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Nemo could get lost in acidic oceanIf you’ve seen the movie Finding Nemo, then you’ll know that Nemo the clown fish got lost and had to try and find his way back to his home reef.
8th Feb 2009 From a fish that hums to PavarottiIf you like to warble in the shower or in the bath then you probably don't realise that you are in fact taking a step closer to the origins of your singing talent, namely fish. 27th Jul 2008 Giant shark mystery solvedBasking sharks, the second largest sharks in the world, have been tracked on epic, thousand-mile migrations into the deep waters of the West Atlantic, solving a long-standing mystery of where they spend the winter. Gregory Skomal from the Massachusetts Division of Marine Fisheries in the US led a team of scientists who tagged 25 basking sharks off the coast of New England.
As the satellites began beaming information back to the team they were amazed when the sharks kept on swimming south, into the Caribbean Sea and beyond. One shark even crossed the equator ending up at the mouth of the Amazon River on the Brazilian coast where it hung around for a month. Their discovery has revolutionised our understanding of these mysterious basking sharks which until now were thought only to live in temperate waters. They have never been seen in this part of the world before, probably because they swim very deep down between 200 and 1000 metres. The obvious explanation for their migrations is that these cold-blooded sharks need to find warmer water with lots of plankton, their favourite food. But what puzzles Skomal and his team is why the sharks bother going so far south. If food and warmer water were all they were after they could stay in northern Florida. Why bother going all the way to Brazil? One idea they came up with is that the sharks are moving to as yet undiscovered birthing and nursery grounds. Amazingly, scientists have never seen a young or embryonic basking shark, so we know virtually nothing about how they breed. Previously it was thought that basking sharks form many separate sub-populations but now it seems they are well connected and could form a single ocean-wide population. That raises important issues of how we protect them, since any impacts on basking sharks in one area could have affects on the population as a whole. It could be nations around the world will need to get together and create a global basking shark conservation programme. And this study just goes to show just how much more we still have to learn about some of the biggest creatures that roam the oceans today.
10th May 2009 Squid don’t just see with their eyesSquid, those slippery denizens of the deep, may not only see through their enormous round eyes but it seems they can also detect light all along their bodies as well.
A type of bioluminescent bacteria called Vibrio fischeri live inside the squid ink sacs in a two-way symbiotic relationship that benefits both squid and bacteria. The bacteria help the squid camouflage themselves against the bright ocean surface and in return, the bacteria get a safe place to live with all the nutrients that they need. The bacteria emit a constant glow but the squid can control how much of that light escapes by changing the shape of the ink sac tissues, rather like the iris can let more or less light into an eye. The squid ink sac even has a transparent layer across the surface that acts like a rudimentary lens controlling the direction of the emitted light. By letting more or less light through from the bacteria, squid can match themselves to the brightness of the sea surface that varies depending on how deep down they are and what time of day it is. The question is, how do the squid know how light the ocean is around them? It now seems that they might not only use their eyes, but the ink sacs also have a role to play in detecting ambient light. McFall-Ngai have discovered that the ink sack tissues housing the luminous bacteria contain genes that produce proteins associated with light detection, including some similar to ones found in the retina – the light detecting layer of cells in the eye. They also hooked up an ink sac to an electroretinogram – electrodes that are usually used to measure the electrical responses of a retina when light is shone on it. They found similar electric signals were generated by the squid ink sac, indicating that it is sensitive to light. The researchers don’t yet know exactly how these second light-receptors evolved. It could be a form of genetic or evolutionary “tinkering”, a technical term in which existing components of a living system are reassembled and tinkered and put to use in new combinations or locations. More studies are needed to delve deeper into exactly what is going on. This study sheds light into a remarkable symbiotic relationship between bacteria and large animals, something that is particularly important for us humans to understand since we rely on trillions of bacteria living inside us to keep us healthy. We may not glow brightly at night, but eight out of ten of our major organs have some sort of bacteria living in them. 7th Jun 2009 Trawling and the Damage DoneLes Watling, University of HawaiiLes - Trawling is a method of fishing that started in Britain in the 14th century where someone found out that if you took a net and held it open in some way and hauled it behind a boat you could get a lot of fish. You also get a lot of stuff. I’ve actually been looking at effects of fishing for about fifteen years and I’ve been in submarines and I’ve had cameras on remote vehicles. What I generally see is that where an area’s been trawled there’s not much living on the surface of the ocean floor. We know that trawlers also dig in to the sediment. They disrupt all kinds of things. Generally if you go to an area that’s trawled it’s really noticeable.
