Partners:
Focus On:
What is IPY
Popular Tags
IPY Search
IPY Blogs
By Jan Strugnell, British Antarctic Survey
I am a molecular phylogeneticist at Cambridge University (funded by a Lloyd’s Tercentenary Foundation Fellowship) and I am investigating the molecular evolutionary history of Antarctic and deep sea octopus. I am therefore on board to sample any octopus we catch in our trawls for later DNA sequencing and also to preserve them for later investigation and identification. Specifically I am using octopus as model organisms to test the hypothesis that the Antarctic has acted as a centre for evolutionary innovation and radiation and as a source of taxa that have invaded the deep sea. I am also interested in investigating how past glaciation in Antarctica has effected octopus speciation, and also at the effect of the Antarctic Circumpolar...
Published in
IPY Blogs
Tagged under
Photo: Scott Island with Haggit’s Pillar to the left. By John Mitchell
By John Mitchell, Voyage Leader
After completion of the first abyssal station in the northern part of our survey – at a depth of 3500m – we moved on to our last seamount station next to Scott Island. Scott Island is very small (400m by 200m) and isolated, lying about 310 nautical miles northeast from Cape Adare. Its companion – Haggit’s Pillar – is an impressive 62m high volcanic stack sitting 200m northwest of the island. We are sampling in this area to compare the biodiversity with that of the Balleny...
Published in
IPY Blogs
Tagged under
Monday, 10 March 2008 19:29
Professor Huigen Yang: Developing China's Polar Research Capacity
Written by International Polar Foundation
As part of an ongoing coverage of China's IPY Polar research projects and activities, SciencePoles interviewed Professor Yang Huigen, the new Director of the Polar Research Institute of China (PRIC), responsible for carrying our scientific research in the Polar Regions, operating Chinese research stations and vessels, and promoting cooperation with international Polar research organisations.
In this interview, Professor Yang discusses the current upgrade of China's Polar research infrastructure, including existing Chinese research stations in the Arctic and Antarctic, the Chinese ice breaker Xue Long, and the planned...
Monday, 10 March 2008 16:22
FSU IPY Cruise: Meet FSU Professor & Chief Scientist Kevin Speer
Written by CLIVAR Section I6S
Chief Scientist Kevin Speer, geared up for brisk weather on an upper deck of the R/V Roger Revelle, watches whales near the ship on the CLIVARIS6 cruise in the Southern ocean. (Photo Credit: Brett Longworth, a participant from Woods Hole Oceanographic Institution)
Greetings. I’m Kevin Speer, Chief Scientist on the current CLIVAR cruise, Professor of Oceanography at the Florida State University. I’m a physical oceanographer and earned my Ph.D. at MIT and Woods Hole Oceanographic Institution - Joint Program, 1988.
I joined the FSU Department of Oceanography faculty in 1999 as an associate professor and am ...
Published in
IPY Blogs
Tagged under
By Jan strugnell, British Antarctic Survey
We have been incredibly lucky that the ice conditions have allowed us to enter Pine Island Bay, (in the Amundsen Sea) to carry out the BIOPEARL sampling programme as planned. In many previous years, Pine Island Bay has been inaccessible, due to a thick ice sheet, and so we are very fortunate that it is open at this time.
Literally nothing is known of the benthic fauna of the Amundsen sea, south of latitude 66° south, because no one has sampled here previously. Therefore anything we find here is a new record of a species in this area!
Phot...
Published in
IPY Blogs
Tagged under
Saturday, 08 March 2008 18:33
Trip to Unamed Island - it's all about the poo.
Written by CAML-James Clark Ross
By Dr James Smith, geologist on board James Clark Ross.
The purpose of our visit to ‘Unnamed Island’ was to follow up to a trip made by one of our colleagues at BAS, Dr. Jo Johnson who visited the island in 2006. Jo, then on the German research ship RV Polarstern, was busy collecting rock samples from around Pine Island Bay to date the thinning history of the West Antarctic Ice Sheet since its last glacial maximum (about 18,000 years ago).
Photo: Adelie Penguins from the Un-named island in Pine Island Bay (Amundsen Sea). BAS
This work forms part of the GRADES-QWAD programme at BAS, which i...
Published in
IPY Blogs
Tagged under
Thursday, 06 March 2008 18:05
FSU IPY Cruise: Meet graduate student Austin Todd
Written by CLIVAR Section I6S
My name is Austin Todd, and I am a first-year M.S. student in physical oceanography at FSU. This is actually my fifth year at FSU, where I completed a B.S. in meteorology and mathematics, and I am currently working under Dr. Eric Chassignet in ocean modeling in the Gulf of Mexico.
On this I6S cruise, I am part of the CTD (conductivity, temperature, and depth) operations group. We basically run most of the operations of the CTD, including preparation, deployment, monitoring, and recovery of the CTD sampling apparatus. Our group is responsible for obtaining water samples from all depths of the ocean selected for sampling...
Published in
IPY Blogs
Tagged under
By John Mitchell, Voyage Leader.
Now we are out of the inner Ross Sea the focus of the voyage has changed to sampling seamounts (underwater mountains) and the abyss (seafloor in the deep ocean 2000–4000 m). We’re surveying a series of seamounts, concentrating on the Scott complex around Scott Island north of the Ross Sea, at about 68 ºS, 180º followed by the Admiralty chain further to the west. Even further west are the Balleny Islands and associated seamounts, which will not be visited this trip as they have already been sampled during previous Tangaroa voyages. The composition of the fauna has gradually changed and reduced in quantity (but not quality) as we have moved north and is now ‘transitional’ i.e., is a mixture containing fauna typical of both the Ross ...
Published in
IPY Blogs
Tagged under
March 2, 2008
By John Mitchell, Voyage Leader
Having left the inner Ross Sea, we passed through the ever-thickening ice barrier between the open water in the polynya to the south and the open ocean to the northeast. In the ice barrier, we had to push through ribbons of thick pack ice with relatively open ‘leads’ that were filled with grease ice and newly formed soft pancake ice. Although our progress was slow at times, it was only about 24 hours before we arrived at our first seamount site, dubbed South Scott Seamount.
Photo: Tangaroa proceeding through close pack ice towards an open lead in the dista...
Published in
IPY Blogs
Tagged under