Seasonal variability of phytoplankton community structure in the subtropical western North Pacific

被引:29
作者
Fujiki, Tetsuichi [1 ]
Sasaoka, Kosei [1 ]
Matsumoto, Kazuhiko [2 ]
Wakita, Masahide [3 ]
Mino, Yoshihisa [4 ]
机构
[1] Japan Agcy Marine Earth Sci & Technol, Res & Dev Ctr Global Change, 2-15 Natsushimacho, Yokosuka, Kanagawa 2370061, Japan
[2] Japan Agcy Marine Earth Sci & Technol, Dept Environm Geochem Cycle Res, 2-15 Natsushimacho, Yokosuka, Kanagawa 2370061, Japan
[3] Japan Agcy Marine Earth Sci & Technol, Mutsu Inst Oceanog, 690 Kitasekine, Mutsu, Aomori 0350022, Japan
[4] Nagoya Univ, Inst Space Earth Environm Res, Chikusa Ku, Nagoya, Aichi 4648601, Japan
关键词
CHEMTAX; Fast-repetition-rate fluorometry; North Pacific subtropical gyre; Phytoplankton blooms; Pigments; CLASS ABUNDANCES; CHLOROPHYLL-A; OCEAN; HPLC; GYRE; SEA; PHOTOSYNTHESIS; FLUORESCENCE; DYNAMICS; ATLANTIC;
D O I
10.1007/s10872-015-0346-9
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
During 2010-2012 in the northwestern region of the North Pacific subtropical gyre, we examined seasonal variability of the phytoplankton community with respect to structure and photo-physiological status using the chemotaxonomy program CHEMTAX and fast-repetition-rate fluorometry. Total chlorophyll a standing stock in the upper 150 m (E integral TChl a) varied from 25.5 to 89.0 mg m(-2) during periods of relatively deep vertical mixing (40-207 m), but was fairly constant (18.6-27.2 mg m(-2)) during stratification periods. Prymnesiophytes, chlorophytes, chrysophytes, prasinophytes, and/or diatoms comprised major portions of the E integral TChl a during mixing periods. Diatoms became the most abundant group (29-43 %) in February 2011, when large phytoplankton blooms were observed, whereas Prochlorococcus was the dominant component (15-46 %) during stratification periods. During mixing periods, nitrate and nitrite (NO3 + NO2) concentrations occasionally exceeded 0.5 mu mol kg(-1) in surface waters, and F (v)/F (m) (photochemical efficiency of photosystem II) ranged from approximately 0.40-0.50 within the euphotic zone. During stratification periods, however, NO3 + NO2 concentrations were very low (< 0.1 mu mol kg(-1)) from the surface to 50-95 m, and F (v)/F (m) was in the range of 0.25-0.40 in the upper mixed layer. The seasonal variability of phytoplankton community structure in this region was related to the nutrient supply from deep waters. Additionally, we compared our data to published values at the time-series station ALOHA, located in the eastern region of the NPSG. At Sta. ALOHA in 2011, E integral TChl a was almost constant (19.5-26.4 mg m(-2)) throughout the year and was consistently dominated by Prochlorococcus (61-81 %). These results suggest that the phytoplankton community in the northwestern region of the NPSG is seasonally variable and composed of diverse groups compared with the eastern region of the NPSG.
引用
收藏
页码:343 / 358
页数:16
相关论文
共 29 条
[1]   A comparison of HPLC pigment signatures and electron microscopic observations for oligotrophic waters of the North Atlantic and Pacific Oceans [J].
Andersen, RA ;
Bidigare, RR ;
Keller, MD ;
Latasa, M .
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 1996, 43 (2-3) :517-537
[2]   PHOTOSYNTHETIC PICOPLANKTON COMMUNITY STRUCTURE IN THE SUBTROPICAL NORTH PACIFIC-OCEAN NEAR HAWAII (STATION ALOHA) [J].
CAMPBELL, L ;
VAULOT, D .
DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS, 1993, 40 (10) :2043-2060
[3]   QUANTUM YIELD, RELATIVE SPECIFIC ABSORPTION AND FLUORESCENCE IN NITROGEN-LIMITED CHAETOCEROS-GRACILIS [J].
CLEVELAND, JS ;
PERRY, MJ .
MARINE BIOLOGY, 1987, 94 (04) :489-497
[4]   Temporal and vertical variability in photosynthesis in the North Pacific Subtropical Gyre [J].
Corno, Guido ;
Letelier, Ricardo M. ;
Abbott, Mark R. ;
Karl, David M. .
LIMNOLOGY AND OCEANOGRAPHY, 2008, 53 (04) :1252-1265
[5]   Mixed layer depth over the global ocean:: An examination of profile data and a profile-based climatology -: art. no. C12003 [J].
de Boyer Montégut, C ;
Madec, G ;
Fischer, AS ;
Lazar, A ;
Iudicone, D .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2004, 109 (C12) :1-20
[6]   STUDY OF PLANKTON DYNAMICS AND NUTRIENT CYCLING IN CENTRAL GYRE OF NORTH PACIFIC OCEAN [J].
EPPLEY, RW ;
RENGER, EH ;
VENRICK, EL ;
MULLIN, MM .
LIMNOLOGY AND OCEANOGRAPHY, 1973, 18 (04) :534-551
[7]   In situ observation of phytoplankton productivity by an underwater profiling buoy system:: use of fast repetition rate fluorometry [J].
Fujiki, Tetsuichi ;
Hosaka, Takuji ;
Kimoto, Hideshi ;
Ishimaru, Takashi ;
Saino, Toshiro .
MARINE ECOLOGY PROGRESS SERIES, 2008, 353 :81-88
[8]   Distribution and photo-physiological condition of phytoplankton in the tropical and subtropical North Pacific [J].
Fujiki, Tetsuichi ;
Matsumoto, Kazuhiko ;
Saino, Toshiro ;
Wakita, Masahide ;
Watanabe, Shuichi .
JOURNAL OF OCEANOGRAPHY, 2013, 69 (01) :35-43
[9]   SUBSURFACE CHLOROPHYLL MAXIMUM IN THE TROPICAL AND SUBTROPICAL WESTERN PACIFIC-OCEAN - VERTICAL PROFILES OF PHYTOPLANKTON BIOMASS AND ITS RELATIONSHIP WITH CHLOROPHYLL-A AND PARTICULATE ORGANIC-CARBON [J].
FURUYA, K .
MARINE BIOLOGY, 1990, 107 (03) :529-539
[10]   HPLC determination of phytoplankton pigments using N,N-dimethylformamide [J].
Furuya K. ;
Hayashi M. ;
Yabushita Y. .
Journal of Oceanography, 1998, 54 (2) :199-203