Articles | Volume 10, issue 8
https://doi.org/10.5194/bg-10-5481-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/bg-10-5481-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
15 Aug 2013
Research article |
| 15 Aug 2013
Cesium, iodine and tritium in NW Pacific waters – a comparison of the Fukushima impact with global fallout
P. P. Povinec
Centre for Nuclear and Accelerator Technologies (CENTA), Department of Nuclear Physics and Biophysics, Faculty of Mathematics, Physics and Informatics, Comenius University, 84248 Bratislava, Slovakia
M. Aoyama
Department of Geochemistry, Meteorological Research Institute, Tsukuba, Japan
D. Biddulph
NSF Arizona AMS Laboratory, University of Arizona, Tucson, Arizona 85721, USA
R. Breier
Centre for Nuclear and Accelerator Technologies (CENTA), Department of Nuclear Physics and Biophysics, Faculty of Mathematics, Physics and Informatics, Comenius University, 84248 Bratislava, Slovakia
K. Buesseler
Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts, USA
C. C. Chang
NSF Arizona AMS Laboratory, University of Arizona, Tucson, Arizona 85721, USA
Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA
R. Golser
VERA Laboratory, Faculty of Physics, University of Vienna, Vienna, Austria
X. L. Hou
Center for Nuclear Technology, Technical University of Denmark, Risø, Roskilde, Denmark
M. Ješkovský
Centre for Nuclear and Accelerator Technologies (CENTA), Department of Nuclear Physics and Biophysics, Faculty of Mathematics, Physics and Informatics, Comenius University, 84248 Bratislava, Slovakia
A. J. T. Jull
NSF Arizona AMS Laboratory, University of Arizona, Tucson, Arizona 85721, USA
Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA
Institute for Nuclear Research (ATOMKI), 4026 Debrecen, Hungary
J. Kaizer
Centre for Nuclear and Accelerator Technologies (CENTA), Department of Nuclear Physics and Biophysics, Faculty of Mathematics, Physics and Informatics, Comenius University, 84248 Bratislava, Slovakia
M. Nakano
Japan Atomic Energy Agency, 4-33 Muramatsu, Tokai-mura, Naka-gun, Ibaraki 319-1194, Japan
H. Nies
Environment Laboratories, International Atomic Energy Agency, Monte Carlo 9800, Monaco
L. Palcsu
Institute for Nuclear Research (ATOMKI), 4026 Debrecen, Hungary
L. Papp
Institute for Nuclear Research (ATOMKI), 4026 Debrecen, Hungary
M. K. Pham
Environment Laboratories, International Atomic Energy Agency, Monte Carlo 9800, Monaco
P. Steier
VERA Laboratory, Faculty of Physics, University of Vienna, Vienna, Austria
L. Y. Zhang
Center for Nuclear Technology, Technical University of Denmark, Risø, Roskilde, Denmark
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Yayoi Inomata and Michio Aoyama
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2022-374, https://doi.org/10.5194/essd-2022-374, 2022
Revised manuscript under review for ESSD
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Behavior of 137Cs in surface seawater in the global ocean was analyzed by using the Historical Artificial radioactivity database in Marine environment. Approximately 32 % of 137Cs existed in the surface seawater in 1970. The 137Cs released into the North Pacific Ocean by large scale nuclear weapons tests transported to the Indian Ocean and then Atlantic Ocean with 4-5 decadal, whereas 137Cs released from nuclear reprocessing plants transported northward in the Arctic Ocean with decadal scale.
Elena Ceballos-Romero, Ken O. Buesseler, and María Villa-Alfageme
Earth Syst. Sci. Data, 14, 2639–2679, https://doi.org/10.5194/essd-14-2639-2022, https://doi.org/10.5194/essd-14-2639-2022, 2022
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Thorium-234 is widely used for studying the removal rate of material on sinking particles from the upper ocean and for determining the downward flux of carbon. In this study, we present a compilation of the 50 years of 234Th measurements in the ocean and provide a broad overview of the character of the datasets. This provides a valuable resource useful to better understand and quantify how the contemporary oceanic carbon uptake functions and how it will change in future.
Daniel Glückman, Karin Hain, Claudia Joseph, Volker Metz, Francesca Quinto, Peter Steier, and Horst Geckeis
Saf. Nucl. Waste Disposal, 1, 153–154, https://doi.org/10.5194/sand-1-153-2021, https://doi.org/10.5194/sand-1-153-2021, 2021
Michio Aoyama, Sabine Charmasson, Yasunori Hamajima, Celine Duffa, Daisuke Tsumune, and Yutaka Tateda
Biogeosciences Discuss., https://doi.org/10.5194/bg-2021-10, https://doi.org/10.5194/bg-2021-10, 2021
Manuscript not accepted for further review
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Results of observations of the 3H activity concentrations at Fukushima coast showed the large effect of 3H flux through the rivers to coastal waters. The 3H activity concentration close to Fukushima accident site was significantly high compared to the 3H activity concentration in surrounding waters both north and south of the FNPP1 site and in river waters. The 3H/137Cs activity ratios in coastal waters were 1.2–2.2, which is significantly high compared to that observed just after the accident.
Michio Aoyama, Sabine Charmasson, Yasunori Hamajima, and Celine Duffa
Biogeosciences Discuss., https://doi.org/10.5194/bg-2020-491, https://doi.org/10.5194/bg-2020-491, 2021
Manuscript not accepted for further review
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Our results showed that the dissolved radiocaesium activities were generally higher at coastal sites and decreased with distance from shore. The portion of particulate 137Cs to the total 137Cs ranged from 0.13 to 0.96.
The ratio of 137Cs to 134Cs activity in organic particles did not change with distance from shore and generally remained around 1.
The 137Cs / 134Cs activity ratio in seawater was estimated to be 1.074 ± 0.015 which was in good agreement with the ratio of 1.06 in core unit 1.
Zoltán Kern, Dániel Erdélyi, Polona Vreča, Ines Krajcar Bronić, István Fórizs, Tjaša Kanduč, Marko Štrok, László Palcsu, Miklós Süveges, György Czuppon, Balázs Kohán, and István Gábor Hatvani
Earth Syst. Sci. Data, 12, 2061–2073, https://doi.org/10.5194/essd-12-2061-2020, https://doi.org/10.5194/essd-12-2061-2020, 2020
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Here we present the spatially continuous gridded database for amount-weighted annual mean tritium activity in precipitation for the period 1976 to 2017 for the Adriatic–Pannonian region, with a special focus on the years after 2010, which are not represented by existing global models. This AP3H database is capable of providing reliable spatiotemporal input for hydrogeological applications at any place within Slovenia, Hungary, and their surroundings.
Luyuan Zhang, Xiaolin Hou, Sheng Xu, Tian Feng, Peng Cheng, Yunchong Fu, and Ning Chen
Atmos. Chem. Phys., 20, 2623–2635, https://doi.org/10.5194/acp-20-2623-2020, https://doi.org/10.5194/acp-20-2623-2020, 2020
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To trace the long-range transport of air pollutants and understand the atmospheric effect of iodine, the daily-resolution temporal variations of 129I and 127I in aerosols from a monsoonal city indicate the East Asian monsoon and fossil fuel combustion plays crucial roles on transport of 129I from Europe to East Asia and on elevated 127I concentrations. Through linking iodine isotopes with five major air pollutants, this study proposes the possible role of iodine in urban air pollution.
Michio Aoyama
Earth Syst. Sci. Data, 12, 487–499, https://doi.org/10.5194/essd-12-487-2020, https://doi.org/10.5194/essd-12-487-2020, 2020
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A global nutrient gridded dataset that might be the basis for studies of more accurate spatial distributions of nutrients and their changes in the global ocean was created. This is an SI-traceable dataset of nitrate, phosphate, and silicate concentrations based on certified reference materials or reference materials (CRMs/RMs) of seawater nutrient concentration measurements used during many cruises by the author.
Yayoi Inomata, Michio Aoyama, Yasunori Hamajima, and Masatoshi Yamada
Ocean Sci., 14, 813–826, https://doi.org/10.5194/os-14-813-2018, https://doi.org/10.5194/os-14-813-2018, 2018
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Analysing increased 137Cs and 134Cs / 137Cs ratio derived from the Fukushima Nuclear Power Plant accident in the Sea of Japan and its marginal sea, we found a rapid transport process associated with subduction in the subtropical mode water (STMW) formation region and obduction in the north East China Sea. The integrated amount of FNPP1 137Cs entering the Sea of Japan until 2016 was estimated to be 0.21 ± 0.03 PBq, which corresponds to 5.1 (3.4–8.0) % of the total amount of FNPP1 137Cs in the STMW.
