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Seasonal variation of water-column light utilization efficiency for primary production in Saroma-ko Lagoon

Published online by Cambridge University Press:  13 January 2021

Akihiro Shiomoto Open the ORCID record for Akihiro Shiomoto [Opens in a new window]  and
Yushi Kamuro
Akihiro Shiomoto*
Affiliation:
Faculty of Bioindustry, Tokyo University of Agriculture, 196 Yasaka, Abashiri, Hokkaido099-2493, Japan
Yushi Kamuro
Affiliation:
Graduate School of Environmental Science, Hokkaido University, North 10 West 5, Kita-ku, Sapporo, Hokkaido060-810, Japan
*
Author for correspondence: Akihiro Shiomoto, E-mail: [email protected]
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Abstract

In Saroma-ko Lagoon, where scallop aquaculture is a thriving commercial activity, monitoring primary production is essential for determining the amount of scallops that can be farmed. Using the primary production data obtained so far, we calculated Ψ, an index of water-column light utilization efficiency, and clarified its seasonal variation. Ψ tended to be lower in the spring bloom season (February–April), and higher in the late autumn to winter (October–December). Low chlorophyll-normalized production, an index of growth rate, resulted in lower values, while low daily irradiance resulted in higher values. The values of Ψ from our study had a range of 0.05–1.42 gC gChl-a−1 mol photons−1 m2 (N = 56). These values were within the previously reported range of 0.07–1.92 (gC gChl-a−1 mol photons−1 m2) for seawater and fresh water worldwide. Therefore, it is likely that Ψ varies from 0.05–2 gC gChl-a−1 mol photons−1 m2, being affected by conditions of phytoplankton growth and sunlight intensity, regardless of whether samples are collected from seawater or fresh water. Using the median Ψ value of 0.45 gC gChl-a−1 mol photons−1 m2 obtained in this study, primary production was 0.3–3.5 times the actual production at Saroma-ko Lagoon. Using this method, primary production can be easily and constantly monitored, facilitating the sustainable development of scallop aquaculture.

Keywords

Chlorophyll-achlorophyll-normalized productionlight utilization efficiencyprimary productionSaroma-ko LagoonΨ
Type
Research Article
Information
Journal of the Marine Biological Association of the United Kingdom , Volume 101 , Issue 1 , February 2021 , pp. 39 - 47
Copyright
Copyright © The Author(s), 2021. Published by Cambridge University Press