Les - Usually what happens is anything that’s standing up from the bottom – anything like a sponge or coral that’s growing up from the bottom – that’s usually bent over, broken or removed. If it’s a muddy bottom then the gear digs into the bottom. The important thing to realise is that most of the animals that live in the muddy bottom live in the upper 3 or 4 cm. You don’t have to dig in very far before you’ve disrupted the burrows and tubes of all these small things. Meera - They’ve been disrupted but what impact does that have? Les - It depends. Some animals recover from this disruption okay, which means they can make a new burrow or two, but a lot of animals invest a huge amount of energy into making the burrow. In fact in some cases some of the marine worms, for example, they’ve lost the ability to remake a tube. Then that’s it. They’re laying on the surface and they could be eaten by a fish or any other thing that comes along. They’ve lost their protection, as it were. Other animals raise their young in their burrows and tubes. If that’s destroyed then the babies may not be able to burrow their way out of this mud that’s been disturbed. We tend to see species in these trawled areas that have really high reproduction. They’re weeds in the best sense of the word. They have high reproduction, they can re-colonise. They’re capable of getting their house blown down, if you want to think of it that way. They’ll rebuild it real fast: all that sort of stuff. You tend to lose the things that have a longer, more stable lifestyle. Especially if it’s an area that’s trawled repeatedly. If a person drags a trawler over an area once then a lot of things will survive that. Maybe half of the things that live there will survive that. There will be a certain amount of re-colonisation that can occur in two years. A lot of times trawling occurs over and over again. Fishermen have their particular favourite spots. When you go to those areas you find that the whole bottom community has really changed to these weedy type species. This from a fish perspective might not be so bad. Fish can eat those weedy species to so you could get flat fishes, for example. It’s been shown in the North Sea that if you re-trawl areas a lot you can get flat fishes but you might not get other kinds of fish because their food is missing. You create a completely different bottom community and a new ecosystem, as it were. One parallel that I like to use is what happens when you go in and, as happened in North America for example, colonists came. The cut down all the forest and they turned it into pasture land. So we lost all the birds that nested in the trees. It’s a very similar kind of thing. The community’s still productive for growing sheep or cattle or whatever but you have lost the outliers there. Meera - How much of the world’s marine ecosystem is being affected by trawling? Les - That’s a hard estimate to make. We looked at the number of fishing vessels and where they were around the world about ten years ago. We figured that about half of the continental shelves of the world get trawled each year. That number is obviously fluctuating because fisheries have collapsed in a lot of these areas. It may be the collapse of some of these continental shelf fisheries that will allow some of this biodiversity to recover. Meera - What do you think the solution is? What can we now aim to do knowing this?
Meera - I guess if that does happen do you think that the effects that trawling has had so far is reversible? Les - It’s reversible. The time scales are going to be long the deeper you go in the sea. I have a project that has just finished looking at an area that had been closed to trawling for six years. It doesn’t look at all anything like the areas that have never been trawled. That’s six years on. If you go into really deep water we know on the sea mounts, for example, that corals recruit at extremely low rates. We had a study where we were looking for coral recruits on the sea mounts of the North Atlantic and we found one on a block that had been put out for a year and a half. Meera - So I guess fishing can be reduced but the outlook is quite promising. It’s not something that’s just going to be left disturbed. Les - Promising in the long run. Yeah. For the continental shelves, for areas that have rocky-stony-marl bottoms those we’re looking at 25-50 years probably for recovery time: before the big things like sponges start to re-grow. The deeper you go though the longer I’m certain that sea mounts that have had all the corals removed from the top will not have corals again for a century or two centuries. This is a really long time. August 2008 Robots of the OceanJules Jaffe, Scripps Institution of Oceanography University of California, San DiegoJules - Over the past decade we’ve developed a rather large vehicle, something on the order of a Volkswagen Beetle-sized vehicle which has the capability of adjusting its buoyancy. On it we put laser and we put some very sensitive cameras. We put that off the ship. It weighs almost a tonne so it’s hardly something you could go out on your row boat to put in the water! You need a fairly large ship. We’ve learned a lot of interesting things. The problem we kept coming up against (and it becomes more obvious) the more we process out data and the more we think about it is that we’re just sampling one place at one time. Even though we get a nice picture from that place and there are inferences we can make; we’re starting to work on distributed networks. Instead of having just one sampler in one place at one time we’ve got a small army of these things and they’re all going up and down in the water. They’re all sampling and they’re all sampling different places at different times. If we know where they are and we know when they were there and we have the appropriate sensors on them we can start to reconstruct this three-dimensional distribution of these organisms and actually look at mechanism as opposed to just looking at, more or less, existence.
