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The Distribution of Planktonic Protists Along a Latitudinal Transect in the Northeast Pacific Ocean

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(1)Ocean and Polar Research. Vol. 26(2):287-298. June 2004. Article. §ÿ ï·>ö* *êö 8ž ¦F öÿ>~ ª

(2) ·Bê1*ÁR781ÁBë*2 ž~&v š·" (402-751) žÂ7 Β Ï*ÿ 253 2 ‚“š·’ö š&~ãÁ¶ö’¦ (425-600) ãVê nÖ nÖÖړ ÒBŽ 29^ 1. The Distribution of Planktonic Protists Along a Latitudinal Transect in the Northeast Pacific Ocean Eun Jin Yang1*, Joong Ki Choi1, and Woong-Seo Kim2 1. Department of Oceanography, Inha University Incheon 402-751, Korea 2 Marine Geoenvironment and Resources Research Division,/ KORDI Ansan P.O. Box 29, Seoul 425-600, Korea Abstracts : As a part of Korea Deep Ocean Study program, we investigated the distribution of planktonic protists in the upper 200 m of the northeast Pacific from 5oN to 17oN, along 131o30'W. Area of divergence was formed at 9oN which is boundaries of the north equatorial counter current (NECC) and the north equatorial current (NEC) during this cruise. Chlorophyll-a concentration was higher in NECC than in NEC area. Pico chl-a(<2 µm) to total chl-a accounted for average 89% in the study area. The contribution of pico chl-a to total chl-a was relatively high in NEC area than in NECC area. Biomass of planktonic protists, ranging from 635.3 to 1077.3 mgC m−2(average 810 mgC m−2), was most enhanced in NECC area and showed distinct latitudinal variation. Biomass of HNF ranged from 88.7 to 208.3 mgC m−2 and comprised 15% of planktonic protists. Biomass of ciliates ranged from 123.6 to 393.0 mgC m−2 and comprised 25% of planktonic protists. Biomass of HDF ranged from 407.2 to 607.8 mgC m−2 and comprised 60% of planktonic protists. HDF was the most dominant component in both NECC and NEC areas. Nano-protist biomass accounted for more than 50% of total protists in the both areas. The contribution of nanoprotist to total protists biomass was relatively higher in NEC area than in NECC. The biomass of planktonic protists was significantly correlated with phytoplankton biomass in this study area. The size structure of phytoplankton biomass coincided with that of planktonic protists. This suggested that the structure of the planktonic protists community and the microbial food web were dependent on the size structure of the phytoplankton biomass. However, biomass and size structure of planktonic protist communities might be significantly influenced by physical characteristics of the water column and food concentration in this study area. Key words : §ÿ ï·(Northeast Pacific Ocean), ¦F öÿb(planktonic protists), «³'· fÞÎ ~(heterotrophic dinoflagellates), RÎÏ~(ciliates), «³'· ²ÞÎ~(heterotrophic nanoflagellates). 1. B. †. š·~ ‚'êöB ¦F öÿbf ²; 5 ² *Corresponding author. E-mail : [email protected]. ; ÿb2·’Ê~ 7º‚ ’W¶‚ «³'· ²ÞÎ ~, RÎÏ~, «³'· fÞÎ~, OÖÏ~, FÏ~‚ ’W>Ú ® (Stoecker and Capuzzo 1990). ¦F öÿ bf ·f ’Vf ç&'b‚ †ž ê&Ò ‚ÿb‚ ž š ê~ ö.æ vªj /ê~–, ·‚ ’V~ _š.

