Posts tagged Antarctica

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Around Mac-town

Getting supplies at the Berg Field Center

Getting supplies at the Berg Field Center

We are now fully packed and our mobile research sled is ready to go. We are waiting for some final repairs on the Pisten-Bully which will pull our supply sled. The mobile laboratory sled will be pulled by the Sno-Cat Tucker, which also has cab space for six (riding in the mobile lab would probably be too bouncy). At 8:30 this morning I went to the Berg Field Center (BFC) to plan out all the food for the expedition. The BFC is well stocked, and I I was able to find lots of high energy food: pasta and sauces, rice pilaf, couscous. I also went heavy on the snacks, as you can’t have too many calories when you are living on the sea-ice: cookies, crackers, granola, Cadbury bars, energy bars, gorp, you name it! Most importantly I picked up a bunch of hot drinks and instant soups, as a cup of tea or a bowl of soup can really make a difference in keeping you warm.

Comfort Zone: the upstairs loft of the Berg Field Center

Deep in the Comfort Zone: the upstairs loft of the Berg Field Center

After packaging all of our food I went over to the equipment loft and picked up extra camping equipment. We will be sleeping on the ice, so I grabbed some extra mattress pads, and also found some low-profile tents which (hopefully) won’t blow away in the wind. The equipment area really is an oasis: the staff are super organized and friendly, and there is always great music playing. And it smells of wood (most of McMurdo Station generally smells more like machinery).

A pile of Nansen sleds next to the Berg Field Center

A pile of Nansen sleds next to the Berg Field Center

As I was leaving the Berg Field Center I saw a pile of old Nansen Sleds. I always associated Fridjof Nansen with the Nansen Bottle, which is arguably one of the key inventions of modern oceanography - I didn’t know about the sled. Nansen was a colorful explorer and inventor, and his Wikipedia entry is well worth a read. Unfortunately we won’t be using the Nansen sleds… maybe next trip.

The only espresso in town: the McMurdo Coffee House

The only espresso in town: the McMurdo Coffee House

Much of the rest of the afternoon was spent running errands around McMurdo, or ‘Mac-town’: I filled our water carboys, went to the gas station and filled 10 jerry-cans with 50 gallons of fuel, and shuttled science gear down to the sled using a borrowed truck. I’m getting to know McMurdo better, and by walking around so much, I find all kinds of interesting places. On the right is the McMurdo Coffee House, the only place in town to get an espresso. The coffee house is a great place to come in from the cold, especially when you are waiting for the science delivery truck to free up so you can borrow it again.

Church of the Snows

Church of the Snows

McMurdo has all kinds of amenities: there is a radio station, a barber shop, a store, two bars, library and a post office. There is a church (pictured on the left), a gym, and there was even a bowling alley (it was structurally unsound and had to be closed). For entertainment there are classes, clubs, and movie nights. Every Wednesday and Sunday there is a science lecture series, and anyone can go and hear about all of the interesting science which goes on in Antarctica.

Well, I will sign off for now. Tomorrow morning we will begin our trek across the ice, and I should get some sleep and be fresh for the day. Our router and internet antenna were installed this afternoon, so my next posting should be from somewhere on the McMurdo Sound sea ice. Tomorrow’s forecast: mid-teens, light snow, reduced winds. Great weather for phytoplankton research!

Ice diatoms!

Last-minute adjustments to our mobile science sled

Last-minute adjustments to our mobile science sled

Today has been a day of preparations, as tomorrow we hope to leave McMurdo Station and head out on the sea ice. Our mobile sled is almost ready for deployment: the carpenters who work for the US Antarctic Program are quite amazing, and our sled has filtration racks for separating different sizes of plankton, incubation chambers, and a mobile clean room for trace metal analyses. All of this in a 6 x 12 foot space! I’ll have more photographs in the posts to come, but it very much a sled of the 21st century.