Jules - The ocean, as you’ve already highlighted, is particularly opaque to electromagnetic radiation. Acoustics, on the other hand, as has been known by animals that have evolved over 100s of millions of years, can go very far. Our plan is to have these vehicles localising each other acoustically and we can communicate with one of them that is fairly close to us. They can distribute that message among the entire group by relaying that information. We think we can evolve sensor systems which can sense tens of kilometres instead tens of metres. Chris - Would they be carried by ocean currents? You’d deploy a range of these things over a certain distance and the natural current would move them along? Jules - Absolutely, we’ve actually had a wonderful insight into one of the advantages of our technology. We would like to be in the frame of reference of the organism itself. When you’re sitting on a ship and you’re bobbing up and down and you stick something in the water, that thing’s going to be moving around. We found out a long time ago that it makes more sense to put the vehicle in the water and let it go with the flow, as we say, and to have maybe tens or even a hundred of these things. It allows us not only to take a snapshot of their evolving environment but also to track them. There are many enigmas in oceanography that we don’t understand having to do with small animals that, say, are born onshore and have a pelagic part of their live where they go out to sea maybe for three months: a baby barnacle or something like that. Somehow they get back. To be honest, I don’t have an idea how they do that. Most of the people I know who study these things don’t have an idea how they do that! We can not only study this ten kilometre area but we can watch it evolve and be transported in time. Maybe start to unravel some of these riddles of how organisms survive in the ocean. Chris - What you’re building at the moment – is that going to be one of these vehicles? Jules - That’s correct. What we’re looking at here, Chris, is something about the size of a soccer ball which has been cut in half. We’re looking inside at the electronics of this device. Chris - It looks like something that should be in Star Wars, actually... Jules - There’s a good story about that actually. In our last grant proposal to the national science foundation we wanted to put in a colour graphic of these devices. My colleague actually put the Death Star and shrunk it down. He created a picture where you have about 20 of these Death Stars communicating with each other. In fact we’re not that far away.
Jules - Yeah! Basically, we have this pretty simple thing. It’s a soccer ball with a bunch of electronics inside it. The soccer ball’s thick enough that we can send it down to about 80m of depth without imploding. The computer has sensors that tell it what the depth of the vehicle is. By adjusting its buoyancy (its volume in the ocean) we can actually send it down and keep it at a certain depth in the sea. What we also have on this vehicle: on the bottom here is an acoustic transmitter and receiver. We call that a transducer. It can send sound and receive sound. These are actually modems. They’re actually communicating devices which allows these vehicles to talk to each other. They can actually range off each other. That allows us, knowing their depth and knowing how far they are from each other to estimate their 3D positions. Now imagine a fleet of maybe 100 of these things slowly descending in the sea, localising off each other; each equipped with some method of sensing plankton density or perhaps other things like zooplankton using acoustics. Using these hundred or so samples we can now create a 3D time-varying record of the evolution of a volume that might be 5km X 5km X 80m deep. Chris - How long does it take you to develop something like this from concept to getting something that you can put into the pacific? Jules - You’ve touched a very tender subject with me. You might have noticed I have a bit of comedy associated with my personality so what I tell my students is that if you’re pregnant you’re guaranteed within 9 months but if you’re an engineer and you’re building a vehicle it could be ten years. We’re sort of giving birth. This has been an exciting week for us because ten years from the inception of this we’ve now started to test these things in the ocean on modem communication. It’s really exciting but by the time – I tell our students that science is not something if you want immediate gratification – the time you think of the thing, write the proposal, perhaps get it rejected a few times before it’s funded, do the research, get the results, process the data, publish it and go to colleagues and tell them what you’ve done it can often be a 7-10 year period. November 2008 Keeping Tabs on JellyfishJon Houghton, Queen's University BelfastBen - We now have John Houghton on the line. Thanks very much for joining us. You are studying turtles so why is it that you’re tagging jellyfish?