Shigeto Nishino, Takashi Kikuchi, Amane Fujiwara, Toru Hirawake, and Michio Aoyama
Biogeosciences, 13, 2563–2578, https://doi.org/10.5194/bg-13-2563-2016, https://doi.org/10.5194/bg-13-2563-2016, 2016
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We analysed mooring and ship-based data obtained from a biological hotspot in the southern Chukchi Sea. Mooring data were collected for the first time in this site and were captured during spring and autumn blooms with high chlorophyll a concentrations. The data suggest that a dome-like structure of the bottom water and nutrient regeneration at the bottom play important roles in maintaining the autumn bloom of the biological hotspot.
Luyuan Zhang, Xiaolin Hou, and Sheng Xu
Atmos. Chem. Phys., 16, 1971–1985, https://doi.org/10.5194/acp-16-1971-2016, https://doi.org/10.5194/acp-16-1971-2016, 2016
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Speciation analysis of long-lived anthropogenic iodine isotopes (129I) in time series Danish aerosols shows that secondary emission from heavily 129I-contaminated seawater is a major source of 129I in the Atmosphere, at least in North Europe. Iodide is the major form of water-soluble iodine, while NaOH-soluble iodine is the dominant species of iodine in aerosol, which is likely bound with organic substances. The contribution of Fukushima-derived 129I is estimated to be negligible in Europe.
E. E. Black and K. O. Buesseler
Biogeosciences, 11, 5123–5137, https://doi.org/10.5194/bg-11-5123-2014, https://doi.org/10.5194/bg-11-5123-2014, 2014
T. P. Guilderson, S. J. Tumey, T. A. Brown, and K. O. Buesseler
Biogeosciences, 11, 4839–4852, https://doi.org/10.5194/bg-11-4839-2014, https://doi.org/10.5194/bg-11-4839-2014, 2014
J. Kameník, H. Dulaiova, K.O. Buesseler, S. M. Pike, and K. Št'astná
Biogeosciences, 10, 6045–6052, https://doi.org/10.5194/bg-10-6045-2013, https://doi.org/10.5194/bg-10-6045-2013, 2013
D. Tsumune, T. Tsubono, M. Aoyama, M. Uematsu, K. Misumi, Y. Maeda, Y. Yoshida, and H. Hayami
Biogeosciences, 10, 5601–5617, https://doi.org/10.5194/bg-10-5601-2013, https://doi.org/10.5194/bg-10-5601-2013, 2013
M. L. Estapa, K. Buesseler, E. Boss, and G. Gerbi
Biogeosciences, 10, 5517–5531, https://doi.org/10.5194/bg-10-5517-2013, https://doi.org/10.5194/bg-10-5517-2013, 2013
I. I. Rypina, S. R. Jayne, S. Yoshida, A. M. Macdonald, E. Douglass, and K. Buesseler
Biogeosciences, 10, 4973–4990, https://doi.org/10.5194/bg-10-4973-2013, https://doi.org/10.5194/bg-10-4973-2013, 2013
N. Casacuberta, P. Masqué, J. Garcia-Orellana, R. Garcia-Tenorio, and K.O. Buesseler
Biogeosciences, 10, 3649–3659, https://doi.org/10.5194/bg-10-3649-2013, https://doi.org/10.5194/bg-10-3649-2013, 2013
M. Aoyama, M. Uematsu, D. Tsumune, and Y. Hamajima
Biogeosciences, 10, 3067–3078, https://doi.org/10.5194/bg-10-3067-2013, https://doi.org/10.5194/bg-10-3067-2013, 2013
M. A. Charette, C. F. Breier, P. B. Henderson, S. M. Pike, I. I. Rypina, S. R. Jayne, and K. O. Buesseler
Biogeosciences, 10, 2159–2167, https://doi.org/10.5194/bg-10-2159-2013, https://doi.org/10.5194/bg-10-2159-2013, 2013
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Biogeosciences, 19, 5401–5418, https://doi.org/10.5194/bg-19-5401-2022, https://doi.org/10.5194/bg-19-5401-2022, 2022
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We have investigated the adaptive response of phytoplankton growth to changing light, nutrients, and temperature over the North Pacific using two physical-biological models. We compare modeled chlorophyll and primary production from an inflexible control model (InFlexPFT), which assumes fixed carbon (C):nitrogen (N):chlorophyll (Chl) ratios, to a recently developed flexible phytoplankton functional type model (FlexPFT), which incorporates photoacclimation and variable C:N:Chl ratios.
Jens Terhaar, Thomas L. Frölicher, and Fortunat Joos
Biogeosciences, 19, 4431–4457, https://doi.org/10.5194/bg-19-4431-2022, https://doi.org/10.5194/bg-19-4431-2022, 2022
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Estimates of the ocean sink of anthropogenic carbon vary across various approaches. We show that the global ocean carbon sink can be estimated by three parameters, two of which approximate the ocean ventilation in the Southern Ocean and the North Atlantic, and one of which approximates the chemical capacity of the ocean to take up carbon. With observations of these parameters, we estimate that the global ocean carbon sink is 10 % larger than previously assumed, and we cut uncertainties in half.
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Biogeosciences, 19, 3209–3224, https://doi.org/10.5194/bg-19-3209-2022, https://doi.org/10.5194/bg-19-3209-2022, 2022
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Zhibo Shao and Ya-Wei Luo
Biogeosciences, 19, 2939–2952, https://doi.org/10.5194/bg-19-2939-2022, https://doi.org/10.5194/bg-19-2939-2022, 2022
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Non-cyanobacterial diazotrophs (NCDs) may be an important player in fixing N2 in the ocean. By conducting meta-analyses, we found that a representative marine NCD phylotype, Gamma A, tends to inhabit ocean environments with high productivity, low iron concentration and high light intensity. It also appears to be more abundant inside cyclonic eddies. Our study suggests a niche differentiation of NCDs from cyanobacterial diazotrophs as the latter prefers low-productivity and high-iron oceans.
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Biogeosciences, 19, 2599–2625, https://doi.org/10.5194/bg-19-2599-2022, https://doi.org/10.5194/bg-19-2599-2022, 2022
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Decadal trends of fugacity of CO2 (fCO2), total alkalinity (AT), total carbon (CT) and pH in surface waters are investigated in different domains of the southern Indian Ocean (45°S–57°S) from ongoing and station observations regularly conducted in summer over the period 1998–2019. The fCO2 increase and pH decrease are mainly driven by anthropogenic CO2 estimated just below the summer mixed layer, as well as by a warming south of the polar front or in the fertilized waters near Kerguelen Island.
Priscilla Le Mézo, Jérôme Guiet, Kim Scherrer, Daniele Bianchi, and Eric Galbraith
Biogeosciences, 19, 2537–2555, https://doi.org/10.5194/bg-19-2537-2022, https://doi.org/10.5194/bg-19-2537-2022, 2022
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This study quantifies the role of commercially targeted fish biomass in the cycling of three important nutrients (N, P, and Fe), relative to nutrients otherwise available in water and to nutrients required by primary producers, and the impact of fishing. We use a model of commercially targeted fish biomass constrained by fish catch and stock assessment data to assess the contributions of fish at the global scale, at the time of the global peak catch and prior to industrial fishing.
Rebecca Chmiel, Nathan Lanning, Allison Laubach, Jong-Mi Lee, Jessica Fitzsimmons, Mariko Hatta, William Jenkins, Phoebe Lam, Matthew McIlvin, Alessandro Tagliabue, and Mak Saito
Biogeosciences, 19, 2365–2395, https://doi.org/10.5194/bg-19-2365-2022, https://doi.org/10.5194/bg-19-2365-2022, 2022
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Dissolved cobalt is present in trace amounts in seawater and is a necessary nutrient for marine microbes. On a transect from the Alaskan coast to Tahiti, we measured seawater concentrations of dissolved cobalt. Here, we describe several interesting features of the Pacific cobalt cycle including cobalt sources along the Alaskan coast and Hawaiian vents, deep-ocean particle formation, cobalt activity in low-oxygen regions, and how our samples compare to a global biogeochemical model’s predictions.
Nicolas Metzl, Claire Lo Monaco, Coraline Leseurre, Céline Ridame, Jonathan Fin, Claude Mignon, Marion Gehlen, and Thi Tuyet Trang Chau
Biogeosciences, 19, 1451–1468, https://doi.org/10.5194/bg-19-1451-2022, https://doi.org/10.5194/bg-19-1451-2022, 2022
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During an oceanographic cruise conducted in January 2020 in the south-western Indian Ocean, we observed very low CO2 concentrations associated with a strong phytoplankton bloom that occurred south-east of Madagascar. This biological event led to a strong regional CO2 ocean sink not previously observed.
