Friday 31 October 2008
Small is beautiful (well ... sometimes)
Below are shown some of the strange and alien-looking creatures that are being picked up in our samples. (left: amphipod releasing egg; right: copepod; bottom left: ctenophore; bottom center: pelagic polycheate; bottom right: salp).

At the moment, zooplankton samples are being collected both by multi-nets (which can sample at different depths) and by Bongo (which collects larger amounts of zooplankton, but from the whole water column). Samples are being used to determine community composition, the geographical and depth distribution of different species as well as for stable isotope studies that investigate the importance of different zooplankton taxa as a food source for fish and squid.
In addition to being an important food source, zooplankton also harbor the juvenile stages of many commercially and ecologically important fish species. These are called the ichthyoplankton. During the life-cycle of most fish, it is the early juvenile stages that are most at risk from their environment. Due to their small size, the ichthyoplankton are at the mercy of the currents and individual larvae cannot protect themselves against predators. This is why the majority of fish die when they are very young (often >99%). It is frequently the success or failure of this planktonic life-stage that determines the potential success of adult fish stocks.
(left: fish larvae; center: fish larva; right: cephalopod larva)


text and images by: Sven Kaehler
Monday 27 October 2008
If its Monday .. we must be heading east ...again!!

th. Dotted along the plateau are sampling stations where we collect bottles of water for oxygen, salinity, nutrient, chlorophyll and zooplankton concentrations from top to bottom...in some places this takes minutes because the seafloor is only 30 m deep!.
Saturday 25 October 2008
Cures from the Deep: The Search for New Pharmaceuticals from Deep Water Western Indian Ocean Marine Sponges.
erties is the cornerstone of modern drug discovery. Traditionally, these new chemical entities have been procured from several sources including the vast natural product reservoirs characteristic of terrestrial and marine ecosystems. Many marine organisms (invertebrates e.g. sponges; algae and micro-organisms) produce natural products (biomolecules) as chemical defence agents against predation or in a chemically mediated response to, inter alia, inter-species competition for limited resources (e.g. space on a reef or nutrients) and intra-species communication (e.g. larval settling cues). Surprisingly, many of these marine natural products also possess medicinal properties and internationally several marine derived chemical compounds are currently in development as new anti-cancer and anti-inflammatory drugs.
The coastline of southern Africa, and the deeper waters off its shores, sustains a unique diversity of endemic marine fauna and flora that can offer rich rewards for marine natural products chemists in search of novel bioactive marine natural products with medicinal properties. For the last fifteen years Professor Mike Davies-Coleman’s marine natural products research group at Rhodes University has been systematically searching for new marine natural products, with medicinal potential, from the marine invertebrates occurring off the coast of South Africa, Mozambique and Marion Island in the Southern Ocean. While the southern African inshore benthic communities are reasonably accessible with the aid of SCUBA, accessing offshore deepwater invertebrate communities is logistically problematic, and the marine sponge material collected as part of the Macarene Leg of the ASCLME cruise will be crucial in enhancing our knowledge of Western Indian Ocean marine biomolecular diversity.
king together to discover possible new marine medicines and has strong research links to the National Cancer Institute in the USA and marine natural product research groups in the USA, Canada, Australia and New Zealand. Marine sponge material collected during this ASCLME cruise will be screened for natural products that are able to either kill oesophageal cancer cells or activate enzymes that halt the onset of arthritis and osteoporosis. The Eastern Cape Province of South Africa has the highest reported incidence of oesophageal and cervical cancer in South Africa and the identification of marine natural products exhibiting cytotoxicity towards the former cancer is an important component of marine drug discovery efforts at Rhodes University.Saturday 18 October 2008
Tropical storm approaching
