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• W2115296816 endingPage "80" @default.
• W2115296816 startingPage "55" @default.
• W2115296816 abstract "Phytoplankton pigments were measured using HPLC during non-ENSO conditions in mid-summer along a South Pacific transect from 67° S to the equator along 170° W. Highest concen- trations of chlorophyll a (chl a) occurred in the Polar and the Subtropical Fronts (PF and STF, respec- tively) with concentrations exceeding 500 ng l -1 . In the STF, there was a distinct subsurface chl a maximum (SCM) at 40 m, which gradually deepened northward to 120 m in the Subtropical Conver- gence Zone. Northwards, the SCM shoaled to about 30 m in the Equatorial Zone (EZ). Relatively high concentrations of fucoxanthin and 19'-butanoyloxyfucoxanthin occurred in the nutrient-rich waters south of the Subantarctic Front, and CHEMTAX analyses indicated that diatoms, chrysophytes, pelagophytes, and haptophytes dominated the phytoplankton assemblage. Northward of the PF to the STF, where silicate concentrations were <1 µM, pelagophytes and coccolithophorids dominated the water column; diatoms were virtually absent, and Phaeocystis, prasinophytes, cryptophytes, and chlorophytes contributed significantly to the total algal biomass. Phaeocystis populations were dom- inant at or below the 1% light level. In the South Pacific Gyre (SPG), Synechococcus (Syn) and Prochlorococcus (Pro) were major components of the phytoplankton assemblage with Pro dominant as indicated by both flow cytometry and by the ratio of divinyl chl a:total chl a (0.43 ± 0.07). Photo- acclimation by Pro in the SPG was pronounced, with a higher average divinyl chl a per cell ratio in the SCM (1.1) relative to values (0.1) in the upper waters (0 to 100 m). Primary production rates exceeding 1 µg C l -1 h -1 occurred at the surface in the STF. Surface primary production rates were generally < 0.4 µg C l -1 h -1 across the SPG, but exceeded 1.4 µg C l -1 h -1 at the equator. In the EZ, Pro dominated the phytoplankton assemblage, but Phaeocystis and prasinophytes were also major constituents of the assemblage." @default.
• W2115296816 created "2016-06-24" @default.
• W2115296816 creator A5031036380 @default.
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• W2115296816 date "2003-01-01" @default.
• W2115296816 modified "2023-10-13" @default.
• W2115296816 title "Phytoplankton assemblage structure and primary productivity along 170°W in the South Pacific Ocean" @default.
• W2115296816 cites W1502045764 @default.
• W2115296816 cites W1522127495 @default.
• W2115296816 cites W1539227095 @default.
• W2115296816 cites W1557663486 @default.
• W2115296816 cites W1602534227 @default.
• W2115296816 cites W1603575405 @default.
• W2115296816 cites W1633519431 @default.
• W2115296816 cites W19207140 @default.
• W2115296816 cites W1966178736 @default.
• W2115296816 cites W1966541856 @default.
• W2115296816 cites W1967073483 @default.
• W2115296816 cites W1968807401 @default.
• W2115296816 cites W1971781571 @default.
• W2115296816 cites W1974081534 @default.
• W2115296816 cites W1975895334 @default.
• W2115296816 cites W1979705183 @default.
• W2115296816 cites W1981683033 @default.
• W2115296816 cites W1984449218 @default.
• W2115296816 cites W1985634470 @default.
• W2115296816 cites W1988040809 @default.
• W2115296816 cites W1988131321 @default.
• W2115296816 cites W1989036528 @default.
• W2115296816 cites W1989194442 @default.
• W2115296816 cites W1989416720 @default.
• W2115296816 cites W1993013648 @default.
• W2115296816 cites W1993505574 @default.
• W2115296816 cites W1994177646 @default.
• W2115296816 cites W1996716727 @default.
• W2115296816 cites W1997232238 @default.
• W2115296816 cites W1998099852 @default.
• W2115296816 cites W1998142256 @default.
• W2115296816 cites W2000165886 @default.
• W2115296816 cites W2004359105 @default.
• W2115296816 cites W2006583314 @default.
• W2115296816 cites W2007789939 @default.
• W2115296816 cites W2011567753 @default.
• W2115296816 cites W2013581855 @default.
• W2115296816 cites W2014469718 @default.
• W2115296816 cites W2016476895 @default.
• W2115296816 cites W2017867653 @default.
• W2115296816 cites W2023764468 @default.
• W2115296816 cites W2023862376 @default.
• W2115296816 cites W2025700565 @default.
• W2115296816 cites W2027311792 @default.
• W2115296816 cites W2028124547 @default.
• W2115296816 cites W2030597240 @default.
• W2115296816 cites W2031050703 @default.
• W2115296816 cites W2031098678 @default.
• W2115296816 cites W2033094203 @default.
• W2115296816 cites W2036011657 @default.
• W2115296816 cites W2037334191 @default.
• W2115296816 cites W2038423224 @default.
• W2115296816 cites W2039115276 @default.
• W2115296816 cites W2040366534 @default.
• W2115296816 cites W2040460517 @default.
• W2115296816 cites W2047041933 @default.
• W2115296816 cites W2047352962 @default.
• W2115296816 cites W2048583521 @default.
• W2115296816 cites W2049195872 @default.
• W2115296816 cites W2053834856 @default.
• W2115296816 cites W2055296120 @default.
• W2115296816 cites W2057455497 @default.
• W2115296816 cites W2059533740 @default.
• W2115296816 cites W2060215611 @default.
• W2115296816 cites W2061720155 @default.
• W2115296816 cites W2062314376 @default.
• W2115296816 cites W2063398520 @default.
• W2115296816 cites W2064594927 @default.
• W2115296816 cites W2065275468 @default.
• W2115296816 cites W2065563101 @default.
• W2115296816 cites W2067320688 @default.
• W2115296816 cites W2071661462 @default.
• W2115296816 cites W2071870883 @default.
• W2115296816 cites W2074398453 @default.
• W2115296816 cites W2074418233 @default.
• W2115296816 cites W2074695462 @default.
• W2115296816 cites W2075269932 @default.
• W2115296816 cites W2076830566 @default.
• W2115296816 cites W2079037803 @default.
• W2115296816 cites W2079493774 @default.
• W2115296816 cites W2079829413 @default.
• W2115296816 cites W2085615216 @default.
• W2115296816 cites W2086305222 @default.
• W2115296816 cites W2089056406 @default.
• W2115296816 cites W2089650688 @default.
• W2115296816 cites W2090785061 @default.
• W2115296816 cites W2090878061 @default.

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