Darren R. Clark, Andrew P. Rees, Charissa M. Ferrera, Lisa Al-Moosawi, Paul J. Somerfield, Carolyn Harris, Graham D. Quartly, Stephen Goult, Glen Tarran, and Gennadi Lessin
Biogeosciences, 19, 1355–1376, https://doi.org/10.5194/bg-19-1355-2022, https://doi.org/10.5194/bg-19-1355-2022, 2022
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Measurements of microbial processes were made in the sunlit open ocean during a research cruise (AMT19) between the UK and Chile. These help us to understand how microbial communities maintain the function of remote ecosystems. We find that the nitrogen cycling microbes which produce nitrite respond to changes in the environment. Our insights will aid the development of models that aim to replicate and ultimately project how marine environments may respond to ongoing climate change.
Martí Galí, Marcus Falls, Hervé Claustre, Olivier Aumont, and Raffaele Bernardello
Biogeosciences, 19, 1245–1275, https://doi.org/10.5194/bg-19-1245-2022, https://doi.org/10.5194/bg-19-1245-2022, 2022
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Part of the organic matter produced by plankton in the upper ocean is exported to the deep ocean. This process, known as the biological carbon pump, is key for the regulation of atmospheric carbon dioxide and global climate. However, the dynamics of organic particles below the upper ocean layer are not well understood. Here we compared the measurements acquired by autonomous robots in the top 1000 m of the ocean to a numerical model, which can help improve future climate projections.
Marie Barbieux, Julia Uitz, Alexandre Mignot, Collin Roesler, Hervé Claustre, Bernard Gentili, Vincent Taillandier, Fabrizio D'Ortenzio, Hubert Loisel, Antoine Poteau, Edouard Leymarie, Christophe Penkerc'h, Catherine Schmechtig, and Annick Bricaud
Biogeosciences, 19, 1165–1194, https://doi.org/10.5194/bg-19-1165-2022, https://doi.org/10.5194/bg-19-1165-2022, 2022
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This study assesses marine biological production in two Mediterranean systems representative of vast desert-like (oligotrophic) areas encountered in the global ocean. We use a novel approach based on non-intrusive high-frequency in situ measurements by two profiling robots, the BioGeoChemical-Argo (BGC-Argo) floats. Our results indicate substantial yet variable production rates and contribution to the whole water column of the subsurface layer, typically considered steady and non-productive.
Filippa Fransner, Friederike Fröb, Jerry Tjiputra, Nadine Goris, Siv K. Lauvset, Ingunn Skjelvan, Emil Jeansson, Abdirahman Omar, Melissa Chierici, Elizabeth Jones, Agneta Fransson, Sólveig R. Ólafsdóttir, Truls Johannessen, and Are Olsen
Biogeosciences, 19, 979–1012, https://doi.org/10.5194/bg-19-979-2022, https://doi.org/10.5194/bg-19-979-2022, 2022
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Ocean acidification, a direct consequence of the CO2 release by human activities, is a serious threat to marine ecosystems. In this study, we conduct a detailed investigation of the acidification of the Nordic Seas, from 1850 to 2100, by using a large set of samples taken during research cruises together with numerical model simulations. We estimate the effects of changes in different environmental factors on the rate of acidification and its potential effects on cold-water corals.
Guorong Zhong, Xuegang Li, Jinming Song, Baoxiao Qu, Fan Wang, Yanjun Wang, Bin Zhang, Xiaoxia Sun, Wuchang Zhang, Zhenyan Wang, Jun Ma, Huamao Yuan, and Liqin Duan
Biogeosciences, 19, 845–859, https://doi.org/10.5194/bg-19-845-2022, https://doi.org/10.5194/bg-19-845-2022, 2022
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A predictor selection algorithm was constructed to decrease the predicting error in the surface ocean partial pressure of CO2 (pCO2) mapping by finding better combinations of pCO2 predictors in different regions. Compared with previous research using the same combination of predictors in all regions, using different predictors selected by the algorithm in different regions can effectively decrease pCO2 predicting errors.
Shantelle Smith, Katye E. Altieri, Mhlangabezi Mdutyana, David R. Walker, Ruan G. Parrott, Sedick Gallie, Kurt A. M. Spence, Jessica M. Burger, and Sarah E. Fawcett
Biogeosciences, 19, 715–741, https://doi.org/10.5194/bg-19-715-2022, https://doi.org/10.5194/bg-19-715-2022, 2022
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Ammonium is a crucial yet poorly understood component of the Southern Ocean nitrogen cycle. We attribute our finding of consistently high ammonium concentrations in the winter mixed layer to limited ammonium consumption and sustained ammonium production, conditions under which the Southern Ocean becomes a source of carbon dioxide to the atmosphere. From similar data collected over an annual cycle, we propose a seasonal cycle for ammonium in shallow polar waters – a first for the Southern Ocean.
Jannes Koelling, Dariia Atamanchuk, Johannes Karstensen, Patricia Handmann, and Douglas W. R. Wallace
Biogeosciences, 19, 437–454, https://doi.org/10.5194/bg-19-437-2022, https://doi.org/10.5194/bg-19-437-2022, 2022
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In this study, we investigate oxygen variability in the deep western boundary current in the Labrador Sea from multiyear moored records. We estimate that about half of the oxygen taken up in the interior Labrador Sea by air–sea gas exchange during deep water formation is exported southward the same year. Our results underline the complexity of the oxygen uptake and export in the Labrador Sea and highlight the important role this region plays in supplying oxygen to the deep ocean.
Céline Ridame, Julie Dinasquet, Søren Hallstrøm, Estelle Bigeard, Lasse Riemann, France Van Wambeke, Matthieu Bressac, Elvira Pulido-Villena, Vincent Taillandier, Fréderic Gazeau, Antonio Tovar-Sanchez, Anne-Claire Baudoux, and Cécile Guieu
Biogeosciences, 19, 415–435, https://doi.org/10.5194/bg-19-415-2022, https://doi.org/10.5194/bg-19-415-2022, 2022
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We show that in the Mediterranean Sea spatial variability in N2 fixation is related to the diazotrophic community composition reflecting different nutrient requirements among species. Nutrient supply by Saharan dust is of great importance to diazotrophs, as shown by the strong stimulation of N2 fixation after a simulated dust event under present and future climate conditions; the magnitude of stimulation depends on the degree of limitation related to the diazotrophic community composition.
Matthew P. Humphreys, Erik H. Meesters, Henk de Haas, Szabina Karancz, Louise Delaigue, Karel Bakker, Gerard Duineveld, Siham de Goeyse, Andreas F. Haas, Furu Mienis, Sharyn Ossebaar, and Fleur C. van Duyl
Biogeosciences, 19, 347–358, https://doi.org/10.5194/bg-19-347-2022, https://doi.org/10.5194/bg-19-347-2022, 2022
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A series of submarine sinkholes were recently discovered on Luymes Bank, part of Saba Bank, a carbonate platform in the Caribbean Netherlands. Here, we investigate the waters inside these sinkholes for the first time. One of the sinkholes contained a body of dense, low-oxygen and low-pH water, which we call the
acid lake. We use measurements of seawater chemistry to work out what processes were responsible for forming the acid lake and discuss the consequences for the carbonate platform.
Gerhard Fischer, Oscar E. Romero, Johannes Karstensen, Karl-Heinz Baumann, Nasrollah Moradi, Morten Iversen, Götz Ruhland, Marco Klann, and Arne Körtzinger
Biogeosciences, 18, 6479–6500, https://doi.org/10.5194/bg-18-6479-2021, https://doi.org/10.5194/bg-18-6479-2021, 2021
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Low-oxygen eddies in the eastern subtropical North Atlantic can form an oasis for phytoplankton growth. Here we report on particle flux dynamics at the oligotrophic Cape Verde Ocean Observatory. We observed consistent flux patterns during the passages of low-oxygen eddies. We found distinct flux peaks in late winter, clearly exceeding background fluxes. Our findings suggest that the low-oxygen eddies sequester higher organic carbon than expected for oligotrophic settings.
Matthieu Bressac, Thibaut Wagener, Nathalie Leblond, Antonio Tovar-Sánchez, Céline Ridame, Vincent Taillandier, Samuel Albani, Sophie Guasco, Aurélie Dufour, Stéphanie H. M. Jacquet, François Dulac, Karine Desboeufs, and Cécile Guieu
Biogeosciences, 18, 6435–6453, https://doi.org/10.5194/bg-18-6435-2021, https://doi.org/10.5194/bg-18-6435-2021, 2021
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Phytoplankton growth is limited by the availability of iron in about 50 % of the ocean. Atmospheric deposition of desert dust represents a key source of iron. Here, we present direct observations of dust deposition in the Mediterranean Sea. A key finding is that the input of iron from dust primarily occurred in the deep ocean, while previous studies mainly focused on the ocean surface. This new insight will enable us to better represent controls on global marine productivity in models.