(3) 288. Yang, E.J. et al.. ¢ Î"'b‚ S~, 7;ÿb 2·’Ê~ 7º _š öš >V r^ö š· ê~ V&¦ö ^b _š " 7; ÿb2·’Ê _šj Ö~º ö.æ * " FVbî~ B~ö 7º‚ †j ‚ (Sieburth et al. 1978; Azam et al. 1983: Sheldon et al. 1986; Rassoulzadegan et al. 1988; Sherr et al. 1988). *;'b‚ öÿ b~ bïf žšöB b2·’Ê" F҂ ª¢ š–, š· ¢¢ ¢N ÖK~ 10-70% 6º 100% š çræ ²j~V r^ö š· _š~ ê²B~ö 7º ~² V‚ (Pierce and Turner 1992). ß® §ÿ ï· " ?f n'· šöB b2·’Ê bïf 7; ÿ b2·’Êö² Î"'b‚ šÏF > ìº ² b 2·’Ê(<2 µm)b‚ ’W>Ú ®V r^ö &f j &~ n'· >öB š‚ ² b2·’Êj š Ï~º öÿb~ †f ž š" jvšB ß® 7 º~² ’> ® (Sherr et al. 1986; Verity et al. 1996). §ÿ 'ê ï· æf š~~ ßWö V¢ B‚ ž bÒ, z' ~ã ßWj ¾æÚº >b‚ Bãb‚ Ë ~º §'ê š~f ÿãb‚ Ë~º 'ê >~& “¦' b‚ ò¾  ãêšöB “æ'ž BÖj ;W~º > š (Pickard and Emery 1982). šf ?š š~~ ßWö ~‚ >Z 5 BÖ~ ;Wf ‚[>Zö '·" ³ê¢ à &Ê, ;rÒjf b2·’Ê~ ÖKj ;zÎ. (Betzer et al. 1984; Chavez and barber 1987; Chavez et al. 1996; Hyun et al. 1998; Son et al. 2001). šBræ §ÿ ï·öB ¦F öÿbö &‚ ’º 'ê ï·j 7b‚ ~ þÒf ¢îö~ šç Vê& B®~ Vö 76'b‚ –Ò >îb–, "‚ b2·’Êö &‚ ²; ÿb2·’Ê~ S†" öÿb~ bïö &‚ –Ò& šÚ r . ¾ ïjVö öÿb~ Î  –÷j &çb‚ ‚ ’º b² >î (Landry et al. 1995; Chavez et al. 1996; Verity et al. 1996; Brown and Landry 2003; Landry et al. 2003; Yang et al. 2003).  –Ò>f §ÿ ï· >~ §'ê >~&f § 'ê š~&¢ Ž~º >b‚ š~~ ßWö V¢ B ‚ ž bÒ z' ßWj ¾æÞ (š·>Ö¦ 2003).  ’º §ÿ ï· >öB š~ö ~‚ >Z~ ß Wö Vž ¦F öÿb~ bï ªf –÷’–ö & ~ –Ò~& . 6‚ ¦F öÿb" b2·’Ê~ &ê¢ Ûš §ÿ ï· >~ ‚' êöB ¦F öÿb~ 7ºWö &š ¢~~& .. 2. \O» –Ò> B  –Òº. 2003j. 7ú. Korea. Deep. Ocean. Fig. 1. Map of study area showing location of sampling sites.. Study(KODOS) 03-3 öÒ V* ÿn §ÿ ï· 5oN17oNf 131o30'W ’*öB 1oN *Ïb‚ C 13B ;6 öB >¯>îb–, ' ;6f *êê‚ ;6 N5-;6 N17‚ ‚V~& (Fig. 1). –Ò>~ ¢>'ž >ZßW f BË~ Î'ê š~& 5oN šÎöB ¾æ¾–, ÿË~ §'ê >~º 5oN-10oNöB ¾æ¾, 10oN-30oN Қ öBº BË~ §'ê š~& ¾æÂ . 10oN¢ 7b‚ ~ Îã" §ãb‚ NF~ >š pÚæ–, ‚š b [f 10oN¢ 7b‚ ~ §ãöBº »jæ Îã öBº pÚæº ßWj ž (Wyrtki and Kilonsky 1984).  –ÒV*öº Î'ê š~~ ßWj ;{~² "æº p~b–, 9oNj 7b‚ B֚ ;W>Ú 9oN~ Îã>öBº §'ê >~~ ßWj &, 9oN ~ §ã>öBº §'ê š~~ ßWj & . ¾ §'ê š~ö *~‚ 15oN~ 80 m pšöB Ïß*ç š ¢¦ B~&b–, 14oN-15oNöBº “æ'b‚ 7 Î~ intrathermocline eddy& ¾æ¾º ßûj & ( š·>Ö¦ 2003). ¦F öÿb~ *šï ªC >[Ú öÿb~ bïj 2k~V *~ 0, 10, 20, 30, 50, 75, 100, 120, 150, 200 mf #ƒ² ‚&[ (chlorophyll maximum layer)öB š>¢ 1000 ml j>~  Lugol's ‡b‚ ‚«³ê 1% >² ;~& . ;B òº þ ‚ Ú>š öÿb~ &Vj *š ò¢ 50 mlræ &¢p² ‚ ê S-R chamberf sedimentation chamber¢ ÒÏ~ 7 *ã(Nikon Type 104)" ; 7 *ê *ã(Olympus IX 70)b‚ &V~& . «³' · ² ÞÎ~f ²; «³'· fÞÎ~(<20 µm)~ bïj 2k~V *š 150 ml~ š>¢ j>~ & æšr–~š‚ ‚«³ê 1%& >² ;‚ ê ïÿ &~ þ ‚ Ú>~& . Ú>B ò 100-120 ml ¢ 0.45 µm nuclepore polycarbonate black filterf 5 µm.

(4) Planktonic Protists in the Northeast Pacific Ocean. nuclepore polycarbonate black filter‚ '' "~ DAPI(Porter and Feig 1980)‚ ‚«³ê 5 µg ml−1& > ² "ï‚ ê ;7*ã(Nikon type 104)j ÒÏ~ « ³ '·Wj ’ª~& . ¦F öÿb~ ê²ï *~8 «³'· ² ÞÎ~~ ê²ïf *ã~öB Ú'j ’‚ ê Børsheim and Bratbak(1987)~ *~8ž 220 fgC µm−3j šÏ~ ’~& . ž öÿbf *ã ~öB ' ^ ’V¢ G;‚ ê ^ Ï'j Edler (1979)~ O»ö V¢ ’~& . F« RÎÏ~(tintnnnids) º carbon(pg) = 44.5 + 0.053 lorica volum(µm3)(Verity and Langdon 1984)~ ö V¢ ’~&b–, b'š ìº n Î RÎÏ~(oligotrichs)º 0.19 pgC µm−3(Putt and Stoecker 1989)~ *~8j ÒÏ~ ~Ö~& . fÞÎ~~ ê² ïf Edler(1979)~ O»ö V¢ Ï'j ’‚ê MendenDeuer and Lessard(2000)~ þž Carbon(pg) = 0.216. 289. [volume, m3]0.939j šÏ~ ' ^~ ê²ïj ’~&. . OÖÏ~~ ê²ïf Michaels et al.(1995)~ j š Ï~ G;~& . #ƒ²-a ³ê ' ;6~ 0, 10, 30, 50, 75, 100, 120, 150, 200 m f #ƒ² ‚&[öB š>¢ j>~ Turner Design Fluorometer(10-AU)¢ ÒÏ~ *ËöB G;~& . ’Vê #ƒ²-a ³êº PC membrane filter pape(2 µm pore size)¢ šÏ~ ’V’V¢ ‚ ê, 2 µm š~~ ² ’Vf 2 µm šçb‚ ’V¢ ’ª~& . ’V ê #ƒ²-a ³ê¢ G;~V *~ š> 1000-2,300 ml ¢ Millipore "æ(0.45 µm pore size)‚ "‚ ê  "æ¢ 90% j^Êö ~;ê ºÂ‚ ê .&8j G ;~& . ò ªC 5 Ûê¾Ò. Fig. 2. Depth distribution of chlorophyll-a concentration and depth integrated chlorophyll-a along a latitudinal transect in the study area..

