2 Falkowski P G, Laws E A, Barber R T, et al. Phytoplankton and their role in primary, new, and export production. In: Fasham M J R, ed. Ocean Biogeochemistry: The Role of the Ocean Carbon Cycle in Global Change. New York: Springer, 2003. 99-121
[2]
4 Harrison K G. Role of increased marine silica input on paleo-pCO2 levels. Paleoceanography, 2000, 15: 292-298
[3]
9 Zhao M X, Mercer J L, Eglinton G, et al. Comparative molecular biomarker assessment of phytoplankton paleoproductivity for the last 160 kyr off Cap Blanc, NW Africa. Org Geochem, 2006, 37: 72-97
14 Ning X, Chai F, Xue H, et al. Physical-biological oceanographic coupling influencing phytoplankton and primary production in the South China Sea. J Geophys Res, 2004, 109, doi: 10.1029/2004JC002365
23 Jing Z Y, Qi Y Q, Hua Z L, et al. Numerical study on the summer upwelling system in the northern continental shelf of the South China Sea. Cont Shelf Res, 2009, 29: 467-478
[10]
24 Ning X, Lin C, Hao Q, et al. Long term changes in the ecosystem in the northern South China Sea during 1976-2004. Biogeosciences, 2009, 6: 2227-2243
[11]
29 Chen Y L. Spatial and seasonal variations of nitrate-based new production and primary production in the South China Sea. Deep-Sea Res Part I-Oceanogr Res Pap, 2005, 52: 319-340
[12]
30 Gan J P, Li L, Wang D X, et al. Interaction of a river plume with coastal upwelling in the northeastern South China Sea. Cont Shelf Res, 2009, 29: 728-740
36 Jiang Y W, Chai F, Wan Z W, et al. Characteristics and mechanisms of the upwelling in the southern Taiwan Strait: A three-dimensional numerical model study. J Oceanogr, 2011, 67: 699-708
38 Chu P C, Li R. South China Sea isopycnal-surface circulation. J Phys Oceanogr, 2000, 30: 2419-2438
[17]
41 Xu J P, Shi M, Zhu B K, et al. Several characteristics of water exchange in the Luzon Strait. Acta Oceanol Sin, 2004, 23: 11-22
[18]
49 Li K Z, Yin J Q, Huang L M, et al. Monsoon-forced distribution and assemblages of appendicularians in the northwestern coastal waters of South China Sea. Estuar Coast Shelf Sci, 2010, 89: 145-153
[19]
1 Falkowski P G, Barber R T, Smetacek V. Biogeochemical controls and feedbacks on ocean primary production. Science, 1998, 281: 200-206
[20]
3 Martin J H, Coale K, Johnson K, et al. Testing the iron hypothesis in ecosystems of the equatorial Pacific Ocean. Nature, 1994, 371: 123-129
6 Kohfeld K E, Quéré C L, Anderson R F, et al. Role of marine biology in glacial-interglacial CO2 cycles. Science, 2005, 308: 74-78
[23]
7 Cerme?o P, Dutkiewicz S, Harris R P, et al. The role of nutricline depth in regulating the ocean carbon cycle. Proc Natl Acad Sci USA, 2008, 105: 20344-20349
15 Chen Y L, Chen H Y. Seasonal dynamics of primary and new production in the northern South China Sea: The significance of river discharge and nutrient advection. Deep-Sea Res Part I-Oceanogr Res Pap, 2006, 53: 971-986
21 Han A, Dai M, Kao S-J, et al. Nutrient dynamics and biological consumption in a large continental shelf system under the influence of both a river plume and coastal upwelling. Limnol Oceanogr, 2012, 57: 486-502
25 Chen Y L, Chen H Y, Karl D M, et al. Nitrogen modulates phytoplankton growth in spring in the South China Sea. Cont Shelf Res, 2004, 24: 527-541
[34]
26 Xu J. Nutrient limitation in the Pearl River Estuary, Hong Kong waters and adjacent South China Sea waters. Doctor Dissertation. Hong Kong: Hong Kong University of Science and Technology, 2007
31 Gan J P, Lu Z M, Dai M H, et al. Biological Response to intensified upwelling and to a river plume in the northeastern South China Sea: A modeling study. J Geophys Res, 2010, 115: C09001, doi: 10.1029/2009JC005569
[38]
32 Zhao H, Tang D L, Wang D X. Phytoplankton blooms near the Pearl River Estuary induced by Typhoon Nuri. J Geophys Res, 2009, 114: C12027, doi: 10.1029/2009JC005384
[39]
33 Chow C H, Hu J H, Centurioni L R, et al. Mesoscale Dongsha Cyclonic Eddy in the northern South China Sea by drifter and satellite observations. J Geophys Res, 2008, 113: C04018, doi: 10.1029/2007JC004542
39 Qu T. Upper-layer circulation in the South China Sea. J Phys Oceanogr, 2000, 30: 1450-1460
[42]
40 Qu T. Evidence for water exchange between the South China Sea and the Pacific Ocean through the Luzon Strait. Acta Oceanol Sin, 2002, 21: 175-185
[43]
42 Tian J W, Yang Q, Liang X, et al. Observation of Luzon Strait transport. Geophys Res Lett, 2006, 33: L19607, doi: 10.1029/2006GL026272.
[44]
43 Yang Q X, Tian J W, Zhao W. Observation of Luzon Strait transport in summer 2007. Deep-Sea Res Part I-Oceanogr Res Pap, 2010, 57: 670-676
[45]
44 Chen G X, Hu P, Hou Y J, et al. Intrusion of the Kuroshio into the South China Sea in September 2008. J Oceanogr, 2011, 67: 439-448
[46]
45 Nan F, Xue H J, Chai F, et al. Identification of different types of Kuroshio intrusion into the South China Sea. Ocean Dyn, 2011, 61: 1291-1304
[47]
46 Su J, Pohlmann T. Wind and topography influence on an upwelling system at the eastern Hainan coast. J Geophys Res, 2009, 114: C06017, doi: 10.1029/2008JC005018
[48]
47 Su J, Wang J, Pohlmann T, et al. Theinfluence of meteorological variation on the upwelling system off eastern Hainan during summer 2007-2008. Ocean Dyn, 2011, 61: 717-730
50 Xiu P, Chai F, Shi L, et al. A census of eddy activities in the South China Sea during 1993-2007. J Geophys Res, 2010, 115: C03012, doi: 10.1029/2009J C005657