EGU Blogs

Green Tea and Velociraptors

Spice up your science with these 10 simple steps

What an awful title, eh. Well, you can avoid making this mistake! A recent Guardian post by Conversation UK’s Akshat Rathi (he’s popular on the blog today!) discusses some of the common mistakes in popular science writing and how best to avoid them. It’s fairly general, and by no means exhaustive, and mainly for more writing about science than science writing (er, the latter being formal publication in peer-reviewed journal, I guess).

But a more interesting recent find was a wonderful paper by Kaj Sand-Jensen from 2007 entitled ‘How to write consistently boring scientific literature‘,  all about, well, you guessed it, avoiding some common pitfalls when writing science articles. So in true Buzzfeed style, here are the top 10 tips of how to be a terrible science writer, with some personal comments after.

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The greatest mass extinction in the history of life

In palaeontology, there are so many things more important than dinosaurs. For example, the study of large-scale patterns in the history of life on Earth, commonly known as macroevolution, is all about uncovering patterns of speciation and extinction. We are currently about to enter the sixth mass extinction within the last 542 million years of life on Earth, so figuring out exactly what happened during periods of elevated extinction and ecosystem catastrophe is pretty damn important if we want to offset as much damage as possible.

Recently, a suite of new papers have been published giving detailed insight into the environmental and biological patterns and processes throughout the Permian-Triassic mass extinction, an event 252 million years ago that saw the demise of greater than 90% of life on this planet (numbers vary depending on which measure you use). What I’d like to offer here are bitesize summaries of each, and show that there is much more important research out there in palaeontology than just ‘woo new dinosaur’.

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Every time you publish behind a paywall, a kitten dies.

“Every day, people are denied access to something they have a right to.”

That’s the opening line from a new appeal from students Joe McArthur and David Carroll. Open Access describes a form of publication of research where articles are made instantly available for free, and with unlimited reusability rights, as long as the source is attributed. There are many pseudo-open access ‘definitions’ out there from publishers to obfuscate its use, but this is the only real, least restrictive one.

There has been a global open access movement over the last 10-15 years, which has accelerated so rapidly in the last year or two that many research funders and institutions, as well as government bodies, have developed open access policies. However, despite this progress, large commercial publishers like Wiley, Taylor and Francis, and Elsevier are still the most profitable industry in the world (with margins even higher than Apple), the majority of their profits coming from obscene charges for pdfs and library subscriptions for research articles and journals.

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Middle-Earth gets a geological makeover

As if J. R. R. Tolkien wasn’t brilliant enough with his creation of Middle-Earth, it appears that using his numerous maps and illustrations provided, supplemented by observations from within the texts themselves, a geological reconstruction can be achieved! I recently came across this old article from the Proceedings of the J. R. R. Tolkien Centenary Conference, Oxford, England, 1992, and figured it was worth sharing.

The first attempt at a geological history of Middle-Earth was Margaret Howes in 1967 in a piece entitled “The Elder Ages and Later Glaciations off the Pleistocene Epoch”. Here, she endeavoured to recapitulate the successive geomorphologies from the time when Morgoth (the real bad guy in Middle-Earth) was overthrown to beyond the time when Aragorn adopted rule over Gondor. However, this work has been recognised as being too far adrift from Tolkien’s original creations, drawing in too much from Earth’s own recent geological history.

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