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Suzuki Koji

Faculty of Environmental Earth Science Earth System Science Marine and Atmospheric GeochemistryProfessor
Institute for the Promotion of Business-Regional CollaborationProfessor

Researcher basic information

■ Degree
  • 博士(理学), 名古屋大学
■ URL
researchmap URLホームページURL■ Various IDs
Researcher number
  • 40283452
ORCID IDJ-Global ID■ Research Keywords and Fields
Research Keyword
  • Marine phytoplankton
  • Ice Algae
  • Primary Production
  • Biological Oceanography
  • Marine Biogeochemistry
  • Algal Ecophysiology
Research Field
  • Environmental Science/Agriculture Science, Environmental dynamic analysis, 生物海洋学
  • Environmental Science/Agriculture Science, Environmental dynamic analysis, 海洋生物地球化学
  • Life Science, Aquatic bioproduction science, 一次生産
■ Educational Organization

Career

■ Career
Career
  • Oct. 2016 - Present
    Hokkaido University, Faculty of Environmental Earth Science, Professor
  • Apr. 2007 - Sep. 2016
    Hokkaido University, Faculty of Environmental Earth Science, Associate Professor
  • Dec. 2002 - Mar. 2007
    Hokkaido University, Graduate School of Environmental Earth Science, Associate Professor
  • Apr. 2001 - Nov. 2002
    Nagoya University, Hydrospheric Atmospheric Research Center, 助手
  • Apr. 1996 - Mar. 2001
    Nagoya University, 大気水圏科学研究所, Research Associate
  • Apr. 1993 - Mar. 1996
    日本学術振興会, 特別研究員(DC1)
Committee Memberships
  • 2025 - Present
    Elsevier, Progress in Oceanography Associate Editor
  • 2024 - Present
    SCOR Working Group 170 PRIMO Full Member
  • 2021 - Present
    Frontiers in Marine Science Associate Editor
  • 2021 - Present
    SCOR Working Group165 MixONET Associate Member
  • 2021 - Present
    日本学術会議地球惑星科学委員会, GEOTRACES小委員会委員
  • 2019 - Present
    東京大学大気海洋研究所, 共同利用研究運営委員会委員
  • 2018 - Present
    BioGeoSCAPES International Implementation Committee Member
  • 2018 - Present
    日本学術会議環境学委員会, IMBeR小委員会委員
  • 2009 - Present
    European Geosciences Union (EGU), Biogeosciences Associate Editor

Research activity information

■ Awards
  • Jan. 2017, 北海道大学, 教育総長賞(奨励賞)
    鈴木光次
  • Feb. 2016, 北海道大学, 研究総長賞(奨励賞)
    鈴木光次
■ Papers
■ Other Activities and Achievements
  • Characteristics of transparent exopolymer particles (TEP) distribution in the Oyashio during diatom bloom period in spring of 2010
    NOSAKA YUICHI; SUZUKI KOJI; YAMASHITA YOUHEI; SAITO HIROAKI; TAKAHASHI KAZUTAKA, Abstracts of Annual Meeting of the Geochemical Society of Japan, 58, 0, 273, 273, 2011
    2010年4月および6月の親潮域において,植物プランクトンの群集組成と光合成特性と共に,透明細胞外重合体粒子(TEP)分布の特徴を調査した.4月は珪藻ブルームが発生し,表層(5m深)における植物プランクトンの光合成活性が相対的に高かったのに対し,6月は珪藻ブルームが終焉し,光合成活性も低かった.4月における表層のTEP濃度は,6月と比較して,2-3倍高かった.観測期間中,表層のTEP濃度とSi(OH)<sub>4</sub>/NO<sub>3</sub>比の間に高い相関(r = 0.94, p < 0.01, n = 6)がみられたことから,珪藻類の栄養塩取り込み活性がTEP生産を支配していたことが示唆された., GEOCHEMICAL SOCIETY OF JAPAN
■ Books and other publications
  • The 5th Workshop on High-Performance Liquid Chromatography (HPLC) Intercomparison on Phytoplankton Pigments (HIP)
    Canuti, E.; Allerup, M.; Bracher, A.; Brotas, V.; Capellacci, S.; Carabelli, C.; Casabianca, S.; Develoouse, I.; Dias, A.; Dimier, C.; Flander-Putrle, V.; Laloux, M.; Lami, A.; Kenemer, C.; Kumar, S.; Peeken, I.; Penna, A.; Raman, M.; Ras, J.; Ricci, F.; Salaün, J.; Schluter, L.; Suzuki, K.; Thomas, C.; Tirkey, A.; Tracana, A.; Uitz, J.; Vijaya; Krishna, A.; Vlaemnick, B.; Zaccagnini, A.
