Phytoplankton processes. Part 2. Rates of primary production and factors controlling algal growth during the Southern Ocean Iron RElease Experiment (SOIREE)

被引:76
作者
Gall, MP
Strzepek, R
Maldonado, M
Boyd, PW
机构
[1] NIWA, Natl Inst Water & Atmospher Res Ltd, Christchurch, New Zealand
[2] McGill Univ, Dept Biol, Montreal, PQ H2T 2V8, Canada
[3] Univ British Columbia, Dept Bot, Vancouver, BC V6T 1Z4, Canada
[4] Univ British Columbia, Dept Oceanog, Vancouver, BC V6T 1Z4, Canada
[5] Univ Otago, Dept Chem, Ctr Chem & Phys Oceanog, Natl Inst Water & Atmospher Res Ltd,NIWA, Dunedin, New Zealand
关键词
D O I
10.1016/S0967-0645(01)00009-1
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
The Southern Ocean Iron RElease Experiment (SOIREE) fertilised 200km(2) of polar waters (mixed-layer depth, 65 m) south of Australia in February 1999. During the 13-d SOIREE, iron enrichment stimulated primary production, algal growth and biogenic silica production rates. A floristic shift from small to large cells resulted in a greater contribution to community production by diatoms, which contributed > 60% to community production towards the end of SOIREE. Column-integrated rates of primary production increased by more than 10-fold, and community production rates (normalised to chlorophyll) had doubled by day 4, but then declined after day 6 to initial rates. Iron enrichment increased the growth rates of the algal community from 0.02 to 0.15d(-1) (based on changes in in-situ chlorophyll concentrations), from 0.02 to 0.2 d(-1) (based on algal carbon), and more than doubled initial rates (based on C-14) to 0.2 d(-1) during SOIREE. However, these iron-elevated rates were less than the maximum rates (0.69 d(-1)) predicted for waters at 2.5 degreesC, Community biogenic silica production rates increased by 6-fold, i.e. to a lesser extent than primary production rates, resulting in a 2-fold reduction in the silicic-acid:carbon uptake ratio. Shipboard perturbation experiments indicated that iron, rather than both iron and light, limited algal growth in these waters. However, a significant increase in light attenuation in situ due to algal self-shading, suggested that light limitation of algal growth might become significant after day 13 at this locale. Limitation of algal growth by both iron land silicic acid and/or zinc) within iron-fertilised waters after day 8 of SOIREE was not evident from the results of a shipboard experiment. A simple mathematical model of particulate organic carbon (POC) potential export during SOIREE predicted large increases in export, due to both elevated production rates and a floristic shift to large cells. However, no significant increase in POC export was observed during SOIREE. (C) 2001 Elsevier Science Ltd. All rights reserved.
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页码:2571 / 2590
页数:20
相关论文
共 74 条
[1]   Importance of stirring in the development of an iron-fertilized phytoplankton bloom [J].
Abraham, ER ;
Law, CS ;
Boyd, PW ;
Lavender, SJ ;
Maldonado, MT ;
Bowie, AR .
NATURE, 2000, 407 (6805) :727-730
[2]   Primary production in Southern Ocean waters [J].
Arrigo, KR ;
Worthen, D ;
Schnell, A ;
Lizotte, MP .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1998, 103 (C8) :15587-15600
[3]   Southern Ocean iron enrichment promotes inorganic carbon drawdown [J].
Bakker, DCE ;
Watson, AJ ;
Law, CS .
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 2001, 48 (11-12) :2483-2507
[4]   RATES OF PHYTOPLANKTON CELL-DIVISION IN THE FIELD AND IN IRON ENRICHMENT EXPERIMENTS [J].
BANSE, K .
LIMNOLOGY AND OCEANOGRAPHY, 1991, 36 (08) :1886-1898
[5]  
BARTZ R, 1978, OCEAN OPTICS, V5, P102
[6]   Spring development of phytoplankton biomass and composition in major water masses of the Atlantic sector of the Southern Ocean [J].
Bathmann, UV ;
Scharek, R ;
Klaas, C ;
Dubischar, CD ;
Smetacek, V .
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 1997, 44 (1-2) :51-67
[7]   A consumer's guide to phytoplankton primary productivity models [J].
Behrenfeld, MJ ;
Falkowski, PG .
LIMNOLOGY AND OCEANOGRAPHY, 1997, 42 (07) :1479-1491
[8]   Role of iron, light, and silicate in controlling algal biomass in subantarctic waters SE of New Zealand [J].
Boyd, P ;
LaRoche, J ;
Gall, M ;
Frew, R ;
McKay, RML .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1999, 104 (C6) :13395-13408
[9]   EVIDENCE OF THE POTENTIAL INFLUENCE OF PLANKTONIC COMMUNITY STRUCTURE ON THE INTERANNUAL VARIABILITY OF PARTICULATE ORGANIC-CARBON FLUX [J].
BOYD, P ;
NEWTON, P .
DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS, 1995, 42 (05) :619-639
[10]   Phytoplankton dynamics in the NE subarctic Pacific [J].
Boyd, P ;
Harrison, PJ .
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 1999, 46 (11-12) :2405-2432