Enrichment of alkanes within a phytoplankton bloom during an in situ iron enrichment experiment in the western subarctic Pacific

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• 作者：Sohiko Kameyama ; Urumu Tsunogai ; Fumiko Nakagawa ; Motoki Sasakawa ; Daisuke D. Komatsu ; Akira Ijiri ; Junko Yamaguchi ; Takeo Horiguchi ; Hiroshi Kawamura ; Aika Yamaguchi ; Atsushi Tsuda
• 关键词：Iron-enrichment experiment ; Non-methane hydrocarbons ; Trace gases ; Stable isotopic composition ; Phytoplankton ; Subarctic Pacific Ocean
• 刊名：Marine Chemistry
• 出版年：2009
• 出版时间：20 June 2009
• 年：2009
• 卷：115
• 期：1-2
• 页码：92-101
• 全文大小：576 K

文摘

During the Subarctic Pacific Iron Experiment for Ecosystem Dynamics Study ΙΙ (SEEDS-II), we monitored variations in the concentrations of non-methane hydrocarbons (NMHCs), CH₃Cl, N₂O, and CH₄ within a phytoplankton bloom. Stable isotopic compositions were also determined to evaluate the sources of the variations. Although there was little variation in either the concentrations or the stable isotopic compositions of alkenes, CH₃Cl, N₂O, and CH₄ during the 23-day observation period, alkane concentrations increased substantially as the phytoplankton bloomed. The column-integrated quantities of alkanes increased to 3 times pre-bloom levels for C₂H₆, 5 times for C₃H₈, and 20 times for n-C₄H₁₀. The δ¹³C values of both C₂H₆ and C₃H₈ remained almost constant while concentrations increased, whereas that of n-C₄H₁₀ increased by about 12‰. To evaluate the sources of the alkanes produced during the bloom, we compared their δ¹³C values with those of alkanes produced in axenic phytoplankton cultures in our laboratory. We concluded that during the SEEDS-ΙΙ experiment the major portions of C₂H₆ and C₃H₈ were produced during the autolysis of diatoms cells, whereas n-C₄H₁₀ was produced during autolysis of other phytoplankton cells such as cryptophytes and dinoflagellates.