    Jan. 2025, 9789268238752, [Joint work]
  • Kuroshio Current: Physical, Biogeochemical, and Ecosystem Dynamics
    Takeyoshi Nagai; Hiroaki Saito; Koji Suzuki; Motomitsu Takahashi
    Wiley - American Geophysical Union, Jun. 2019, 9781119428428, 1 online resource (x, 312 p., [8] p. of plates), English, [Peer-reviewed], [Joint editor]
  • Advances in Above- and In-Water Radiometry, Vol. 3: Hybridspectral Next-Generation Optical Instruments
    Hooker, S.B; R.N. Lind; J.H. Morrow; J.W. Brown; R.M. Kudela; H.F. Houskeeper; K. Suzuki
    NASA Scientific and Technical Information Program, NASA Goddard Space Flight Center, Nov. 2018, [Internationally co-authored], [Joint work]
  • Advances in Above- and In-Water Radiometry, Vol. 2: Autonomous Atmospheric and Oceanic Observing Systems
    Hooker, S.B; R.N. Lind; J.H. Morrow; J.W. Brown; R.M. Kudela; H.F. Houskeeper; K. Suzuki
    NASA Scientific and Technical Information Program, NASA Goddard Space Flight Center, Nov. 2018, [Internationally co-authored], [Joint work]
  • Advances in Above- and In-Water Radiometry, Vol. 1: Enhanced Legacy and State-of-the-Art Instrument Suites
    Hooker, S.B; R.N. Lind; J.H. Morrow; J.W. Brown; K. Suzuki; H.F. Houskeeper; T. Hirawake; E.R. Maúre
    NASA Scientific and Technical Information Program, NASA Goddard Space Flight Center, Nov. 2018, [Internationally co-authored], [Joint work]
  • 海洋観測ガイドライン
    日本海洋学会編; 鈴木光次, 植物色素; 基礎生産; 海水中の光
    日本海洋学会, Jul. 2018, [Peer-reviewed], [Contributor]
  • 海洋生態学
    日本生態学会編; 鈴木光次, 基礎生産過程; 海洋生態系の食物関係
    共立出版, Feb. 2016, 9784320057456, xi, 305p, 図版 [4] p, Japanese, [Contributor]
  • 環境分析ガイドブック
    日本分析化学会編; 鈴木光次, 植物プランクトン
    丸善, Jan. 2011, 9784621082775, xx, 823p, 図版 [4] p, Japanese, [Contributor]
  • 地球温暖化の科学
    北海道大学大学院環境科学院編; 鈴木光次, 地球温暖化による海洋生態系の変化
    北海道大学出版会, Mar. 2007, 9784832981812, xii, 246p, Japanese, [Contributor]
  • オゾン層破壊の科学
    北海道大学大学院環境科学院編; 鈴木光次, 紫外線による海洋生態系への影響; 水中の放射伝達
    北海道大学出版会, Mar. 2007, 9784832981799, vi, 408p, Japanese, [Contributor]
  • 第5版 実験化学講座 環境化学
    日本化学会編; 鈴木光次, 植物プランクトン
    丸善, Jan. 2007, 9784621078068, xiii, 519p, Japanese, [Contributor]
  • 水の分析
    日本分析化学会北海道支部編; 鈴木光次, クロロフィルa
    化学同人, Jun. 2005, 9784759809916, x, 472p, Japanese, [Contributor]
  • 地球環境調査計測事典第3巻沿岸域編
    鈴木光次, 逆相高速液体クロマトグラフィーによるクロロフィルとカロチノイドの測定及びフィコビリンタンパク質の測定; 蛍光法による基礎生産速度の測定
    フジ・テクノシステム, 2002, 4938555891, 3冊, Japanese, [Contributor]
■ Syllabus
  • 対流圏化学特論, 2024年, 修士課程, 環境科学
  • 大気海洋化学基礎論, 2024年, 修士課程, 環境科学院
  • 生物地球化学基礎論, 2024年, 修士課程, 環境科学院
  • 環境と人間, 2024年, 学士課程, 全学教育
■ Affiliated academic society
  • American Geophysical Union
  • Phycological Society of America
  • Association for the Sciences of Limnology and Oceanography
  • 日本海洋学会
  • 日本地球化学会
  • European Geosciences Union
■ Research Themes
  • Evaluation of the role of gel particles in oceanic material cycles
    Grants-in-Aid for Scientific Research
    01 Apr. 2025 - 31 Mar. 2028
    野坂 裕一; 鈴木 光次; 伊佐田 智規
    Japan Society for the Promotion of Science, Grant-in-Aid for Scientific Research (C), Tokai University, 25K15420
  • 広域高頻度高精度観測から解明する微細藻類の動態変化
    2023 - 2028
    鈴木 光次
    人為起源二酸化炭素の増加に伴い、海洋の主要一次生産者である微細藻類(植物プランクトン)の動態の変化が危惧されています。本研究では、協力商船と研究船を用いた前例の無い高頻度、高精度観測を通して、世界の海の中でも生産力の高い北太平洋中高緯度域の炭素隔離能力に対して重要な働きをする植物プランクトンの現存量、群集組成、生産力の季節変化と年々変化を把握し、温暖化と海洋酸性化の影響を定量的に明らかにします。