(5) 290. Yang, E.J. et al.. –Ò>öB ¦FW RÎÏ~º b'š ìº nÎ R ÎÏ~(oligotrichs)f b'j < ®º F« RÎÏ~ (tintinnids)‚ ’ª~ ªC~& . «³'· fÞÎ~º ’² Protoperidinium sp. ?š b'j < ®º F' (thecate) fÞÎ~f Gyrodinium sp.f Gymnodinium sp. ?f b'j < ®æ pf Z'(athecate) fÞÎ~‚ ’ ª~& . '  Қ~ æï ç&&ê ªCf '  ~ ;6ö Vž >ê bï 8j šÏ~ SAS package(ver. 8.1)‚ ªC~& .. 3. Ö. . #ƒ²-a ³ê #ƒ²-a ³êº Î ;6öB 0.518 µg l−1 š~~ ³ ê¢ & (Fig. 2). #ƒ² ‚&[f ' ;6ê‚ B‚. ž pšöB ¾æÒb–, &*êöB *ê‚ .>ƒ pÚæº ãËj & . §'ê >~&ö *~‚ ;6 N5-N8öBº ‚[ b[öB #ƒ² ³ê& ¸² ª ~& . ;6 N10 š§~ *ê >öBº #ƒ² ‚& [š 6N pÚæšB >N£[" ¢~~º ·çj &. . > 120 mræ Ö‚ >ZÚ #ƒ²-a ³êº ;6 N6öB 30.2 mg chl. m−2b‚ &Ë ¸² ¾æÒb–, N9 ¢ Bž~ *ê‚ .>ƒ 6N Ôjæº ãËj &. . –ÒV* ÿn ’Vê #ƒ²-a ³ê 7 ² #ƒ ²-a ³êº *Ú #ƒ²-a ³ê~ ï 89%¢ Næ~& b–, §'ê >~&~ ;6 N5-N9öBº ï 82%, ; 6 N15¢ Bž‚ §ãê š~&ö *~‚ ;6öBº ï  92% šç~ ¸f Ö6†j & . ¦F öÿb~ *šï ª

(6) ¦F öÿbf «³'· ²ÞÎ~(Heterotrophic nanoflagellates; HNF), ¦FW RÎÏ~(Ciliates), «³' · fÞÎ~(Heterotrophic dinoflagellates; HDF), OÖÏ ~(Radiolaria)‚ ’ª~& . –Ò>öB «³'· ² ÞÎ~º &¦ªš 2-5 µm‚ ’W>Ú ®î . «³'· ²ÞÎ~~ *šïf 48-1,180 cells ml−1‚ ª~&b –, ï 455 cells ml−1 ¾æÒ (Fig. 3). «³'· ² ÞÎ~~ >ç ªº ‚[ b[öB jv' ¸f ª ¢ &b–, #ƒ² ‚&[ ~¦‚ ÚJ.>ƒ Ô² ª ~º ãËj & . ;6ê ªº ;6 N5f N6, Ò  ;6 N11öB jv' ¸² ª~&b–, ;6 N13, N14, N17öB Ôf ª¢ & . ¦F RÎÏ~~ *š ïf 0.07-3.2 cells ml−1‚ ª~&b–, ï 0.8 cells ml−1‚ ¾æÒ (Fig. 3). ¦F RÎÏ~~ >ç ªº ; 6 N5-N7~ ‚[ b[ ¦"öB ¸f ª¢ &b¾, *ê >b‚ .>ƒ #ƒ² ‚&[ ¦"öB ¸² ¾. æÒ . ;6ê ª ßWf &*ê >ž ;6 N6öB &Ë ¸f ª¢ &, *ê >ž ;6 N17öB &Ë Ôf *šïj & . –Ò>~ ¦F RÎÏ~  7 &Ë Ö6~ ¾æÂ f nÎ RÎÏ~‚, 0.06 -2.9 cells ml−1‚ ª~&b–, *šïf ;6 N16öB &Ë ¸² ¾æÒ . –Ò>öB &VB nÎ RÎÏ~ ~ &¦ªf Strombidium spp., Strobilidium spp., Tontonia spp. b‚ ’W >î . 6‚ F« RÎÏ~ f 0.2 cells ml−1 š~~ Ôf *šï ª¢ &b–, ;6 N7 öB &Ë ¸² ¾æÒ . F« RÎÏ~~ «–Wf  & šöB ¢>'b‚ ª~ ®º R« b'j < º Rabdonella, Proplectella, Dadayiella, Petalotricha, Epiplocylis, Amphorella, Steenstrupiella, Eutintinus, Xystonellopsis, Undella, Dictyocysta, Salpingella b‚ ’W>î .  ž *Î~ f ¢¦ >öB Â*~& b¾ 0.05 cells ml−1 š~~ Ôf *šï 8j & . 6 ‚ 20 µm š~~ ²; RÎÏ~º &¦ªš nÎ RÎ Ï~ b‚ ¾æÒb–, š ~ *šï ªº 0.011.6 cells ml−1(ï 0.4 cells ml−1)‚ *Ú RÎÏ~  7öB ï 40-63%(ï 52%)¢ Næ~& . *Ú RÎ Ï~ö ²; RÎÏ~~ VNf ;6 N6öB &Ë ¸~, ;6 17öB &Ë Ô~ . ²; nÎ~~ &¦ ªf Strombidium spp.f Strobilidium spp. š "‚ ª º ©b‚ &V>î . «³'· fÞÎ~~ *šïf 2-62 cells ml−1‚ ª ~&b–, ï 23 cells ml−1‚ ¾ æÒ (Fig. 3). «³'· fÞÎ~~ >ç ªº «³' · ²ÞÎ~ 5 RÎÏ~f FÒ~² &*ê ;6öB º ‚[ b[öB ¸f ª¢ &b–, *ê‚ .> ƒ #ƒ² ‚&[öB ¸f ª¢ & . ;6ꂺ ; 6 N5f N6öB &Ë ¸f ª¢ &b–, Ïß *ç š ¾æÂ ;6 N9f ;6 N15öBê ² ¸² ¾æÒ. . «³'· fÞÎ~~ *šïf F' fÞÎ~ö j š Z' fÞÎ~ö ~š ¸f ª¢ &b–, Z' f ÞÎ~~ &¦ªf 20 µm š~~ ²; «³'· fÞ Î~ž ©b‚ &V>î . Z' fÞÎ~~ &¦ªf Gymnodinium spp.f Gyrodinium spp.‚ ’W>Ú ®b –, F' fÞÎ~~ &¦ªf Protoperidium spp.‚ ’W >î . ¾ ;6 N15~ 80 mf N16~ 50 m~ > öB F' fÞÎ~ž Protoperidinum sp.~ ¸f *šï f ߚ† ò‚ *çb‚ &V>î . 6‚ OÖÏ~º  &f j& šöB 9² Â*~º b‚ &¦ª š b'·b‚ ’W>Ú ® . š f ;rÒj ¶, .¶, Ƕ, FV êJb¶b‚ ·‚ '· O j ‚ . š· ‚'êöB ·‚ « š Â*~& æò, –Ò>öB OÖÏ~~ *šïf 50 cells l−1 š ~~ Ôf ª¢ , «³'· öÿb 7öB 7º~.

