日本地球惑星科学連合2015年大会

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セッション記号 M (領域外・複数領域) » M-IS ジョイント

[M-IS26] 生物地球化学

2015年5月28日(木) 09:00 〜 10:45 104 (1F)

コンビーナ:*楊 宗興(東京農工大学)、柴田 英昭(北海道大学北方生物圏フィールド科学センター)、大河内 直彦(海洋研究開発機構)、山下 洋平(北海道大学 大学院地球環境科学研究院)、座長:吉川 知里(東京工業大学大学院総合理工学研究科)、布浦 拓郎(独立行政法人海洋研究開発機構海洋生命理工学研究開発センター)

09:30 〜 09:45

[MIS26-03] 親潮黒潮移行域における真核ピコ植物プランクトンの系統群組成

*片岡 剛文1山口 晴代1桑田 晃2河地 正伸1 (1.国立環境研究所、2.東北区水産研究所)

キーワード:真核ピコ植物プランクトン, フローサイトメトリ, パイロシーケンス, 18S rDNA, 時空間的分布, 親潮黒潮移行域

Eukaryotic picophytoplankton (less than 3 μm) is ecologically and biogeochemically significant component in the marine microbial food web. Recently, studies about marine microbial diversity have been accelerated using molecular techniques, but basic information of picophytoplankton about diversity is still limited because of (i) lacking the 18S rDNA data in public database and (ii) fragile trait of the cell preventing sample collection. In this study, we investigated the phylogenetic diversity of surface community in one of the productive region of Japan, Oyashio and Kuroshio transition region. For the spatiotemporal comparison, seawater samples were collected from four geographically different sites with seasonal replicates (five seasons): Oyashio, Oyashio—Kuroshio transition regions, and mouth and head of the Sendai Bay. In order to better analyze the picophytoplankton community, we applied an efficient approach based on pyrosequencing of the 18S rDNA amplicon using flowcytometry sorting of cryopreserved cells. From the cleaned 10,000 reads came from the sorted 2,500 cells, 90−120 operational taxonomic units (OTUs: 95% cut off) were observed in each site and dominated by three higher level taxonomic groups: Stramenopiles (31—43%), Alveolata (16—35%) and Rhizaria (7—12%). Of the total of 217 OTUs, 40 OTUs were common among sites, and those included 21 OTUs common among five seasons, indicating spatially and temporally widespread distributing OTUs in this area. On the other hand, 21—38 OTUs were detected only in a site, indicating the local population. Multivariate analyses of OTUs compositions showed seasonal change of the community in each site (nMDS) and showed that the compositions were grouped by seasons (p<0.01) rather than by geographical difference (p=0.5). Thus, the phylogenetic composition of picophytoplankton in the Oyashio—Kuroshio transition region were composed of widespread and local phylotypes, and dynamically changed among seasons.