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Autor:
Aya Omata, Kenshi Kuma, Nanako Hioki, Satoko Ishikawa, Ren Uchida, Yoshihiko Kamei, Keiichiro Sakaoka, Shohgo Takagi, Hiromichi Ueno, Yutaka Isoda
Publikováno v:
Journal of Geophysical Research: Oceans. 118:1257-1271
[1] We measured water-column iron concentrations from west to east along 47°N in the subarctic North Pacific, and in the Bering Sea. In the North Pacific dissolved Fe (D-Fe) showed surface depletion, mid-depth maxima at 1000–1500 m (west, 1.3–1.