Léo Berline, Andrea Michelangelo Doglioli, Anne Petrenko, Stéphanie Barrillon, Boris Espinasse, Frederic A. C. Le Moigne, François Simon-Bot, Melilotus Thyssen, and François Carlotti
Biogeosciences, 18, 6377–6392, https://doi.org/10.5194/bg-18-6377-2021, https://doi.org/10.5194/bg-18-6377-2021, 2021
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While the Ionian Sea is considered a nutrient-depleted and low-phytoplankton biomass area, it is a crossroad for water mass circulation. In the central Ionian Sea, we observed a strong contrast in particle distribution across a ~100 km long transect. Using remote sensing and Lagrangian simulations, we suggest that this contrast finds its origin in the long-distance transport of particles from the north, west and east of the Ionian Sea, where phytoplankton production was more intense.
Anna Teruzzi, Giorgio Bolzon, Laura Feudale, and Gianpiero Cossarini
Biogeosciences, 18, 6147–6166, https://doi.org/10.5194/bg-18-6147-2021, https://doi.org/10.5194/bg-18-6147-2021, 2021
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During summer, maxima of phytoplankton chlorophyll concentration (DCM) occur in the subsurface of the Mediterranean Sea and can play a relevant role in carbon sequestration into the ocean interior. A numerical model based on in situ and satellite observations provides insights into the range of DCM conditions across the relatively small Mediterranean Sea and shows a western DCM that is 25 % shallower and with a higher phytoplankton chlorophyll concentration than in the eastern Mediterranean.
Elvira Pulido-Villena, Karine Desboeufs, Kahina Djaoudi, France Van Wambeke, Stéphanie Barrillon, Andrea Doglioli, Anne Petrenko, Vincent Taillandier, Franck Fu, Tiphanie Gaillard, Sophie Guasco, Sandra Nunige, Sylvain Triquet, and Cécile Guieu
Biogeosciences, 18, 5871–5889, https://doi.org/10.5194/bg-18-5871-2021, https://doi.org/10.5194/bg-18-5871-2021, 2021
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We report on phosphorus dynamics in the surface layer of the Mediterranean Sea. Highly sensitive phosphate measurements revealed vertical gradients above the phosphacline. The relative contribution of diapycnal fluxes to total external supply of phosphate to the mixed layer decreased towards the east, where atmospheric deposition dominated. Taken together, external sources of phosphate contributed little to total supply, which was mainly sustained by enzymatic hydrolysis of organic phosphorus.
Zouhair Lachkar, Michael Mehari, Muchamad Al Azhar, Marina Lévy, and Shafer Smith
Biogeosciences, 18, 5831–5849, https://doi.org/10.5194/bg-18-5831-2021, https://doi.org/10.5194/bg-18-5831-2021, 2021
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This study documents and quantifies a significant recent oxygen decline in the upper layers of the Arabian Sea and explores its drivers. Using a modeling approach we show that the fast local warming of sea surface is the main factor causing this oxygen drop. Concomitant summer monsoon intensification contributes to this trend, although to a lesser extent. These changes exacerbate oxygen depletion in the subsurface, threatening marine habitats and altering the local biogeochemistry.
France Van Wambeke, Vincent Taillandier, Karine Desboeufs, Elvira Pulido-Villena, Julie Dinasquet, Anja Engel, Emilio Marañón, Céline Ridame, and Cécile Guieu
Biogeosciences, 18, 5699–5717, https://doi.org/10.5194/bg-18-5699-2021, https://doi.org/10.5194/bg-18-5699-2021, 2021
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Simultaneous in situ measurements of (dry and wet) atmospheric deposition and biogeochemical stocks and fluxes in the sunlit waters of the open Mediterranean Sea revealed complex physical and biological processes occurring within the mixed layer. Nitrogen (N) budgets were computed to compare the sources and sinks of N in the mixed layer. The transitory effect observed after a wet dust deposition impacted the microbial food web down to the deep chlorophyll maximum.
Frédéric Gazeau, France Van Wambeke, Emilio Marañón, Maria Pérez-Lorenzo, Samir Alliouane, Christian Stolpe, Thierry Blasco, Nathalie Leblond, Birthe Zäncker, Anja Engel, Barbara Marie, Julie Dinasquet, and Cécile Guieu
Biogeosciences, 18, 5423–5446, https://doi.org/10.5194/bg-18-5423-2021, https://doi.org/10.5194/bg-18-5423-2021, 2021
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Our study shows that the impact of dust deposition on primary production depends on the initial composition and metabolic state of the tested community and is constrained by the amount of nutrients added, to sustain both the fast response of heterotrophic prokaryotes and the delayed one of phytoplankton. Under future environmental conditions, heterotrophic metabolism will be more impacted than primary production, therefore reducing the capacity of surface waters to sequester anthropogenic CO2.
Loes J. A. Gerringa, Martha Gledhill, Indah Ardiningsih, Niels Muntjewerf, and Luis M. Laglera
Biogeosciences, 18, 5265–5289, https://doi.org/10.5194/bg-18-5265-2021, https://doi.org/10.5194/bg-18-5265-2021, 2021
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For 3 decades, competitive ligand exchange–adsorptive cathodic stripping voltammetry was used to estimate the Fe-binding capacity of organic matter in seawater. In this paper the performance of the competing ligands is compared through the analysis of a series of model ligands.
The main finding of this paper is that the determined speciation parameters are not independent of the application, making interpretation of Fe speciation data more complex than it was thought before.
Frédéric Gazeau, Céline Ridame, France Van Wambeke, Samir Alliouane, Christian Stolpe, Jean-Olivier Irisson, Sophie Marro, Jean-Michel Grisoni, Guillaume De Liège, Sandra Nunige, Kahina Djaoudi, Elvira Pulido-Villena, Julie Dinasquet, Ingrid Obernosterer, Philippe Catala, and Cécile Guieu
Biogeosciences, 18, 5011–5034, https://doi.org/10.5194/bg-18-5011-2021, https://doi.org/10.5194/bg-18-5011-2021, 2021
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This paper shows that the impacts of Saharan dust deposition in different Mediterranean basins are as strong as those observed in coastal waters but differed substantially between the three tested stations, differences attributed to variable initial metabolic states. A stronger impact of warming and acidification on mineralization suggests a decreased capacity of Mediterranean surface communities to sequester CO2 following the deposition of atmospheric particles in the coming decades.
Carolin R. Löscher
Biogeosciences, 18, 4953–4963, https://doi.org/10.5194/bg-18-4953-2021, https://doi.org/10.5194/bg-18-4953-2021, 2021
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The Bay of Bengal (BoB) is classically seen as an ocean region with low primary production, which has been predicted to decrease even further. Here, the importance of such a trend is used to explore what could happen to the BoB's low-oxygen core waters if primary production decreases. Lower biological production leads to less oxygen loss in deeper waters by respiration; thus it could be that oxygen will not further decrease and the BoB will not become anoxic, different to other low-oxygen areas.
Bo Liu, Katharina D. Six, and Tatiana Ilyina
Biogeosciences, 18, 4389–4429, https://doi.org/10.5194/bg-18-4389-2021, https://doi.org/10.5194/bg-18-4389-2021, 2021
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We incorporate a new representation of the stable carbon isotope 13C in a global ocean biogeochemistry model. The model well reproduces the present-day 13C observations. We find a recent observation-based estimate of the oceanic 13C Suess effect (the decrease in 13C/12C ratio due to uptake of anthropogenic CO2; 13CSE) possibly underestimates 13CSE by 0.1–0.26 per mil. The new model will aid in better understanding the past ocean state via comparison to 13C/12C measurements from sediment cores.
Neil J. Wyatt, Angela Milne, Eric P. Achterberg, Thomas J. Browning, Heather A. Bouman, E. Malcolm S. Woodward, and Maeve C. Lohan
Biogeosciences, 18, 4265–4280, https://doi.org/10.5194/bg-18-4265-2021, https://doi.org/10.5194/bg-18-4265-2021, 2021
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Using data collected during two expeditions to the South Atlantic Ocean, we investigated how the interaction between external sources and biological activity influenced the availability of the trace metals zinc and cobalt. This is important as both metals play essential roles in the metabolism and growth of phytoplankton and thus influence primary productivity of the oceans. We found seasonal changes in both processes that helped explain upper-ocean trace metal cycling.
Hannah L. Bourne, James K. B. Bishop, Elizabeth J. Connors, and Todd J. Wood
Biogeosciences, 18, 3053–3086, https://doi.org/10.5194/bg-18-3053-2021, https://doi.org/10.5194/bg-18-3053-2021, 2021
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To learn how the biological carbon pump works in productive coastal upwelling systems, four autonomous carbon flux explorers measured carbon flux through the twilight zone beneath an offshore-flowing filament of biologically productive water. Strikingly different particle classes dominated the carbon fluxes during successive stages of the filament evolution over 30 d. Both flux and transfer efficiency were far greater than expected, suggesting an outsized filament impact in California waters.
