Influence of zinc and iron enrichments on phytoplankton growth in the northeastern subarctic Pacific

被引:90
作者
Crawford, DW
Lipsen, MS
Purdie, DA
Lohan, MC
Statham, PJ
Whitney, FA
Putland, JN
Johnson, WK
Sutherland, N
Peterson, TD
Harrison, PJ
Wong, CS
机构
[1] Univ Southampton, Southampton Oceanog Ctr, Sch Ocean & Earth Sci, Southampton SO14 3ZH, Hants, England
[2] Univ British Columbia, Dept Earth & Ocean Sci, Vancouver, BC V6T 1Z4, Canada
[3] Fisheries Oceans Canada Inst Ocean Sci, Sect Ocean Climate Chem, Sidney, BC V8L 4B2, Canada
[4] Florida State Univ, Dept Oceanog, Tallahassee, FL 32306 USA
关键词
D O I
10.4319/lo.2003.48.4.1583
中图分类号
Q [生物科学];
学科分类号
07 ; 0710 ; 09 ;
摘要
Near-surface seawater from the northeastern subarctic Pacific was incubated on deck for 8 d, supplemented with (1) control, no additions (2) +Zn (3) +Fe (4) +Zn+Fe. Concentrations of total Zn and Fe at time zero (t(0)) and in the control remained at similar to0.1-0.2 nmol L-1. In the control, chlorophyll (<0.3 mg m(-3)), C-14 uptake into POC and PIC, and inorganic nutrients all remained relatively constant. Addition of Zn slightly but significantly increased chlorophyll (p < 0.05), decreased phosphate (p < 0.01) and nitrate (p < 0.05), and in P versus E experiments, increased P-m > 10-fold and P-m(chl) 2-3-fold. The abundance of small diatoms and coccolithophores was higher in the +Zn treatment compared to the control. The +Fe and +Zn+Fe treatments, compared to the control, both showed > 10-fold increases in chlorophyll and C-14 Uptake into POC and PIC and complete removal of nitrate (less than or equal to 0.2 mmol m(-3)). However, differences were observed in size-fractionated data; the +Zn+Fe treatment had significantly lower percent chlorophyll in the > 20-mum fraction (p < 0.01) and a higher percentage in the 0.2-5-mum fraction (p < 0.01) than the +Fe treatment. In P versus E experiments, both +Fe treatments increased P-m and alpha around 100-fold and P-m(chl) and alpha(chl) by 5-10-fold compared to the control. The +Fe treatment showed a slightly higher alpha(chl) and slightly lower P-m(chl) than the +Zn+Fe treatment. Abundance of large diatoms, small diatoms, small flagellates, and coccolithophores all increased substantially (similar to7-1,000-fold) in response to Fe addition, whereas dinoflagellate abundance only doubled. The +Zn+Fe treatment had higher abundances of small-diatoms and small flagellates than the +Fe treatment. We conclude that Zn additions had limited influence on conventional indices of phytoplankton growth compared to Fe, but that there might be subtle influences of Zn that require further attention.
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页码:1583 / 1600
页数:18
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