(7) Planktonic Protists in the Northeast Pacific Ocean. 291. Fig. 3. Depth distribution of abundance of heterotrophic nanoflagellates, ciliates and heterotrophic dinoflagellates along a latitudinal transect in the study area (Units: cells ml−1).. æ pf b‚ ¾æÒ . ¦F öÿb~ `÷\– > 120 mræ Ö‚ «³'· ²ÞÎ~~ bï f 88.7-208.3 mgC m−2(ï 120.4 mgC m−2)‚ ª~ &b–, «³'· ²ÞÎ~º ¦F öÿb~ 10-22% ¢ Næ~ ï 15%¢ V~º ©b‚ ¾æÒ (Fig.. 4; Fig. 6). ¦F öÿbö «³'· ²ÞÎ~~ V Nf «³'· ²ÞÎ~~ bïš &Ë ¸~~ ;6 N5öB &Ë ¸² ¾æÒ . RÎÏ~~ ê²ïf 123.6 -393.0 mgC m−2(ï 208.2 mgC m−2)‚ ª~&b–, *Ú ¦F öÿb~ 15-40%¢ Næ~, ï 25%¢ Næ~& (Fig. 4; Fig. 6). RÎÏ~7 nÎ RÎÏ~~.

(8) 292. Yang, E.J. et al.. Fig. 4. Carbon biomass of heterotrophic nanoflagellates, ciliates and heterotrophic dinoflagellates along a latitudinal transect in the study area.. bïf 62-90%¢ Næ~º ©b‚ ¾æÒb–, ;6 N6öB &Ë ¸f VNj & . F« RÎÏ~º R ÎÏ~ bï~ 0.7-13%¢ Næ~&b–, ;6 N7öB &Ë ¸f VNj & . Î ;6öB nÎ RÎÏ~ º F« RÎÏ~ö jš ï 8V šç~ ¸f bï ª¢ & . «³'· fÞÎ~~ bïf 407.2607.6 mgC m−2(ï 480.4 mgC m−2)‚ ª~& (Fig. 4; Fig. 6). š f *Ú ¦F öÿbö 55-65%¢ Næ ~–, ï 60%¢ Næ~ ¦F öÿb7 &Ë Ö6~ º b‚ ¾æÒ . 7 Z' «³'· fÞÎ~º 58% šç Ö6~& . ;6 N16öB F' «³'· fÞ Î~& ¦F öÿb~ 10% šç Ö6‚ ©j Bž‚. š, –Ò V* ÿn Â*‚ Z' «³'· fÞÎ~º F ' «³'· fÞÎ~~ bïö jš 20V šç ¸f. ©b‚ ¾æÒ .  ž OÖÏ~~ bïf 6.2-21.5 mgC m−2(ï 11.7 mgC m−2)‚ ª~&b–, ¦F ö ÿb~ ï 1.5%¢ Næ~& (Fig. 4; Fig. 6). «³' · ²ÞÎ~, RÎÏ~, «³'· fÞÎ~f OÖÏ~ ¢ Ž~º >ê ¦F öÿb~ bïf 0.47-18 µgC l−1(ï 5.8 µgC l−1)‚ ª~& (Fig. 5). ¦F ö ÿb bï~ >ç ªº ;6 N5-N10öBº ‚[ b[ ¦"öB ¸² ¾æÒb–, *ê >b‚ .> ƒ #ƒ² ‚&[~ pšf ¢~~º ·çj & . > 120 mræ Ö‚ >ZÚ ¦F öÿb~ bïf 635.3-1077.3 mgC m−2(ï 810 mgC m−2)‚ ¾æÒ. (Fig. 5). *Ú ¦F öÿb~ bïf §'ê >~&ö *~‚ ;6 N5, ;6 N6" ;6 N9öB &Ë ¸² ª ~&b–, §'ê š~&ö *~‚ ;6 N17öB &Ë Ô.

(9) Planktonic Protists in the Northeast Pacific Ocean. 293. Fig. 5. Vertical distribution of planktonic protists biomass along a latitudinal transect in the study area (Units: µgC l−1).. Fig. 6. Carbon biomass of planktonic protists along a latitudinal transect in the study area. (A) is cumulative carbon biomass, (B) is relative percent of protists group and (C) is cumulative of protists size group..