Dawn and Abigail check out the row of Scott tents available for check-out at the Berg Field Center

We are also assembling our equipment list for camping on the ice, and the list is impressive: tents, coleman stoves, fuel, kitchen boxes, ice screws, shovels, jerry cans, carabiners, spare sleds, and a hurdy gurdy. Don’t ask me what that last thing is, I’ve been told it is a ‘fuel transfer unrelated to the musical instrument. The place to get all of these items is the Berg Field Center, which is a storehouse of mountaineering and back-country equipment available to all scientists doing Antarctic field work. For someone who likes mountaineering as much as I do, visiting the Berg Field Center is like letting loose a kid in a candy store - the place just oozes exploration.

Dawn and Mak learn about drive belts

Dawn and Mak learn about drive belts and engine parts

In the afternoon our group attended a class on snowmobiles use and maintenance. Our research sled will be pulled by a Tucker Sno-Cat, and our lighter open-air equipment sleigh will be pulled by a Pisten Bully. Both of these machines are major workhorses in and around Antarctica, but they are slow: the Pisten Bully moves along at 6 mph. So for added flexibility we decided to bring along a pair of snowmobiles. With snowmobiles, we will be able to ride ahead and scout for hazard on the ice, as well as run back to McMurdo to pick up extra equipment or drop off samples. Driving a snowmobile is similar to riding a motorcycle, although the snowmobile doesn’t have any real gears, and snowmobiles reek of partially burned fuel (dirty two-stroke engines). As part of our training we ran a mogul course, and learned how to ride on ice and on slopes, and now I understand we are all certified ‘snow machine technicians’.

Diatoms growing in the ice

A layer of plankton growing in the sea ice

Hard to believe, but in between training sessions and lab set-up, Dawn has been able to have a look at some of the diatoms that Abigail and I brought back from our sea-ice training (see yesterday’s blog). On the right is a picture of a piece of ice from one of the holes we drilled when we were determining the thickness of the ice in cracks, and you can see that there is layer of ice discolored with pigment. These are microscopic plankton living in the ice, and for something non-mobile, living in the ice is ideal in some ways. Plankton embedded in the ice are protected from being eaten by krill and other grazing zooplankton, and ice plankton are also at the top of the water column, so they receive maximal sunlight. We transported our samples of ice back to the lab, and Dawn was able to put them under a light microscope with a camera attached and generate this picture:

Ice Diatoms: chain forming Fragilariopsis (center), ribbons of Amphiprora (squares with oval centers), and colonies of Nitzschia (long ovals growing end-to-end)

These are all diatoms, and not only could Dawn identify all of them without a guide, she could correctly spell them. Diatoms are glass shelled plankton famous for having some of the most beautiful patterned shapes in the ocean (see an SEM image here to get the idea). Diatoms play a vital role in the global carbon cycle, as the they remove large amounts of carbon dioxide from the atmosphere before dying and sinking to the bottom of the ocean. Large blooms of diatoms and other plankton may ultimately help remove much of the greenhouse gasses resulting from fossil fuel use, and is only one of many reasons why we are down here studying them.

Sea-ice class

Our Hagglund for sea ice training was named MOONRAKER

"Moonraker" was the Hagglund we drove onto McMurdo Sound for measuring sea ice

Today Abigail Noble and I took a Hagglund transporter out onto the Ross Sea to learn the basics of sea ice safety and ice dynamics. The sea ice on McMurdo Sound can be 2 meters thick, but this ice is constantly changing, and when you drive along its surface, you can’t assume that it is uniformly 2 meters thick. The ice near land is called fast ice, and is generally stable, but as you move further out into the Ross Sea, the ice transitions into something called first-year drift ice.

Paul, our instructor, points out a meter-wide crack

First year ice is an extremely dynamic environment: big plates of sea ice move about in a shifting pattern of cracks, and these cracks break open, refreeze, and break again, progressively widening. Large cracks can be a serious hazard as you drive across the ice: some cracks are dozens of feet wide, and if the ice is thin in the crack, your vehicle could get stuck — or worse! The cracks are often buried under the snow, but with a sharp eye you can often spot the textural and snow color changes which give the cracks away. See if you can spot the crack in the above photo.

Hand Drills

Michele and our instructor Paul use a hand drill

Once we identified our crack, we set about determining the thickness of the ice at the edge. We started with a hand-crank drill, and surprisingly it took only a few minutes of labor to drill through 72 inches of sea ice. The minimum thickness needed for vehicle travel is 30 inches, so this crack didn’t present any problems for us to cross.