    科学技術振興機構, 戦略的な研究開発の推進/戦略的創造研究推進事業/CREST, 23829302
  • 北太平洋中高緯度域の新生産に貢献するケイ藻類と窒素固定ラン藻類の動態変化の解明
    科学研究費助成事業
    01 Apr. 2023 - 31 Mar. 2027
    鈴木 光次; 高尾 信太郎
    北太平洋を定期的に航行する協力商船New Century 2(トヨフジ海運株式会社)を用いて、航海中、船底から船内実験室まで汲み上げられた表層海水を昼間に毎日1回採取した。ケイ藻類および窒素固定ラン藻類の動態を評価するための植物プランクトン色素試料と遺伝子(DNAおよびRNA)試料については、海水の濾過を行い、得られたフィルター試料を冷凍保存した。水温、塩分、光合成有効放射量、硝酸塩濃度、海水中の二酸化炭素分圧については、同商船に備えた各種センサーで連続測定した。硝酸塩センサーデータの検証・校正等のための海水栄養塩試料は、冷凍保存し、陸上で分析した。また、2023年6月に学術研究船白鳳丸(海洋研究開発機構)を用いた西部北太平洋亜寒帯域KH-23-2次研究航海に参加し、協力商船観測と同様の試料および環境データを取得した。
    上記の協力商船および研究船で取得した植物プランクトン色素試料を超高速液体クロマトグラフィー(UHPLC)で解析を行った。また、2014年以後に上記の協力商船で取得した遺伝子試料について、ケイ藻類と窒素固定ラン藻類に特有の遺伝子断片のコピー数を定量PCR法で評価した。さらに、次世代シーケンサーによるアンプリコンシーケンス解析を行い、ケイ藻類とその群集組成の把握を行った。ケイ藻類の現存量、組成、生産力に対する各環境因子(水温、塩分、硝酸塩とそれ以外の栄養塩(リン酸塩、ケイ酸塩等)の濃度とそれらの比、海水炭酸系パラメータ、中規模渦運動エネルギー、海面高度等)の影響を評価した。
    日本学術振興会, 基盤研究(B), 北海道大学, 23K28206
  • Elucidation of microbial factors that control the amount and physicochemical properties of atmospheric organic nitrogen aerosols in the subarctic ocean
    Grants-in-Aid for Scientific Research
    01 Apr. 2023 - 31 Mar. 2026
    宮崎 雄三; 鈴木 光次; 山下 洋平
    秋季の南部オホーツク海上で学術研究船新青丸により大気・表層海水試料を採取し、前年度までに同海域で採取済みの試料と併せ、化学組成分析を行った。その結果、微小エアロゾル質量に対し有機物が約50%を占め支配的であり、水溶性成分の割合が大きいことが明らかになった。さらに有機物の安定炭素同位体比の測定から、観測されたエアロゾルのうち、海氷後退後の春季の植物プランクトンブルーム期で71%、ブルーム衰退期で64% が海洋起源であると推定された。エアロゾル中の水溶性有機炭素(WSOC)と分子トレーサー濃度との相関関係から、観測された海洋由来のWSOCの大部分は、海水飛沫による一次生成ではなく、α-ピネンや硫化ジメチルの酸化生成物に関連する前駆物質からの二次生成の寄与が大きいことが示唆された。さらにブルーム期の水溶性有機エアロゾル中のC:N平均比はブルーム衰退期の平均比より有意に低く、海洋表層の微生物活動に関連した有機態窒素エアロゾル生成の影響が大きいことが示唆された。実際、表層海水においてブルーム期の溶存態有機炭素(DOC):溶存態有機窒素(DON)の平均比(12.8)もブルーム衰退期の平均比(14.7)より有意に低く、ブルーム期のDOCとDONはオホーツク海で研究期間に優占的な珪藻類であるFragilariopsis cylindrusのようなアイスアルジーに関係していることが示唆された。これらの結果から、領域的な海洋表層から大気に放出生成される有機物の領域的な気候影響を評価する上で、植物プランクトンブルーム期のアイスアルジーに由来する有機物のエアロゾル二次生成の重要性が明らかになった。
    Japan Society for the Promotion of Science, Grant-in-Aid for Scientific Research (B), Hokkaido University, 23K28207
  • Formation of water nutritional property including iron and silicate at the termination of global ocean conveyor belt
    Grants-in-Aid for Scientific Research
    05 Jul. 2021 - 31 Mar. 2026
    西岡 純; 中村 知裕; 三寺 史夫; 山下 洋平; 鈴木 光次; 小畑 元; 近藤 能子; 安田 一郎; 三角 和弘; 南 秀樹
    2006年、2007年、2010年、2011年、2014年、2018年に北海道大学低温科学研究所とロシア極東海洋気象学研究所の共同研究として実施したロシア船を用いたオホーツク海とベーリング海の観測データを、1998年から2017年までに北太平洋で実施した観測航海のデータと統合し、各測点の水柱内の塩分、水温、密度、溶存酸素、Fe、Si、N、Pデータを含む栄養物質データセットを作成整備しHPで公開した。上記データセットを用いた解析を実施し、東経155度の北太平洋中層水(NPIW)から表層に向けた上向きのFeおよび主要栄養塩のフラックスと、HPLC植物色素データから得られる表層の生物種組成情報を比較した。生物種組成情報を取り出してフラックスとの関係を見ると、下層から表層への栄養物質フラックスと珪藻の現存量との間には良い相関がみられた。亜寒帯ジャイア域と黒潮・親潮移行域でNPIW循環から表層に供給されるFeやSiなどの栄養物質によって、珪藻の増殖が支えられていることが初めて示された。また、堆積物由来溶存鉄の長距離輸送メカニズムの解明を目指して、NPIW循環域における溶存Feの化学形態別分布を解析した。その結果、オホーツク海陸棚堆積物から運ばれてくるFeは、粒子状やコロイド状が主な形態であるのに対し、中層水循環により長距離輸送されるFeは腐植錯体Feであることを示唆した
    Japan Society for the Promotion of Science, Grant-in-Aid for Scientific Research (S), Hokkaido University, 21H05056
  • Exploratory research on new source of atmospheric reactive nitrogen focusing on marine nitrogen-fixing organisms
    Grants-in-Aid for Scientific Research
    09 Jul. 2021 - 31 Mar. 2023
    Miyazaki Yuzo