(10) 294. Yang, E.J. et al.. Table 1. Pearson's correlation coefficients between heterotrophic protists and phytoplankton. NC PC HNF Ciliates HDF Radioraria Nanoprotists Microprotists Protists. TC 0.688*** 0.981*** 0.336** 0.547*** 0.460*** 0.335*** 0.435*** 0.579*** 0.528***. NC 0.536*** 0.080 0.239 0.301** 0.228 0.140 0.288** 0.208. PC. HNF. Ciliates. HDF. 0.368*** 0.573*** 0.488*** 0.330** 0.469*** 0.597*** 0.559***. 0.524*** 0.720*** 0.294** 0.823*** 0.549*** 0.798***. 0.629*** 0.232 0.635*** 0.940*** 0.806***. 0.212 0.971*** 0.687*** 0.956***. Radiolaria Nanoprotists Microprotists. 0.243** 0.295** 0.284**. 0.638*** 0.951***. 0.830***. Note: Significant correlation were defined as ***P<0.0001, **P<0.001 (TC, Total chlorophyll-a; NC, Net-nano chlorophyll-a (>2 µm); PC, Pico chlorophyll-a(<2 µm); HNF, Heterotrophic nanoflagellates; HDF, Heterotrophic dinoflagellates; Nanoprotists, HNF + <20 µm ciliates + <20 µm HDF; n=121).. f 8j & . ¦F öÿb b2·’Ê~ ê ^b  *~ ç^&ê¢ 2k~V *~ ¦F öÿb~ ' " ’Vê #ƒ²-a ³ê Қö ç& &ê¢ ªC~& (Table 1). *Ú ¦F öÿb~ b ï" #ƒ²-a ³ê Қöº ¸f ç&&ê¢ &b– (R=0.53, p<0.0001), ¦F öÿb~ '  5 ’Vê –÷’–f #ƒ²-a ³ê~ ’V Қöê ¸f ç&& ê¢ & . «³'· ²ÞÎ~f RÎÏ~º ² #ƒ²-af ¸f ç&&ê¢ &b–, «³'· fÞÎ~ º 2 µm šç~ #ƒ²-a 5 ² #ƒ²-af ç&Wš ¸f ©b‚ ¾æÒ . OÖÏ~º ² #ƒ²-af ç &Wš ®rj "î . 20 µm š~~ ²; öÿ bf ² #ƒ²-a ³êf ¸f ç&&ê¢ &b–, 20 µm šç~ ²; öÿbf ² #ƒ²-a 5 2 µm šç~ #ƒ²-af Îv ç&Wš ®º ©b‚ ¾æÒ . 6‚ öÿb –÷ Қöê ¸f ç&&ê¢ & .. 4. Æ. ~. §ÿ'ê ï· >f *;'ž n'· >b‚ š ~~ ßWö V¢ >Z& ’ª>–, š‚ ž~ ǂ bÒ z'ž ~ãj ;W‚ (Pickard and Emery 1982). ß® ‚B‚ š~ Fÿ" "V'ž Ïß *çb‚ ž~ >çbš ;~² ;W>º 'ê ï· ž" > " >Z~ bš £‚ W[zB §ï· ~~æ~ n;B >Zfº ž ßWj < ®b–, bÒ' ~ã æzö ~š 2·’Ê~ –÷’–º 'V ž ßWj  ž (Wyrtki and Kilonsky 1984; Moum et al. 1989; Brown and Landry 2003). §ÿ ï·>öB š*ö >¯B KODOS –Òö ~~š, §'ê š~(NEC)f § 'ê >~(NECC)~ ãêšö *~‚ 8oN-10oN ҚöB. “æ'ž B֚ ;W>–, š‚ ž~ >ç b[š » jæ, '·"𠳦‚ bš ‚[b‚ Ïß>Ú  "æ >ö b ÖKj ;zÎ (Hyun et al. 1998; š· >Ö¦ 1999, 2003). 6‚ §'ê š~&ö *~‚ *ê >öBº ê.'ž >N£[j ;W~ >N£[š p  Â]‚ W[zB >Z¢ ;W~–, '·"š Ôf *; 'ž n'· š~ ßWj ¾æÞ (Son et al. 2001; š ·>Ö¦ 2003).  –ÒV* ÿn §ÿ ï· >f § 'ê >~f §'ê š~& ò¾º 9oNöB Ïß *çš B~ –Ò>~ >Zº bÒ, z'ž ßWö Nš ¢ &b–, b2·’Ê~ bï" –÷f >Zö V ¢ ž ßWj & (š·>Ö¦ 2003). šf ?f ~ã ßWö V¢ –ÒV* ÿn Â*‚ ¦F öÿb~ b ïf &*ê >ž ;6 N5-N9öB &Ë ¸² ª~& b–, ;6 N9 š§~ *ê‚ .>ƒ Ôjæº ãËj & . V¢B §'ê ï·~ ¦F öÿb~ bï f ‚[ b[š p, '·"𠳦‚ 'ê ¦"~ & *ê >öB ¸² ª~–, W[z& Â]~² ;WB n'· š~ *ê >b‚ .>ƒ 6N bïš Ô ² ª~ §ÿ ï·öB š*ö –ÒB b2·’ Ê" öÿb ~ ªf F҂ ãËj & (Peña et al. 1990; Chavez et al. 1996; Landry et al. 1996; Liu et al. 1996; Brown and Landry 2003). 6‚ –Ò>f 1998j¦V 2000jræ~ –Ò¢ ۚ bÒ z' ºž ö ~š ^b –÷š æz¢ šº >b‚ ¾æÒ b–, 1998j –ÒöB öÿb~ bïf 'ê B֚ ;WB 8oN¢ 7b‚ &*ê >b‚ .>ƒ ¸~, *ê >b‚ .>ƒ Ôjæº ãËj & (Yang et al. 2004).  –Ò >" ÿ¢‚ >öB šBræ~ – Ò¢ ۚ §ÿ ï· >~ ¦F öÿb~ bï ªº bÒ'ž >Z ßWö ~š 'Ëj Aº ©b‚ ¾æÒ (š·>Ö¦ 1998, 1999, 2000)..

