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So, on with my work….Antarctica. It’s the Earth’s largest, driest ice desert, and nothing really lives there….except hardy penguins and scientists! This is because despite its desolation and isolation, there are parts of it that are very very important, more important than most people realise – its ice. Antarctica’s ice sheets are really humongous, and unlike the ice in the North Pole which floats on the sea like an ice cube, Antarctica’s ice sits on top of the worlds fifth biggest continent. This map shows how Europe compares to the Antarctic continent in terms of size:
If any of the ice that sits on Antarctica melts, it will flow into the oceans and sea level will rise all over the planet.  Unfortunately for us, Antarctica’s ice contains enough water to raise sea level globally by around 60 meters – thats about the height of the clock face on Big Ben! 
Now, as I’m sure most of you know, us humans are contributing to global warming. There are still lots of unanswered questions about what effect this will have on the Earth – this is because our planet’s climate (which is a system made up of the ocean, atmosphere, ice and land) is probably the most complex thing we have ever tried to understand. I am trying to figure out how Antarctica’s ice sheets will respond to global warming, so that we can be prepared for what the future might hold. 
How do I do this? Well, I study marine sediments, or muds, that lie all around the continent of Antarctica. (Watch this video about the Intergrated Ocean Drilling Program, an organisation made up of hundreds of scientists who get to go to  really cool places to dig muds up from the ocean floor! http://www.youtube.com/watch?v=uHE34BgebgY ). These muds are deposited by ocean currents or carried in icebergs from the land, and they show us a window into how the ice sheets of Antarctica have behaved in the past. They are extracted as cores, which are really long (sometimes thousands of metres long). This is a photo of one of the cores that I am working on right now:
In particular, I study muds from a time from between 5 and 3 million years ago (called the Pliocene Epoch) when the Earth’s climate was very similar to how it is going to be at the end of this century. By building a picture of how the ice sheets behaved during the Pliocene, we can more accurately predict how they will behave in the future. 
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If you want to know anything about climate change, or Antarctica or about the Earth, or prehistoric life or anything sciencey, I would love to recieve a question! Fire away! 😀

So, a typical day for me involves missioning it across London to get to South Kensignton, where I work (right next door to the Science Museum AND the Natural History Museum, where I get to work behind the scenes sometimes!). I get to my office, and read a million emails from colleagues and people I am working with all over the world. My work involves lots of laboratory work, so I head downstairs to the basement to our ‘clean lab’ to check on some experiments. A ‘clean lab’ is a completely enclosed room with its own seperate clean air supply, which prevents any dirt or dust from getting in – this means people can work in a very very clean environment. You have to wear head-to-toe overalls, with a hat and rubber shoes, and gloves. A bit of effort but it is required! After checking on any experiments, I go to our mass spectrometer laboratory – a mass spectrometer is a very loud and expensive machine that seperates different elements (e.g. potassium, iron) by their masses, meaning we can work out what a compound is made of….quite nerdy stuff but pretty cool! I look at the elements neodymium and strontium…..After the labs is lunch, and then on to a meeting with fellow climate change researchers about an exhibition we are helping to design at the Science Museum….thats about it, although I can say that everyday is different, and I also get to go all over the world (New York, Texas, Spain, the Czech Republic to name a few) with my research…