Acronym: SEEDS 2004
Program: Iron Synthesis [FeSynth]
URL: Project Web Site
Start date: 2004-07
End date: 2004-08
Geolocation: Western subarctic gyre in the North Pacific at 48.5°N, 165°E, (i.e. 93 km SE of SEEDS I)
Description:

As at August 2008 the Tsuda 2007 paper is the only one to carry a general description.

The first iron addition was carried out from 0:50 GMT on 20 July to 0:00 GMT on 21 July (GMT).
Day 1 was defined as 21 July (GMT).

Tsuda, A., et al. (2007): Evidence for the grazing hypothesis: Grazing reduces
phytoplankton responses of the HNLC ecosystem to iron enrichment in the western
subarctic pacific (SEEDS II). J. Oceanogr. 63(6), 983-994.

A mesoscale iron-enrichment study (SEEDS II) was carried out in the western
subarctic Pacific in the summer of 2004. The iron patch was traced for 26
days, which included observations of the development and the decline of the
bloom by mapping with sulfur hexafluoride. The experiment was conducted at
almost the same location and the same season as SEEDS (previous iron-
enrichment experiment). However, the results were very different between
SEEDS and SEEDS II. A high accumulation of phytoplankton biomass (~18
mg chl m–3) was characteristic of SEEDS. In contrast, in SEEDS II, the
surface chlorophyll-a accumulation was lower, 0.8 to 2.48 mg m–3, with no
prominent diatom bloom. Photosynthetic competence in terms of Fv/Fm for
the total phytoplankton community in the surface waters increased after the
iron enrichments and returned to the ambient level by day 20. These results
suggest that the photosynthetic physiology of the phytoplankton assemblage
was improved by the iron enrichments and returned to an iron-stressed
condition during the declining phase of the bloom. Pico-phytoplankton (<2
μm) became dominant in the chlorophyll-a size distribution after the bloom.

 We observed a nitrate drawdown of 3.8 μM in the patch (day 21), but there
was no difference in silicic acid concentration between inside and outside the
patch. Mesozooplankton (copepod) biomass was three to five times higher
during the bloom-development phase in SEEDS II than in SEEDS. The
copepod biomass increased exponentially. The grazing rate estimation
indicates that the copepod grazing prevented the formation of an extensive
diatom bloom, which was observed in SEEDS, and led to the change to a pico-
phytoplankton dominated community towards the end of the experiment.

SEEDS II was conduced in the same western subarctic Pacific region as the
initial SEEDS experiment, and was an international collaborative study utilizing two
research vessels (R.V. Hakuho Maru and R.V. Kilo Moana).
This experiment was designed to characterize the evolution of the fertilized patch
over a longer time scale (1 month) and with a greater range of parameters than
measured during SEEDS.

The preliminary results from SEEDS II showed both the iron-induced increase
and subsequent decline in phytoplankton biomass. However, the iron-initiated
bloom was much less intense than observed in SEEDS. Chlorophyll-a concentrations
increased only 2 to 3 times over initial values, and the drawdown of nutrients and pCO2
were small.

Related files

SEEDS 2004 Project Documentation
SEEDS 2004 Workshop Summary

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More information about project Subarctic Pacific Iron Experiment for Ecosystem Dynamics Study II
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