Matthieu Roy-Barman, Lorna Foliot, Eric Douville, Nathalie Leblond, Fréderic Gazeau, Matthieu Bressac, Thibaut Wagener, Céline Ridame, Karine Desboeufs, and Cécile Guieu
Biogeosciences, 18, 2663–2678, https://doi.org/10.5194/bg-18-2663-2021, https://doi.org/10.5194/bg-18-2663-2021, 2021
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The release of insoluble elements such as aluminum (Al), iron (Fe), rare earth elements (REEs), thorium (Th) and protactinium (Pa) when Saharan dust falls over the Mediterranean Sea was studied during tank experiments under present and future climate conditions. Each element exhibited different dissolution kinetics and dissolution fractions (always lower than a few percent). Changes in temperature and/or pH under greenhouse conditions lead to a lower Th release and a higher light REE release.
Stéphanie H. M. Jacquet, Dominique Lefèvre, Christian Tamburini, Marc Garel, Frédéric A. C. Le Moigne, Nagib Bhairy, and Sophie Guasco
Biogeosciences, 18, 2205–2212, https://doi.org/10.5194/bg-18-2205-2021, https://doi.org/10.5194/bg-18-2205-2021, 2021
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We present new data concerning the relation between biogenic barium (Baxs, a tracer of carbon remineralization at mesopelagic depths), O2 consumption and prokaryotic heterotrophic production (PHP) in the Mediterranean Sea. The purpose of this paper is to improve our understanding of the relation between Baxs, PHP and O2 and to test the validity of the Dehairs transfer function in the Mediterranean Sea. This relation has never been tested in the Mediterranean Sea.
Natacha Le Grix, Jakob Zscheischler, Charlotte Laufkötter, Cecile S. Rousseaux, and Thomas L. Frölicher
Biogeosciences, 18, 2119–2137, https://doi.org/10.5194/bg-18-2119-2021, https://doi.org/10.5194/bg-18-2119-2021, 2021
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Marine ecosystems could suffer severe damage from the co-occurrence of a marine heat wave with extremely low chlorophyll concentration. Here, we provide a first assessment of compound marine heat wave and
low-chlorophyll events in the global ocean from 1998 to 2018. We reveal hotspots of these compound events in the equatorial Pacific and in the Arabian Sea and show that they mostly occur in summer at high latitudes and their frequency is modulated by large-scale modes of climate variability.
Christopher Holder and Anand Gnanadesikan
Biogeosciences, 18, 1941–1970, https://doi.org/10.5194/bg-18-1941-2021, https://doi.org/10.5194/bg-18-1941-2021, 2021
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A challenge for marine ecologists in studying phytoplankton is linking small-scale relationships found in a lab to broader relationships observed on large scales in the environment. We investigated whether machine learning (ML) could help connect these small- and large-scale relationships. ML was able to provide qualitative information about the small-scale processes from large-scale information. This method could help identify important relationships from observations in future research.
Paul J. Tréguer, Jill N. Sutton, Mark Brzezinski, Matthew A. Charette, Timothy Devries, Stephanie Dutkiewicz, Claudia Ehlert, Jon Hawkings, Aude Leynaert, Su Mei Liu, Natalia Llopis Monferrer, María López-Acosta, Manuel Maldonado, Shaily Rahman, Lihua Ran, and Olivier Rouxel
Biogeosciences, 18, 1269–1289, https://doi.org/10.5194/bg-18-1269-2021, https://doi.org/10.5194/bg-18-1269-2021, 2021
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Silicon is the second most abundant element of the Earth's crust. In this review, we show that silicon inputs and outputs, to and from the world ocean, are 57 % and 37 % higher, respectively, than previous estimates. These changes are significant, modifying factors such as the geochemical residence time of silicon, which is now about 8000 years and 2 times faster than previously assumed. We also update the total biogenic silica pelagic production and provide an estimate for sponge production.
Caroline Ulses, Claude Estournel, Marine Fourrier, Laurent Coppola, Fayçal Kessouri, Dominique Lefèvre, and Patrick Marsaleix
Biogeosciences, 18, 937–960, https://doi.org/10.5194/bg-18-937-2021, https://doi.org/10.5194/bg-18-937-2021, 2021
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We analyse the seasonal cycle of O2 and estimate an annual O2 budget in the north-western Mediterranean deep-convection region, using a numerical model. We show that this region acts as a large sink of atmospheric O2 and as a major source of O2 for the western Mediterranean Sea. The decrease in the deep convection intensity predicted in recent projections may have important consequences on the overall uptake of O2 in the Mediterranean Sea and on the O2 exchanges with the Atlantic Ocean.
Fuminori Hashihama, Hiroaki Saito, Taketoshi Kodama, Saori Yasui-Tamura, Jota Kanda, Iwao Tanita, Hiroshi Ogawa, E. Malcolm S. Woodward, Philip W. Boyd, and Ken Furuya
Biogeosciences, 18, 897–915, https://doi.org/10.5194/bg-18-897-2021, https://doi.org/10.5194/bg-18-897-2021, 2021
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We investigated the nutrient assimilation characteristics of deep-water-induced phytoplankton blooms across the subtropical North and South Pacific Ocean. Nutrient drawdown ratios of dissolved inorganic nitrogen to phosphate were anomalously low in the western North Pacific, likely due to the high phosphate uptake capability of low-phosphate-adapted phytoplankton. The anomalous phosphate uptake might influence the maintenance of chronic phosphate depletion in the western North Pacific.
Florian Ricour, Arthur Capet, Fabrizio D'Ortenzio, Bruno Delille, and Marilaure Grégoire
Biogeosciences, 18, 755–774, https://doi.org/10.5194/bg-18-755-2021, https://doi.org/10.5194/bg-18-755-2021, 2021
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This paper addresses the phenology of the deep chlorophyll maximum (DCM) in the Black Sea (BS). We show that the DCM forms in March at a density level set by the winter mixed layer. It maintains this location until June, suggesting an influence of the DCM on light and nutrient profiles rather than mere adaptation to external factors. In summer, the DCM concentrates ~55 % of the chlorophyll in a 10 m layer at ~35 m depth and should be considered a major feature of the BS phytoplankton dynamics.
Robyn E. Tuerena, Joanne Hopkins, Raja S. Ganeshram, Louisa Norman, Camille de la Vega, Rachel Jeffreys, and Claire Mahaffey
Biogeosciences, 18, 637–653, https://doi.org/10.5194/bg-18-637-2021, https://doi.org/10.5194/bg-18-637-2021, 2021
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The Barents Sea is a rapidly changing shallow sea within the Arctic. Here, nitrate, an essential nutrient, is fully consumed by algae in surface waters during summer months. Nitrate is efficiently regenerated in the Barents Sea, and there is no evidence for nitrogen loss from the sediments by denitrification, which is prevalent on other Arctic shelves. This suggests that nitrogen availability in the Barents Sea is largely determined by the supply of nutrients in water masses from the Atlantic.
Cited articles
Aarkrog, A., Baxter, M. S., Bettencourt, A. O., Bojanowski, R., Bologa, A., Charmasson, S., Cunha, I., Delfanti, R., Duran, E., Holm, E., Jeffree, R., Livingston, H. D., Mahapanyawong, S., Nies, H., Osvath, I., Pingyu, L., Povinec, P. P., Sanchez, A., Smith, J. N., and Swift, D.: A comparison of doses from 137Cs and 210Po in marine food: A major international study, J. Environ. Radioact., 34, 69–90, 1997.
Aldahan, A., Alfimov, V., and Possnert, G.: 129I anthropogenic budget: Major source and sink, Appl. Geochem., 22, 606–618, 2007.
Aoyama, M. and Hirose, K.: Artificial radionuclides database in the Pacific Ocean: HAM database, Sci. World J., 4, 200–215, 2004.
Aoyama, M., Hirose, K., and Igarashi, Y.: Re-construction and up-dating our understanding on the global weapons tests 137Cs fallout, J. Environ. Monitor., 8, 431–438, 2006.
Aoyama, M., Tsumune, D., and Hamajima, Y.: Distribution of 137Cs and 134Cs in the North Pacific Ocean: impacts of the TEPCO Fukushima-Daiichi NPP accident, J. Radioanal. Nucl. Chem., https://doi.org/10.1007/s10967-012-2033-2, 2012.
Aoyama, M., Uematsu, M., Tsumune, D., and Hamajima, Y.: Surface pathway of radioactive plume of TEPCO Fukushima NPP1 released 134Cs and 137Cs, Biogeosciences, 10, 3067–3078, https://doi.org/10.5194/bg-10-3067-2013, 2013.
