Skirting around thin ice
نویسنده
چکیده
paths with someone who was clearly born in the wrong century — an avid knitter, a lutist, or someone who will actually sit down and write a letter. These anachronisms are harder to find in science, but they do exist. In fact, a small band of them revealed themselves during a research cruise this summer to the Arctic Ocean. You might not think to look for an 19th Century scientist on a bright red, 420-foot-long icebreaker. After all, the “Healy” is bristling with high-tech toys. There’s a remotely operated submarine that can dive more than 2500 meters beneath the waves. The sub’s high-definition TV cameras reveal in stunning detail what’s crawling around on the bottom of the sea. Scientists aboard the ship also revel at daily access to email, even in latitudes so extreme that the communication pathway is a low-bandwith connection to polar-orbiting Iridium satellites. But Bodil Bluhm from the University of Alaska notes with irony that it takes this kind of set-up to do the kind of science she was born for. And that is to explore the natural history of a world that feels pretty well revealed by now. As Bluhm stood on deck one July day, sorting excitedly through a catch of sea-floor critters brought up in a trawl net, she remarked, “I actually would like to have lived 150 years ago in the early explorer phase” of ocean exploration. Then she thought better of it. “I would probably have sat at home and waited for my sailor husband to come back, or something. It’s good I’m here now.” The Arctic Ocean is one of the few places left on Earth where you can promise in your grant proposal that you will discover species entirely new to science — and not have to worry about eating your words. This 30-day expedition was designed as a biodiversity survey, looking at everything from invertebrates that cling to the bottom of ice floes, to graceful pelagic jellies, and benthic brittlestars that somehow thrive on the organic instrumentation, as well as new molecular tools, including a largescale collection of transgenic fly lines Rubin is planning to develop. Among the first group of appointees, computational biologist Sean Eddy perhaps stands out as one who was drawn to the essential idea of Janelia. Eddy was looking to have a smaller lab, with what he describes as “sort of the MRC and Bell Labs kind of style,” that would suit his interests in software development and his group’s mixture of theoretical and experimental work. “I was immediately attracted — even before they knew what they were going to do at the Farm — when Gerry Rubin started standing up and saying ‘this is the culture that we’re going to build.’ This was always my dream. I went up to him after that first time and I said, ‘Gerry, I don’t even care what you people work on there, I want to be considered.’” Though Eddy plans to initially continue his current work on computational biology and noncoding RNAs, he feels a pull in the direction of studying neural circuitry — a problem that he initially set out to tackle in C. elegans as a postdoc at the MRC. “I do dream about getting back into neurobiology... at Janelia Farm I’m going to be surrounded by all these great neurobiologists, and I’ll just be able to soak it all in.” He has a special interest in what he sees as Sydney Brenner’s “original question” — how a model organism like the worm integrates everything from sensory input to behavioral output. Conveniently, Brenner will be a Senior Fellow at Janelia, along with former Bell Labs director and former Lawrence Berkeley National Lab head Charles Shank. According to Shank, despite their different interests — Schank has a background in chemistry and an interest in optics — he and Brenner are proving that even Senior Fellows enjoy branching out. “I’ve had just an enormous good time talking with Sydney and the way he thinks about biology and technology... I’ve learned a great deal from Sydney already. Current Biology Vol 15 No 19 R782
منابع مشابه
Thin ice impacts on surface salt flux and ice strength: Inferences from advanced very high resolution radiometer
Temperatures and albedos derived from satellite imagery are combined with a thermodynamic ice model to estimate thin ice thickness distributions over the Beaufort and the northern Greenland seas. The study shows that thin ice (thinner than 1 m) occupied over half the area in the seasonal ice zones in November and December of 1990 but dropped significantly in April 1991; the Beaufort Shelf showe...
متن کاملSkirting around the Transition State
As the availability of fossil fuels and their impact on the environment receive ever increasing attention, there is a global push towards the development of energy systems that make use of alternative forms of chemical energy. Of the many interesting possibilities, the hydrogen molecule holds a place of particular prominence due to its very clean combustion. In the proposed Hydrogen Economy, th...
متن کاملDouble Laser for Depth Measurement of Thin Films of Ice
The use of thin films is extensive in both science and industry. We have created an experimental system that allows us to measure the thicknesses of thin films (with typical thicknesses of around 1 µm) in real time without the need for any prior knowledge or parameters. Using the proposed system, we can also measure the refractive index of the thin film material exactly under the same experimen...
متن کاملSnowball Earth: A thin-ice solution with flowing sea glaciers
[1] The late Neoproterozoic era, 600–800 Myr ago, was marked by at least two intervals of widespread cold that left glacial deposits at low paleolatitudes. Both ‘‘Snowball’’ solutions with global ice cover and ‘‘Slushball’’ solutions with ice-free tropical oceans have been proposed to explain the paleomagnetic data. The Snowball model is best able to explain the auxiliary geological evidence, p...
متن کاملA Study on Extracting the Trend of Thin Ice Distribution in the Sea of Okhotsk Using Amsr-e and Amsr2 Data
Passive microwave radiometers onboard satellite can penetrate clouds and can monitor the global sea ice distribution on daily basis. It is not easy to extract sea ice thickness information from satellite data. In 2012, the authors have developed a method to detect thin ice area using the brightness temperature data derived from the passive microwave sensor AMSR-E onboard Aqua satellite. The bas...
متن کاملComment on ‘‘Snowball Earth: A thin-ice solution with flowing sea glaciers’’ by David Pollard and James F. Kasting
[1] Pollard and Kasting [2005] (hereinafter referred to as PK) have coupled an energy-balance climate model to an ice-shelf flow model, to investigate the Snowball Earth episodes of the Neoproterozoic, 600–800 million years ago, when the ocean apparently froze all the way to the equator [Hoffman and Schrag, 2002]. PK’s particular concern was to investigate the possibility that over a wide equat...
متن کاملذخیره در منابع من
با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید
برای دانلود متن کامل این مقاله و بیش از 32 میلیون مقاله دیگر ابتدا ثبت نام کنید
ثبت ناماگر عضو سایت هستید لطفا وارد حساب کاربری خود شوید
ورودعنوان ژورنال:
- Current Biology
دوره 15 شماره
صفحات -
تاریخ انتشار 2005