1996
DOI: 10.1007/bf02239460
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Geographical and seasonal variations in abundance, biomass and estimated production rates of microzooplankton in the Inland Sea of Japan

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Cited by 107 publications
(68 citation statements)
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“…As thraustochytrids are epibiotically abundant (Karling 1981), it is reasonable to expect the ratio from the particle-bound populations to be larger than that from the planktonic populations. The abundance of planktonic thraustochytrids was 3 to 4 orders of magnitude lower than that of heterotrophic nanoflagellates (average 43 pm3) in the Seto Inland Sea (Iwamoto et al 1994), but 10 times larger than that of the ciliate microzooplankton in the same area (103 to 106 pm3; Uye et al 1996). The biovolume of the observed thraustochytrids was approximately 65 to 4200 pm3, assuming a spherical shape with a diameter of 5 to 20 pm.…”
Section: Ecological Implicationsmentioning
confidence: 93%
“…As thraustochytrids are epibiotically abundant (Karling 1981), it is reasonable to expect the ratio from the particle-bound populations to be larger than that from the planktonic populations. The abundance of planktonic thraustochytrids was 3 to 4 orders of magnitude lower than that of heterotrophic nanoflagellates (average 43 pm3) in the Seto Inland Sea (Iwamoto et al 1994), but 10 times larger than that of the ciliate microzooplankton in the same area (103 to 106 pm3; Uye et al 1996). The biovolume of the observed thraustochytrids was approximately 65 to 4200 pm3, assuming a spherical shape with a diameter of 5 to 20 pm.…”
Section: Ecological Implicationsmentioning
confidence: 93%
“…, Uye et al 1996, Uye & Shimazu 1997, its seasonal fluctuation is extremely wide, from ca. 10 to ca.…”
Section: ϫ3mentioning
confidence: 99%
“…Integrated POC concentrations in the upper 50 m of the water column were approximately one third in winter (4 to 8 gC m Abundances of the different groups of the plankton were transformed into carbon biomass by using the following equations: bacteria = 20 fgC cell -1 (Lee & Fuhrman 1987), flagellates = 6500 fgC cell -1 (Børsheim & Bratbak 1987), tintinnids = pgC = (µm 3 ) × 0.053 + 444.5 (Verity & Langdon 1984), thecate dinoflagellates = pgC = (µm 3 ) × 0.13 (Edler 1979), copepod nauplii = ngC = 1.51 × 10 -5 LC 2.94 (LC: length of cephalothorax; Uye et al 1996), calanoid copepods = 26.9 µgC cop -1 (González et al 2000, Hirst et al 2003, euphausiids = 3812 µgC euph ). The dominant taxa in spring were the thecate dinoflagellate genera Diplopsalis and Protoperidinium, whereas, in winter, tintinnids (genus Salpingella) and thecate dinoflagellates (genera Ceratium and Protoperidinium) dominated at Stns 44 and 20.…”
Section: Chl a And Poc Concentrationsmentioning
confidence: 99%