Bailly du Bois, P., Laguionie, P., Boust, D., Korsakissok, I., Didier, D., and Fievet, B.: Estimation of marine source-term following Fukushima Dai-ichi accident, J. Environ. Radioact., 114, 2–9, 2012.
Biddulph, D. L., Beck, J. W., Burr, G. S., Donahue D. J., Hatheway, A. L., and Jull, A. J. T.: Measurement of the radioisotope 129I at the NSF-Arizona AMS, Nucl. Instrum. Methods Phys. Res. B, 172, 693–698, 2000.
Bowyer, T. W., Biegalski, S. R., Cooper, M., Eslinger, P. W., Haas, D., Hayes, J. C., Miley, H. S., Strom, D. J., and Woods, V.: Elevated radioxenon detected remotely following the Fukushima nuclear accident, J. Environ. Radioact., 102, 681–687, 2011.
Buesseler, K., Aoyama, M., and Fukasawa, M.: Impacts of the Fukushima nuclear power plants on marine radioactivity, Environ. Sci. Technol., 45, 9931–9935, 2011.
Buesseler, K. O., Jayne, S. R., Fisher, N. S., Rypina, I. I., Baumann, H., Baumann, Z., Breier, C. F., Douglass, E. M., George, J., Macdonald, A. M., Miyamoto, H., Nishikawa, J., Pike, S. M., and Yoshida, S.: Fukushima-derived radionuclides in the ocean and biota off Japan, P. Natl. Acad. Sci. USA, 109, 5984–5988, 2012.
Casacuberta, N., Masqué, P., Garcia-Orellana, J., Garcia-Tenorio, R., and Buesseler, K. O.: 90Sr and 89Sr in seawater off Japan as a consequence of the Fukushima Dai-ichi nuclear accident, Biogeosciences, 10, 3649–3659, https://doi.org/10.5194/bg-10-3649-2013, 2013.
Charette, M. A., Breier, C. F., Henderson, P. B., Pike, S. M., Rypina, I. I., Jayne, S. R., and Buesseler, K. O.: Radium-based estimates of cesium isotope transport and total direct ocean discharges from the Fukushima Nuclear Power Plant accident, Biogeosciences, 10, 2159–2167, https://doi.org/10.5194/bg-10-2159-2013, 2013.
Chino, M., Nakayama, H., Nagai, H., Terada, H., Katata, G., and Yamazawa, H.: Preliminary estimation of release amounts of 131I and 137Cs accidentally discharged from the Fukushima Daiichi nuclear power plant into the atmosphere, J. Nucl. Sci. Technol., 48, 1129–1134, 2011.
Dietze, H. and Kriest, I.: 137Cs off Fukushima Dai-ichi, Japan – model based estimates of dilution and fate, Ocean Sci., 8, 319–332, https://doi.org/10.5194/os-8-319-2012, 2012.
He, P., Aldahan, A., Possnert, G., and Hou, X.: A summary of global 129I in marine waters, Nucl. Instrum. Methods Phys. Res. B, 294, 537–541, 2013.
Hernández-Ceballos, M. A., Hong, G. H., Lozano, R. L., Kim, Y. I., Lee, H. M., Kim, S. H., Yeh, S. W., Bolívar, J. P., and Baskaran, M.: Tracking the complete revolution of surface westerlies over Northern Hemisphere using radionuclides emitted from Fukushima, Sci. Total Environ., 438, 80–85, 2012.
Hirose, K.: Fukushima Dai-ichi nuclear power plant accident: summary of regional radioactive deposition monitoring results, J. Environ. Radioact., 111, 13–17, 2012.
Honda, M., Aono, T., Aoyama, M., Hamajima, Y., Kawakami, H., Kitamura, M., Masumoto, Y., Miyazawa, Y., Takigawa, M., and Saino, T.: Dispersion of artificial caesium-134 and -137 in the Western North Pacific one month after the Fukushima accident, Geochem. J., 46, 1–9, 2012.
Hou, X. L.: Determination of 14C and 3H in reactor graphite and concrete for decommission. Appl. Rad. Isotopes, 62, 871–882, 2005.
Hou, X. L., Dahlgaard, H., and Nielsen, S. P.: Iodine-129 time series in Danish, Norwegian and Northwest Greenland coast and the Baltic Sea by seaweed, Estuar. Coast. Shelf Sci., 51, 571–584, 2000.
Hou, X. L., Dahlgaard, H., and Nielsen, S. P.: Chemical speciation analysis of 129I in seawater and a preliminary investigation to use it as a tracer for geochemical cycle study of stable iodine, Mar. Chem., 74, 145–155, 2001.
Hou, X. L., Fogh, C. L., Kučera, J., Andersson, K. G., Dahlgaard, H., and Nielsen, S. P.: Iodine-129 and Cesium-137 in Chernobyl contaminated soil and their chemical fractionation, Sci. Total Environ., 308, 97–109, 2003.
Hou, X. L., Aldahan, A., Nislen, S., Possnert, G., Nies, H., and Hedfords, J.: Speciation of 129I and 127I in seawater and implications for sources and transport pathways in North Sea, Environ. Sci. Technol., 41, 5993–5999, 2007.
Hou, X. L., Aldahan, A., Nielsen, S. P., and Possnert, G.: Time Series of 129I and 127I Speciation in Precipitation from Denmark, Environ. Sci. Technol., 43, 6522–6528, 2009a.
Hou, X. L., Hansen, V., Aldahan, A., Possnert, G., Lind, O. C., and Lujaniene, G.: A review on speciation of iodine-129 in the environmental and biological samples, Anal. Chim. Acta, 632, 181–196, 2009b.
Hou, X. L., Povinec, P. P. L. Y., Zhang, L. Y., Biddulph, D., Chang, C.-C., Fan, Y. K., Golser, R., Ješkovský, M., Jull, A. J. T., Liu, Q., Shi, K. L., Steier, P., and Zhou, W. J.: Iodine-129 in seawater offshore Fukushima: Distribution, speciation, sources, and budget, Environ. Sci. Technol., 47, 3091–3098, 2013.
IAEA, International Atomic Energy Agency: Chernobyl's Legacy: Health, Environmental and Socio-Economic Impacts, IAEA, Vienna, 2003.
IAEA, International Atomic Energy Agency: Sediment Distribution Coefficients and Concentration Factors for Biota in the Marine Environment, Technical Reports Series no. 422, IAEA, Vienna, 2004.
IAEA, International Atomic Energy Agency: Worldwide marine radioactivity studies (WOMARS), Radionuclide levels in oceans and sea, IAEA-TECDOC-1429, IAEA, Vienna 2005.
IAEA, International Atomic Energy Agency: Briefings on Fukushima nuclear accident, www.iaea.org/, 2011.
Inomata, Y., Aoyama, M., and Hirose, K.: Analysis of 50-y record of surface 137Cs concentrations in the global ocean using the HAM-global database, J. Environ. Monitor., 11, 116–125, 2009.
Inoue, M., Kofuji, H., Nagao, S., Yamamoto, M., Hamajima, Y., Yoshida, K., Fujimoto, K., Takada, T. , and Isoda, Y.: Lateral variation of 134Cs and 137Cs concentrations in surface seawater in and around the Japan Sea after the Fukushima Dai-ichi Nuclear Power Plant accident, J. Environ. Radioact., 109, 45–51, 2012a.
Inoue, M., Kofuji, H., Y. Hamajima, Y., Nagao, S., Yoshida, K., and Yamamoto, M.: 134Cs and 137Cs activities in coastal seawater along Northern Sanriku and Tsugaru Strait, northeastern Japan, after Fukushima Dai-ichi Nuclear Power Plant accident, J. Environ. Radioact., 111, 116–119, 2012b.
Ito, T., Aramaki, Kitamura, T., Otosaka, S., Suzuki, T., Togawa, O., Kobayashi, T., Senjyu, T., Chaykovskaya, E. L., Karasev, E. V., Lishavskaya, T. S., Novichkov, V. P., Tkalin, A. V., Shcherbinin, A. F., and Volkov, Y. N.: Anthropogenic radionuclides in the Japan Sea: their distributions and transport processes, J. Environ. Radioact., 68, 249–267, 2003.
JG: Japanese Government Report, http://www.kantei.go.jp/jp/Topics/2011/iaea_houkokusho.html (last access: 10 July 2012), 2011.
Kanai, Y.: Monitoring of aerosol in Tsukuba after Fukushima nuclear power plant incident in 2011, J. Environ. Radioact., 111, 33–37, 2012.