A tropical depression has been evolving in the vicinity of Diego Garcia over the past week. The non-frontal synoptic scale low-pressure system definitely has some indications of cyclonic wind circulation as can be seen in the adjacent synoptic chart and satellite image courtesy of the Mauritius Meteorological Service. Winds circulate clockwise around low-pressure and cyclonic systems in the southern hemisphere. Gusts associated with tropical depressions are generally less than 90 km per hour whereas in a true tropical cyclone winds can range from 150 to over 300 km per hour. The red cross in the satellite image Friday 17 October 2008
Barbeque on the high seas
From 14-15 October we were sampling stations in the vicinity of the Cargados Carajos Shoals (see adjacent Google Earth Image). The shoals consist of 16 small islands (and some 34 cays) and are classified as a dependency of Mauritius. The shoals used to be a volcanic island that over time eroded until it became submerged and a coral atoll was left behind. The length of the Mascarene Plateau cruise and the lack of any port calls over the five week period will place strain on both scientists and crew. It was therefore decided at the start of the cruise that we will have two barbeque (braai) parties at locations where we could safely anchor the ship to rest and recuperate. The Cargados Carajos Shoals presented just such an opportunity and it was decided, after completing the last station, to anchor off Coco Island (île aux Cocos at 16°50'S, 59°30'E).Thursday 16 October 2008
Demersal Trawling
The demersal trawling programme is producing some very colourful fishes of fascinating variety. We caught 38 species in our first half-hour trawl and the total is now up to nearly 130 species. Five of our bottom trawls so far have been in about 20-30 m depth and the species found at this depth are now becoming very familiar to us, so sorting is becoming quicker and easier. I was able to name all of the fish in this morning’s sample in a very short time. Smith’s Sea Fishes is proving an excellent guide to identify these fishes even though we are well away from
the sea area covered by this famous book. This illustrates the role of the Agulhas current in spreading these species down the south east African coast.Before I left Grahamstown, Eric Anderson, SAIAB’s expert on deeper water fishes, told me that the deeper waters around the Mascarene Plateau were very poorly explored and that many species caught in waters around 300 m deep are likely
to be new. I’m not sure how true that comment will prove to be, but I’m certainly having difficulty identifying some apparently common large species from deeper water trawls in 200 m and 300 m. I’m still searching the literature and thus won’t put pictures of these on the web yet to ask for help, but may do so before the end of the cruise.
not far short of 2 m long, held up in the photo by Jackie Hill, and also a sawshark, Pliotrema warreni, whose toothy snout became so entangled in the netting that it had to be cut free. Other common fishes are a variety of trigger fishes, fusiliers, butterfly fishes and other tropical reef fishes. The opening of the codend at the end of each trawl continues to be eagerly anticipated, to see what new species spill out on to the deckWednesday 15 October 2008
What are we doing here?
The Mascarene Plateau, in the Southwestern Indian Ocean, is about 2200 km in
length, running from the Seychelles Bank at 4°S to the island of
Mauritius at20°S. As you can see on the left its oriented roughly north–south similar to a crescent. It is characterised by a series of islands, banks and shoals separated by deeper ridges and channels. The main banks are called the Seychelles Plateau, the Saya de Malha Bank, the Nazareth Bank and the Cargados-Carajos Bank. These are typically 20-100 m deep, coral topped and sometimes break the surface to form small islands – in fact we will anchor off Coco island later today! The Plateau is surrounded by steeply descending slopes so that water depths rapidly increase to 3000-4000 m on either side of the plateau - as you can see from the figure below. The nature of this long fractured plateau is thought to form a barrier to the surrounding ocean circulation. Some of the shoals are more than 250 km wide. The Mascarene Plateau is a rare example of an extensive shallow-shelf sea completely detached from land boundaries and is, except for the Shoals of Capricorn Marine Programme and Darwin Initiative in 2000 – 2001, a largely unexplored marine ecosystem.
So what do we hope to see?
The most northerly part of the study area is under the influence of the northeast
monsoon from December to February, but during the remainder of the year the whole area is under the influence of the Southeast Trades and the South Equatorial Current (SEC). Recent studies in this area suggest that the shallow Mascarene Plateau acts as a barrier to the predominantly westward zonal flow of the SEC causing it to split into a number of tributaries, which then become channelled through the deep gaps separating the shoals. This creates some interesting questions as to the effect this channeling has on the plateau's ecosystem.

