日本地球惑星科学連合2021年大会

講演情報

[E] ポスター発表

セッション記号 M (領域外・複数領域) » M-IS ジョイント

[M-IS05] 南大洋・南極氷床が駆動する全球気候変動

2021年6月6日(日) 17:15 〜 18:30 Ch.20

コンビーナ:関 宰(北海道大学低温科学研究所)、野木 義史(国立極地研究所)、岡 顕(東京大学大気海洋研究所)、菅沼 悠介(国立極地研究所)

17:15 〜 18:30

[MIS05-P20] Molecular analysis of individual fecal pellets collected by using gel sediment traps in the Indian sector of the Southern Ocean

*佐野 雅美1、真壁 竜介1,2,3、黒沢 則夫4、茂木 正人2,1、小達 恒夫1,3 (1.国立極地研究所、2.東京海洋大学、3.総合研究大学院大学、4.創価大学)

キーワード:セジメントトラップ、動物プランクトン、南大洋、沈降粒子

Sinking particles, an important contributor to biological carbon pump, consist of various types of particles. Export efficiencies and sinking speeds are different among types of sinking particles, for example, phytodetritus and fecal pellets. In the Southern Ocean, the contribution of fecal pellets to carbon flux is expected to be high because of the high abundance of the large zooplankton, such as salps and krills, which excrete fast-sinking large fecal pellets. However, in the Indian sector of the Southern Ocean, the krill-independent ecosystem is expected to be important. It is difficult to identify producer of fecal pellets based on morphological information, and fecal pellets contains large amounts of amorphous materials which are difficult to be identified by microscopic analysis. Little is yet known of the sinking process of fecal pellets. In this study, we applied molecular method to individual fecal pellets collected by gel sediment traps for estimating fecal pellet producers and the sinking process of fecal pellets.
Fecal pellet samples were collected from a station (63.5°S, 110°E) during the Southern Ocean cruise of the T/V Umitaka Maru of Tokyo University of Marine Science and Technology. The trap system consisted of gel-filled sediment traps deployed at 50, 200 and 500 m depths. Traps were left to drift for 24h (17 January 2019 to 18 January 2019). After recovery, each gel was preserved at <-60°C until analysis. DNA was extracted from individual fecal pellets picked up from gel under a stereo microscope. Sizes of the fecal pellets were varied (<50 μm to 500 μm diameter). To assess the eukaryotic community structure of the fecal pellets, the 18S rRNA gene V9 region was amplified by using primers 1389F and 1510R and the amplicons were sequenced by high throughput sequencer. Bioinformatics analysis of the sequence data were performed using mothur (Schloss et al. 2009). For estimating zooplankton community structures in this station, VMPS and MOHT nets were towed. Collected zooplankton samples were sorted and counted under a stereo microscope.
Eukaryotic community composition of the fecal pellets in 50 m and 200 m mainly consist of Stramenopiles, Metazoa and Dinophyta. This result indicated that the fecal pellets were excreted by particle feeders. Metazoan community composition of the fecal pellets in 50 m and 200 m mainly consist of copepods (>90%) and were homogenized among all types of fecal pellets which were excreted by various species. Thus, it is considered that the fecal pellets were repackaged several times even in 50 m depth which was just under the Chlorophyll a maximum (40 m depth) and did not sink directly from 50 m to 200 m. Metazoan community composition also showed that potential producers of large fecal pellets were Malacostraca, which include Euphausiids, and Heterobranchia, which include Limacina, but Malacostraca was quite rare. Thus, producer of large fecal pellets is considered to be Limacina. Not only salps and krills, but also Limacina should be focused as fast-sinking large fecal pellet producer which will affect to the efficiency of the transport of POC in this area. We will also discuss zooplankton community structures as potential producers of fecal pellets.