Japan Geoscience Union Meeting 2016

Presentation information


Symbol A (Atmospheric and Hydrospheric Sciences) » A-CG Complex & General

[A-CG23] Coastal Ecosystems ? 1. Water Cycle and Land-Ocean Interactions

Tue. May 24, 2016 5:15 PM - 6:30 PM Poster Hall (International Exhibition Hall HALL6)

Convener:*Jun Shoji(Hiroshima University), Ryo Sugimoto(Faculty of Marine Biosciences, Fukui Prefectural University), Makoto Yamada(Research Institute for Humanity and Nature), Masahiko Ono(National Institute of Advanced Industrial Science and Technology)

5:15 PM - 6:30 PM

[ACG23-P04] A comparative study of in situ primary productivity under different sites of submarine groundwater discharge impacts in Japanese coasts

*Ryo Sugimoto1, Katsuhiro Kitagawa1, Saori Nishi1, Hisami Honda2, Makoto Yamada2, Shiho Kobayashi3, Jun Shoji4, Shinji Ohsawa5, Makoto Taniguchi2, Osamu Tominaga1 (1.Faculty of Marine Biosciences, Fukui Prefectural University, 2.Research Institute for Humanity and Nature, 3.Field Science Education and Research Center, Kyoto University, 4.Hiroshima University, 5.Institute for Geothermal Sciences, Kyoto University)

Keywords:Primary productivity, 222Rn, Submarine groundwater discharge, Coastal seas

In recent years, a number of studies have shown that submarine groundwater discharge (SGD) is an alternative nutrient pathway and can drive primary production in coastal seas. However, very little is known about an exact relationship between input of groundwater and response of primary production. To clarify the relationship, we conducted in situ measurements of primary productivity using stable 13C tracer method under different strength sites of SGD in the Japanese coasts (Site A: Obama Bay, Site B: Beppu Bay and Site C: the coastal area of Mt. Chokai) in summer from 2013 to 2015. Simultaneously, 222Rn activity was measured as SGD index. 222Rn activity in Site A, B and C varied from 0.8 to 6.0 dpm L-1, 3.6 to 11.2 dpm L-1 and 0.4 to 444.5 dpm L-1, respectively. In situ primary productivity in Site A, B and C ranged from 7.0 to 49.5 μg C L-1 h-1, 10.7 to 38.4 μg C L-1 h-1 and 0.8 to 11.8 μg C L-1 h-1, respectively. In site A, there was significant relationship between in situ primary productivity and 222Rn activity. Although light intensity and water temperature were different in each station and month, concentrations of nutrients limited primary productivity. In site B and C, concentrations of dissolved inorganic nitrogen and phosphorus showed significant increasing trends with an increase of 222Rn activity, indicating nutrients in coastal regions were mainly derived from the SGD. However, there were no clear relationships between in situ primary productivity and 222Rn activity, since primary production would be limited by light intensity as well as nutrients. Our experimental studies clearly showed that nutrients through the SGD affect crucial impact on primary production in coastal ecosystems.