Earth Sciences is a truly interdisciplinary subject that seeks to understand the structure and history of our planet, and to predict the future of the Earth, atmosphere and oceans.
In both teaching and research, our focus is on the physical processes that formed and now influence the Earth, and on testing hypotheses by observation, experiment and modelling. The quality of our research is recognised internationally, as well as nationally (in 2008 we were ranked in the top 5 UK Earth and Environmental Sciences for research by the Higher Education Funding Council for England). We enjoy active collaboration with other departments of high repute at Bristol, including Physics, Chemistry, Mathematics, Geography, and Archaeology and Anthropology.
Situated at the heart of a bustling and vibrant city, the Department of Earth Sciences at Bristol is an exciting and attractive place to work or study. Its BSc, MSci and MSc graduates are sought after by key employers, but many go on to postgraduate study. Of those who take jobs, 95% are in graduate-level employment within 6 months (source: www.unistats.com). The staff, researchers and students come from many countries, bringing new ideas and a truly international feel to our community.
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Scientific debate sparked over carbon sink data
Apparently conflicting results published by researchers from Bristol's QUEST programme reveal the difficulties of accurately estimating sources and "sinks" of CO2, although all of the authors agree that the only way to control climate change is through a drastic reduction in global CO2 emissions - 18.11.09 |
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No slow-down in global CO2 emissions
Evidence published today in Nature Geoscience, by Drs Pru Foster, Pierre Friedlingstein, Jo House and Prof Colin Prentice from the University’s QUEST programme, suggests that the rise in atmospheric CO2 emissions continues to outstrip the ability of the world’s natural ‘sinks’ to absorb carbon. - 18.11.09 |
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Controversial new climate change results
Recently-published research by Dr Wolfgang Knorr, a member of QUEST's core team at University of Bristol, shows that the balance between the airborne and the absorbed fraction of carbon dioxide has stayed the same since 1850, despite a huge rise in emissions over the same period. This suggests that oceans and ecosystems have a greater capacity to absorb CO2 than had been previously expected - 09.11.09 |
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£295,000 for release of Bristol dinosaur
After 210 million years of being entombed in rock, the Bristol Dinosaur (aka Thecodontosaurus) is about to be released. Thanks to a Heritage Lottery Fund (HLF) grant awarded to the University of Bristol, Prof Mike Benton and his team will expand their labs., employing a specialist preparator to free the bones and an education officer to visit local schools. |
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Andesites are a blend of new and old volcanic material
In a letter published today in Nature, and highlightend on NERC's PlanetEarth online website, Prof Jon Blundy and colleague Dr Olivier Reubi of ETH Zurich show that andesitic magmas which are erupted in arc volcanoes around the world do not come from pure molten rock. Chemical study of tiny droplets of silicate liquid, trapped in crystals in andesite rocks has revealed that, instead, that they come from a mixture of silica melts and old crystal residues - 29.10.09 |
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Why giant sea scorpions got so big
Research by James Lamsdell and Dr Simon Braddy, published today in Biology Letters, sheds new light on why eurypterids (giant sea scorpions) became so large and eventually died out. Their work shows that competition with armoured vertebrates and environmental pressures affected the two main eurypterid lineages differently, but that both responded by increase in size of the animals. - 14.10.09. |
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1,000 fossil-hunters come to Bristol
Over 1,000 paleontologists from all over the world are arriving in Bristol this week for an international conference at the University of Bristol. For the first time since its foundation in 1940, the Society of Vertebrate Paleontology (SVP) is holding its annual meeting outside the Americas. - 22.09.09 |
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Fossil water scorpion was ancestor of giant sweep-feeders
New finds of a fossil water scorpion that lived in rivers around Bristol some 370 Million years ago have shown Bristol palaeontologists what the animal looked like and how it was related to other eurypterids. Work by Dr Simon Braddy and James Lamsdell from Bristol,and colleague Dr Erik Tetlie from Norway, is published in the journal Palaeontology - 17.09.09 |
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Reptiles stood upright after mass extinction
Having studied fossil tracks of reptiles from below and above the end Permian mass extinction boundary, Prof Mike Benton and Palaeobiology student Tai Kubo found that , medium and large-sized reptiles of the had changed from walking with a sprawling gait, to walking with their legs tucked uder their bodies. The results and a discussion of their implications was published today in the journal Palaeontology -15.09.09 |
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New data illuminates Antarctic ice cap formation
Dr Gavin Foster is part of a team that has shown that the formation of the Antarctic ice-cap, some 33.5 million years ago, was directly linked to declining levels of carbon dioxide in the atmosphere. The study, involving researchers from Bristol, Cardiff and Texas A&M universities, and using microfossils from East Africa is published in Nature online. - 13.09.09 |
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No universal driver for plankton evolution
During his MSc project, Palaeobiology student Ben Kotrc analysed the relative importance of abiotic versus biotic effect on the evolution of marine plankton. The results of the work, supervised by Dr Daniela Schmidt and recently published in PNAS, show that both competition with other organisms and long term climatic changes influence evolutionary change in radiolarians. - 08.09.09 |
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New predictions for sea level rise
Using data from fossil corals and temperature records from ice cores, Dr Mark Siddall and colleagues from Switzerland and the US have tested projections of future sea level rise. Their model, details of which have just been published in Nature Geoscience, predicts a rise of between 7- 82 cm by the end of this century (depending on the amount of warming that occurs). This is similar to the figures projected by the IPCC report of 2007. - 26.07.09 |
© 2008 Earth Sciences, University of Bristol
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