miércoles, 29 de septiembre de 2010

Lucifer I is over

Phase I of the Lucifer project is over. The objectives of the study are the biogeochemical consequences of (1) the vertical mixing and the consequent planktonic bloom in the oceanic subtropical waters around the Canary Islands, (2) the influence of the lunar cycle observed in zooplankton in the transport of organic carbon towards the mesopelagic zone, and (3) the process of natural fertilization with iron promoted by the deposition of Saharan dust which is produced in several events during winter around the Canary Islands. During phase I, we performed a weekly sampling in the oceanic waters north of the Canary Islands from February to June 2010 in order to study the so-called late winter bloom in subtropical waters. We also studied the effect of a strong event of dust deposition, increasing production in synchrony with the lunar cycle.

Temperature, salinity and fluorescence were measured using a CTD SeaBird 25 and an in situ fluorometer. Primary production as 13C, chlorophyll, abundance of bacteria, phytoplankton cells, microzooplankton abundance, and mesozooplankton, biomass, gut fluorescence, electron transfer system (ETS), and aminoacyl t-RNA sinthetase (AARS) activities were also measured at four oceanic stations to the north of Gran Canaria Island. We also collected dust particles using active samplers near the study site for the measurement of metal composition (iron, nickel, cadmium, manganese,..).


Figure 1. True color image of the dust storm observed over the Canary Islands the 18th March, 2010. The image was provided by NASA/GSFC, MODIS Rapid Response through http://rapidfire.sci.gsfc.nasa.gov.

During March 2010, an important event of Saharan dust (Figure 1) took place around the islands. Values of dust particles smaller than 10 µm (PM10) reached values of 300 µg•m-3 in Gran Canaria Island, near our sampling area. Preliminary data showed no response of phytoplankton biomass to the massive dust deposition, at least at a weekly timescale. However, we measured a sharp increase of zooplankton biomass after this event. The bloom lasted for more than one month, indicating an important influence of the dust over the area. Flow citometry, 13C, microzooplankton and proxies of metabolic activity in zooplankton are being measured but our preliminary results show that the effect of this dust deposition event did not promoted any increase in chlorophyll, similar to some common results reported in the literature.
However, we wonder whether the increase in productivity is rapidly transferred to higher trophic levels through micro- and mesozooplankton in this warm water environment, avoiding the accumulation of phytoplankton biomass in the mixed layer. The consequences of this finding will restrain the use of remote sensing data to assess the effect of dust fertilization in the ocean. Finally, the active carbon flux promoted by the diel vertical migrants is a scarcely studied mechanism of the biological pump. Predation by this fauna upon the zooplankton crop observed after the dust deposition, shunted this epipelagic biomass to the mesopelagic zone. This transport will be the objective of Lucifer phase II which will start next November.

Santiago Hernández-León
IMBER Newsletter, Issue No. 15, September 2010

miércoles, 24 de febrero de 2010

IMBER endorsement

The IMBER (Integrated Marine Biogeochemistry and Ecosystem Research) endorsement sub-committee sent us a letter last week informing about their acceptance of the LUCIFER project. The endorsement will serve to help coordinate national and regional IMBER research activities and to share data among scientists. It will also serve as a recognition that our objectives are under the umbrella of IMBER international project. If you are interested in looking at the endorsed projects by IMBER please visit http://www.imber.info/endorsed_projects.html.

Below are some pictures of the sampling activities carried out recently on board the "Atlantic Explorer". Thanks to Alejandro Ariza for the photos.

Federico Maldonado at work with the double WP-2 net

Federico again with the microplankton net

The Bongo net

Idem

Alejandro Ariza deploying the 30 liter Niskin bottle

Almudena Folgado, Alejandro Ariza and Mar Benavides in a democratic attitude

The oceanographic team. From left to right: Laia Armengol, Mar Benavides (biting the apple...), Almudena Folgado, Sabrina Sánchez and Federico Maldonado

Idem with Alejandro Ariza. Nice team

Victor Sepúlveda at work

Alejandro, Federico and Almudena

Sabrina, Almudena and Federico

lunes, 14 de diciembre de 2009

Dust composition

Our colleague Mar Benavides sent us a nice paper about the composition and age of dust in Northwest Africa by Eglinton et al. Thank you very much. Below is the abstract. The paper is available on request and it is of interest for those working on the geology and chemistry of dust.


The introduction of the paper is really very original as they quote the first description of the dust clouds from the Sahara. The citation is from somebody named Charles Darwin who sail this area on board a ship called H.M.S. Beagle. Below is the text.


Nice description, like in a blog.

domingo, 25 de octubre de 2009

Meeting

Next week, those engaged in sampling during the project (oceanography and aerosols) are invited to a new meeting. Next Thursday at 10:00 a.m could be a good day and a good time to start, but you have to send an e-mail to the IP in order to agree with this date. If some of you are not able to come this day, the IP will look for another day.

The IP will give a short talk about the history and objectives of the project for the new members and he will present the dueties before sampling and the sampling program.

Do not forget to e-mail the IP.

lunes, 5 de octubre de 2009

Remember important dust events

After a long period without news, Lucifer strikes back again. Today an interesting paper by Viana et al. (2002) in which we found that during the famous dust event from February 2000, there was somebody measuring the dust deposition in Gran Canaria (prima!). Therefore, we can have an idea of the amount of dust promoting a bloom in the ocean, the one we measured at that time. This data is really interesting for the now starting project. The paper is available on request (as usual). Somebody knows somebody from this research group?





miércoles, 29 de julio de 2009

Two interesting papers

Below are the abstract of two interesting papers. The first one is a nice paper by Benoit-Bird et al. about the influence of the lunar cycle in the nigthtime vertical position of the deep scattering layers. Observe the technology they are using to measure the biomass of micronekton. Impressive. The second one is a remote sensing paper dealing with the dust deposition in the Mediterranean and the increase or not in chlorophyll. They conclude that increases in chlorophyll is an artefact of the remote sensing measurements. So, dust fertilize or not? Interesting question.




martes, 7 de julio de 2009

Saharan Dust Storms and Plankton in the Ocean

The number of June 19, 2009 of ScienceDaily published the effort made by German and Cape Vert institutions to disentangle the relationship between dust storms and plankton fertilization. As you can see, we have good competence in the study of the effect of dust. They have money, good equipment and a boat. For the followers of this blog, below is the content of the article. I think we can benefit from their work very south of the Canaries. Perhaps, we should start to think about a join meeting to discuss our results.


As our colleague Gara Frachy saids, they are using the same kind of picture we use here but in their area of research. Perhaps, we follow the same objectives...


The tropical Atlantic waters around Cape Verde are very low in plant nutrients. Nitrogen is in especially short supply and limits the growth of the phytoplankton, the tiny plants that are at the basis of the food chain in the ocean. In this area, the nutrients fall out from the sky: Trade winds carry Saharan dust rich in iron and phosphorus which can fertilize the surface of the ocean.
This was one of the reasons for the IFM-GEOMAR and other German and UK institutions to establish an observatory on the Cape Verde island Sao Vicente. The Tenatso Observatory now supports long-term measurements of dust and greenhouse gases as well as an oceanographic mooring and regular sampling expeditions by the small Cape Verdean research vessel Islandia.
“We’re testing whether Saharan dust can promote the growth of a particular type of microbe, a cyanobacteria. These cyanobacteria can fertilize the surface of the ocean by fixing the abundant nitrogen gas that is dissolved in seawater”, says Prof. Julie LaRoche from IFM-GEOMAR, co-leader of the expedition.
There is plenty of nitrogen gas in the atmosphere but it needs to be "fixed" so that it turns into a fertilizer which is available to phytoplankton. The enigmatic cyanobacteria UCYN-A seems to be a very special nitrogen fixer. In contrast to other cyanobacteria, it is probably incapable of producing oxygen. This in turns enables it to fix nitrogen during the day while others cannot.
The Trade Winds and frequent dust storms that make this area so important for ocean research also complicate the scientists’ work. Dust samples are collected with filters on top of the atmospheric observatory. The collection of the water samples, however, requires sailing on the Islandia for several hours to the ocean observatory located 130 kilometres offshore in a surrounding water depth of 3600 metres. The samples are returned to laboratories that have been established at Cape Verde’s “National Institute for Fishery Development” where the dust experiments are conducted.
"The working conditions are difficult and some trips on the Islandia are like a roller coaster. But overall it’s a very positive work experience, thanks to our supportive Cape Verdean colleagues, the crew of the Islandia, and the general ambience on the islands “, says Stefanie Sudhaus , Ph.D. student at IFM-GEOMAR and member of the last expedition. Loaded with plenty of data from their experiments and confident that the experiments will deliver new discoveries, the scientists have returned to Kiel. During the expedition they were accompanied by scientists from the Max Planck Institute for Marine Microbiology, the Alfred Wegener Institute for Polar and Marine Research, Leibniz Institute for Baltic Sea Research and the Leibniz Institute for Tropospheric Research.

Research Project at the Cape Verde

Scientists from German and Cape Verdean institutes have started collecting data at Cape Verde Observatory Tenatso in 2008, measurements that they hope to continue in order to follow the effect of global change in the tropical Atlantic Ocean. Their research is part of the SOPRAN project (Surface Ocean Processes in the Anthropocene) that is largely supported by the German Federal Ministry of Education and Research (BMBF).

Nitrogen fixers and UCYN-A
There is plenty of nitrogen gas (N2) in the atmosphere but only few organisms are able to "fix" it so that it turns into a fertilizer with biologically useful molecules. Cyanobacteria or blue-green algae are amongst the most important nitrogen-fixers. Until recently scientists thought that single-cell organisms could only fix the nitrogen during the night because during the day, oxygen is released through photosynthesis and inhibits nitrogen fixation by poisoning the enzyme responsible for it.
The cyanobacterium UCYN-A doesn’t seem to work like that. It lacks the genes for photosystem II that are needed for the oxygen release and apparently cannot fix carbon dioxide into sugars. Thus, it may utilize light energy in other ways and forgoes photosynthesis, as is normally carried out by land plants and other algae. Although this organism has never been isolated in pure culture, an initial characterization of its genome was published in 2008 by the group of Jonathan Zehr at University of Santa Cruz (Zehr et al. 2008, Science Vol. 322 no. 5904, pp. 1110-1112).