We drove on, and the next major crack we encountered was 15 feet wide, and had multiple zones where it had frozen, fractured, and refrozen again. Because each of the fractures can be of different thickness, the entire width of the crack needed to be characterized.

Abigail breaks out the power equipment!

The rule of thumb around McMurdo is that a tracked vehicle can drive across a crack if the gap to be bridged is less than 1/3 of the vehicle’s length. The Moonraker has a track which is 72 inches long, so we need to make sure that any thin spots in the crack zone were less than 24″ wide. To really drill a large number of holes quickly, out came the power tools. In the picture on the left, Abigail uses a gasoline powered drill to quickly drill a dozen survey holes. The thickness of our 15 foot crack was 80 inches at the edges, but as you progressed toward the center, the crack thinned out to 31″ thick - still thick enough to drive across, but useful information, and you wouldn’t want to proceed across a 15 foot crack not knowing how thick it was in the center. The water which flowed up through the holes we cut in the ice was thick with plankton living just underneath the ice, and we were able to collect a few samples to take back to the lab.

Paul shows us how to set an ice screw

Paul shows us how to set an ice screw.

Our next exercise in class was learning how to fix things to the ice surface - this is especially important for us, as we will be camping on the sea ice for a number of days, and we will need a way to keep our tents and gear from blowing away. Our first demonstration was using ice screws, which are slowly twisted into the ice until they are solidly embedded. The screws have a loop at the end where you can thread a rope or attach a clip. This clip becomes the point of attachment for your tent or equipment.

The Abalakov thread

The Abalakov thread

The problem with ice screws is they heat up in the sun, which melts the ice and quickly loosens the screw. While you can attempt to cover the screws with snow, in windy conditions the snow blows away, as does your tent. Paul showed us a nifty way to use the ice screws to make two holes in the ice, both at 45 degree angles, and the holes meet down in the ice. You can then thread a small piece of rope through the holes and use this rope to tie down your equipment. This is called an Abalakov thread, and will hold down your tent even in the windiest conditions. Very useful information!

On the way back to McMurdo Station we stopped at one of the major features in the McMurdo Sound, the Erebus Ice Tongue, a glacier which starts on the slopes of the Erebus Volcano and flows down into McMurdo Sound, where it floats across the water for 8 miles.

Abigail goes inside the Erebus Glacier through an ice cave

Since the Erebus Ice tongue originates on land, it is freshwater, and like any glacier, it is criss-crossed with massive cracks known as crevasses. We stopped at one of these crevasses which had become an ice cave. The entrance was raised above the sea ice, and we had to slide down into the cave via a long chute. The inside was absolutely beautiful: vapor from the sea ice had recrystallized in the interior, coating the walls and ceiling with what looked to be diamonds. Many of the crystals were hexagonal and the size of a silver dollar, and to me it was like walking about in a hall of jewels. I’ll include a close up at the end of this post so you can see what it looked like.

Tomorrow will be spent gathering provisions and making sure we have all of the right equipment for our trip. Should be busy - we are set to depart across the ice on Wednesday, so keep an eye out for more posts.

A room full of diamonds inside an Erebus Glacier ice cave

A room full of diamonds inside the Erebus Glacier

Happy Camp

That's me pulling a sled into our base camp: 'happy camp'

Our project on the Ross Sea will take us far from heated facilities of McMurdo Station, so all members of our team need to attend “Happy Camp”, a two day course on snow camping and basic Antarctic survival. Happy Camp is held out on the McMurdo Ice Shelf, and it is an immersion program in the true sense of the word: after a brief lecture and inspection of our Extreme Cold Weather (ECW) gear, we were driven out to the ice shelf, where the lectures continued al fresco on the Antarctic ice. There is nothing like the sound of flag markers snapping in the icy wind to keep your mind focused on listening very carefully to everything our instructors had to say. The goal of the first day was to familiarize the group with Antarctic survival basics: providing shelter, keeping warm, and keeping fed and hydrated. The idea was to give a day’s worth of hands-on training, after which our instructors would leave and we would spend the night on the ice.

