Sunday, July 09, 2023

Century-old mystery of 'Blood Falls' may be solved

Cheryl Santa Maria
Digital Journalist
Published on Jul. 6, 2023
WEATHER NETWORK

The waters under the glacier are home to ancient strains of bacteria that have remained untouched for centuries, potentially providing insight into life on other planets.

In 1911, British geologist Thomas Griffith Taylor discovered a phenomenon in Antarctica that would dazzle and confound scientists for years: a strange waterfall that appeared to be dripping blood.

The water in the waterfall, at the base of a glacier now called, aptly, "Blood Falls" starts clear but quickly turns red.

Researchers have been trying to solve the mystery for more than a century, with a new analysis from John Hopkins providing further insight. The findings appear in the journal Frontiers in Astronomy and Space Sciences.

With the help of sensitive transmission electron microscopes, a research team examined water samples from the falls, detecting "an abundance" of small, iron-laden nanospheres that oxidize, turning the water red.

"As soon as I looked at the microscope images, I noticed that there were these little nanospheres, and they were iron-rich, and they have lots of different elements in them besides iron—silicon, calcium, aluminum, sodium—and they all varied," research scientist Ken Livi said in a statement.

The nanospheres have likely evaded scientists due to their miniscule size and also because it was widely believed minerals were causing the discolouration, not nanospheres.

"In order to be a mineral, atoms must be arranged in a very specific, crystalline, structure. These nanospheres aren't crystalline, so the methods previously used to examine the solids did not detect them," Livi said.

Fueling space exploration

The waters under the glacier are home to ancient strains of bacteria that have remained untouched for centuries, potentially providing insight into life on other planets.

In fact - the renewed interest in Mars exploration is what inspired the recent analysis of the waters at Blood Falls. Researchers wanted to study the water as if it were a Martian landing site.

"What would happen if a Mars Rover landed in Antarctica? Would it be able to determine what was causing the Blood Falls to be red? It's a fascinating question and one that several researchers were considering," Livi said.

While the team solved the Blood Falls mystery, the research revealed the analysis is incomplete - and this is notable had the work been been conducted on a cold planet like Mars, where environmental materials may be nanosized. It suggests that if Martian rovers aren't fitted with all the right equipment, they may miss things when analyzing samples.

In the Blood Falls study, the spectroscopic equipment that found the nanospheres could not travel to Antarctica and was sent to an overseas lab.
Content continues below

"To truly understand the nature of rocky planets' surfaces, a transmission electron microscope would be necessary, but it is currently not feasible to place one on Mars," Livi said.

The Mystery Of Why Antarctica's Blood Falls Oozes Red Has Been Revealed

It's now clear why the glacier waterfall in East Antarctica runs a bloody red.

TOM HALE
Senior Journalist
Published July 7, 2023


Bloody hell! Check out the size of the tent on the left for scale.
Image credit: Peter Rejcek/NSF/Public Domain

When British geographer Thomas Griffith Taylor made his daring venture through East Antarctica in 1911, his expedition stumbled across a terrifying sight: the edge of a glacier appearing to ooze a stream of blood. After a century of speculation, the cause of the Blood Falls has been pinpointed. 

Scientists in the US used powerful transmission electron microscopes to analyze samples of Blood Falls' water and found an abundance of iron-rich nanospheres that turn red when oxidized.

"As soon as I looked at the microscope images, I noticed that there were these little nanospheres and they were iron-rich, and they have lots of different elements in them besides iron – silicon, calcium, aluminum, sodium – and they all varied," Ken Livi, a research scientist in the Whiting School's Department of Materials Science and Engineering at Johns Hopkins University, said in a statement.

Known for its rich red color, iron oxide had previously been a prime suspect in the mystery of Blood Falls. However, this fancy imaging technique has helped researchers get a clearer picture of why its leaking waters are such a vibrant red hue – and why some previous studies have fallen flat.

"In order to be a mineral, atoms must be arranged in a very specific, crystalline, structure. These nanospheres aren't crystalline, so the methods previously used to examine the solids did not detect them," explained Livi.

You might assume its blood-red waters are the most unusual feature of the Antarctic’s Blood Falls, but this geological feature is full of oddities. 

Scientists have found that the red water seeping out of the Blood Falls originates in a saltwater lake that’s lain trapped in the ice for 1.5 to 4 million years. In fact, this lake is just one part of a much larger underground system of hyper-salty lakes and aquifers.

Analysis of the water indicated that the buried bodies of super salty water are home to a rare subglacial ecosystem of bacteria – despite an almost total absence of oxygen. This means the bacteria are persisting for millions of years without photosynthesis and likely sustain themselves through cycling iron from the brine. 

Given these otherworldly properties, scientists believe that Blood Falls could be studied to gain a deeper understanding of other planets elsewhere in the solar system. 

"With the advent of the Mars Rover missions, there was an interest in trying to analyze the solids that came out of the waters of Blood Falls as if it was a Martian landing site," Livi said. "What would happen if a Mars Rover landed in Antarctica? Would it be able to determine what was causing the Blood Falls to be red? It's a fascinating question and one that several researchers were considering.”

The new study was published in the journal Frontiers in Astronomy and Space Sciences.

No comments: