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IFM-GEOMAR

Leibniz-lnstitut fur Meereswisse st

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IFM-GEOMAR Re�

2002-2004

From the Seafloor to the Atmosphere - Marine Sciences at IFM-GEOMAR Kiel -

lune 2005

(2)

Preface

F

or the first time, the Leibniz Institute of Marine Sciences (IFM-GEOMAR) presents a joint report of its research activities and de­

velopments in the years 2002-2004. In Janu­

ary 2004 the institute was founded through a merger of the former Institute for Marine Re­

search (IfM) and the GEOMAR Research Center for Marine Geosciences. This report addresses friends and partners in science, politics and private enterprises. It gives an insight into the scientific achievements of IFM-GEOMAR and its predecessor institutes during the last three years.

---IFM - GEOMAR Report 2002-2004 ---�·

(3)

IFM-GEOMAR

Leibniz-lnstitut fur Meereswisse st

'IN•

r

,. j.

a n d er U n iv er sit at Kie I Iv O

I

o -:::·

O

'

c

,,....

'1--· ::::

t::. /.�/ � I

IFM-GEOMAR Re�

2002-2004

From the Seafloor to the Atmosphere - Marine Sciences at IFM-GEOMAR Kiel -

lune 2005

(4)

Preface

F

or the first time, the Leibniz Institute of Marine Sciences (IFM-GEOMAR) presents a joint report of its research activities and de­

velopments in the years 2002-2004. In Janu­

ary 2004 the institute was founded through a merger of the former Institute for Marine Re­

search (IfM) and the GEOMAR Research Center for Marine Geosciences. This report addresses friends and partners in science, politics and private enterprises. It gives an insight into the scientific achievements of IFM-GEOMAR and its predecessor institutes during the last three years.

---IFM - GEOMAR Report 2002-2004 ---�·

(5)

3.8 Dust Fertilization of the Tropical North Atlantic stimulates Nitrogen Fixation

P

hytoplankton productivity is an important sink for atmospheric C02 and has been sug- gested to alter global C02 concentrations. Giv- en that the nutrient availability exerts a streng control on the productivity of phytoplankton populations it is of great importance to under- stand which nutrients Iimit productivity. Alter- nate views exists: Biological oceanographers argue that supply of bound nitrogen (N) Iimits phytoplankton productivity and biomass, while geochemists assert that over geological times- cales nitrogen fixation should provide the fixed N necessary for primary production and that availability of biologically utilizable phosphorus compounds (P) control primary productivity.

1t has been shown that iron is a very important limiting nutrient for phytoplankton growth in the Pacific and southern ocean. There in situ iron fertilization of nutrient rich surface waters result in phytoplankton blooms. Iran has also been suggested as a potential nutrient limit- ing nitrogen fixation due to the iron rich ni- tragen fixing enzyme nitrogenase. The oligo- trophic tropical North Atlantic is considered a hot spot for n1trogen fixation. Satellite images regularly show spectacular dust clouds enter- ing the tropical North Atlantic from the Sahara and Sahel zone that can provide iron and also P to the surface ocean (Fig. 1). This region is subjected to some of the highest mineral dust deposition rates in the world, and has high dis- solved iron concentrations in surface waters relative to other oceanic basins. As such, the tropical North Atlantic is a region where the phytoplankton community is least likely to be iron limited. Therefore, surface waters have been assumed to be replete in iron with re- spect to nitrogen fixation.

During the METEOR 55 and 60 cruises (Octo- ber - November 2002, and March April 2004 respectively) to the tropical North Atlantic we have attempted to determine the role of the nutrients N, P and Fe in controlling primary productivity and nitrogen fixation using a nu- trient addition bioassay approach. Additions of Saharan dust were also made to investigate whether this aeolian input could provide limit- ing nutrients. Our results showed that at all sites phytoplankton biomass and primary pro- duction were limited by N (Fig. 2). Afterrelief

of N Iimitation, further stimulation was seen with the addition of P and then iron. The find- ing of N Iimitation of the phytoplankton com- munity stresses the importance for nitrogen fixing organisms, diazotrophs, in this system.

