Abstract
The content of chlorophyll (Chl), the intensity of delayed fluorescence (DF), the primary production (PP), and the concentrations of macronutrients were measured in the northwestern part of the Sea of Japan during cruise 30 of R/V Professor Gagarinskii in the autumn of 2000. Sixty-three stations were executed in two steps: October 12–17 (stations 2–34) and October 29–November 3 (stations 35–63). At all the stations, CTD probes were performed. Three cross sections were executed twice within a 2-to 3-week interval, during which structural changes in the hydrological fields took place due to the development of an upwelling. During this time, the length of a day and the daily photosynthetically active radiation (PAR) decreased notably. The vertical profiles of Chl and DF showed pronounced maxima. The waters of the shallow-water stations were characterized by an increased Chl content as compared to the deep-water stations. The content of Chl in the photosynthetic layer amounted from 11 to 30 mg/m2; the PP values were from 120 to 520 mg C/m2/day. At the shallow-water stations, during the second step, the Chl concentration increased by roughly 60% (on average, from 0.47 ± 0.22 to 0.77 ± 0.42 mg/m3); the PP value grew by about 40% (from 268 ± 67 to 370 ± 72 mg C/m2/day). At the deep-water stations, this increase was small (the Chl concentration and PP value increased from 0.37 ± 0.20 to 0.41 ± 0.18 mg/m3 and from 356 ± 72 to 377 ± 74 mg C/m2/day, respectively). The changes noted proceeded due to the increase in the nutrient concentrations during the time between the two surveys, despite the decrease in the length of the day and of the daily PAR. The observations performed showed that, during the autumn time, the horizontal water advection across the shelf, caused by the development of the upwelling, plays the key role in the variations of the production characteristics of the Primor’e coastal zone.
Similar content being viewed by others
References
O. D. Barteneva, E. A. Polyakova, and N. P. Rusin, Regime of Natural Illumination on the Territory of the USSR (Gidrometeoizdat, Leningrad, 1971) [in Russian].
M. E. Vinogradov, E. A. Shushkina, and V. I. Vedernikov, “The Features of Epipelagic Ecosystems of the Pacific from Satellite and Expeditionary Data. Primary Production and Its Seasonal Variations,” Okeanologiya 36(2), 241–249 (1996) [Oceanology 36 (2), 222–230 (1996)].
I. A. Goncharenko, V. G. Federyakov, A. Yu. Lazaryuk, and V. I. Ponomarev, “Thematic AVHRR Data Processing by the Example of the Studies of a Near-Shore Upwelling,” Issled. Zemli Kosmosa, No. 2, 97–107 (1993).
I. A. Zhabin, O. L. Gramm-Osipova, and G. I. Yurasov, “Wind-Induced Upwelling off the Northwestern Coast of the Japan Sea,” Meteorol. Gidrol., No. 10, 82–86 (1993).
V. I. Zvalinskii and F. F. Litvin, “Dependence of Photosynthesis on the Concentration of Carbon Dioxide and on the Intensity and Spectral Composition of the Light,” Fiziol. Rastenii 35(3), 444–457 (1988).
G. N. Ivanov-Frantskevich, “On the Vertical Stability of Water Layers,” Trudy Inst. Okeanol. Akad. Nauk SSSR 19, 1–45 (1956).
O. I. Koblents-Mishke, “Extract and Non-Extract Techniques for Determination of Photosynthetic Pigments in a Sample,” in Modern Methods for Quantitative Estimation of Marine Plankton Distribution (Nauka, Moscow, 1983), pp. 114–125 [in Russian].
O. I. Koblents-Mishke and V. I. Vedernikov, “Primary Production,” in Oceanology. Ocean Biology: Vol. II. Biological Productivity of the Ocean, Ed. by M. E. Vinogradov (Nauka, Moscow, 1977), pp. 183–209 [in Russian].
S. Yu. Ladychenko, “Changes in the Thermal Structure of the Surface Waters off the Coasts of Primor’e in the Autumn Period of 2000,” in Oceanological Studies (Dal’nauka, Vladivostok, 2002), pp. 73–83 [in Russian].
D. N. Matorin, I. R. Vasil’ev, P. S. Venediktov, and S. P. Zakharkov, “Method for Continuous Probing of Active Phytoplankton in Basins through Delayed Luminiscence Registration,” Gidrobiol. Zh. 22(2), 87–89 (1986).