    This study aimed to elucidate the contribution of marine nitrogen-fixing microorganism (Trichodesmium) to the formation of atmospheric reactive nitrogen by a laboratory incubation experiment. During the incubation period of approximately two months, it was observed that dissolved nitrogen was exuded from Trichodesmium during the exponential phase of the growth stage. Throughout the experiment, ammonium/ammonia and water-soluble organic nitrogen (WSON) were the major reactive nitrogen components in both particulate and gas phases. Overall results showed that the atmospheric emission of acidic WSON was more evident during the exponential and stationary growth phases, while the emissions of basic reactive nitrogen were more significant during the decline and death phases. This study demonstrated the sea-to-air emissions of ammonia and WSON associated with the growth and decline of nitrogen-fixing microorganism for the first time.
    Japan Society for the Promotion of Science, Grant-in-Aid for Challenging Research (Exploratory), Hokkaido University, 21K19835
  • Organic nitrogen aerosol in the marine atmosphere: Which factors control the amount of organic nitrogen in marine microbial activity?
    Grants-in-Aid for Scientific Research
    Apr. 2019 - Mar. 2022
    Miyazaki Yuzo
    Shipboard measurements of atmospheric aerosols and surface seawater in the subtropical North Pacific indicated that organic nitrogen, produced and exuded by nitrogen-fixing microorganisms in surface seawater, significantly contributed to the formation of atmospheric organic nitrogen aerosols. Laboratory experiments of incubation of nitrogen-fixing microorganisms followed by atmospheric measurements confirmed sea-to-air emissions of organic nitrogen associated with the growth of nitrogen-fixing microorganisms. Furthermore, the experiment revealed that the emission of organic nitrogen, mainly consisted of highly-volatile, basic components, increased during the decay of microorganisms.
    Japan Society for the Promotion of Science, Grant-in-Aid for Scientific Research (B), Hokkaido University, 19H04233
  • Toward understanding changes in the photosynthetic capability of microalgae with their vulnerable species after sea ice melt
    Grants-in-Aid for Scientific Research
    Apr. 2018 - Mar. 2021
    Suzuki Koji
    In this study, we carried out laboratory incubation experiments using a representative, isolated diatom strain of sea ice microalgae, and clarified changes in the photosynthetic capability of the strain during the formation, frozen or melting periods of sea ice. Additionally, we collected sea ice with ice algae from the Sea of Okhotsk in winter, and then performed an ice melt study. During the latter experiment, morphological changes, decreases in photosynthetic pigment concentration and so on were observed in microalgal cells immediately after sea ice melt. Then cell viability of pennate diatoms became lower. On the other hand, most centric diatoms fully recovered until approximately 3 days after sea ice melt, and they were able to photosynthesize and grow actively. Based on the results obtained from this study, we published 9 original papers from international journals.
