The paper in Nature Ecology & Evolution is here: http://rdcu.be/yizP
For nearly ten years I have been travelling to the deep subduction zones beneath the Pacific to deploy full ocean depth rated ‘lander’ vehicles to the deepest places on Earth.With a small band of likeminded individuals we do this regularly to redress the chronic under-exploration of the deepest 45% of the oceans.We use bespoke camera and traps to investigate biodiversity, ecology, life history, behaviour, zonation, phylogenetics, physiology and all sorts of other fascinating things relating to good old fashioned natural history, albeit at extraordinary high pressures. The ‘Hadal Zone’ (6 to 11km deep) is where we work and we take some pride in carving out a career in traditional marine exploration and discovery in arguably the last great marine frontier, and without having to wrestle with anthropogenic impacts (although it is increasing difficult these days).
While at the University of Aberdeen, through a friend-of-a-friend deal I managed to get a small ‘taster’ sample of amphipods from 8000 metres deep in the Kermadec Trench (Off New Zealand) analysed at the James Hutton Institute. After a few weeks the word came back that the sample was “more contaminated than an earthworm in Aberdeen” (not that Aberdonian earthworms are any kind of benchmark for pollution of course), but that was encouraging, albeit not necessarily setting this up for a good news story.
Thomas G. Thompson. Likewise, in November that year we managed nearly 50 deployments from 5000 to 10,600 m in the Mariana Trench from the RV Falkor. So after Prof. Stuart Piertney and I had spent too long at sea in the Western Pacific, amongst many interesting scientific discoveries, we had our samples for this particular study.
Falkor, somewhere over the Mariana Trench in 2014. © Dr. Paul H. Yancey, Whitman College.
So here’s the depressing bit: we found that regardless of depth (between 7000 and 10,500m), regardless of species (in this case benthic amphipods), regardless of trench (the Mariana and the Kermadec), we found these scavenging crustaceans were loaded with both PCBs and PBDEs. There were striking variations between trenches and between PCB and PBDEs levels (which we brought Dr. Toyo Fujii in to statistically test), but the salient finding is that man’s footprint is thoroughly imprinted on some of the most extreme and remote marine environments on Earth.
Fig 2. Hirondellea gigas from full ocean depth. (10,890m). The amphipods are highly adapted to intercept and consume just about anything organic that falls from the surface – from particulates to whale carcasses, unfortunately that also includes any contamination picked up at the surface © Dr. Alan Jamieson, Newcastle University.
are immense in the context of the physiological adaptations organisms require for survival, and equally clever engineering solutions for human exploration, but the 11km that so easily swallows Mount Everest is still only 11km.Here is my perspective: 11km is only half the length of Manhattan Island, 11km is the width of the Mississippi River at its widest point, I could legally drive 11km in less than 6 minutes, a friend of mine could drive 11km in 4 min 6 s, and Mo Farah could run 11km in less than 30 minutes. Doesn’t seem that far now does it? In reality the deep sea just isn’t that remote, and the great depth and pressures perform nothing but an imaginary defence against the effects of what we do ‘up here’. The bottom line is that the deep sea - most of planet earth - is anything but exempt from the consequences of what happens above it, and it is about time we recognised that: The legacy and reach of mankind’s influence is most vivid by its impact on the most remote and inaccessible habitats on Earth.
Fig 3. Hirondellea gigas, from the deepest place on Earth: Challenger Deep in the Mariana Trench (10,890m). Body Lengths are between 20-30mm. © Dr. Alan Jamieson, Newcastle University.