Modern Methods for Hydrochemical Studies of the Ocean (IO RAN, Moscow, 1992) [in Russian].
Yu. I. Sorokin, “Determination of the Productivity of Phytoplankton Photosynthesis in the Water Column Using C14,” Fiziol. Rastenii 6, 118–125 (1959).
Yu. I. Sorokin, “Vertical Structure and Production of the Microplanktonic Community in the Japan Sea during the Summer Period,” Okeanologiya 14(2), 327–332 (1974).
P. Ya. Tishchenko, L. D. Talley, V. B. Lobanov, et al., “Seasonal Variability of the Hydrochemical Conditions in the Sea of Japan,” Okeanologiya 43(5), 683–695 (2003) [Oceanology 43 (5), 643–655 (2003)].
V. P. Shuntov, Biology of the Far East Seas of Russia (TINRO-tsentr, Vladivostok, 2001) [in Russian].
G. I. Yurasov, “Features of the Water Structure and Dynamics in the Northern Part of the Japan Sea,” Available from VINITI, No. 168-V95 (Moscow, 1995).
M. J. Behrenfeld and P. G. Falkowski, “Photosynthetic Rates Derived from Satellite-Based Chlorophyll Concentration,” Limnol. Oceanogr. 42, 1–20 (1997).
M. J. Behrenfeld and P. G. Falkowski, “A Consumer’s Guide to Phytoplankton Primary Production Models,” Limnol. Oceanogr. 42, 1479–1491 (1997).
M. J. R. Fasham, “Variations in the Seasonal Cycle of Biological Production in Subarctic Oceans: A Model Sensitivity Analisys,” Deep-Sea Res. 42, 1111–1149 (1995).
G.-C. Gong and G.-J. Liu, “An Empirical Primary Production Model for the East China Sea,” Cont. Shelf Res. 23, 213–224 (2003).
Y. Kano, N. Baba, and S. Ebara, “Chlorophyll a and Primary Production in the Japan Sea.” Oceanogr. Mag. 34, 31–39 (1984).
M. Kawamiya, M. J. Kishi, Y. Yamanaka, and N. Suginohara, “An Ecological-Physical Coupled Model Applied tTo Station Papa,” J. Oceanogr 50, 635–664 (1995).
S.-W. Kim, S.-I. Saitoh, J. Ishizaka, et al., “Temporal and Spatial Variability of Phytoplankton Pigment Concentrations in the Japan Sea Derived from CZCS Images,” J. Oceanogr. 56, 527–538 (2000).
J. T. Kirk, “The Nature and Measurement of the Light Environment in the Ocean,” in Primary Production and Biogeochemical Cycles in the Sea (Plenum, New York, 1992), pp. 9–29.
V. B. Lobanov, “PICES IX Japan/East Sea Cruise,” PICES Press 9(1), 31–34 (2001).
D. A. Pilgrim, “Measurement and Estimation of the Extinction Coefficient in Turbid Estuarine Waters,” Cont. Shelf Res. 7, 1425–1428 (1987).
T. Platt, “Primary Production of the Ocean Water Column As a Function of Surface Light Intensity: Algorithms for Remote Sensing,” Deep-Sea Res. 33(2), 149–163 (1986).
Determination of Photosynthetic Pigments in Seawater. Monogr. on Oceanogr. Metodol.) (SCOR-UNESCO, Paris, 1966).
J. F. Talling, “Photosynthetic Characteristics of Some Freshwater Plankton Diatoms in Relation to Underwater Radiation,” New Phytol. 56, 29–50 (1957).
V. I. Zvalinsky, “A New Approach to the Modeling of Marine Ecosystems,” PICES Scientific Report, No. 16, 43–59 (2001).
Author information
Authors and Affiliations
Additional information
Original Russian Text © V.I. Zvalinskii, V.B. Lobanov, S.P. Zakharkov, P.Ya. Tishchenko, 2006, published in Okeanologiya, 2006, Vol. 46, No. 1, pp. 27–37.
Rights and permissions
About this article
Cite this article
Zvalinskii, V.I., Lobanov, V.B., Zakharkov, S.P. et al. Chlorophyll, delayed fluorescence, and primary production in the northwestern part of the Sea of Japan. Oceanology 46, 23–32 (2006). https://doi.org/10.1134/S0001437006010048
Received:
Accepted:
Issue Date:
DOI: https://doi.org/10.1134/S0001437006010048