The Southern Ocean Iron RElease Experiment (SOIREE) - introduction and summary

被引:90
作者
Boyd, PW [1 ]
Law, CS
机构
[1] Univ Otago, Dept Chem, Ctr Chem & Phys Oceanog, NIWA,Natl Inst Water & Atmospher Res, Dunedin, New Zealand
[2] Plymouth Marine Lab, Plymouth PL1 3DH, Devon, England
关键词
D O I
10.1016/S0967-0645(01)00002-9
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
This volume is dedicated to the Southern Ocean Iron RElease Experiment (SOIREE), the first in situ iron fertilisation experiment performed in the polar waters of the Southern Ocean. SOIREE was an interdisciplinary study involving participants from six countries, and took place in February 1999 south of the Polar Front in the Australasian-Pacific sector of the Southern Ocean. Approximately 3800 kg of acidified FeSO4. 7H(2)O and 165 g of the tracer sulphur hexafluoride (SF,) were added to a 65-m deep surface mixed layer over an area of similar to 50 km(2). Initially, mean dissolved iron concentrations were similar to 2.7 nM, but decreased to ambient levels within days, requiring subsequent additions of 1550-1750 kg of acidified FeSO4. 7H(2)O on days 3, 5 and 7 of the experiment. During the 13-day site occupation there were iron-mediated increases in phytoplankton growth rates, with marked increases in chlorophyll a (up to 2 mu gl(-1)) and production rates (up to 1.3 g Cm-2 d(-1)). These resulted in subsequent changes in the pelagic ecosystem structure, and in the cycling of carbon, silica and sulphur, such as a 10% drawdown of surface CO2. The SOIREE bloom persisted for > 40 days following our departure from the site, as observed via SeaWiFS remotely sensed observations of Ocean Colour. Papers in this volume report in detail on aspects of this study, from the oceanographic setting of the experiment to a modelling simulation of the SOIREE bloom. A CD-ROM accompanies this volume and contains the main SOIREE datasets and ancillary information including the pre-experiment 'desktop' database study for site-selection, and satellite images of the SOIREE bloom. (C) 2001 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:2425 / 2438
页数:14
相关论文
共 61 条
[31]   The impact of in situ Fe fertilisation on the microbial food web in the Southern Ocean [J].
Hall, JA ;
Safi, K .
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 2001, 48 (11-12) :2591-2613
[32]   Modeling the bloom evolution and carbon flows during SOIREE: Implications for future in situ iron-enrichments in the Southern Ocean [J].
Hannon, E ;
Boyd, PW ;
Silvoso, M ;
Lancelot, C .
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 2001, 48 (11-12) :2745-2773
[33]  
HART T. JOHN, 1934, DISCOVERY REPTS [GOV DEPENDENCIES FALKLAND ISLS], V8, P1
[34]   A MODEL OF THE FORMATION OF MARINE ALGAL FLOCS BY PHYSICAL COAGULATION PROCESSES [J].
JACKSON, GA .
DEEP-SEA RESEARCH PART A-OCEANOGRAPHIC RESEARCH PAPERS, 1990, 37 (08) :1197-1211
[35]   Modeling phytoplankton blooms and carbon export production in the Southern Ocean: dominant controls by light and iron in the Atlantic sector in Austral spring 1992 [J].
Lancelot, C ;
Hannon, E ;
Becquevort, S ;
Veth, C ;
De Baar, HJW .
DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS, 2000, 47 (09) :1621-1662
[36]   Biological response to iron fertilization in the eastern equatorial Pacific (IronEx II). III. Dynamics of phytoplankton growth and microzooplankton grazing [J].
Landry, MR ;
Constantinou, J ;
Latasa, M ;
Brown, SL ;
Bidigare, RR ;
Ondrusek, ME .
MARINE ECOLOGY PROGRESS SERIES, 2000, 201 :57-72
[37]   Nitrous oxide flux and response to increased iron availability in the Antarctic Circumpolar Current [J].
Law, CS ;
Ling, RD .
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 2001, 48 (11-12) :2509-2527
[38]   Sulphur hexafluoride as a tracer of biogeochemical and physical processes in an open-ocean iron fertilisation experiment [J].
Law, CS ;
Watson, AJ ;
Liddicoat, MI ;
Stanton, T .
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 1998, 45 (06) :977-994
[39]  
LAW CS, UNPUB VERTICAL MIXIN
[40]  
MALDONADO MT, 2001, IN PRESS LIMNOLOGY O