier sealed beneath it a small body of water which contained an ancient community of microbes. Trapped below a thick layer of ice, they have remained there ever since, isolated inside a natural time capsule. Evolving independently of the rest of the living world, these microbes exist without heat, light, or oxygen, and are essentially the definition of "primordial ooze." The trapped lake has very high salinity and is rich in iron, which gives the waterfall its red color. A fissure in the glacier allows the subglacial lake to flow out, forming the falls without contaminating the ecosystem within.
More @ wiki

2 comments:

annom said...

The microbes do not cause the blood falls or colour, do they? What do they live on?

cybrbeast said...

From the wiki:

"Chemical and microbial analyses both indicate that a rare subglacial ecosystem of autotrophic bacteria developed that metabolizes sulfate and ferric ions.[3][4] According to geomicrobiologist Jill Mikucki at Dartmouth College, water samples from Blood Falls contained at least 17 different types of microbes, and almost no oxygen.[3] An explanation may be that the microbes use sulfate as a catalyst to respire with ferric ions and metabolize the microscopic amounts of organic matter trapped with them. Such a metabolic process had never before been observed in nature."

I think the microbes may be responsible for the soluble form of iron being present.