I haven’t posted here as much as I have wanted to recently due to a combination of factors. Firstly my laptop broke, secondly I’ve been busy at work now that the arm has healed up (x-rays of the fracture here), and thirdly I’ve also been conducting an osteoarchaeological side project. (I’m also expertly, somewhat even academically, ignoring a slew of deadlines which are fast approaching for a few writing projects). However this is just a quick post to say that there should be a few posts over the next month or so. A few of these posts have been drafted earlier in the year and are half-finished, but it is hoped they’ll be finished shortly.
In the meantime, and in non-osteo news, I couldn’t help but notice two particularly interesting science articles on the BBC news website earlier today. Both news articles are probably not new to geologists, oceanographers or geophysicists, but they have certainly piqued my interest. There is evidence that biological life, in the form of microbes, have been found living at a depth of 2400m beneath the seabed off the coast of Japan. Although the organisms are single-celled they do seem to manage to survive on a diet of hydrocarbon compounds whilst only expending low amounts of energy. The microbes have been found in coring samples from an ancient coal bed system, which was drilled by the International Ocean Discovery program in 2012 in the Shimokita Peninsula, Japan. Amazingly the drill was sent down through 1000m of seawater and through 2446m of rock under the seabed itself. At such depths there is little water, limited nutrients, no light and no oxygen, yet life still survives. Tantalizingly research still remains to be conducted on how the microbes came to be at this location and at this great depth. Read the article here on the BBC.
The other science news article deals with water of a different order. The world’s oldest deep water is present in a much greater volume than previously estimated. Located within the Earth’s crust, where some of the oldest rock can also be found, ancient water has been sampled through boreholes and mines and the revised estimate of the volume suggests there is around 11 million cubic kilometres present in the crust. The world’s oldest dated water has been located in present day Canada in a mine located 2.4km down into the crust, estimates put the water at around 1 billion to 2.5 billion years old (yup billion!). The fact that the water is so old, and preserved so well, has surprised many and also revises the estimates of hydrogen produced on earth. Previously it was thought that continental crust produced almost zero hydrogen compared to ocean crusts. Again, the full article can be found here on the BBC (1).
Both news articles are the result of research coming from the currently ongoing 47th American Geophysical Union Fall Meeting in San Francisco (15th-19th December with a whooping 24,000 delegates!), which covers Earth and space science topics. I’ll certainly be keeping an eye out for further news as this is incredibly interesting as scientific research continues to extend our knowledge of where, and how, life not only survives but seemingly thrives.
(1). The scientific literature has not been referenced in this post but I will update once this becomes either available and/or when I have the time.
In other extreme life news the New Scientist magazine has reported the filming of a fish (a possible snailfish) at the depth of 8143m below the surface at the Marianas Trench, in the Pacific Ocean. The Marianas Trench is the deepest part of the world’s oceans, and the filmed footage of the snailfish at this extreme depth highlights once again how life can survive in hostile environments. The intense pressure at this depth places severe limitations on the function of muscle and nerve tissues, however snailfish are known to survive in such intense pressure environments with another species, Pseudoliparis amblystomopsis, having been studied and recorded at depths of 7703m before.