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Crozet Cruising - Thursday 22/12/2005

You have heard about incredible trawl catches, deploying and recovering the landers ROBIO and FRESP, but so far little about our other important activity of collecting sediment (mud!). Most organisms that live at the sea floor rely on food from above, arriving as phytodetritus on the sea floor (see previous blogs), or as part of a more constant drizzle of smaller particles settling slowly, or being swept along the bottom by currents. The habitat can be very variable, depending on the supply of food and how it arrives, the substrate (hard rock or soft sediment), the depth of water and the depth within the sediment itself. At Crozet (M5 at least), we are dealing with sediments. The method we use to collect undisturbed sediments is with a hydraulically dampened coring device, or megacorer for short. This allows us to recover undisturbed sediments from great depth, in core tubes of 10 cm diameter that are then carefully extruded and sliced.

The megacorer with its catch of sediment
 
The megacorer with its catch of sediment
Sediment core from M5
 
Sediment core from M5. Notice the black band, which is an occasional feature of cores collected here. This material is probably a lens of volcanic sand that has washed down-slope form the island
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The sediments are not really typical abyssal sediments and even at 4000 m water depth, they do seem to be influenced by the Crozet Platform, a very large volcanic mountain which rises steeply from the sea bed and expresses itself above sea level as the Crozet Islands. In our trawls, we have picked up fairly sizable pieces of pumice, which presumably derive from previous eruptions, but there are also pockets of volcanic sand/gravel which has probably been eroded from the islands and tumbled down the slope to settle in patches in the deep water. There have also been plenty of rounded volcanic pebbles in our trawls, which probably come from the Crozet beaches or sub tidal zones. Some of these have had kelp (seaweed) stalks attached to them, which gives us another clue as to where they come from.

The Crozet Islands
The Crozet Islands – looking appealing!

So, what is the interest in what really is a pile of mud? Firstly it is to sample and study the organisms from bacteria, through meiofauna (less than 0.5 mm) to macrofauna (less than 10 mm) and to understand their community structure and diversity. Secondly it is to study the chemistry of the organic material through the sediment. One of the main issues that we are trying to investigate is whether or not the organic chemicals contained in the phytodetritus arriving at the sea floor influence the types of animals living here. Deep-sea animals require certain vitamins and if they do not have a supply of these (in the phytodetritus) then it seems likely they won’t do well.

zeaxanthin
3-D chemical structure of zeaxanthin, a molecule made up of carbon (grey), hydrogen (white) and oxygen (red). This compound, a carotenoid similar to Vitamin A, is biosynthesised only by photosynthesising organisms, but it and its relatives may be important vitamins for other animals. For example zeaxanthin may have a role to play in protecting the eggs and larvae of some holothurians.
 
In order to assess the importance of the chemistry of material arriving at the sea floor to the animals that live there, we have been using sediment traps and pumps to collect phytodetritus. It is also useful for us to study the profiles in the sediments of the organic chemicals, so we can determine how quickly they are taken up by the sedimentary community and also how they are transformed. We can’t do this on the ship, so we carefully slice the sediment cores and freeze the sections at -80°C so that they can be transported home and analysed in our laboratories. This is a long and painstaking process and it will probably be at least a year before we have enough data to say that we have a molecular picture of the Crozet sedimentary environment! Chemists have a hard time on cruises – they watch everyone else getting fantastic knowing that it is going to take them ages to get theirs!
 
Last updated 4/02/08