At all sites tested during METEOR 55 we de- tected nitrogen Fixation, and the addition of P and Fe tagether stimulated nitrogen fixation (Fig. 2). Conversely, additions of inorganic N (added as N03· and NH4 +) inhibited diazotroph- ic activity. Saharan dust additions also result- ed in enhanced primary productivity, bacterial production, and nitrogen fixation, though not at all stations tested, indicating that the dust supplies microbial populations with the nutri- ents that at times Iimit different processes.

Given the high atmospheric loading of iron to the eastern tropical North Atlantic we were surprised to find that iron addition stimulated diazotrophy. 1t is generally argued that iron concentrations in our study area are in excess of diazotroph iron requirements, but our find- ings suggest that total dissolved iron concen- tration is a poor index of bioavailability, per- haps due to temporal variation in the chemical speciation of dissolved iron. It is also possible that the Ievei of iron required to saturate dia- zotroph growth has been underestimated. The important role of iron in our study region im- plies that the control of nitrogen Fixation by

Figure 1: Dust storm over the subtropical and tropi- cal North Atlantic from the African continent ob- served by SeaWiFS satellite Images on February 26th, 2000.

- - - IFM - GEOMAR Report 2002-2004 - - - -·

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3. Scientific Highlights

Limitation of prlmary production by N Co-limitation ofthe N2 lixation by P and Fe

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Figure 2: Effects of nutrient (N, P, Fe) additions on primary produc- tion (= C02 fixation) and nitrogen fixation (= N2 fixation) in natural plankton communities of the tropical Atlantic. The map at the top shows the cruise track and the location of the bioassay experiments.

Results shown are indicated by red star and red line indicates control response.

0 0.5 1.5

Mean Annual Dust column loading (g m-2)

Carbon Fixation Nitrogen Fixetion Chlorophyll Biomass C) Bacterlel Productlvlty

Figure 3: Mean annual dust column loading to the North Atlantic cal- culated using MODIS aerosol optical thickness data from April 200 - March 2004. Overlayed on the map are the sites of the nutrient enrichment bioassay experiments with colors indicating the presence of a Stimulation of C02 fixation (red), N1 fixation (blue), Chlorophyll biomass (green), and bacterial productivity (yellow) by dust. Note:

Sampieanalysis for N2 fixation have been completed for sites south of 20°N.

iron should be even greater in other oceanic regions that receive less dust deposition. Our results have important implications for understanding controls on marine microbial productivity and how it relates to

co2

fixa-

tion in the North Atlantic. First, contrary to recent suggestions, our experiments demon- strate that the total primary productivity of the

natural plankton community in the tropical/sub -tropical Atlantic is N- limited. Second, they demonstrate that nitrogen fixation is co-limited by iron and P in a region where mineral dust deposition is high and iron should be in excess. Further studies are required to determine whether this co-limitation is wide- spread. Finally, our results suggest that dust, when supplied at high Ieveis locally, can relieve N Iimi- tation of primary production, iron and P Co-limitation of diazotrophy, and N and P co-limitation of bacte- rial production.

The tropical North Atlantic is a re- gion of high dust deposition. It is also considered one of the most important areas globally for ni- tragen fixation. Dust deposition is highly episodic, and has varied widely on geological timescales. If dust deposition can to some extent relieve nutrient Iimitation of ma- rine microbial communities as our results demonstrate (Fig. 3), the postulated link between changes in dust deposition as seen between glacial and interglacial periods and changes of eiemental cycles in the ocean by plankton may be even strenger than initially suggested.

IFM-GEOMAR Contributions Mills, M.M., Ridame, C., Davey, M., LaRoche, J., and Geider, R.J., 2004: Iren and phosphorus co-limit nitro- gen fixation in the Eastern Tropical North Atlantic. Nature, 429, 292- 294.

LaRoche, J., and Breitbarth, E., 2005: The importance of Trichode- smium in the global nitrogen cycle.

Journal of Sea Research, 53, 67- 91.

Matthew Mills and Julie LaRoche

·~---

IFM - GEOMAR Report 2002-2004 - - - -

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