Kawamura, H., Kobayashi, T., Furuno, A., In, T., Ishikawa, Y., Nakayama, T., Shima, S., and Awaji, T.: Preliminary numerical experiments on oceanic dispersion 131I and 137Cs discharged into the ocean because of the Fukushima Dai-ichi nuclear power plant disaster, J. Nucl. Sci. Technol., 48, 1349–1356, 2011.
Levy, I., Povinec, P. P., Aoyama, M., Hirose, K., Sanchez-Cabeza, J. A., Comanducci, J.-F., Gastaud, J., Eriksson, M., Hamajima, Y., Kim, C. S., Komura, K., Osvath, I., Roos, P., and Yim, S. A.: Marine anthropogenic radiotracers in the Southern Hemisphere: New sampling and analytical strategies, Progr. Oceanogr., 89, 120–133, 2011.
Livingston, H. D. and Povinec, P. P.: Anthropogenic marine radioactivity, Ocean Coast. Manage., 43, 689–712, 2000.
Livingston, H. D. and Povinec, P. P.: A millennium perspective on the contribution of global fallout radionuclides to ocean science, Health Phys., 82, 656–668, 2002.
Lujaniené, G., Jokšas, K., Šilobritiené, B., and Morkūniené, R.: Physical and chemical characteristics of 137Cs in the Baltic Sea, Radioactiv. Environ., 8, 165–179, 2006.
Lujaniené, G., Aninkevicius, V., and Lujanas, V: Artificial radionuclides in theatmosphere over Lithuania, J. Environ. Radioact., 100, 108–119, 2009.
Masson, O., Baeza, A., Bieringer, J., Brudecki, K., Bucci, S., Cappai, M., Carvalho, F. P., Connan, O., Cosma, C., Dalheimer, A. Didier, D., Depuydt, G., De Geer, L. E., De Vismes, A., Gini, L., Groppi, F., Gudnason, K., Gurriaran, R., Hainz, D., Halldorsson, O., Hammond, D., Hanley, O. Holey, K. Homoki, Zs., Ioannidou, A. , Isajenko, K., Jankovick M., Katzlberger, C., Kettunen, M., Kierepko, R., Kontro, R. Kwakman, P. J. M., Lecomte, M. , Leon Vintro, L. Leppänen, A.- P., Lind, B., Lujaniene, G., Mc Ginnity, P., Mc Mahon, C., Mala H., Manenti, S., Manolopoulou, M., Mattila, A., Mauring, A., Mietelski, J. W., Møller, B. S., Nielsen, P., Nikolick J., Overwater, R. M. W., Palsson, S. E., Papastefanou, C., Penev, I., Pham, M. K., Povinec, P. P., Ramebäck, H., Reis, M. C. , Ringer, W., Rodriguez, A., Rulík, P., Saey, P. R. J., Samsonov, V., Schlosser, C., Sgorbati, G. , Silobritiene, B. V., Söderström, C., Sogni, R., Solier, L., Sonck, M., Steinhauser, G., Steinkopff, T. , Steinmann, P., Stoulos, S., Sykora, I., Todorovic, D., Tooloutalaie, N., Tositti, L., Tschiersch, J., Ugron, A., Vagena, E., Vargas, A., Wershofen, A. H., and Zhukova, O.: Tracking of airborne radionuclides from the damaged Fukushima Dai-Ichi nuclear reactors by European networks, Environ. Sci. Technol., 45, 7670–7677, 2011.
Masumoto, Y., Miyazawa, Y., Tsumune, D., Kobayashi, T., Estournel, C., Marsaleix, P., Lanerolle, L., Mehra, A., and Garraffo, Z. D.: Oceanic dispersion simulation of Cesium-137 from Fukushima Dai-ichi nuclear power plant, Elements, 8, 207–212, 2012.
MEXT, Ministry of Education, Culture, Sports, Science and Technology: Monitoring information of environmental radioactivity levels, http://radioactivity.mext.go.jp/en/ (last access: 10 October 2012), 2011.
Miyazawa, Y., Masumoto, Y., Varlamov, S. M., and Miyama, T.: Transport simulation of the radionuclide from the shelf to open ocean around Fukushima, Cont. Shelf Res., 50–51, 16–29, 2012a.
Miyazawa, Y., Masumoto, Y., Varlamov, S. M., Miyama, T., Takigawa, M., Honda, M., and Saino, T.: Inverse estimation of source parameters of oceanic radioactivity dispersion models associated with the Fukushima accident, Biogeosciences, 10, 2349–2363, https://doi.org/10.5194/bg-10-2349-2013, 2013.
Mizutani, T., Koarashi, J., and Takeishi, M.: Monitoring of low-level radioactive liquid effluentin Tokai reprocessing plant, J. Nucl. Sci. Technol., 46, 665–672, 2009.
Morino, Y., Ohara, T., and Nishizawa, M.: Atmospheric behavior, deposition, and budget of radioactive materials from the Fukushima Daiichi nuclear power plant in March 2011, Geophys. Res. Lett., 38, L00G11, https://doi.org/10.1029/2011GL048689, 2011.
Nakano, M. and Povinec, P. P.: Oceanic general circulation model for the assessment of the distribution of 137Cs in the world ocean, Deep-sea Res. II, 50, 2803–2816, 2003a.
Nakano, M. and Povinec, P. P.: Modelling the distribution of plutonium in the Pacific Ocean, J. Environ. Radioact., 69, 85–106, 2003b.
Nakano, M. and Povinec, P. P.: Long-term simulations of the 137Cs dispersion from the Fukushima accident in the world ocean, J. Environ. Radioact., 111, 109–115, 2012.
NERH, Nuclear Emergency Response Headquarters, Government of Japan: Report of the Japanese Government to the IAEA Ministerial Conference on Nuclear Safety – The accident at TEPCO's Fukushima Nuclear Power Stations, http://www.iaea.org/newscenter/focus/fukushima/japan-report/ (last access: 10 October 2012), 2011.
NISA, Nuclear and Industrial Safety Agency: Regarding the Evaluation of the Conditions on Reactor Cores of Unit 1, 2 and 3 related to the Accident at Fukushima Daiichi Nuclear Power Station, Tokyo Electric Power Co. Inc., http://www.meti.go.jp/english/earthquake/nuclear/japan-challenges/pdf/japan-challenges_d.pdf (last access: 10 November 2012), 2011.
NSCJ, Nuclear Safety Commission of Japan: Trial estimation of emission of radioactive materials (131I, 137Cs) into the atmosphere from Fukushima Dai-ichi nuclear power station, Tokyo, http://www.nsr.go.jp/archive/nsc/NSCenglish/index.htm, 2011.
Palcsu, L., Major, Z., Köllő, Z., and Papp, L.: Using an ultrapure 4He spike in tritium measurements of environmental water samples by the 3He-ingrowth method, Rapid Comm. Mass Spectr., 24, 698–704, 2010.
Pham, M. K., Betti, M., Povinec, P. P., Alfimov, V., Biddulph, D., Gastaud, J., Kieser, W. E., Lopez Gutierez J. M., Possnert, G., Sanchez-Cabeza, J. A., and Suzuki, T.: Certified reference material IAEA-418: 129I in Mediterranean Sea water, J. Radioanal. Nucl. Chem., 286, 121–127, 2010.
Pham, M. K., Betti, M., Nies, H., and Povinec, P. P.: Temporal changes of 7Be, 137Cs and 210Pb activity concentrations in surface air at Monaco and their correlation with meteorological parameters, J. Environ. Radioact., 102, 1045–1054, 2011a.
Pham, M. K., Betti, M., Povinec, P. P., Benmansour, M., Bünger, V., Drefvelin, J., Engeler, C., Flemal, J. M., Gascó, C., Guillevic, J., Gurriaran, R., Groening, M., Happel, J. D., Herrmann, J., Klemola, S., Kloster, M., Kanisch, G., Leonard, K., Long, S., Nielsen, S., Oh, J.-S., Rieth, P. U., Östergren, I., Pettersson, H., Pinhao, N., Pujol, L., Sato, K., Schikowski, J., Varga, Z., Vartti, V. P., and Zheng, J.: A certified reference material for radionuclides in the water sample from Irish Sea (IAEA-443), J. Radioanal. Nucl. Chem., 288, 603–611, 2011b.
Pham, M. K., Povinec, P. P., Nies, H., and Betti, M.: Dry and wet deposition of 7Be, 210Pb and 137Cs in Monaco air during 1998–2010: seasonal variations of deposition fluxes, J. Environ. Radioact., 120, 45–57, 2013.
Povinec, P. P., Oregioni, B., Jull, A. J. T., Kieser, W. E., and Zhao, X.-L.: AMS measurements of 14C and 129I in seawater around radioactive waste dump sites, Nucl. Instrum. Methods Phys. Res. B, 172, 672–678, 2000.
