Weather:
The clouds are back, but the air temperature is warm (mid- 60's); the seas are
relatively calm.
Science Update:
Today's Objectives:
1) Day 3 of the 5 day "Pressure Dive" with ROV Jason (dive J2-730) to collect
pressure data on a circuit of 10 Benchmarks (green dots on map at right) - in
progress!
Magnetite Producers
One of the challenges of studying microbes and talking about your work with
friends is that microorganisms (by their very nature) are really hard to see!
Dr. Jim Holden of University of Massachusetts at Amherst has a great way to
share his research, or at least to show the activity of the microbes he's studying
at Axial Seamount. Jim determines sites where he wants to collect vent fluids
with the fluid sampler on ROV Jason (below left). The submersible's arm removes
the sampler from its holster on the front payload basket (below center) and
then the submersible's pilot works with Jim to get it positioned exactly where
he wants to collect a sample. Fluid samples are collected in bottles on ROV
Jason until it returns to the surface.
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Sampling microbes at El Guapo Vent (left) in the International Hydrothermal Vent Field (see map above) with the fluid sampler (center). Fluids are collected from the vent and delivered through the metal hose on the left of the device into bags in bottles (right) on ROV Jason. |
Once back on the surface, Jim extracts microbes from the vent fluid samples
and completes several sets of experiments with the samples. One such experiment
is to investigate the byproduct produced when the sample is in the presence
of rust. To maintain consistency of all his experiments, Jim needs the "rust"
component to be standardized so uses the mineral ferrihydrite (a hydrous ferric
oxyhydroxide Fe3+4O6(H2O) see photo below left). He inoculates (squirts) an
aliquot (a portion of the fluid sample) of the vent water sample with the microbes
he's studying into ferrihydrite in solution and lets the reactions proceed.
The results are shown in the image below right in which Jim is holding a magnet
against the test tube to show that the microbes have changed the ferrihydrite
to produce a byproduct, which Jim believes is the mineral magnetite (Fe3O4).
We can't complete the mineral identification on the ship, but similar byproducts
have been produced by this type of hyperthermophilic (an organism that likes
to live at high temperature) microbe in previous work Jim has done in his lab
at Amherst. These kinds of microbes grow optimally at very high temperatures
(between 80-100° C).
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Test tubes used to detect the presence of hyperthermophilic microbes in vent fluids collected from Anemone Vent of the ASHES Hydrothermal Vent Field at Axial Seamount. In both images, the test tube on the left contains the ferrihydrite solution. The test tube on the right in both images is the byproduct collected after inoculation. Note that in the image on the right, a magnet is used to show that the byproduct in the right side test tube is magnetic. |
Test tubes with Jim's samples can demonstrate the presence of hyperthermophilic
microbes in vent fluids collected from Anemone Vent of the ASHES Hydrothermal
Vent Field at Axial Seamount. In both images, the test tube on the left contains
the ferrrihydrite solution. The test tube on the right in both images is how
it looked after inoculation and incubation. Note that in the image on the right,
a magnet is used to show that the byproduct in the right side test tube is magnetic.
So not only has Jim been able to collect and at least partly characterize microbes
at Axial Seamount, he also has an easy visualization to help demonstrate the
activities of those organisms to those of us who can't actually see the microorganisms!