23 January, 1997
From the modern lab in the remote field camp:
Today I checked those rotifers again. I found that some rotifers left in
FLM and filtered lake water, had eaten between 18 and 32 beads.
These rotifers had access to the beads for 24 hours. There were some rotifers
who had eaten no FLMs at all. Should I be concerned about those that
eat nothing? Do I count them in the feeding rate that I calculate? I also
found another interesting thing. I found 6 rotifers who's entire bodies were
glowing greenish, the same color as the FLMs. None of the glowing
rotifers had any beads in their guts. The only place that I find glowing
rotifers is those rotifers exposed to the FLMs. How do I deal with these
rotifers. Have they eaten the beads and excreted them already? What
other questions does this raise in your mind? Send me your ideas.
I have now decided to make some fluorescently labeled phytoplankton and
feed these to the rotifers. Maybe they don't all like to eat latex
beads. I want to find some way to collect more consistent data with
rotifer feeding. SO, I will try the phytoplankton. But that will have to
wait until tomorrow because today I am walking across the Canada Glacier
with the New Zealand moss and plant physiologist people. They arrived at
our field camp yeaterday and will be here for several days.
The hike was really fun. We used crampons and grippers to climb up onto
the glacier. The view from up there is spectacular with as many as 10
glaciers in clear view. The surface is quite smooth and covered with
about 6 - 10 cm of snow. The walking is easy until you hit a patch on
ice where wind has removed the snow. I can see all the measuring stakes
in the glacier as well as the instrumentation for radient energy
measurement. The narrow part of the glacier is about 4 km and the walk
takes about an hour and a half. I am getting all sorts of help from the
three men with whom I am hiking. Since I am a first timer on the glacier
surface, they are all eager to help and explain what needs to be done. We
all carry ice axes and one begins to feel like a real mountineer up
here. The huge granite peaks of a multitude of colors surround us. Many
ice falls are clearly visible. The only thing that interrupts the
serenity is the hum of the onmipresent helicopters. Some of the pilots
like to buzz the "beakers". Beakers are the scientists that they find in
the field. We are no exception.
Once we reach the other side of the glacier, we scramble down the rock
debris and on to the fields of moss and lichen. While there are not many
species, there are lots of plants in the terraine protected from the
wind by the glacier and getting water from melt of the glacier on its
sunny side. Some of the algae are bright green, others are a real yellow.
All of the mosses and lichens are very tiny. I would not have recognized
the moss for what they are without the help of the experts.
The moss scientists are measuring the recovery rates from destruction
that occured from footprints before it was declared a SSSI site. We spent
several hours measuring the growth spread that has occured over disturbed
areas. This site was last measured in 1989. Care musat be taken when
doing the measuring to not cause more damage. When walking in this area,
one can only step on rocks. One's path must be carefully planned.
After doing the science, we hiked back along the face and leading edge of
the glacier. Sometimes this led us onto the lake surface. It has been a
long and interesting day. I heard much about the New Zealander's opinion
about research done by U.S. scientists. They do not have the funding
support nor the facilities that our scientists have. They were quite
pleased to have been invited to stay at our field camp.
Tomorrow I will get back to the rotifers. We are expecting many DVs
including the prime minister of New Zealand and some folks from the
Office of Polar Programs. Busy times here. Study Hard!
Contact the TEA in the field at
.
If you cannot connect through your browser, copy the
TEA's e-mail address in the "To:" line of
your favorite e-mail package.
|