Povinec, P. P., Badie, C., Baeza, A., Barci-Funel, G., Bergan, T. D., Bojanowski, R., Burnett, W., Eikenberg, J., Fifield, L. K., Serradell, V., Gastaud, J., Goroncy, I., Herrmann, J., Hotchkis, M. A. C., Ikaheimonen, T. K., Jakobson, E., Kalimbadjan, J., La Rosa, J. J., Lee, S.-H., Liong Wee Kwong, L., Lueng, W. M., Nielsen, S. P., Noureddine, A., Pham, M. K., Rohou, J.-N., Sanchez-Cabeza, J. A., Suomela, J., Suplinska, M., and Wyse, E.: Certified reference material for radionuclides in seawater IAEA-381 (Irish Sea water), J. Radioanal. Nucl. Chem., 251, 369–374, 2002.
Povinec, P. P., Livingston, H. D., Shima, S., Aoyama, M., Gastaud, J., Goroncy, I., Hirose, K., Huyhn-Ngoc, L., Ikeuchi, Y., Ito, To., La Rosa, J., Liong Wee Kwong, L., Lee, S.-H., Moriya H., Mulsow, S., Oregioni, B., Pettersson, H., and Togawa, O.: IAEA'97 expedition to the NW Pacific Ocean – results of oceanographic and radionuclide investigations of the water column, Deep-Sea Res. II, 50, 2607–2638, 2003a.
Povinec, P. P., Bailly Du Bois, P., Kershaw, P. J., Nies, H., and Scotto, P.: Temporal and spatial trends in the distribution of 137Cs in surface waters of Northern European Seas – A record of 40 years of investigations, Deep-Sea Res. Pt. II, 50, 2785–2801, 2003b.
Povinec, P. P., Hirose, K., Honda, T., Ito, T., Scott, E. M., and Togawa, O.: Spatial distribution of 3H, 90Sr, 137Cs and 239,240Pu in surface waters of the Pacific and Indian Oceans – GLOMARD database, J. Environ. Radioact., 76, 113–137, 2004.
Povinec, P. P., Aarkrog, A., Buesseler, K. O., Delfanti, R., Hirose, K., Hong, G. H., Ito, T., Livingston, H. D., Nies, H., Noshkin, V. E., Shima, S., and Togawa, O.: 90Sr, 137Cs and 239,240Pu concentration surface water time series in the Pacific and Indian Oceans – WOMARS results, J. Environ. Radioact., 81, 63–87, 2005a.
Povinec, P. P., Comanducci, J. F., and Levy-Palomo, I.: IAEA-MEL's underground counting laboratory (CAVE) for the analysis of radionuclides in the environment at very low-levels, J. Radioanal. Nucl. Chem., 263, 441–445, 2005b.
Povinec, P. P., Lee, S. H., Liong Wee Kwong, L.,Oregioni, B., Jull, A. J. T., Kieser, W. E., Morgenstern, U., and Top, Z.: Tritium, radiocarbon, 90Sr and 129I in the Pacific and Indian Oceans, Nucl. Instrum. Methods Phys. Res. B, 268, 1214–1218, 2010.
Povinec, P. P., Breier, R., Coppola, L., Groening, M., Jeandel, C., Jull, A. J. T., Kieser, W. E., and Top, Z.: Tracing of water masses using a multi-isotope approach in the southern Indian Ocean, Earth Planet. Sci. Lett., 302, 14–26, 2011.
Povinec, P. P., Hirose, K., and Aoyama, M.: Radiostronium in the western North Pacific: Characteristics, behavior, and the Fukushima impact, Environ. Sci. Technol., 46, 10356–10363, 2012a.
Povinec, P. P., Eriksson, M., Scholten, J., and Betti, M.: Marine Radioactivity Analysis, in: Handbook on Radioactivity Analysis, edited by: L'Annunziata, M. F., Academic Press, Amsterdam, 770–832, 2012b.
Povinec, P. P., Gera, M., Hirose, K., Lujaniené G., Nakano, M., and Plastino, W.: Dispersion of Fukushima radionuclides in the global atmosphere and the ocean, Appl. Rad. Isot., in press, https://doi.org/10.1016/j.apradiso.2013.03.058, 2013.
Raisbeck, G. M. and Yiou, F.: 129I in the oceans: origins and applications, Sci. Total Environ., 237/238, 31–41, 1999.
Rypina, I. I., Jayne, S. R., Yoshida, S., Macdonald, A. M., Douglass, E., and Buesseler, K.: Short-term dispersal of Fukushima-derived radionuclides off Japan: modeling efforts and model-data intercomparison, Biogeosciences Discuss., 10, 1517–1550, https://doi.org/10.5194/bgd-10-1517-2013, 2013.
Schlosser, P., Bayer, R., Boenisch, G., Cooper, L. W., Ekwurzel, B., Jenkins, W. J., Khatiwala, S., Pfirman, S., and Smethie, W. M.: Pathways and residence times of dissolved pollutants in the ocean derived from transient tracers and stable isotopes, Sci. Total Environ., 237/238, 15–30, 1999.
Shima, S., Gasa, S., Iseda, K., Nakayama, T., and Kawamura, H.: Distribution of anthropogenic radionuclides in the water column off Rokkasho, Japan, in: Radionuclides in the Environment, edited by: Povinec, P. P., Sanchez-Cabeza J. A., Elsevier, Amsterdam, 2006, 83–95.
Stohl, A., Seibert, P., Wotawa, G., Arnold, D., Burkhart, J. F., Eckhardt, S., Tapia, C., Vargas, A., and Yasunari, T. J.: Xenon-133 and caesium-137 releases into the atmosphere from the Fukushima Dai-ichi nuclear power plant: determination of the source term, atmospheric dispersion, and deposition, Atmos. Chem. Phys., 12, 2313–2343, https://doi.org/10.5194/acp-12-2313-2012, 2012.
Suzuki, T., Minakawa, M., Amano, H., and Togawa, O.: The vertical profiles of iodine-129 in the Pacific Ocean and the Japan Sea before the routine operation of a new nuclear fuel reprocessing plant, Nucl. Instr. Methods Phys. Res. B, 268, 1229–1231, 2010.
Suzuki, T., Otosaka, S., Kuwabara, J., Kawamura, H., and Kobayashi, T.: Iodine-129 concentration in seawater near Fukushima before and after the accident at the Fukushima Daiichi Nuclear Power Plant, Biogeosciences Discuss., 10, 1401–1419, https://doi.org/10.5194/bgd-10-1401-2013, 2013.
Takemura, T., Nakamura, H., Takigawa, M., Kondo H., Satonuma, T., Miyasaka, T., and Nakajima, T.: A numerical simulation of global transport of atmospheric particles emitted from the Fukushima Daiichi nuclear power plant, Scientific Online Letters on the Atmosphere, 7, 101–104, 2011.
TEPCO, Tokyo Electric Power Company: Result of radioactive nuclide analysis around Fukushima Daiichi Nuclear Power Station, http://www.tepco.co.jp/en/press/corp-com/release/11042103-e.html (last access: 20 December 2012), 2011.
TEPCO, Tokyo Electric Power Company: Fukushima Nuclear Accidents Investigation Report, http://www.tepco.co.jp/en/nu/fukushima-np/interim/index-e.html (last access: 20 December 2012), 2012.
Toyama, C., Muramatsu, Y., Uchida, Y., Igarashi, Y., Aoyama, M., and Matsuzaki, H.: Variations of 129I in the atmospheric fallout of Tokyo, Japan: 1963–2003, J. Environ. Radioact., 113, 116–122, 2012.
Tsumune, D., Tsubono, T., Aoyama, M., and Hirose, K.: Distribution of oceanic 137Cs from the Fukushima Dai-ichi Nuclear Power Plant simulated numerically by a regional ocean model, J. Environ. Radioactiv., 111, 100–108, 2012.
Tsumune, D., Tsubono, T., Aoyama, M., Uematsu, M., Misumi, K., Maeda, Y., Yoshida, Y., and Hayami, H.: One-year, regional-scale simulation of 137Cs radioactivity in the ocean following the Fukushima Daiichi Nuclear Power Plant accident, Biogeosciences Discuss., 10, 6259–6314, https://doi.org/10.5194/bgd-10-6259-2013, 2013.
Tumey, S. J., Guilderson, T. P., Brown, T. A., Broek, T., and Buesseler, K. O.: Input of 129I into the western Pacific Ocean resulting from the Fukushima nuclear event, J. Radioanal. Nucl. Chem., 296, 957–962, 2013.
UNSCEAR, United Nations Scientific Committee on the Effects of Atomic Radiation: Sources and Effects of Ionizing Radiation. Report to the General Assembly, United Nations, New York, USA, 2008.
Yoshida, N. and Kanda, J.: Tracking the Fukushima Radionuclides, Science, 336, 1115–1116, 2012.
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