Brian showing the class how to anchor a Scott tent

The first key item is the need for shelter, and we started with setting up tents and creating wind barriers. The best tent for Antarctic camping was designed over 100 years ago: the Scott tent, a four-sided teepee-like structure which can withstand winds up to 100 mph (most mountaineering tents tend to deform at wind speeds above 50 mph). The Scott tent has a wide skirt, so you can pile snow all around it for extra stability, and the tie downs can be buried deep in the snow - with a well placed snow anchor, the line to the tent will snap long before the anchor pulls out of the snow.

Quarrying snow blocks for our wall

For additional wind shelter we learned how to quarry blocks of snow right from the surface. The snow on the ice shelf is well packed, and it is easy to carve large blocks of snow which felt just like polystyrene, and with them you could create walls and igloo shelters. We also learned how to build emergency snow trenches, which are slots carved down into the snow. Once you have dug down a few feet, a sleeping space is widened at the bottom, large enough to sit up in comfortably and roll around. The top is covered with snow blocks or (in an emergency) an inverted sled. Abigail elected to spent the night in one of these trenches, and she said that it was surprisingly warm and quiet. We also created a 5 foot tall windbreak out of snow blocks - this wall ran between the Scott tents, and kept the icy glacial winds from blowing our gear away.

Michelle fires up a stove in the snow galley

We also used a combination of trenching and snow blocks to create our ‘snow galley’, a temporary kitchen dug down in the snow and out of the wind. You can’t have a campfire in Antarctica, but a hot beverage is the next best thing, and in a survival situation if could save your life. For our evening meal we stuck to the basics: instant soups, noodles, rice and freeze-dried meals - I don’t remember Lipton Cup-of-Soup ever tasting quite so good!

Happy Camp before we retired for the night

Happy Camp before we all retired for the night. Snow huts and snow trenches are still being dug on the left, and you can see the snow wall and the two Scott tents. The flags are so we can find our way around camp in whiteout conditions.

The next day everyone was surprised at how well they slept - no one had any complaints of being cold, and the sleeping bags kept everyone warm. My only mistake was forgetting to bring my toothpaste inside the sleeping bag before I went to bed: it froze solid, and took hours to thaw back into a usable paste.

Learning how to use an emergency HF Radio

The next day we learned how to use emergency communication equipment: VHF hand-held radios and and emergency HF radios. Cell phones don’t work in Antarctica - no coverage - and Iridium satellite phones work poorly near the poles. Handheld radio will work well in the vicinity of McMurdo Station, but if you are deep in the field, the best option is a surprisingly low-tech option: the High Frequency Radio. An HF radio works by bouncing radio waves off the ionosphere, so as long as you know the the broadcast frequency and direction you can trim your antenna and communicate without having line-of-sight ability. Our HF radio seemed like it was from the Vietnam war era, and it felt like we were calling in an airstrike rather than calling the South Pole station and asking about the current weather conditions.

A simulated white-out search and rescue exercise using buckets to limit both vision and communication

A simulated white-out search and rescue exercise using buckets to limit both vision and communication

For our last exercise, we modeled what would happen if weather conditions deteriorated so badly that a white-out occurred. In Antarctica, whiteouts can occur with little warning, and are extremely dangerous, as the swirling snow will drop the visibility to zero, and it is easy to become lost and disoriented. To simulate the experience of trying to find someone in a whiteout, we did the famous bucket-head exercise: we roped up with buckets on our heads and tried to find a person within a few hundred feet of our instruction hut. The buckets are quite effective: you can’t see anything, and your ability to hear and be heard is almost impossible with the wind. Despite the buckets, the wind and the cold, we actually found our person!

So now our group is all certified to leave McMurdo base and camp in the field. The next class on the horizon is sea-ice class, where we will learn how test the strength and thickness of sea ice as we take our sleds out onto McMurdo Sound. That will be tomorrow: until then - keep warm!

