Dissolved Fe in the western and central North Pacific Ocean was characterized by surface depletion, middepth maxima and, below that, a slight decrease with depth similar to the vertical distributions of nutrients, apparent oxygen utilization, Fe(III) hydroxide solubility, and humic‐type fluorescence (H‐flu) intensity. Dissolved Fe concentrations ([D‐Fe], <0.22‐μm fraction) in the deep water column were one‐half lower in the central region (0.3–0.6 nM) than the western region (0.5–1.2 nM) although the Fe(III) solubility ([Fe(III)sol], <0.025‐μm fraction) levels and distributions in deep waters were almost the same between both regions with middepth maxima (∼0.6 nM) at 500–1500‐m depth range and then a gradual decrease to ∼0.3 nM at 5000‐m depth. Higher [D‐Fe] than [Fe(III)sol] in the deep water column of the western region results from the higher production of dissolved Fe from the decomposition of sinking particulate organic matter in the western region than the central region because of the high atmospheric and/or lateral Fe inputs in the western region. Similarity between [D‐Fe] level and [Fe(III)sol] value at each deep water depth in the central region may be attributed to [D‐Fe] being nearly in the solubility equilibrium with Fe(III) hydroxide in seawater. Strong linear correlation between [D‐Fe] and H‐flu intensity in the central region and relatively similar linear relationships between [Fe(III)sol] and H‐flu intensity in the western and central regions are the first confirmation that humic‐type fluorescent dissolved organic matter may be responsible for [D‐Fe] in the deep water column as natural organic ligands complexing with Fe(III).

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Spatiotemporal distributions of anthropogenic radionuclides in marine surface sediments off Miyagi, Fukushima, and Ibaraki Prefectures were analyzed on the basis of data collected during the monitoring program launched by the Japanese Ministry of Education, Sports, Science and Technology in 2011 right after the Fukushima Dai-ichi Nuclear Power Plant accident began. Concentrations of ¹³⁷Cs in the surface sediments varied spatially by two orders of magnitude, from 1.7 to 580 Bq kg-dry⁻¹, and there was no obvious correlation between ¹³⁷Cs concentration and the proximity of the sampling location to the accident site. The total inventory of ¹³⁷Cs accumulated in the upper 3 cm of surface sediments in the monitoring area was estimated to be 3.78 × 10¹³ Bq, that is, 0.1–2% of the total ¹³⁷Cs flux from the plant to the ocean as a result of the accident (the percentage depends on the model used to estimate the total flux). The spatial variations of ¹³⁷Cs concentration and inventory depended on two main factors: the ¹³⁷Cs concentration in the overlying water during the first several months after the accident and the physical characteristics of the sediments (water content and bulk density). The temporal variations of the concentrations of other anthropogenic radionuclides (⁹⁰Sr, ⁹⁵Nb, ^{110 m}Ag, ¹²⁵Sb, ¹²⁹Te, and ^{129 m}Te) in the sediments were also investigated. Activity ratios of these nuclides to ¹³⁷Cs suggest that the nuclides themselves were not homogenized before they were removed from seawater to the sediments

[1] The vertical distributions of dissolvable (unfiltered) Fe concentrations in semi-closed oceanic regions, such as the Japan Sea and the Bering Sea, are characterized by a gradual increase with depth in the intermediate and deep waters. However, there is a rapid decrease in the dissolvable Fe concentration over the narrow depth range between deep and bottom waters with constantly lower concentrations observed in the bottom waters of the Japan Sea (Japan Basin), probably from the injection of newly formed bottom water. In addition, the rapid increase in dissolvable Fe concentrations in bottom waters in the western North Pacific Ocean may be due to the resuspension of sediments from the seafloor or the slope. However, there are no differences of labile dissolved (

The activities of artificial radionuclides in seawater samples collected off the coast of Miyagi, Fukushima, and Ibaraki Prefectures were measured as part of a monitoring program initiated by the Japanese Ministry of Education, Sports, Science and Technology immediately after the Fukushima Dai-ichi Nuclear Power Plant accident. The spatial and temporal distributions of those activities are summarized herein. The activities of strontium-90, iodine-131, cesium-134 and -137 (i.e. ⁹⁰Sr, ¹³¹I, ¹³⁴Cs, and ¹³⁷Cs) derived from the accident were detected in seawater samples taken from areas of the coastal ocean adjacent to the power plant. No ¹³¹I was detected in surface waters (≤ 5 m depth) or in intermediate and bottom waters after 30 April 2011. Strontium-90 was found in surface waters collected from a few sampling stations in mid-August 2011 to mid-December 2011. Temporal changes of ⁹⁰Sr activity in surface waters were evident, although the ⁹⁰Sr activity at a given time varied widely between sampling stations. The activity of ⁹⁰Sr in surface waters decreased slowly over time, and by the end of December 2011 had reached background levels recorded before the accident. Radiocesium, ¹³⁴Cs and ¹³⁷Cs, was found in seawater samples immediately after the accident. There was a remarkable change in radiocesium activities in surface waters during the first 7 months (March through September 2011) after the accident; the activity reached a maximum in the middle of April and thereafter decreased exponentially with time. Qualitatively, the distribution patterns in surface waters suggested that in early May radiocesium-polluted water was advected northward; some of the water then detached and was transported to the south. Two water cores with high ¹³⁷Cs activity persisted at least until July 2011. In subsurface waters radiocesium activity was first detected in the beginning of April 2011, and the water masses were characterized by σ_t (an indicator of density) values of 25.5–26.5. From 9–14 May to 5–16 December 2011, the depths of the water masses increased with time, an indication that deepening of the isopycnal surfaces with time can be an important mechanism for the transport of radiocesium downward in coastal waters. During 4–21 February 2012, the water column became vertically homogeneous, probably because of convective mixing during the winter; the result was nearly constant values of radiocesium activity throughout the water column from the surface to the bottom (~200 m depth) at each station