Characterization of settling particles in the Bering Sea and implications for vertical transportation of multiple elements by diatom frustules

Author:

Emoto Mariko1,Takahashi Kozo2,Akagi Tasuku1

Affiliation:

1. Department of Earth and Planetary Sciences, Faculty of Science, Kyushu University

2. Hokusei Gakuen University

Publisher

Geochemical Society of Japan

Subject

Geochemistry and Petrology,Geophysics

Reference18 articles.

1. Akagi, T. (2013a) Revision of the dissolution kinetics of aggregated settling particles. Mem. Fac. Sci. Kyushu Univ. Ser. D Earth & Planet. Sci. 33, 1–5.

2. Akagi, T. (2013b) Rare earth element (REE)-silicic acid complexes in seawater to explain the incorporation of REEs in opal and the “leftover” REEs in surface water: New interpretation of dissolved REE distribution profiles. Geochim. Cosmochim. Acta 113, 174–192.

3. Akagi, T., Fu, F.-f., Hongo, Y. and Takahashi, K. (2011) Composition of rare earth elements in settling particles collected in the highly productive North Pacific Ocean and Bering Sea: Implications for siliceous-matter dissolution kinetics and formation of two REE-enriched phases. Geochim. Cosmochim. Acta 75, 4857–4876.

4. Akagi, T., Emoto, M., Tadkada, R. and Takahashi, K. (2013) Diatom frustule is an impure entity: Determination of biogenic aluminum and rare earth element composition in diatom opal and its implication on marine chemistry. Distoms: Diversity and Distribution, Role in Biotechnology and Environmental Impacts, 127.

5. Byrne, R. H. and Kim, K.-H. (1990) Rare earth element scavenging in seawater. Geochim. Cosmochim. Acta 54, 2645–2656.

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