Taking cores from the sediments on the seabed can help researchers understand the (distant) past, how the earth looked like back then and how it became the way it is today.
There are many scientists from different fields of research on Oden during Arctic Ocean 2016. One benefit of being on the cruise (except getting to collect your own data, of course), is getting to know them and learning about their work.
We attended a tour in the lab of the sediment coring group. Grace Shephard (geologist and post doc at the University of Oslo) and Luz María Mejía (from Universidad de Oviedo, soon to be post doc at the ETH) analyse the seabed sediment cores we have collected during the trip.
Taking cores from the sediments on the seabed can help researchers understand the (distant) past, how the earth looked like back then and how it became the way it is today. The Arctic Ocean is not well mapped, and samples from this area will help a lot in puzzling together the Earths history. In the seabed samples they can find biogenic material (a mix of organic and inorganic materia, like ancient animals, shells or plants), rocks (that can have been dragged with ice from far away, see photo below) and other things that can tell researchers a lot about the past environmental conditions.
Several seabed cores are collected at different places during the cruise. The cores are sampled from the seabed with a corer, which is deployed from the aft deck (back) of the ship by a team of crew and technicians. Taking a core can take 3-4 hours depending on water depth and ice conditions. Actually, most of the time is spent just waiting for the corer to reach the seabed and taking it back up, since the water can be quite deep (more than 4000 metres). Taking the sample itself on the seabed only takes a few minutes.
The cores on this trip can be up 12 metres long, and they are quite heavy. As you see from the pictures, the seabed sediments include clay, and everyone who has tried lifting clay knows that it can be heavy. The cores come up in plastic cylinders (if you look at the photos you see the white cylinders), which are split into 1.5 metre long units to make carrying and analysing them easier.
They start processing the cores straight away. They have machines to measure sediment properties including temperature, density and magnetic properties, amongst others.
Some core samples are split length-ways for doing analyses and sampling. The researchers observe the core visually, and sketch and note down what they see (lines, patterns, colors, etc). The cores are sampled with small cubes, which are frozen and taken home for further analyses.