Promotion Effect of Asian Dust on Phytoplankton Growth and Potential Dissolved Organic Phosphorus Utilization in the South China Sea

被引:27
作者
Chu, Qiang [1 ,2 ]
Liu, Ying [1 ,3 ]
Shi, Jie [1 ,4 ]
Zhang, Chao [1 ]
Gong, Xiang [5 ]
Yao, Xiaohong [1 ]
Guo, Xinyu [1 ,2 ]
Gao, Huiwang [1 ,4 ]
机构
[1] Ocean Univ China, Key Lab Marine Environm & Ecol, Minist Educ China, Qingdao, Peoples R China
[2] Ehime Univ, Ctr Marine Environm Studies, Matsuyama, Ehime, Japan
[3] Weifang Univ, Coll Chem Chem & Environm Engn, Weifang, Peoples R China
[4] Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao, Peoples R China
[5] Qingdao Univ Sci & Technol, Sch Math & Phys, Qingdao, Peoples R China
关键词
incubation experiments; Asian dust; DOP utilization; oligotrophic region; ultraoligotrophic region; South China Sea; SUBTROPICAL NORTH-ATLANTIC; MESOSCALE IRON ENRICHMENT; NITROGEN-FIXATION; NUTRIENT LIMITATION; MEDITERRANEAN SEA; PACIFIC-OCEAN; SAHARAN DUST; YELLOW SEA; DYNAMICS; MODEL;
D O I
10.1002/2017JG004088
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Dust deposition is an important nutrient source to the South China Sea (SCS), but few in situ experiments were conducted on phytoplankton response to the deposition. We conducted onboard incubation experiments at three stations near Luzon Strait in the SCS, with addition of multiple dissolved inorganic nutrients, Asian dust, and rainwater. From our results, nitrogen and phosphorus were both urgently needed for phytoplankton growth in the SCS, indicated by the evident Chla response to the addition of nitrogen and phosphorus together. Almost no evident response was observed by adding phosphorus or iron alone to incubation waters, although a delayed response of Chla in mass concentration was observed by adding nitrogen alone. The latter implied a possible utilization of dissolved organic phosphorus because of insufficient dissolved inorganic phosphorus in incubation waters. Under such nutrient condition, Asian dust showed an apparent promotion effect on phytoplankton growth by providing sufficient amounts of nitrogen but low phosphorus. Meanwhile, it was found that large sized (> 5m) phytoplankton community showed different responses to dust addition at different stations. At stations A3 and A6, Chaetoceros spp. became the dominant species during the bloom period, while at station WG2, Nitzschia spp. became dominant. In combination with different initial nutrients and Chla levels at the three stations, the different phytoplankton community evolution implied the response difference to external inputs between oligotrophic (stations A3 and A6) and ultraoligotrophic (station WG2) conditions in the SCS.
引用
收藏
页码:1101 / 1116
页数:16
相关论文
共 82 条
[1]   Trace elements in atmospheric precipitation at Northern Jordan measured by ICP-MS: acidity and possible sources [J].
Al-Momani, IF .
ATMOSPHERIC ENVIRONMENT, 2003, 37 (32) :4507-4515
[2]   Marine microorganisms and global nutrient cycles [J].
Arrigo, KR .
NATURE, 2005, 437 (7057) :349-355
[3]   Mesoscale iron enrichment experiments 1993-2005: Synthesis and future directions [J].
Boyd, P. W. ;
Jickells, T. ;
Law, C. S. ;
Blain, S. ;
Boyle, E. A. ;
Buesseler, K. O. ;
Coale, K. H. ;
Cullen, J. J. ;
de Baar, H. J. W. ;
Follows, M. ;
Harvey, M. ;
Lancelot, C. ;
Levasseur, M. ;
Owens, N. P. J. ;
Pollard, R. ;
Rivkin, R. B. ;
Sarmiento, J. ;
Schoemann, V. ;
Smetacek, V. ;
Takeda, S. ;
Tsuda, A. ;
Turner, S. ;
Watson, A. J. .
SCIENCE, 2007, 315 (5812) :612-617
[4]   A mesoscale phytoplankton bloom in the polar Southern Ocean stimulated by iron fertilization [J].
Boyd, PW ;
Watson, AJ ;
Law, CS ;
Abraham, ER ;
Trull, T ;
Murdoch, R ;
Bakker, DCE ;
Bowie, AR ;
Buesseler, KO ;
Chang, H ;
Charette, M ;
Croot, P ;
Downing, K ;
Frew, R ;
Gall, M ;
Hadfield, M ;
Hall, J ;
Harvey, M ;
Jameson, G ;
LaRoche, J ;
Liddicoat, M ;
Ling, R ;
Maldonado, MT ;
McKay, RM ;
Nodder, S ;
Pickmere, S ;
Pridmore, R ;
Rintoul, S ;
Safi, K ;
Sutton, P ;
Strzepek, R ;
Tanneberger, K ;
Turner, S ;
Waite, A ;
Zeldis, J .
NATURE, 2000, 407 (6805) :695-702
[5]   MODELING THE DYNAMICS OF THE NORTH-SEA MESOZOOPLANKTON [J].
BROEKHUIZEN, N ;
HEATH, MR ;
HAY, SJ ;
GURNEY, WSC .
NETHERLANDS JOURNAL OF SEA RESEARCH, 1995, 33 (3-4) :381-406
[6]   Marine nitrogen fixation: what's the fuss? [J].
Capone, DG .
CURRENT OPINION IN MICROBIOLOGY, 2001, 4 (03) :341-348
[7]   One-dimensional ecosystem model of the equatorial Pacific upwelling system. Part I: model development and silicon and nitrogen cycle [J].
Chai, F ;
Dugdale, RC ;
Peng, TH ;
Wilkerson, FP ;
Barber, RT .
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 2002, 49 (13-14) :2713-2745
[8]   Close coupling between phytoplankton growth and microzooplankton grazing in the western South China Sea [J].
Chen, Bingzhang ;
Liu, Hongbin ;
Landry, Michael R. ;
Dai, Minhan ;
Huang, Bangqin ;
Sun, Jun .
LIMNOLOGY AND OCEANOGRAPHY, 2009, 54 (04) :1084-1097
[9]   Spatial and seasonal variations of nitrate-based new production and primary production in the South China Sea [J].
Chen, YFL .
DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS, 2005, 52 (02) :319-340
[10]   Nitrogen modulates phytoplankton growth in spring in the South China Sea [J].
Chen, YLL ;
Chen, HY ;
Karl, DM ;
Takahashi, M .
CONTINENTAL SHELF RESEARCH, 2004, 24 (4-5) :527-541