A Mesoscale Iron Enrichment in the Western Subarctic Pacific Induces a Large Centric Diatom Bloom

Author:

Tsuda Atsushi12345,Takeda Shigenobu12345,Saito Hiroaki12345,Nishioka Jun12345,Nojiri Yukihiro12345,Kudo Isao12345,Kiyosawa Hiroshi12345,Shiomoto Akihiro12345,Imai Keiri12345,Ono Tsuneo12345,Shimamoto Akifumi12345,Tsumune Daisuke12345,Yoshimura Takeshi12345,Aono Tatsuo12345,Hinuma Akira12345,Kinugasa Masatoshi12345,Suzuki Koji12345,Sohrin Yoshiki12345,Noiri Yoshifumi12345,Tani Heihachiro12345,Deguchi Yuji12345,Tsurushima Nobuo12345,Ogawa Hiroshi12345,Fukami Kimio12345,Kuma Kenshi12345,Saino Toshiro12345

Affiliation:

1. Hokkaido National Research Institute, Kushiro, Hokkaido 085-0802, Japan.

2. Department of Aquatic Bioscience, University of Tokyo, Bunkyo, Tokyo 113-8657, Japan.

3. Tohoku National Fisheries Research Institute, Shiogama, Miyagi 985-0001, Japan.

4. Central Research Institute of Electric Power Industry, Abiko, Chiba 270-1194, Japan.

5. National Institute for Environmental Studies, Tsukuba, Ibaraki 305-8506, Japan.

Abstract

We have performed an in situ test of the iron limitation hypothesis in the subarctic North Pacific Ocean. A single enrichment of dissolved iron caused a large increase in phytoplankton standing stock and decreases in macronutrients and dissolved carbon dioxide. The dominant phytoplankton species shifted after the iron addition from pennate diatoms to a centric diatom, Chaetoceros debilis , that showed a very high growth rate, 2.6 doublings per day. We conclude that the bioavailability of iron regulates the magnitude of the phytoplankton biomass and the key phytoplankton species that determine the biogeochemical sensitivity to iron supply of high-nitrate, low-chlorophyll waters.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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