SuppReadme_Jan15_2014

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Supplementary Material:
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Fig. S1: Time series of input data sets from the locations of the Hawaii Ocean Time
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series (HOT; top panels), the JGOFS Equatorial Pacific experiment (EQPAC; 2nd row of
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panels), Ocean Station P (OSP; 3rd row) and KNOT 2 station in the subarctic Pacific (K2;
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lower panels). Locations and references for these sites are given in Supplementary Table
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1 of the text. From left to right, the panels illustrate the climatological variations in (far-
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left) Zeu (green) and Zml (blue), (near-left) the fraction of biomass in the
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microphytoplankton size class, FM, (near-right) the total phytoplankton biomass (PT; red),
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the combined biomass in small (combined pico- and nano-) phytoplankton (PS; blue) and
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the micro-phytoplankton biomass budget (PM; green), and (far-right) the total and size-
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fractionated NPP.
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Fig. S2. Calculation of grazing rates for the locations of the HOT, EQPAC, OSP and K2
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time series sites (from top to bottom). The green curves show the microphytoplankton
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biomass budget (PM) while the blue curves illustrate the changes to small phytoplantkon
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biomass (PS). The panels are ordered left to right illustrating the contribution that each
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process makes to the grazing rates (GM and GS in mg C m-3 d-1; left panels). The second
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from the left panel shows the NPP rates for the two size classes. The middle panel shows
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the time series of non-grazing biological losses for the two size classes and the direct loss
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of large phytoplankton from the mixed layer (AlgEZ/Zeu; shown in red). The second
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panel from the right shows the detrainment losses of PM and PS, and the far right panel
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shows the time rate of change of PM and PS. Note the change of vertical scales in the
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different panels and the general decrease in rates (all in mg C m-3 d-1) from left to right.
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Fig. S3. Time series of TotEZ (red), FecEZ (green) and AlgEZ(blue) fluxes (in mg C m-2
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d-1) for the locations of the HOT, EQPAC, OSP and K2 time series sites.
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Fig. S4: Temporal changes in the global monthly anomalies for a) <TotEZ’> and b) <EZ-
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ratio’>, c) the contribution of each zone of latitude to <TotEZ’> and d) the contribution
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of each zone of latitude to <EZ-ratio’> calculated using the monthly climatology for FM.
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Only data equatorward of 50o latitude are used.
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Supplementary Table 1: Locations of the selected time series sites
Abbreviation
Full Name
BATS
Bermuda Atlantic Time
series Site
North Atlantic Bloom
Experiment
Station ALOHA
NABE
ALOHA
EQPAC
OSP
K2
Nominal
Location
32oN 64oW
Citation
47oN 20oW
Buesseler et al. [1992];
Lampitt et al. [2008]
Karl et al. [1996];
Buesseler et al. [2008]
Bacon et al. [1996]
23oN 158oW
0oN 140oW
JGOFS Equatorial
Pacific Experiment
Ocean Station P
KNOT 2
50oN 145oW
47oN 160oE
Steinberg et al. [2001]
Charette et al. [1999]
Honda et al. [2006];
Buesseler et al. [2008]
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References for Supplementary Table 1:
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Bacon, M.P., J.K. Cochran, D. Hirschberg, T.R. Hammar, and A.P. Fleer, (1996), Export
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flux of carbon at the equator during the EqPac time-series cruises estimated from 234Th
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measurements. Deep-Sea Research II, 43: 1133-1154.
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Buesseler, K.O., M.P. Bacon, J.K. Cochran, H.D. Livingston, (1992) Carbon and nitrogen
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export during the JGOFS North Atlantic Bloom Experiment estimated from 234Th: 238U
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disequilibria. Deep-Sea Res. I 39: 1115-1137.
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Buesseler, K.O., T.W. Trull, D.K. Steinberg, M.W. Silver, D.A. Siegel, S.-I. Saitoh, C.H.
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Lamborg, P.J. Lam, D.M. Karl, N.Z. Jiao, M.C. Honda, M. Elskens, F. Dehairs, S.L.
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Brown, P.W. Boyd, J.K.B. Bishop, R.R. Bidigare (2008), VERTIGO (VERtical
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Transport In The Global Ocean): A study of particle sources and flux attenuation in the
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North Pacific. Deep-Sea Research Part II, 55, 1522-1539.
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Charette, M.A., S.B. Moran, and J.K.B. Bishop, (1999), 234Th as a tracer of particulate
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organic carbon export in the subarctic Northeast Pacific Ocean. Deep-Sea Res. II 46,
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2833-2861.
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Karl, D.M., R. Lukas, (1996), The Hawaii Ocean Time-series (HOT) Program:
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Background, rationale and field implementation. Deep-Sea Res. II 43,129–156.
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Honda, M.C., H. Kawakami, K. Sasaoka, S. Watanabe, and T. Dickey, (2006) Quick
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transport of primary produced organic carbon to the ocean interior, Geophys. Res. Lett.,
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33, L166603, doi: 10.1029/2006GL026466.
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Lampitt, R.S., B. Boorman, L. Browna, M. Lucas, I. Salter, R. Sanders, K. Saw, S.
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Seeyave, S.J. Thomalla, R. Turnewitsch, (2008) Particle export from the euphotic zone:
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Estimates using a novel drifting sediment trap, 234Th and new production. Deep-Sea
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Research I, 55, 1484–1502.
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Steinberg, D.K., Carlson, C.A., Bates, N.R., Johnson, R.J., Michaels, A.F., Knap, A.H.,
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(2001) Overview of the US JGOFS Bermuda Atlantic Time-series Study (BATS): a
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decade-scale look at ocean biology and biogeochemistry. Deep-Sea Research II 48,
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1405–1447.
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