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2018 Vol.23, Issue 1 Preview Page
February 2018. pp. 49-62
Abstract
References
1
Boyd, P. and P. Newton, 1995. Evidence of the potential influence of planktonic community structure on the interannual variability of particulate organic carbon flux. Deep-Sea Research Part I, 42: 619-639.
2
Boyd, P.W., A.J. Watson, C.S. Law, E.R. Abraham, T. Trull, R. Murdoch, et al., 2000. A mesoscale phytoplankton bloom in the polar Southern Ocean stimulated by iron fertilization. Nature, 407: 695-702.
3
Brennwald, M.S., M. Schmidt, J. Oser, and R. Kipfer, 2016. A portable and autonomous mass spectrometric system for on-site environmental gas analysis. Environmental Science & Technology, 50: 13455-13463.
4
Bronk, D.A. and B.B. Ward, (2000). Magnitude of dissolved organic nitrogen release relative to gross nitrogen uptake in marine systems. Limnol. Oceanogr, 45: 1879-1883.
5
C.H. Chang, N.C. Johnson, and N. Cassar, 2014. Neural network-based estimates of Southern Ocean net community production from in-situ O2/ Ar and satellite observation: a methodological study. Biogeosciences, 11: 3279-3297.
6
Cassar, N., B.A. Barnett, M.L. Bender, J. Kaiser, R.C. Hamme, and B. Tilbrook, 2009. Continuous high-frequency dissolved O2/Ar measurements by equilibrator inlet mass spectrometry. Analytical Chemistry, 81: 1855-1864.
7
Cassar, N., P.J. DiFiore, B.A. Barnett, M.L. Bender, A.R. Bowie, B. Tilbrook, et al., 2011. The influence of iron and light on net community production in the Subantarctic and Polar Frontal Zones. Biogeosciences, 8: 227-237.
8
Coale, K.H. and K.W. Bruland, 1985. 234Th:238U disequilibria within the California Current. Limnol. Oceanogr, 30: 22-33.
9
Craig, H., and T. Hayward, 1987. Oxygen supersaturation in the ocean: Biological versus physical contributions. Science, 235: 199-202.
10
Dugdale, R.C. and J.J. Goering, 1967. Uptake of new and regenerated forms of nitrogen in primary productivity. Limnol. Oceanogr, 12: 196-206.
11
Dunne, J., R. Armstrong, A. Gnanadesikan, J. Sarmiento, and R. Slater, 2005. Empirical and mechanistic models for the particle export ratio. Global Biogeochemical Cycles, 19.
12
Eveleth, R., M.-L. Timmermans, and N. Cassar, 2014. Physical and biological controls on oxygen saturation variability in the upper Arctic Ocean. J. of Geophysical Research, 119: 7420-7432.
13
Eveleth, R., N. Cassar, R.M. Sherrell, H. Ducklow, M.P. Meredith, H.J. Venables, et al., 2017. Ice melt influence on summertime net community production along the Western Antarctic Peninsula. Deep-Sea Research Part Ii-Topical Studies in Oceanography, 139: 89-102.
14
Falkowski, P.G., E.A. Laws, , R.T. Barber, and J.W. Murray, 2003. Phytoplankton and their role in primary, new, and export production. In M. J. R. Fasham (Ed.), Ocean Biogeochemistry. Global Change - The IGBP Series (99-121 pp.). Springer Berlin Heidelberg.
15
Ferrón, S., S.T. Wilson, S. Martínez-García, Quay, P.D., and D.M. Karl, 2015. Metabolic balance in the mixed layer of the oligotrophic North Pacific Ocean from diel changes in O2/Ar saturation ratios. Geophysical Research Letters, 42: 3421-3430.
16
Field, C.B., 1998. Primary production of the biosphere: integrating terrestrial and oceanic components. Science, 281, 237-240.
17
Giesbrecht, K.E., R.C. Hamme, and S.R. Emerson, 2012. Biological productivity along Line P in the subarctic northeast Pacific: In situ versus incubation-based methods. Global Biogeochemical Cycles, 26: GB3028.
18
Hahm, D., T.S. Rhee, H.C. Kim, J. Park, Y.N. Kim, H.C. Shin, and S. Lee, 2014. Spatial and temporal variation of net community production and its regulating factors in the Amundsen Sea, Antarctica. J. of Geophysical Research, 119: 2815-2826.
19
Hamme, R., N. Cassar, V. Lance, R. Vaillancourt, M. Bender, P. Strutton, et al. 2012. Dissolved O2/Ar and other methods reveal rapid changes in productivity during a Lagrangian experiment in the Southern Ocean. J. Geophys. Res, 117: C00F12.
20
Hamme, R.C., and J.P. Severinghaus, 2007. Trace gas disequilibria during deep-water formation, 54: 939-950.
21
Howard, E.M., C.A. Durkin, G.M.M. Hennon, F. Ribalet, and R.H.R. Stanley, 2017. Biological production, export efficiency, and phytoplankton communities across 8,000 km of the South Atlantic. Global Biogeochemical Cycles, 31: 1066-1088.
22
IPCC, W., 2013. Climate Change 2013: The Physical Science Basis. (T. F. Stocker, D. Qin, G.-K. Plattner, M. B. Tignor, S. K. Allen, J. Boschung, et al., Eds.) (1-1552 pp.).
23
Kaiser, J., M.K. Reuer, B. Barnett, and M.L. Bender, 2005. Marine productivity estimates from continuous O2/Ar ratio measurements by membrane inlet mass spectrometry. Geophysical Research Letters, 32.
24
Kana, T., C. Darkangelo, M. Hunt, J. Oldham, G. Bennett, and J. Cornwell, 1994. Membrane inlet mass spectrometer for rapid high-precision determination of N2, O2, and Ar in environmental water samples. Anal. Chem., 66: 4166-4170.