McMurdo Station

McMurdo from Observation Hill

McMurdo from Observation Hill

Entering McMurdo is like entering a modern mining town: lots of exposed rock and unpaved streets, above ground utilities and bare-bones architecture. Utilitarian. From the airport we were taken to a briefing room, introduced to our science coordinators, and given our shcedules. Since I am new to McMurdo, I am scheduled for Snow Survival Training, also known as Happy Camp. That will be tomorrow morning. I will also receive training in sea ice travel, as well as how to operate a snowmobile and a pisten bully. All sounds interesting to me, so there should be some good posts in the next few days - stay tuned!

Pressure ridge on the sea ice, Erebus Volcano (with plume of steam) in the background

Pressure ridge on the sea ice, Erebus Volcano (with plume of steam) in the background

After our briefing I picked up linens from the town laundry and checked into the dorm. We are conveniently located in the same building as the dining hall. The downside of this is you can usually smell the tater tots long before they hit the heat lamps. Technically we are not supposed to go into the Crary Lab until we have been certified, so for lack of anything else to do, I grabbed my skis and went out for a short trip on the sea ice. At this time of year the sun never sets, so even though it was almost ten in the evening, it didn’t seem much different than ten in the morning. I skied out on the ice and over towards neighboring Scott Base. The snow on the surface of the sea ice is lightly packed and excellent for cross-country skiing. Along the way to Scott Base was an enormous pressure ridge formed where two plates of sea ice collided. Scale is difficult to see in the above picture, but that ice berm is close to 40 feet tall, and in the background of the photo you can see the snow-covered slopes of the Erebus Volcano.

Weddell Seal sunning on the ice

Weddell Seal sunning on the ice

The pressure ridge creates gaps in the sea ice, andit is through these holes in the sea ice that many of Antarctica’s air breathing animals access the surface. Not far from the base I ran into a Weddell Seal sunning on the ice. It probably helps to have a dark fur coat and a thick layer of blubber! The Weddell seal seemed quite happy though, and we both went on our respective ways. I got to Scott Base just around 11 PM, and realizing I had a tight schedule for the next day, only stayed long enough to grab a photograph and head back to home. Talk to everyone after Happy Camp!

The author with his skis at New Zealand's Scott Base

The author with his skis at New Zealand's Scott Base

Transport to the ice

C-17 on tarmacWednesday morning started with a 5AM taxi ride to the US Antarctic Program’s processing center at the Christchurch airport, where we had to repack our bags and put on our emergency cold weather gear for the flight. Our plane was the C-17 Globemaster III, a large military transport plane more commonly used to deploy troops around the world. The C-17 is the primary wheeled jet aircraft the US Antarctic Program (USAP) uses to cross the southern ocean, and the flight from Christchurch to McMurdo takes about five hours. The other workhorse of the USAP is the LC-130 Hercules, which is a ski-equipped prop plane - flights on the Hercules take 3 hours longer, which makes for a long, rattling flight.

Stripped down interior of the C-17

Stripped down interior of the C-17

The interior of the C-17 is spartan, all wires and insulation, with a few ‘aircraft-style’ seats in the center and jump-seats along the walls. There are no windows, and it is loud, so I wore earplugs most of the time. Unlike most flights though, you can wander up to the flight deck and see the view from the cockpit. As we approached McMurdo Station, I went up and checked out the pack ice conditions on the Ross Sea, and I could clearly see the dimensions of the polynya off of our sampling are near Cape Royds. I could also see the Erebus Volcano steaming away in the background.

C-17 on the sea-ice runway, McMurdo Station

C-17 on the sea-ice runway, McMurdo Station

There are three runways available for use at McMurdo, depending on the time of year and on your aircraft. We landed on the sea ice runway, which is available through late spring when the sea ice gets too thin to support a three hundred thousand pound aircraft. For ski-equipped aircraft there is Williams Field, which is a snow runway. Williams field is actually on the Ross Ice Shelf, so the ice there is a hundred foot thick floating glacier covered with a layer of insulating snow. The third runway is Pegasus Field, a white-ice runway located some distance from town.