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References

Behrenfeld, MJ and Falkowski, PG (1997) Photosynthetic rates derived from satellite-based chlorophyll concentration. Limnology and Oceanography 42, 1–20.CrossRefGoogle Scholar
Bruno, SF, Staker, RD and Sharma, GM (1980) Dynamics of phytoplankton productivity in the Peconic Bay Estuary, Long Island. Estuarine and Coastal Marine Science 10, 247–263.CrossRefGoogle Scholar
Cole, BE and Cloern, JE (1987) An empirical model for estimating phytoplankton productivity in estuaries. Marine Ecology Progress Series 36, 299–305.CrossRefGoogle Scholar
Collos, Y and Slawyk, G (1986) 13C And 15N uptake by marine phytoplankton-IV. Uptake ratios and the contribution of nitrate to the productivity of Antarctic waters (Indian Ocean sector). Deep-Sea Research 33, 1039–1051.CrossRefGoogle Scholar
Falkowski, PG (1981) Light-shade adaptation and assimilation numbers. Journal of Plankton Research 3, 203–216.CrossRefGoogle Scholar
Falkowski, PG and Raven, JA (1997) Aquatic Photosynthesis. Boston, MA: Blackwell Science.Google Scholar
Forget, MH, Sathyendranath, S, Platt, T, Pommier, J, Vis, C, Kyewalynga, MS and Hudon, C (2007) Extraction of photosynthesis-irradiance parameters from phytoplankton production data: demonstration in various aquatic systems. Journal of Plankton Research 29, 249–262.CrossRefGoogle Scholar
Glover, HE (1980) Assimilation numbers in culture marine phytoplankton. Journal of Plankton Research 2, 69–79.CrossRefGoogle Scholar
Hama, T., Miyazaki, T, Ogawa, Y, Iwakuma, T, Takahashi, M, Otsuki, A and Ichimura, S (1983) Measurement of a marine phytoplankton population using a stable ¹3C isotope. Marine Biology 73, 31–36.CrossRefGoogle Scholar
Harrison, WG, Platt, T and Irwin, B (1982) Primary production and nutrient assimilation by natural phytoplankton populations of the Eastern Canadian Arctic. Canadian Journal of Fisheries and Aquatic Sciences 39, 335–345.CrossRefGoogle Scholar
Hashimoto, S and Shiomoto, A (2002) Light utilization efficiency of size-fractionated phytoplankton in the subarctic Pacific, spring and summer 1999: high efficiency of large-sized diatom. Journal of Plankton Research 24, 83–87.CrossRefGoogle Scholar
Honda, M, Sasaoka, K, Kawakami, H, Matsumoto, K, Watanabe, S and Dickey, T (2009) Application of underwater optical data to estimate of primary productivity. Deep-Sea Research I 56, 2281–2292.CrossRefGoogle Scholar
Imai, K, Nojiri, Y, Tsurushima, N and Saino, T (2002) Time series of seasonal variation of primary productivity at station KONT (44°N, 155°E) in the sub-Arctic western North Pacific. Deep-Sea Research II 49, 5395–5408.CrossRefGoogle Scholar
Irwin, B, Caverhill, C and Platt, T (1986) Primary Production on the Grand Banks of Newfoundland in April 1984. Canadian Data Report of Fisheries and Aquatic Science 579, 49 pp.Google Scholar
Isada, T, Kuwata, A, Saito, H, Ono, T, Ishii, M, Yoshiwaka, H and Suzuki, K (2009) Photosynthetic features and primary productivity of phytoplankton in the Oyashio and Kuroshio-Oyashio transition regions of the northwestern Pacific. Journal of Plankton Research 31, 1009–1025.CrossRefGoogle Scholar
Jacques, G and Minas, M (1981) Primary productivity in the Indian sector of the Antarctic Ocean during late summer. Oceanologica Acta 4, 33–41. [In French with English abstract.]Google Scholar
Jordan, MB and Joint, R (1984) Studies on phytoplankton distribution and primary production in the western English Channel in 1980 and 1981. Continental Shelf Research 3, 25–34.CrossRefGoogle Scholar
Larrance, JD (1971) Primary production in the mid-subarctic Pacific region, 1966–68. Fishery Bulletin 69, 595–613.Google Scholar
Maita, Y and Odate, T (1988) Seasonal changes in size-fractionated primary production and nutrient concentrations in the temperate neritic water of Funka Bay, Japan. Journal of the Oceanographical Society of Japan 44, 268–279.CrossRefGoogle Scholar
Malone, TC (1976) Phytoplankton productivity in the apex of the New York Bight: environmental regulation of productivity/chlorophyll a. The middle Atlantic continental shelf and New York Bight. Limnology and Oceanography Special Symposium 2, 260–272.Google Scholar
Morel, A (1978) Available, usable and stored radiant energy in relation to marine photosynthesis. Deep-Sea Research 25, 673–688.CrossRefGoogle Scholar
Nishibe, Y, Takahashi, K, Shiozaki, T, Kakehi, S, Saito, H and Furuya, K (2015) Size-fractionated primary production in the Kuroshio Extension and adjacent regions in spring. Journal of Oceanography 71, 27–40.CrossRefGoogle Scholar
Nosaka, Y, Isada, T, Kudo, I, Saito, H, Hattori, H, Tsuda, A and Suzuki, K (2014) Light utilization efficiency of phytoplankton in the Western Subarctic Gyre of the North Pacific during summer. Journal of Oceanography 70, 91–103.CrossRefGoogle Scholar
Platt, T (1988) Primary production of the ocean water column as a function of surface light intensity: algorithms for remote sensing. Deep-Sea Research 33, 149–163.CrossRefGoogle Scholar
Platt, T and Irwin, B (1971) Phytoplankton Production and Nutrients in Bedford Basin, 1969–1970. Fisheries Research Board of Canada Technical Report 247, 172 pp.Google Scholar
Platt, T and Irwin, B (1972) Phytoplankton Production and Nutrient Measurements in Petpepswick Inlet, 1971–1972. Fisheries Research Board of Canada Technical Report 314, 112 pp.Google Scholar
Platt, T, Irwin, B and Subba Rao, DV (1973) Phytoplankton Productivity and Nutrient Measurements on the Spring Phytoplankton Bloom in Bedford Basin 1971. Fisheries Research Board of Canada Technical Report 423, 42 pp.Google Scholar
Platt, T, Sathyendranath, S, Caverhill, CM and Lewis, MR (1988) Ocean primary production and available light: further algorithms for remote sensing. Deep-Sea Research 35, 855–879.CrossRefGoogle Scholar
Shibanuma, S, Kajihara, M and Miyake, H (1995) Water characteristics in Lake Saroma. Bulletin of the Japanese Society of Fisheries Oceanography 59, 429–437. [In Japanese with English abstract.]Google Scholar
Shiomoto, A (2000) Efficiency of water-column light utilization in the subarctic northwestern Pacific. Limnology and Oceanography 45, 982–987.Google Scholar
Suzuki, R and Ishimaru, T (1990) An improved method for determination of phytoplankton chlorophyll using N,N-Dimethylformamide. Journal of Oceanographical Society of Japan 46, 190–194.CrossRefGoogle Scholar
Tada, K, Kurata, M and Nishihama, Y (1993) Seasonal changes of chlorophyll a and nutrients in Lake Saroma. Bulletin of Plankton Society of Japan 39, 163–165.Google Scholar
Takizawa, T (1982) Characteristics of the Soya Warm Current in the Okhotsk Sea. Journal of Oceanographical Society of Japan 38, 281–292.CrossRefGoogle Scholar
Welschmeyer, NA (1994) Fluorometric analysis of chlorophyll a in the presence of chlorophyll b and pheopigments. Limnology and Oceanography 39, 1985–1992.CrossRefGoogle Scholar
Yoshie, N, Suzuki, K, Kuwata, A, Nishioka, J and Saito, H (2010) Temporal and spatial variations in photosynthetic physiology of diatoms during the spring bloom in the western subarctic Pacific. Marine Ecology Progress Series 399, 39–52.CrossRefGoogle Scholar