    Japan Society for the Promotion of Science, Grant-in-Aid for Scientific Research (B), Hokkaido University, 18H03352
  • Biogeochemical linkage in the polar - subarctic region via sea ice melting water
    Grants-in-Aid for Scientific Research
    Apr. 2017 - Mar. 2021
    Nishioka Jun
    We conducted field observations in the northwestern Bering Sea and the Sea of Okhotsk, which are subpolar marginal seas, and adjacent subarctic waters, and evaluated the effects of the inflow of melting water from the sea ice on the distribution of nutrient such as iron and nutrients, and the growth of phytoplankton species. The results suggest that the East Sakhalin Current within the Sea of Okhotsk and sea ice meltwater carry iron from continental shelf origin over a wide area of the southern Sea of Okhotsk and coastal Oyashio waters, and forming water masses characterized by high nutrient and iron concentrations, which have a significant impact on phytoplankton growth during the spring season. The results of observational studies of the western Bering Sea to East Sakhalin Current showed that the western Bering Sea is an important region that links the subarctic and polar regions through nutrient cycling.
    Japan Society for the Promotion of Science, Grant-in-Aid for Scientific Research (A), Hokkaido University, 17H00775
  • Algorithm development for the identification of Phytoplankton Functional Types (PFTs) with optical hyperspectral data in the coastal waters
    Grants-in-Aid for Scientific Research
    Apr. 2016 - Mar. 2019
    ISADA Tomonori; TANIUCHI Yukiko; SUZUKI Koji
    We developed the algorithm for identification of Phytoplankton Functional Types (PFTs) with optical hyperspectral data of phytoplankton absorption to better understand marine biogeochemical cycles and to accelerate its implications for ocean color remote sensing applications. We selected four PFTs (diatoms, cyanobacteria, green algae, and dinoflagellates) as target PFTs. Our results indicate that an optical hyperspectral data with a derivative spectroscopy/similarity index (SI) method is a promising approach to identify the dominance of each PFT in the ocean. Additionally, we found that derivative spectra of phytoplankton absorption coefficients could be a useful indicator of bio-optical provinces.
    Japan Society for the Promotion of Science, Grant-in-Aid for Young Scientists (B), Hokkaido University, 16K16182
  • Establishment of New Ecozones in the Oceans by Meta-genetic Community Analysis
    Grants-in-Aid for Scientific Research
    28 Jun. 2012 - 31 Mar. 2017
    Tsuda Atsushi; HIRAI Junya; ENDO Hiroshi; SUZUKI Shotaro; TACHIBANA Aiko
    The goal of this project is to clarify the biogeography and biodiversity of micro-organisms, phytoplankton and zooplankton by meta-genomic method using a high throughput sequencer. The metagenomic methods have established for bacteria, archaea, diatoms, haptophytes and calanoid copepods, which were ten-times faster than classical method such as microscopic one without effects of individual's skills and experiences. Using these methods for samples collected from wide areas of the Pacific, we found that phytoplankton and zooplankton were distributed along with the surface current system. However, bacteria and archaea were more effected by their life styles (free-living and attached).
    Japan Society for the Promotion of Science, Grant-in-Aid for Scientific Research on Innovative Areas (Research in a proposed research area), The University of Tokyo, 24121004
  • Elucidation of thermohaline/biogeochemical circulation systems connecting the Sea of Okhotsk with subarctic North Pacific Ocean
    Grants-in-Aid for Scientific Research
    Apr. 2010 - Mar. 2015
    WAKATSUCHI Masaaki; MITSUDERA Humio; NISHIOKA Jun; NAKAMURA Tomohiro; EBUCHI Naoto; WATANABE Yutaka; SUZUKI Koji; KURODA Hiroshi; OHSHIMA Keiichiro; TSUMUNE Daisuke; MATOBA Sumito
    We investigated the thermohaline/biogeochemical circulation systems, connecting the Sea of Okhotsk with the North Pacific, to elucidate a ‘miraculous mechanism’ that supports abundant fisheries resources in the Okhotsk and Oyashio regions. Salinity of the dense shelf water (DSW) over the northern shelf of the Okhotsk Sea controls the strength of the thermohaline circulation of the North Pacific Ocean. DSW salinity is determined by relative contribution among the salinity anomaly that propagates long distance from the subarctic gyre, freshwater anomaly by precipitation, and saline water anomaly rejected during sea ice formation. DSW entrains nutrients such as iron, originating in the Amur River and deposited over the continental shelf, and spreads these materials to the North Pacific Ocean. This study has revealed an exquisite thermohaline-biogeochemical system coupled through DSW and tidal mixing, which controls primary production in the large area of the subarctic North Pacific.
    Japan Society for the Promotion of Science, Grant-in-Aid for Scientific Research (S), Hokkaido University, 22221001
  • Understanding the production of transparent exopolymer particles and its controlling factors during the spring bloom in Oyashio waters
    Grants-in-Aid for Scientific Research
    2010 - 2012
    SUZUKI Koji; SAITO Hiroaki
    Much attention has recently been paid to the dynamics of transparent exopolymer particles (TEP) in seawater, because TEP can play an important role in determining the capability of ocean carbon fixation as adhesives for aggregating marine organic matters. However, no such information has ever been available from the Oyashio region, NW Pacific where biological production is relatively high among the world’s oceans. In this study, we obtained crucial results of TEP production and its controlling factors during the spring bloom in Oyashio waters through field observations and laboratory experiments.