Ben - How do these electronic tags work? I’m guessing these are not the things that report you’re not in your home when you should be? Jon - No but they’re not a million miles away from it. They’re data storage tags and they’re tiny – they’re about the size of your little finger. The ones we’re gonna do this year are quite simple. They’re just going to record depth and temperature and light levels. We just put it on to a jellyfish. It records all the information and then eventually we retrieve the tag. Ben - I’ve seen plenty of jellyfish washed up on the beach. They’re very squidgy sort of fluidy things. How on earth do you attach an electronic tag onto something that’s so amorphous and blobby? Jon - That’s true but there’s jellyfish and there’s jellyfish. I think the ones you’re describing would be called aurelias. They’re common jellyfish. They’re tiny and floppy and wobbly and they would be almost impossible to tag. The ones we’re going after are called barrel jellyfish and they’re massive. They’re nearly a metre across and weigh 27-28kg. They are actually quite big, tough animals. They’re very strong swimmers, they can swim against a current. Actually if you think your jellyfish are looking like a mushroom. You’ve got the stalk part coming out underneath what we call the bell. Quite simply all you do is you just tie a time and depth recorder to a plastic cable tie, swim up to the jellyfish: tie it around. It takes about ten seconds. Ben - Does this affect their behaviour? They must not like having something stuck round their body.
Ben - How long are they going to keep these tags on? When are you expecting to get this data back? Jon - That we don’t know the answer to. The particular jellyfish we’re going after – they’re unusual. Most jellyfish boom and bust for a couple of months in the summer. These guys seem to be around all year. We’re going to put the tags on probably in August and I’m sure they could be turning up anytime between say two months to maybe even a year down the line. So yeah, any time over the next year. Ben - How do you actually collect this data? Does it just float up from where the jellyfish were? Jon - What we’ve got attached to the time-depth recorder, a little dive computer, is just a tiny fishing float. On the fishing float is just a little label with a reward on it. Once the jellyfish dies the whole device just detaches itself from the jelly and floats to the surface. We’re putting them on in big bays where we know they will wash ashore. If you find one on the beach just pick up the reward label and give us a call.
July 2008 Chemistry in its Element - FluorineKira Weismann, Zaarland UniversityThe 37-year old technician spilled only a few hundred milliliters or so in his lap during a routine palaeontology experiment. He took the normal precaution in such situations, quickly dowsing himself with water from a laboratory hose, and even plunged into a nearby swimming pool while the paramedics were en route. But a week later, doctors removed a leg, and a week after that, he was dead. The culprit: hydrofluoric acid (colloquially known as HF), and the unfortunate man was not its first victim.
HF has a long history of destructive behaviour, claiming the lives of several chemists in the 1800s, including the Belgian Paulin Louyet, and the Frenchman Jérôme Nicklès. These brave scientists were battling to be the first to isolate elemental fluorine (F2) from its various compounds, using electrolysis. However, it was Nicklès’ countrymen, Henri Moissan, who succeeded in 1886. To achieve this feat, Moissan not only had to contend with HF – the preferred electrolyte in such experiments – but fluorine itself, a violently reactive gas. His key innovation was to construct an apparatus out of platinum, one of the few metals capable of resisting attack, while cooling the electrolytic solution down to –50 °C to limit corrosion. Moissan’s feat earned him the 1906 Nobel Prize in chemistry, but the celebration was short-lived. Another victim of fluorine’s toxic effects, he died only two months later. Yet Moissan’s method lived on, and is used today to produce multi-ton quantities of fluorine from its ore fluorspar. Ironically, while elemental fluorine is decidedly bad for your health, fluorine atoms turns up in some 20% of all pharmaceuticals. The top-selling anti-depressant Prozac, the cholesterol-lowering drug Lipitor, and the antibacterial Cipro, all have fluorine to thank for their success. How is this possible? Because the flip side of fluorine’s extreme reactivity is the strength of the bonds it forms with other atoms, notably including carbon. This property makes organofluorine compounds some of the most stable and inert substances known to man. Fluorine’s special status also stems from the ‘fluorine factor’, the ability of this little atom to fine-tune the chemical properties of an entire molecule. For example, replacing hydrogen with fluorine can protect drugs from degradation by metabolic enzymes, extending their active lifetimes inside the body. Or the introduced fluorine can alter a molecule’s shape so that it binds better to its target protein. Such precise chemical tinkering can now be carried out in pharmaceutical labs using an array of safe, commercially-available fluorinating agents, or the tricky transformations can simply be out-sourced to someone else.