(11) 295. Planktonic Protists in the Northeast Pacific Ocean. –ÒV* ÿn ¦F öÿb –÷f «³'· ² Þ Î~, RÎÏ~, «³'· fÞÎ~f OÖÏ~~ 4b ‚ ’ª~&b–,  7 «³'· fÞÎ~º *Ú öÿ b~ 60%¢ Næ~ &Ë Ö6~º b‚ ¾æÒ . «³'· fÞÎ~~ *šïf –Ò>öB 1998jö –ÒB 8ö jš ² ¸² ¾æÒb¾(Table 2), š*~ §ÿ 'ê ï· >öB –ÒB Ö"f F҂ ·çj & (Chavez et al. 1996; Vørs et al. 1997). «³'· fÞÎ~~ bï ªº §'ê >~&ö *~‚ &* ê ;6öB ¸~b–, ;6 N15¢ Bž~º §'ê š. ~&ö *~‚ *ê ;6b‚ .>ƒ Ô² ¾æÒ . ; 6 N15öB «³'· fÞÎ~~ jv' ¸f ªº š ;6öB intrathermocline eddy‚ ž‚ “æ'ž Ïß * çš B~ –~~ ³ê& ¸² ¾æÂ ©" &Nš ®º ©b‚ 'B (š·>Ö¦ 2003). «³'· fÞ Î~~ ·‚ ¯ÿf š·~ãöB b2·’Ê~ S¶‚B ß® 7º~–, ß® žš~ öÿb7ö B 7º‚ †j ~º ©b‚ >î (Sherr et al. 1997; Garrison et al. 1998; Levinsen et al. 1999). 1998j –ÒöBê «³'· fÞÎ~~ bïf *Ú öÿb. Table 2. Comparisons of abundance and carbon biomass of planktonic protists reported in the equatorial Pacific Ocean. Region and protists. Month of year. Abundance (cells ml−1). Biomass (µgC l−1). Equatorial Pacific (0o, 140'W) <20 um flagellates February-April 2400 6 Dinoflagellates 24 1.3 Ciliates 0.06 0.08 <20 um flagellates August-October 1700 5.9 Dinoflagellates 29 1.8 Ciliates 0.09 0.16 Central and eastern tropical Pacific (12oN-10oS, 95oW, 110oW, 125oW, 140oW and 170oW) Heterotrophic flagellates Spring (Survey I) 647 ± 311 1.7 ± 1.3 Heterotrophic dinoflagellates 41 ± 13 2.3 ± 2.8 Aplastic ciliates 3.0 ± 2.6 1.5 ± 2.0 Heterotrophic flagellates Fall (Survey II) 772 ± 298 1.5 ± 0.7 Heterotrophic dinoflagellates 59 ± 20 3.1 ± 0.5 Aplastic ciliates 2.1 ± 2.6 1.3 ± 1.4 o o o o o o Equatorial Pacific (10 N-8 S, 110 W; 8 S-12 N, 125 W) Heterotrophic flagellates Spring 559 ± 249 1.4 ± 0.5 Chanoflagellates 25 ± 15 0.1 ± 0.1 Heterotrophic dinoflagellates 41 ± 12 3.0 ± 1.5 Ciliates 4±3 1.0 ± 0.7 Equatorial Pacific (5oN-9oN, 110oW) Heterotrophic flagellates November, 1988 6-110 Chanoflagellates 0-6 Heterotrophic dinoflagellates 11-40 Ciliates o o o Northequatorial Pacific (5 N-11 N, 130 30'W) Heterotrophic flagellates July, 1998 28-465 0.06-1.1 Heterotrophic dinoflagellates 2-46 0.3-4.0 Ciliates 0.01-1.7 0.03-2.9 Northequatorial Pacific (5oN-17oN, 131o30'W) Heterotrophic flagellates July, 2003 48-1180 0.09-3.1 Heterotrophic dinoflagellates 2-62 0.3-8.2 Ciliates 0.07-3.2 0.09-5.5. Reference. Verity et al. (1996). Chavez et al. (1996). Vørs et al. (1997). Chavez et al. (1990). Yang et al. (2003). This study.