    Japan Society for the Promotion of Science, Grant-in-Aid for Scientific Research (B), Hokkaido University, 22310002
  • Ecosystem responses by epipelagic organisms to dust flux and its feedback to climate
    Grants-in-Aid for Scientific Research
    2006 - 2010
    TSUDA Atsushi; MICHIDA Yutaka; SAITO Hiroaki; TAKAHASHI Kazutaka; SUZUKI Koji
    This group provided the biological information to the group who studied the biogenic gasses such as DMS to understand the mechanisms of the variation. Some on-deck incubation experiments showed that diatoms are most important phytoplankton enhanced by typhoon passing and suggested possibilities of altering the carbon cycling and food web structure. Argo-floats with a chlorophyll sensor were deployed. Although we have not observed a typhoon passing, some anomalies of high chlorophyll concentration have been observed. We also found that many copepod species showed seasonal vertical migration behavior, which had recognized as characteristic behavior to polar zooplankton. These results suggest that biological production in the subtropical Pacific is largely depend on the unpredictable spatial and temporal variability of primary production.
    Japan Society for the Promotion of Science, Grant-in-Aid for Scientific Research on Priority Areas, The University of Tokyo, 18067008
  • Clarifying the characteristics of primary production and their physiological mechanisms during spring Oyashio diatom blooms
    Grants-in-Aid for Scientific Research
    2007 - 2009
    SUZUKI Koji; MINAGAWA Jun
    We obtained the data of phytoplankton photosynthesis and iron in the Oyashio region of the NW Pacific during the spring blooms. Coastal Oyashio waters, which contained relatively high amount of iron, stimulated the photosynthetic activity of phytoplankton, especially diatoms. However, diatoms were generally stressed by low iron availability even in the spring blooms. We also determined the effects of temperature, light, and iron availability on photosynthetic features of the representative bloom-forming diatom species isolated from Oyashio waters, through batch culture experiments.
    Japan Society for the Promotion of Science, Grant-in-Aid for Scientific Research (C), Hokkaido University, 19510001
  • Iron behavior and sources regulating primary production in marginal seas (Bering Sea, Okhotsk Sea, Japan Sea)
    Grants-in-Aid for Scientific Research
    2006 - 2009
    KUMA Kenshi; SAITOH Seiichi; ISODA Yutaka; NAGAO Seiya; NAKATSUKA Takeshi; SUZUKI Koji; WATANABE yutaka; NISHIOKA Jun
    Surface mixed layer of the basin region in the Bering Sea is under a typical iron-deficient and nutrient-rich condition with low primary production because of low atmospheric iron input. However, phytoplankton bloom (Breen Belt) is observed at the shelf break region of the Southeastern Bering Sea for a long period in summer. It is suggested that the Green Belt is maintained by the supply of nutrient-rich basin water and iron-rich shelf deep water to the surface water of the shelf break. The tidal mixing in the straits of the Kuril Islands is an important role on supplying nutrient and iron to the surface water of the northwestern North Pacific Ocean and maintaining the high primary production in the Oyashio region. On the contrary, the surface mixed layer in the Japan Sea is characterized by low nutrient and high iron concentrations, resulting from high atmospheric iron input to nutrient-depleted surface water of the Japan Sea close to the Asian continent.
    Japan Society for the Promotion of Science, Grant-in-Aid for Scientific Research (A), Hokkaido University, 18201001
  • Interaction between Metallome and Proteome in the Marine Ecosystem
    Grants-in-Aid for Scientific Research
    2004 - 2006
    SOHRIN Yoshiki; OKAMURA Kei; NORISUYE Kazuhiro; SUZUKI Koji; HASEGAWA Hiroshi; SOHRIN Rumi
    1.Development of chemical speciation and in situ determination of bioactive trace metals
    (1)Determination of suspended particulate Co, Ni, Cu, Zn, Cd and Pb has been developed.
    (2)Determination of dissolved and acid-dissolvable Zr, Hf, Nb, Ta and W has been developed.
    (3)In-situ flow analysis of alkalinity and total carbonate has been developed.
    2.Development of analytical methods for enzymes and proteins of phytoplankton and bacteria
    (1)Detection of Fe-S protein PsaC and PsbA(D1) in photosynthetic system has been developed.
    (2)Anti-ferredoxin and anti-flavodoxin antibodies, which cross-react with ferredoxin and flavodoxin of marine diatoms, respectively, have been developed using synthetic peptides in order to estimate their Fe stress.