The Delta: large tire transport to McMurdo

The Delta: large tire transport to McMurdo

Landing on the ice didn’t seem much different than landing at Lindberg Field in San Diego, which really boggles the mind, as I still have no idea how we actually came to a stop. But the door opened up and there we were in the bright Antarctic afternoon. The weather was cold and windy, but the sunshine felt great. We were loaded into a large tire vehicle known as a Delta and driven across the ice, up the hill, and into McMurdo, known locally as Mac-town.

Polynya opens in the Ross Sea

A helicopter pilot recently sent us an image of the area we are planning to sample, and the stable sea ice we intended to use as a platform for drilling and sampling is now a giant stretch of open seawater!

A polynya opens up in McMurdo Sound, October 2009. In this picture, Cape Royds is in the background, and Stations 7 & 8 are to the left of the ice line, in open water

A large opening like this is a polynya, a term borrowed from the Russian meaning ‘little field’. Polynyas are areas of open water surrounded by sea ice, and can range in size from hundreds of meters to hundreds of square miles. The type of polynya you see in the above picture is a latent heat polynya, and is actually not caused by warming and melting of the ice, but rather by the intense winds which funnel down off the Antarctic ice sheets. These winds are called katabatic winds, and in Antarctica they are formed when cold dense wind drains off high altitude polar ice cap and blows offshore, sending pack ice out to sea and creating large patches of open water. The average elevation of the Antarctic polar ice cap is 10,000 feet, so as rivers of cold dense air sink off the ice cap and down to the coast they gain velocity: katabatic wind speeds at the continental margin have recorded at almost 200 m.p.h.

Polynyas are highly productive areas of the Antarctic ecosystem. The removal of sea ice exposes water to sunlight, allowing microscopic plants - phytoplankton - to bloom, and it is these microscopic plants which form the base of the Antarctic food chain. Large blooms of plankton attract grazing krill and fish, which are in turn food for Antarctica’s more famous air breathing fauna: seals, whales and penguins. In fact, many mainland penguin colonies are located near places where annual polynyas are known to recur, as there is a guaranteed source of food for the nesting penguins.

Looking back at our original expedition plan, we will probably have to adjust the locations of several of the sampling stations: locations 7 and 8 will have to be shelved, and stations 3 & 4 will have to be moved further south towards the Marble Point Traverse. Still, the size and extent of this year’s polynya should generate some excellent data on plankton dynamics, as well as attract some amazing wildlife, so stay tuned!

Proposed Stations for the 2009 Ross Sea transect

Christchurch, New Zealand

Spring in New Zealand, November 2009

Spring in New Zealand, November 2009

Greetings from Christchurch, New Zealand, the anteroom to Antarctica. My colleagues and I have been here for several days now, running last minute errands, getting equipped with cold weather gear, and waiting for a flight south to McMurdo Station. The flight here was remarkable only in it’s length: Los Angeles to Sydney is a 14 hour flight, followed by a 3 hour transfer to Christchurch. During the flight I think I read everything within arms reach, and now have the Quantas system map completely committed to memory. We lost a day when we crossed the International Date Line, but we also seem to have lost a season or two: when we crossed the equator, we traded our California autumn for a brilliant New Zealand spring. Christchurch has a temperate climate, and I don’t recall being in a place with more rhododendron and azalea in bloom.

Display of Antarctic clothing gear issued to participants

Display of Antarctic clothing gear issued to participants

Yesterday Jeff and I reported to the U.S. Antarctic Programs operation base at the Christchurch Airport and were outfitted with the clothes we will need for Antarctic field work in. At the facility there is a giant display of the types of gear available for check out. Some of the gear is mandatory, and I’m not sure who would turn it down: this includes the bright red expedition parkas and insulated overalls, as well as bunny boots, heavily insulated rubber boots for working on the snow. Other gear is available depending on the particulars of your project, and since Jeff Hoffman and I will be working with cold seawater, we picked up a bunch of rubberized insulated gloves with polypropylene liners.