(12) 296. Yang, E.J. et al.. –÷~ 50% šçj Næ~º ©b‚ ¾æÒb–, ž § ÿ 'ê ï·~ –ÒöBê «³'· fÞÎ~º ¦F öÿb~ 50% šçj Næ~º ©b‚ ¾æ¾  –Ò ~ Ö"f ¢~~º ãËj & (Chavez et al. 1996; Vørs et al. 1997). ¦F öÿb7 RÎÏ~º «³'· fÞÎ~ rb‚ 7º‚ b‚ ¾æÒ . ¦F RÎ Ï~~ *šï ªº §ÿ ï· >öB 1998jö – ÒB *šïö jš ² ¸² ¾æÒb¾ 'ê ï· >öB –ÒB 2-3 cells ml−1(Chavez et al. 1996)f 4 cells ml−1(Vørs et al. 1997)ö jš Ôf 8j &. (Table 2). RÎÏ~º *Ú öÿb~ ï 24%¢ Næ ~&b– §'ê š~&ö *~‚ *ê ;6öB jv ' ¸f VNj & . &¦ª š·öB ¦FW RÎÏ ~º F« RÎÏ~ö jš nÎ RÎÏ~ ö ~š 2 VöB 10Vræ z ¸f bï ª¢ ž (Pierce and Turner 1992).  –ÒöBê nÎ RÎÏ~~ bï f F« RÎÏ~ö jš ï 8V šç ¸f ©b‚ ¾ æÒ . ¦F öÿb7 «³'· ²ÞÎ~º ¦F ö ÿb~ ï 15%¢ Næ~&b–, ;6 N5öB &Ë ¸f *šï" Ö6†j & . «³'· ²ÞÎ~º ² 2·’Ê~ 7º‚ S¶‚B, ² 2·’Ê ~ *šï ªf ¢~~ ¾æÂ (Christaki et al. 2001). ;6 N5öB «³'· ²ÞÎ~~ ¸f ªº š ;6öB ;rÒjf Synechococcus~ ¸f *šï ª f &Nš ®º ©b‚ ÒòB (š·>Ö¦ 2003).  –Ò>öB &VB «³'· ²ÞÎ~~ *šïf 1998jö ÿ¢‚ >öB –ÒB «³'· ²ÞÎ~ö jš 2V šç ¸~b¾ §ï· >öB š*ö –Ò B 8" F҂ Ö"¢ & (Chavez et al. 1996; Vørs et al. 1997). šç~ ''~ öB BB ©" ?š ¦F öÿb~ bïf §'ê >~&ö *~‚ &* ê >öB &¦ª ¸² ª ~&b–, *ê >b‚ .>ƒ Ôf ª¢ & . ¾ ;6 N9öB~ ¸f bïf Ïß*çb‚ ž‚ '·" ³ê~ Ã&f š‚ ž‚ b2·’Ê~ ¸f ªf &š ®º ©b‚  'B . 6‚ öÿb~ >ç' ª ßWf &*ê > öBº ‚[ b[öB ¸² ¾æÒb–, *ê‚ .> ƒ #ƒ² ‚&[öB jv' ¸f ª¢ & . šf ?f Ö"º ¦F öÿb~ bï ªº ¢N'b‚ b·’Ê~ bï" &š ®º ©b‚ 'B . n '· >öB «³'· öÿb~ bïf #ƒ²-a ³êf &7‚ &Nj <º ©b‚ >î (Beers and Stewart 1971; Burkill et al. 1995; Dolan and Marrase 1995; Landry et al. 1995; Garrison et al. 1998). –Ò>öB v  Қ~ ç&&ê ªC Ö" ¦F öÿb"  b2·’Ê bï Қö ç&Wš ¸f ©b‚ ¾æÒ. (Table 1). 6‚ ¦F öÿb~ 60% šçj Næ~º ²; öÿb" ² #ƒ²-a Қ~ ¸f ç&& ê, ²; öÿb" ²; 5 ²; #ƒ²-a(>2 µm) Қ ~ ¸f ç&&ê, «³'· fÞÎ~f ²; 5 ²; #ƒ²-a(>2 µm) Қ~ ¸f ç&&ê, «³'· ²Þ Î~f ² #ƒ²-a Қ~ ¸f ç& &ê f š.  Қö &7‚ &ê& ®rj B‚ . ß® § ï· >öB ² b2·’Ê~ Wˆf ²; öÿb~ Sö ~š ’² –.>Úæ–, ‚' ê ÚöB Ö" ²jº ;j š ®º ©b‚ ¾æÒ. (Verity et al. 1996). V¢B  –Ò>öB ¦F ö ÿb~ ’Vê –÷’–º b2·’Ê~ ’Vê ª ·ç" F҂ ãËj &b–, š Ö"º ¦F öÿb " b2·’Ê Қö b-¶~ &ê& ®rj z ~–, b-~ &ê& ^b _šöB 7º‚ –. ºžš F > ®rj ҂ .  –ÒöB ¢N' b‚ ¦F öÿb~ bï ªf –÷’–¢ ÚÚ" r, ¦F öÿb~ bï" ’Vê –÷’–º *êö V¢ Nš¢ šº ©b‚ ¾æÒ . šf ?f Ö"º ' >Z~ ßWö ~š ¢NÖ¶~ bï" ’Vê ª  ·çš š² ¾æÒV r^ö b2·’Êj _š ‚ šÏ~º ¦F öÿb~ bï" ’Vê –÷’–ê š " ç® ¢~~º ·çj ¾æÞ ©b‚ ÒòB . §ÿ ï·" ?š ² b2·’Êö ~š Ö6 ~º >öB ¦F öÿbf ž >ö j~ ß ® 7º~–, ‚[öB b2·’Êö ~š ÖB ê² ~ ôf ¦ªš : b‚ Ž;>º ©  º ‚'  ê~ ^b _š~ ê²B~ö 7º‚ V¢ ‚. (Stoecker et al. 1996; Hall et al. 1999). šf ?š ² b2·’Êš Ö6~º n'· >öB ²; ÿb2· ’Êf ¢N Ö¶~ &Ë 7º‚ ²j¶‚B ï·  &>öB ²; ÿb2·’Êf ¢¢ ¢N ÖK~ 70%ræ ²j~–(Beers and Stewart 1971), 'ê ï· öBº ¢N ÖK~ 70-133%ræ ²j~–(Verity et al. 1996), 1996j~ þÒ V*ö 'ê ï· >öB b2·’Ê ÖK~ ï 69%¢ B–~& (Landry et al. 2003). 6‚ –Ò>" ÿ¢‚ >öB 1998j~ ¢îö Vö –ÒB ¦F öÿbf b2·’Ê~ 85-140%ræ B–~º ©b‚ ¾æÒ (Yang et al. 1998). š‚ Ö"º –Ò>~ ‚' êöB öÿbf _š /~ æzö †š² >w~V r^ö Ö" ²j Қö ; ®º &ê& Fæ>º ©b‚ 'B .  ¾ –ÒV* ÿn b2·’Êö &‚ öÿb~ S &ê& –Ò>æ p~V r^ö öÿb~ 7ºWö &~ ;{~² ¢~† >º ì . ¾ 1998j~ ¢ îö V*ö >¯B ¶òö "–¢ v(Yang et al. 2003),.