    3.Observation of the variation and relationship of metallome and proteome
    (1)Different distributions of Fe, Co, Ni, Cu, Zn and Cd in seawater between the Sulu Sea, South China Sea and Pacific Ocean were observed.
    (2)During the second mesoscale iron enrichment experiments in the western subarctic North Pacific (SEEDS-II), the effects of iron enrichment on the phytoplankton community structure and the speciation of bioactive trace metals were examined.
    (3)On the basis of analysis of photosynthetic proteins, Fe in seawater has been proved to be a major factor controlling the spring bloom of diatoms in the Oyashio region.
    (4)Diurnal dynamics of biomass of nano-flagellates and ciliates in Suruga Bay was investigated.
    (5)The effects of trace metals on the activity of extracellular enzymes of microbes have been proved.
    4.Study on metal uptake mechanism of phytoplankton in culture
    (1) The size distribution of Fe in culture media of phytoplankton was investigated. Fe ligands exuded from phytoplankton were analyzed by LC-MS.
    (2)Membrane proteins revealed in red tide forming phytoplankton Prymnesium parvum under Fe deficiency were analyzed.
    Japan Society for the Promotion of Science, Grant-in-Aid for Scientific Research (A), Kyoto University, 16204046
  • 北西太平洋亜寒帯域における植物プランクトンの死亡とその物質循環過程とのかかわり
    科学研究費助成事業
    2003 - 2005
    鈴木 光次
    近年、海洋植物プランクトンが海洋表層から取り除かれる要因として、沈降や動物プランクトンによる捕食以外に、海洋表層での植物プランクトンの細胞死の重要性が指摘されるようになってきた。しかし,北太平洋における植物プランクトンの細胞死に関する報告は無い。そこで本年度は、春および晩夏の北西太平洋亜寒帯域の親潮域および黒潮親潮移行域の植物プランクトンの細胞生存率(総細胞数に占める生細胞数の割合)の比較を行った。水産総合研究センター若鷹丸によるWK0309航海(2003年9月2日〜21日)およびWK0505航海(2005年5月10日〜29日)において、親潮域および黒潮親潮移行域で、細胞消化法を用いて、植物プランクトンの細胞生存率の見積もりを行なった。2003年の晩夏ではSynechococcus spp.の生存率が59〜75%、真核ウルトラ植物プランクトン(体長<10μm)の生存率が21〜41%であり、真核ウルトラ植物プランクトンはSynechococcus spp.よりも致死率(総細胞数に占める死細胞数の割合)が有意に高かった(p<0.01)。一方、2005年の春では,Synechococcus spp.の約80%、真核ウルトラ植物プランクトンの70%以上が生細胞として検出された。さらに、フコキサンチンを含む植物プランクトン(主に珪藻類とプリムネシオ藻類)の細胞生存率は100%に近い値であった。以上の結果から、本調査海域において、植物プランクトンの細胞生存率に季節変化があることが初めて明らかとなった。また、本調査海域の植物プランクトンの除去過程を考える上で、特に晩夏の植物プランクトンの細胞死は決して無視できない過程であることが示唆された。以上の結果をまとめて、国際誌に投稿するための論文を作成した。
    日本学術振興会, 若手研究(A), 北海道大学, 15681001
  • Dynamics of trace bioelements and their effects on the ecosystem in the marine environment
    Grants-in-Aid for Scientific Research
    2001 - 2003
    SOHRIN Yoshiki; HASEGAWA Hiroshi; SUZUKI Koji; OKAMURA Kei
    1. An analytical method for the determination of trace metals in seawater has been developed on the basis of chelating adsorbent column extraction-ICP mass spectrometry. The distributions of Fe, Co, Ni, Cu, Zn, Cd, and Pb in the North Pacific have been observed. The concentration of acid-dissolvable Fe is higher than that of dissolved Fe, showing the dominance, of labile particulate Fe in seawater. Although dissolved Fe and Zn in summer surface water are depleted in the subarctic North Pacific, they are abundant in the subtropical North Pacific.
    2. We have found that there was an east-west gradient in the photosynthetic, competence of phytoplankton in the subarctic North Pacific in the summer of 1999 and that the difference was probably caused by Fe levels in seawater. A dramatic floristic shift was found by pigment signatures.
    3. We have participated a mesoscale Fe enrichment in the western subarctic North Pacific (SEEDS2001). The photochemical quantum efficiency of algal photosystem suggested that the phytoplankton community was suffered from Fe stress and the Fe enrichment improved the physiological condition. There was some 5 nM of labile particulate Fe in the field. It had been supplied by aeolian dust, but it was not readily available for phytoplankton. The decrease in dissolved Co, Ni, Cu, Zn, and Cd occurred during the phytoplankton bloom.
    4. A sensitive analytical method has been developed using chelating ligand exchange-adsorptive cathodic stripping voltammetry, and Fe ligands derived from eukaryotic phytoplankton have been detected.