The figure left shows the position of the banks and the velocity of the surface circulation. What we can see really clearly here is how these deep gaps influence the surface circulation as the flow associated with the South Equatorial Current is channelled through each gap...
Key Questions
and a cruise track!2. In what way is the flow of the South Equatorial Current affected by the gaps in the Mascarene Plateau?
3. Is the Mascarene Plateau characterised by an increased diversity in habitats and biota?
4. What are the main components in the Mascarene Plateau pelagic ecosystem, its distribution and abundance?
5. What are the biodiversity of the pelagic ecosystem, and the main fauna of the demersal fish community?
6. Can the Mascarene Plateau be considered a Large Marine Ecosystem on its own?
....and that’s what we are doing here.. to answer the questions we are deploying a network of CTD stations, multinet stations, bongos and demersal trawls similar to what you see in the track above....
Keep posted for some answers!
Monday 13 October 2008
Drifting around in the Indian Ocean

History
For many years, ocean currents have been estimated by how they carry objects. For example, sailors measured the speed of their ship through the water using the ship log. They measured their absolute position by celestial navigation (in the good old days, pre-GPS!). The difference between the absolute speed and the speed through the water gave the speed of the currents. Very strong currents, such as the Agulhas Current made a big difference in how long it takes to travel. More recently, researchers began tracking objects while they were drifting. This tracking was first done visually either from a coastline or anchored ship, then using radio, and most recently using satellites. During the 1970s, when satellite tracking became possible, many competing drifter designs were proposed, built and deployed in various studies around the world.
How does a dr
ifter work?The modern drifter is a high-tech version of the "message in a bottle". It consists of a surface buoy and a subsurface drogue attached by a long, thin tether.
!!Drifters basically have a surface float and attached to that a long holey sock known as a drogue. The surface float is on average 40 cm in diameter. It contains: batteries; a transmitter, which relays all the information on a 6-hourly basis to satellite; a thermistor to measure sea surface temperature; a barometer to measure atmospheric pressure, wind speed and direction, as well as a GPS to measure position and the time taken for the drifter to move from one position to another – this way you can measure the surface current speed and direction.
The drogue is centered at 15 meters beneath the surface to “anchor” it to the surface – this prevents strong winds from pushing the drifter around. The outer surface of the drogue is made of nylon cloth. Throughout the drogue, rigid rings support the drogue's cylindrical shape. The drogue is a "holey-sock": each drogue section contains two opposing holes, which allow water to flush through and prevent the drogue from getting “wound up” in strong surface currents.
Once deployed, a drifter lives an average of 400 days before ceasing transmission. Occasionally, drifters are picked up by fishermen or lose their drogue and run aground.
Deploying a drifter
Drifters weigh about 25 kg each. Before deployment, the drogue and tether are bound with paper tape which dissolves in the water,
How much do they cost
Drifters range in price depending on the number of sensors you have. On average you can expect t pay about $2500 per drifter.
Keep posted for more cruise stories!
Does my bum look BIG in this?
Saturday 11 October 2008
Mauritius Cruise
Saturday 04 October 2008
Bye bye Bongo
I hope Tommy will keep you all informed about what is going on aboard the Nansen and continue updating this blog. If anyone else aboard the vessel would like to contribute to the Blog, please send me an email (Tommy has the address) and I will add you to the system.
I am currently using a hotel PC as the hotel's wireless internet seems to be down. I've also apparently left my flash stick on the vessel, so can't carry across the images from the big function last night. I will make a retro-active post as soon as I can.
Friday 03 October 2008
Group Photo
We just had a quick group photograph with many of the delegates from the meeting I mentioned in the last post. Unfortunately, not everyone is in the group photo.David Vousden, the Project Director of the ASCLME Project and Magnus Ngoile, the Policy and Governance Coordinator for the ASCLME Project had to go and meet with one of the Ministers of Mauritius for a in-depth briefing on the project, which is a fantastic opportunity for us. I, of course, am behind the camera!
This is a full-resolution image, so it is around a 1.87 megabyte download to get the whole image if you click on it. This may take some time if you are on a slow connection; once the picture loads in your browser, right click on it and save it to your computer. If anyone has a problem getting this image, I can provide a resized, lower resolution image - let me know.
Thursday 02 October 2008
Big meetings
A large problem with managing transboundary resources is that there are not only many countries involved - itself a major challenge - but also many projects involved. All of them are doing excellent work within the region, but sometimes the communication and cooperation between the projects isn't all it could be. Essentially, what we'd all like to do is work together, so that we don't end up duplicating our efforts and so that we can effectively share our knowledge and results, and perhaps work more closely together where particular focus areas overlap. People have been talking about this for years, but we've never quite managed to get this level of collaboration really going.
For these reasons, we are hosting a pioneering 3 day Regional Project Coordination Forum here in Mauritius, at the Hotel La Plantation, a few minutes north of Port Louis. A dedicated meeting to really introduce the projects to each other and then, perhaps more importantly, spend time talking about joint aims, coordination and how to work together, is exactly what we need - and has, as far as we know, not been done in the region previously.For the last three days, the ASCLME Project has been discussing coordination with its closest partners, with a particular emphasis on cruise coordination, data and information, capacity building and communication; I haven't had a chance to discuss with my colleagues yet how those meetings went, but I think they probably went very well.
The present meeting, however, has a broader vision. Today's meeting is designed to allow projects to briefly introduce themselves and outline their aims and activities. I don't have a full list, but some of the projects either present or represented include the IRD from France, ACEP, WIOMSA, AMESD, FAO and their projects SWIOFC and EAF-Nansen, GOOS-Africa and CLIVAR/TRIO, Indian Ocean Commission, ReCoMaP, RAMP-COI, GEF-WIO Marine Highway Development and Coastal and Marine Contamination Prevention Project, International Knowledge Management, and several other projects whose names I unfortunately do not have in front of me.
I'll go around with a camera later and post some pictures. (Edit: I have added a few pictures).
Wednesday 01 October 2008
En route to the last station
Well, we're finally en route to the last station, just outside Port St. Louis Harbour, we're getting a lovely view of the mountains of Mauritius from here. After that, it's straight into the harbour, then time to clear the customs and immigration formalities. And after that, well, we're getting off the ship and going out! Sigbjørn has declared this evening a "welfare dinner", where everyone goes and eats together on shore.
I think everyone is pretty keen to get off and stand somewhere where you don't get thrown off balance every few minutes, where things stay put where you put them, and you don't have to think every moment "Hmm, if I leave this here, will it break?". Not to mention seeing something other than endless blue ocean, that whilst lovely for a while, does eventually get trying - but it makes you realise how badly named this planet is. We call it "Earth", yet over 2/3rd of it is ocean - and a much bigger fraction of the total biosphere. It's strange to note that humans have seen more of the dark side of the moon than the deep oceans. More of even Mars or some of the more distant planets. We still have a lot to learn out here!Subscribe to Posts [Atom]




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