Expedition clothing window with hundreds of parkas in the background

Expedition clothing window with hundreds of Antarctic parkas visible

Once you have your list of gear items you take it to the supply window of the clothing warehouse, where they issue the correct size and allow you to try everything. It is a bonus not to have to purchase all of this gear for a relatively short trip. After we assembled all of our gear, we were instructed to pack a boomerang bag: the weather in Antarctica changes frequently, and often a flight will have to return back to New Zealand without landing. A boomerang bag is all of the gear you will need in case the flight returns and you can’t access your luggage. The bag contains your survival gear, as well as a spare change of clothes and the all-essential toothbrush.

So now we wait for a flight. The weather has been particularly bad at the South Pole, and so flights to ferry scientists from McMurdo to the Amundsen-Scott base at the South Pole are backed up while the weather clears. Because there are only a limited number of rooms at McMurdo Station, we have to wait until everyone can fly onward to the South Pole before we head down. In the meantime we keep an ear to the ground and wait.

Why Antarctica, and why now?

So why are you going to Antarctica, and why are you going now? A very logical question… basically we are traveling to Antarctica to study microscopic marine plants known as phytoplankton. These organisms range in size from bacteria to diatoms to colonial algae, but all phytoplankton have two things in common: they are small enough to float in the water without sinking, and like all plants, they produce their own food using sunlight and carbon dioxide. They are so small that a cup of seawater may contain a million of them, and because they are at the base of the marine food chain, everything from shrimp to fish to whales depends on their existence as a food source. Phytoplankton are some of the most numerous creatures on earth, and ongoing climate research suggests that these microscopic plants will be the primary sink for absorbing and sequestering excess carbon dioxide greenhouse gasses.

If plankton are everywhere, then why go to Antarctica to study them? Well, it probably comes as no surprise that Antarctic plankton are some of the least studied of all the earth’s organisms, as simply getting to Antarctica is no small feat. But in addition to being one of the least studied environments, polar environments such as Antarctica are among the most endangered: ongoing climate change is affecting the polar regions faster than any other place on the planet, so there is some urgency to catalog what is there and how it is changing, and therefore establish a baseline of fundamental scientific knowledge.

To do this we will be using a number of tools developed for studying organisms which are too small to see. We will go out onto the sea ice and collect samples of water, and in addition to identifying the plankton using a microscope, we will try to identify them by reading and understanding their unique DNA signatures. We will be sequencing both the genes in the plankton, and also the genetic messages, or transcripts, that the plankton are producing. The transcripts are particularly interesting, as capturing them is like intercepting coded messages on what the plankton were doing at the time they were collected. At the same time, other members of our team will be analyzing the protein components of the plankton, and looking to see if the stories told between the DNA sequences and protein identifications match. In the end we hope to gather enough information to assemble a portrait of phytoplankton diversity and function in the Ross Sea.

To wind down this posting, here’s a montage of some of the diatoms we found on last year’s expedition. They really are beautiful!

Diatoms from last year's expedition (Dawn Moran, WHOI)

Diatoms from last year's expedition (Dawn Moran, WHOI)

Trip preparations (inaugural posting!)

Well, we have less than a week left, and we are finalizing and shipping the chemicals and equipment we will need for sampling below the sea ice in the Ross Sea. We have already shipped out several hundred pounds of gear, and more await us in storage down at McMurdo Station in Antarctica. Expedition scientist Jeff Hoffman has already left for New Zealand, and I am still in the process of wrapping up lab work here in San Diego before I fly down to Christchurch, New Zealand and meet up with the rest of the team. I checked the weather on the McMurdo Webcam, and the temperature is well below zero: -13 degrees Centigrade, which is about 8 degrees Fahrenheit. Chilly! So I think I should pick up a few more warm items heading out of town on Friday…

In the posts ahead I will introduce our project and team members and describe what it is we hope to accomplish and why we need to travel all the way to Antarctica to do it. In the meantime I would like to post a satellite image which Mak Saito, our collaborator and co-investigator on this grant, sent to us last month. The satellite image details the various sampling stations we hope to occupy while traversing the McMurdo Sound and southern Ross Sea, and gives you an idea of the scope of our three week project. For the adventurous out there, you can find further images and maps of the area by searching for McMurdo Station in Google Earth.

More posts to follow, so stay tuned!

Ross Sea Stations, November 2009

Satellite image of McMurdo Sound: our proposed sampling stations are in yellow