    5. We have developed a technique to separate and purify RNA from phytoplankton under Fe stress. The composition change in membrane proteins of Fe-stressed phytoplankton has been observed.
    6. Incubation experiments of phytoplankton have shown that the growth of phytoplankton is controlled by the species and concentrations of co-existing organic ligands.
    Japan Society for the Promotion of Science, Grant-in-Aid for Scientific Research (B), Kyoto University, 13440166
  • Bio phile element composition and species composition of marine phytoplaskton
    Grants-in-Aid for Scientific Research
    1997 - 1999
    MASUZAWA Toshiyuki; HAMA Takeo; SUZUKI Koji
    Products of biological production by phytoplankton (organic matter, calcium carbonate and opal) in the euphotic layer of the oceans are starting materials from material cycling of both major (N, P, Si, Ca, etc.) and minor biophile elements in the oceans. The data on elemental compositions from major to trace elements of these marine biological products have been quite limited. The purposes of this study are : to collect marine phytoplankton samples from the subarctic north Pacific and Bering Sea area with a specially designed non-metal NORPAC net, to develop a simple stepwize leaching method for major component analysis and for fractionation of major and trace elements into each major component phases, to obtain multi-element compositions of marine phytoplanlkton samples and to compare the elemental composition and species composition of phytoplankton samples.
    We sampled phytoplankton samples mainly composed of diatom with a size range of 25-335 μm from the subarctic North Pacific and Bering Sea area, developed a simple stepwize leaching method to analyze sea salt, calcium carbonate, organic matter, opal and residual aluminosilicate, determined the fractionation of major and trace elements in to these major components. Species compositions of these phytoplankton samples were identified microscopically. As the results we showed the 12 major and trace element compositions in biogenic phase of these samples and estimated the association of these elements with biogenic phases. The analytical method developed here will become an effective method to clarify the behaviors of these elements associating with biological production in marine environments.
    Japan Society for the Promotion of Science, Grant-in-Aid for Scientific Research (B), Nagoya University, 09440191
  • 海洋植物プランクトンの生化学組成と基礎生産力に対する紫外線の影響
    科学研究費助成事業
    1997 - 1998
    鈴木 光次
    今年度は、南極産の中心目珪藻Chatoceros dichaeta、羽状目珪藻Nitzscha sp.、プリムネシオ藻Phaeocysris sp.のバッチ培養株に白色光線(PAR)及び紫外線(UVA+UVB)を人工的に照射し、各株の光合成系IIの光化学反応の量子収率(F_v/F_m)、有効光吸収断面(σ_)、第一電子受容体(Q_A^-)の酸化時定数(τQ_A^-)に対する紫外線の影響をFast Repetition Rate Fluorometer(FRRF)を用いて調査した。その際、全光エネルギーが約25W/m^2になるように、UVB/PAR比を0.01%、0.25%、2.94%と変化させて、3つの光環境を設定した(以後、それぞれの光環境を順にL1、L2、L3と呼ぶ)。全ての株において、UVB/PAR比のF_v/F_m、σ_、τQ_A^-値をLlのそれぞれの値と比較した結果、これらの間に統計的な有意差は認められなかった。この事は、L2ではこれら株の光合成系IIの反応中心に対してUVBの影響がなかったことを示唆している。しかしながら、L3では、全ての株において、光化学変換効率の指標であるF F mが、LlやL2のそれと比べて、明らかに低下した。また、同様に、L3のτQ_A^-はLlやL2のそれと比較して大きくなった事から、L3では光合成系2と系1間の電子伝達効率が低下したことを示唆している。これらの事から、L3では全ての株の光合成系IIの反応中心がUVBにより損傷を受けたと考えられる。LlやL2において、Phaeocystis sp.のF F mはNitzschiasp.のそれと同程度であったが、L3ではNitzschia sp.のF F m?がPhaeocystis sp.のそれに比べて大きく低下した。このような植物プランクトンのUVBに対する耐性の差は、今後、地上に到達するUVBが増加した場合、植物プランクトン群集構造の変化、延いては海洋の食物連鎖や物質循環の構造を変える事に繋がるかもしれない。この実験の他にも、紫外線照射による生化学物質の合成速度を調べる実験を同時に行い、現在、試料を分析中である。以上をまとめて、投稿論文を早急に作成する予定である。
    日本学術振興会, 奨励研究(A), 名古屋大学, 09780492
■ Industrial Property Rights
  • 濾過採取装置
    Patent right, 大江亮一 (25%); 大廣洋 (25%); 鈴木光次 (50%), 東洋濾紙株式会社; 北海道大学
    特願2016-27268, 16 Feb. 2016
    特開2017-146168, 24 Aug. 2017
    特許第6484572号
    13 Mar. 2019, 東洋濾紙株式会社; 北海道大学