25
Kana, T.M., J.C. Cornwell, and L. Zhong, 2006. Determination of denitrification in the chesapeake bay from measurements of N2 accumulation in bottom water. Estuaries and Coasts, 29: 222-231.
26
Laws, E., P. Falkowski, W. Smith, H. Ducklow, and J. McCarthy, 2000. Temperature effects on export production in the open ocean. Global Biogeochemical Cycles, 14: 1231-1246.
27
Laws, E.A., 1991. Photosynthetic quotients, new production and net community production in the open ocean. Deep-Sea Research, 38: 143-167.
28
Laws, E.A., E. D’Sa, and P. Naik, 2011. Simple equations to estimate ratios of new or export production to total production from satellite-derived estimates of sea surface temperature and primary production. Limnol. Oceanogr.: Methods, 9: 593-601.
29
Li, Z. and N. Cassar, 2016. Satellite estimates of net community production based on O2/Ar observations and comparison to other estimates. Global Biogeochemical Cycles, 30: 735-752.
30
Lockwood, D., P.D. Quay, M.T. Kavanaugh, L.W. Juranek, and R.A. Feely, 2012. High-resolution estimates of net community production and air-sea CO2 flux in the northeast Pacific. Global Biogeochemical Cycles, 26: GB4010.
31
Mächler, L., M.S. Brennwald, and R. Kipfer, 2012. Membrane inlet mass spectrometer for the quasi-continuous on-site analysis of dissolved gases in groundwater. Environmental Science & Technology, 46: 8288-8296.
32
Manning, C.C., R.H.R. Stanley, D.P. Nicholson, J.M. Smith, J. Timothy Pennington, M.R. Fewings, et al., 2017. Impact of recently upwelled water on productivity investigated using in situ and incubation-based methods in Monterey Bay. J. of Geophysical Research, 122: 1901-1926.
33
Martin, J.H., G.A. Knauer, D.M. Karl, and W.W. Broenkow, 1987. VERTEX: carbon cycling in the northeast Pacific. Deep Sea Research Part a. Oceanographic Research Papers, 34: 267-285.
34
Nemcek, N., D. Ianson, and P.D. Tortell, 2008. A high-resolution survey of DMS, CO2, and O2/Ar distributions in productive coastal waters. Global Biogeochemical Cycles, 22: GB2009.
35
Palevsky, H.I., F. Ribalet, and J.E. Swalwell, 2013. The influence of net community production and phytoplankton community structure on CO2 uptake in the Gulf of Alaska. Global Biogeochemical Cycles, 27: 664-676.
36
Park, J., F.I. Kuzminov, B. Bailleul, E.J. Yang, S. Lee, P.G. Falkowski, and M.Y. Gorbunov, 2017. Light availability rather than Fe controls the magnitude of massive phytoplankton bloom in the Amundsen Sea polynyas, Antarctica. Limnol. Oceanogr, 48: 2260-2276.
37
Reuer, M., B. Barnett, M. Bender, P. Falkowski, and M. Hendricks, 2007. New estimates of Southern Ocean biological production rates from O2/Ar ratios and the triple isotope composition of O2. Deep-Sea Research Part I, 54: 951-974.
38
Richardson, T.L. and J. GA, 2007. Small phytoplankton and carbon export from the surface ocean. Science, 315: 838-840.
39
Sabine, C., R. Feely, N. Gruber, R. Key, K. Lee, J. Bullister, et al., 2004. The Oceanic Sink for Anthropogenic CO2. Science, 305: 367-371.
40
Stanley, R.H.R. and W.J. Jenkins, 2013. Noble Gases in Seawater as Tracers for Physical and Biogeochemical Ocean Processes. In P. Burnard (Ed.), The Noble Gases as Geochemical Tracers (55-79 pp.). Berlin, Heidelberg: Springer Berlin Heidelberg.
41
Stanley, R.H.R., J. Kirkpatrick, N. Cassar, B. Barnett, and M. Bender, 2010. Net community production and gross primary production rates in the western equatorial Pacific. Global Biogeochemical Cycles, 24.
42
Stukel, M.R. and M.R. Landry, 2010. Contribution of picophytoplankton to carbon export in the equatorial Pacific: A reassessment of food web flux inferences from inverse models. Limnol. Oceanogr, 55: 2669-2685.
43
Takahashi, T., C. Sweeney, B. Hales, D. Chipman, T. Newberger, J. Goddard, et al., 2012. The changing carbon cycle in the Southern Ocean. Oceanography, 25: 26-37.
44
Tortell, P.D., 2005. Dissolved gas measurements in oceanic waters made by membrane inlet mass spectrometry, 3: 24-37.
45
Ulfsbo, A., N. Cassar, M. Korhonen, S. van Heuven, M. Hoppema, G. Kattner, and L.G. Anderson, 2014. Late summer net community production in the central Arctic Ocean using multiple approaches. Global Biogeochemical Cycles, 2014GB004833.
46
Volk, T. and M.I. Hoffert, 1985. Ocean Carbon Pumps: Analysis of Relative Strengths and Efficiencies in Ocean-Driven Atmospheric CO2 Changes. In The Carbon Cycle and Atmospheric CO2: Natural Variations Archean to Present (99-110 pp.). Washington, D. C.: American Geophysical Union.
Information
  • Publisher :The Korean Society of Oceanography
  • Publisher(Ko) :한국해양학회
  • Journal Title :The Sea Journal of the Korean Society of Oceanography
  • Journal Title(Ko) :한국해양학회지 바다
  • Volume : 23
  • No :1
  • Pages :49-62
  • Received Date : 2017-12-17
  • Revised Date : 2018-01-20
  • Accepted Date : 2018-01-22
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