Fluorochemicals are also a mainstay of industry. One of the most famous is the polymer polytetrafluoroethylene, better known as Teflon, which holds the title of world’s most slippery solid. Highly thermostable and water proof, it’s used as a coating for pots and pans, in baking sprays, and to repel stains on furniture and carpets. Heating and stretching transforms Teflon into Gore-tex, the porous membrane of sportswear fame. Gore-tex’s pores are small enough to keep water droplets out, while allowing water vapour (that is, sweat) to escape. So you can run on a rainy day, and still stay dry. Fluorine plays another important role in keeping you cool, as air-conditioning and household refrigeration units run on energy-efficient fluorocarbon fluids. And fluorine’s uses are not limited to earth. When astronauts jet off into space they put their trust in fluoroelastomers, a type of fluorinated rubber. Fashioned into O-rings and other sealing devices, these materials ensure that aircraft remain leak-free even under extreme conditions of heat and cold. And when accidents do happen, space travellers can rely on fluorocarbon-based fire extinguishers to put the flames out. Fluorine has long been known as the ‘tiger of chemistry’. And while the element certainly retains its wild side, we can reasonably claim to have tamed it. As only a handful of naturally-occurring organofluorine compounds have ever been discovered, some might argue that we now make better use of fluorine than even Nature herself. For more Chemistry in its Element, or the latest in Chemistry news from Chemistry World - visit the Royal Society of Chemistry's Website. August 2009
Fizzy Acids - what happens when you carbonate waterDiscover what happens when you make water fizzy, why it then tastes so tangy and why this could cause problems for shellfish. What you need
What to DoGrate a small amount (2-3 leaves) of raw red cabbage and put it into a glass. Add some tap water and then mash it up as well as you can. Strain out the lumps of cabbage to produce a clear solution. This is your pH indicator, it will behave like litmus changing colour depending on the acidity or alkalinity of your solution (to find out more see this experiment). Test some of your tap water by pouring a small amount of indicator (3-4mm) into a glass and adding tap water. If the solution is bluey purple then you have hard slightly alkaline water, if it is pink then you have slightly acidic water. We want the water to start off slightly alkaline, so add a little bicarbonate of soda to your tap water until it stops testing pink. Split your water into two, carbonate half of it, and leave the other half alone. Now test both the carbonated and uncarbonated water with your red cabbage indicator and see if there is a difference. What may HappenYou should find that the carbonated water makes the water much more acidic than the straight tap water. This is the reason why if you taste the carbonated water it has a tangy, sharp - acidic taste.
First a bottle of normal water is added to the indicator, and then some carbonated water from the soda syphon What is going on?When you carbonate water you are essentially passing high pressure carbon-dioxide through it and a large amount of that carbon dioxide dissolves in the water.
Carbon dioxide is far more soluble in water than are similar gases such as oxygen or nitrogen. It can also react with the water to form dihydrogen carbonate (carbonic acid).
This reaction is reversible, it is continuously occurring in both directions, carbonic acid is being made and destroyed all the time. This means that if you increase the amount of carbon dioxide by increasing the pressure you will increase the speed of the production of carbonic acid reducing the amount of gas. Similarly if you reduce the pressure you will slow the creation of carbonic acid, but it will keep on splitting up to form carbon dioxide gas. This is why if you rapidly reduce the pressure on a carbonated drink it can rapidly turn into foam (see the lemonade volcano experiment). Why is the carbonated water acidic?
The hydrogen carbonate can break up (disassociate) in another way, it can split up into a hydrogen ion (H+) and a hydrogen carbonate (bicarbonate) ion (HCO3-). Any solution containing a lot of free hydrogen ions is acidic. In fact pH (the acid-alkali scale) is just an obscure† measure of the concentration of hydrogen ions in a solution. The reaction is again reversible so if the amount of hydrogen carbonate reduces so does the amount of acid. There is naturally carbon dioxide in the air, and this will dissolve in water making it slightly acidic. This is how water can dissolve away limestone to create caves. As we pump more carbon dioxide into the atmosphere it will make water more acidic, this may cause problems for shellfish whose shells are effectively made of limestone. Are there actually free protons floating around in an acidic solution?Strictly an H+ ion is a hydrogen atom missing an electron - a proton, which does sound unlikely. In fact what happens is that the Hydrogen carbonate reacts with water to form a hydronium ion (H3O+). But all the maths works out the same if you think of hydrogen ions so mostly chemists do.
† It is actually pH = - log10( [concentration of hydrogen ions / mol dm-3] ) ... as I may have said, fairly obscure. It so happens that it makes convenient scale and makes other maths easier for chemists. Written by Dave Ansell |
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