(13) Planktonic Protists in the Northeast Pacific Ocean. ¦F öÿb~ bï 5 ’Vê –÷’–f b2· ’Ê ’Vê bï Қ~ &7‚ &êö &~ Jš " r, §ÿ ï· >~ ‚' êöB ^b   f Ö" ²jҚö ;‚ couplingj ;W~ ¦ F öÿbf ^b _š ÚöB FV ê²~ * ¶‚B 7º‚ †j † ©š . ¾ ^b _š ÚöB ¦F öÿb~ ê²~ šÏ†" *†f >Z ~ ßWö V¢ š² ¾æ¾V r^ö ¦F öÿb~ †ê >Z~ ßWö V¢ Nš& ®j ©b‚ ÒòB . 6‚  –Ò>f 1996j¦V þÒf ¢îö ~ šç Vê *çb‚ ž~ ôf ~ã æz¢ šº š · ê² B~" &NB 7º‚ >š . V¢B ‚'  êöB ¦F öÿbö &‚ æ³'ž ’¢ ۚ Ë V'ž ^b –÷~ bï æzf –÷~ Ö6ê,  Ò b2·’Êö &‚ öÿb~ S{ö &‚  ’& ÖF'b‚ –ÒB š, Ëê * æ’ ~ã æzö Vž §ï· >öB š· ê~ æz ·ç" ê² B~j šš~º– 7º‚ ¶ò‚B ‚ÏF ©š .. Ò. Ò.  ¢^j ^&~² Қ" vª~ Ò*öþ ê b‚ 6Òãî . 6‚  ’¢ >¯~º– ®Ú * Ë ·ë" ò¾Òö êæj & f~ Nf š'" N, Ò N*Ò^ FËþ š~ * ߖö ª" š &¶ö’bV ’öö²ê 6Òãî .  ’º š·>Ö¦ R&D ’"Bž ‘š& 7b¶ö öÒÒ ë’~ ’j æöö ~~ >¯>îÛî .. ^^ò š·>Ö¦. 1998. '98 š& 7b¶ö öÒ B(1). š· >Ö¦ B, 1209 p. š·>Ö¦. 1999. '99 š& 7b¶ö öÒ B(1). š· >Ö¦ B, 780 p. š·>Ö¦. 2000. 2000 š& 7b¶ö öÒ B(1). š ·>Ö¦ B, 594 p. š·>Ö¦. 2003. 2003 š& 7b¶ö öÒ B(1). š ·>Ö¦ B, 770 p. Azam, F., T. Fenchel, J.G. Field, F.S. Gray, and L.A. Meyer-Reil. 1983. The ecological role of water-column microbes in the sea. Mar. Ecol. Prog. Ser., 10, 257-263. Beers, J.R. and G.L. Stewart. 1971. Microzooplankton in the plankton community of the upper waters of the Eastern Tropical Pacific. Deep-Sea Res., 18, 861-883. Betzer, P.R., W.J. Showers, E.A. Laws, C.D. Winn, G.R.. 297. DiTullio, and P.M. Kroopnick. 1984. Primary productivity and particle fluxes on a transect of the equator at 153oW in the Pacific Ocean. Deep-Sea Res., 31, 1-11. Børsheim, K.Y. and G. Bratbak. 1987. Cell volume to cell carbon conversion factors for a bacterivorus Monas sp. enriched from sea waters. Mar. Ecol. Prog. Ser., 36, 171175. Brown, S.L. and M.R. Landry. 2003. Microbial community abundance and biomass along a 180o transect in the equatorial Pacific during an El niño-Southern oscillation cold phase. J. Geophys. Res., 108, 8139. Burkill, P.H., E.S. Edwards, and M.A. Sleigh. 1995. Microzooplankton and their role in controlling phytoplankton growth in the marginal ice zone of the Bellingshausen Sea. Deep-Sea Res. II, 42, 1277-1290. Chavez, F.P. and R.T. Barber. 1987. An estimate of new production in the Equatorial Pacific. Deep-Sea Res., 34, 1229-1243. Chavez, F.P., K.R. Buck, S.K. Service, J. Newton, and R.T. Barber. 1996. Phytoplankton variability in the central and eastern tropical Pacific. Deep-Sea Res. II, 43, 835-870. Christaki, U., A. Giannakourou, F. Wambeke, and G. Gregori. 2001. Nanoflagellates predation on auto-and heterotrophic picoplankton in the oligotrophic Mediterranean Sea. J. Plankton Res., 23, 1297-1310. Dolan, J.R. and C. Marrase. 1995. Planktonic ciliates distribution relative to a deep chlorophyll maximum: Catalan Sea, N.W. Mediterranean, June 1993. Deep-Sea Res., 42, 1965-1987. Edler, L. 1979. Phytoplankton and chlorophyll recommendations for biological studies in the Baltic Sea. Baltic Marine Biologists, p. 13-25. Garrison, D.L., M.M. Gowing, and M.P. Hughes. 1998. Nano-and microplankton in the northern Arabian sea during the southwest Monsoon, August-September, 1995 A US-JGOFS study. Deep-Sea Res. II, 45, 2269-2299. Hall, J.A., M.R. James, and J.M. Bradford-Grieve. 1999. Structure and dynamics of the pelagic microbial food web of the subtropical convergence region east of New Zealand. Aqua. Microb. Ecol., 20, 95-105. Hyun, J.H., J.K. Choi, E.J. Yang, and K.H. Kim. 1998. Biomasss and productivity of bacterioplankton related to surface water divergence in the Northeast Equatorial Pacific Ocean. J. Microbiol., 36, 151-158. Landry, M.R., J. Constantinou, and J. Kirshtein. 1995. Microzooplankton grazing in the central equatorial Pacific during February and August, 1992. Deep-Sea Res. II, 42, 657-671. Landry, M.R., J. Kirshtein, and J. Constantinou. 1996..

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