Transparent exopolymer particles (TEP) link phytoplankton and bacterial production in the Gulf of Aqaba

被引:35
|
作者
Bar-Zeev, Edo [1 ]
Berman-Frank, Ilana [1 ]
Stambler, Noga [1 ,2 ]
Vazquez Dominguez, Evaristo [3 ]
Zohary, Tamar [4 ]
Capuzzo, Elisa [5 ]
Meeder, Efrat [6 ,7 ]
Suggett, David J. [8 ]
Iluz, David [1 ,2 ]
Dishon, Gal [1 ]
Berman, Tom [4 ]
机构
[1] Bar Ilan Univ, Mina & Everard Goodman Fac Life Sci, IL-52900 Ramat Gan, Israel
[2] Bar Ilan Univ, Dept Geog & Environm, IL-52900 Ramat Gan, Israel
[3] Inst Ciencias Mar, Barcelona 08003, Spain
[4] Israel Oceanog & Limnol Res, Yigal Allon Kinneret Limnol Lab, IL-14102 Tiberias, Israel
[5] Napier Univ, Sch Life Sci, Edinburgh EH10 5DT, Midlothian, Scotland
[6] Interuniv Inst Marine Sci Coral Beach, IL-88103 Elat, Israel
[7] Hebrew Univ Edmond J Safra Campus, Inst Earth Sci, IL-91904 Jerusalem, Israel
[8] Univ Essex, Dept Biol Sci, Colchester CO4 3SQ, Essex, England
基金
英国自然环境研究理事会;
关键词
Transparent exopolymer particles; TEP; Bacterial productivity; Primary productivity; Carbon cycling; Size fractionation; Gulf of Aqaba; RED-SEA; NATURAL FLUORESCENCE; ORGANIC PARTICLES; PROTEIN-SYNTHESIS; DIATOM BLOOM; CARBON-CYCLE; DYNAMICS; OCEAN; ABUNDANCE; SIZE;
D O I
10.3354/ame01322
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Variations in transparent exopolymer particles (TEP), bacterial biomass production (BP) and primary productivity (PP) were followed over 52 h at a deep water station in the Gulf of Aqaba (Eilat, Israel) during the spring, in April 2008. About 20 h after the start of the study, there was a short (similar to 15 h) but intense storm event that probably caused a nutrient pulse and, subsequently, a brief outgrowth of diatoms in the euphotic layer. Concentrations of TEP and BP ranged from 23 to 228 mu g gum xanthan equivalents l(-1) and from 0.2 to 0.6 mu g C l(-1) h(-1), respectively. Concentrations of TEP and BP were measured in unfiltered and in GF/C (1.2 mu m)-prefiltered samples. Most of the TEP (59 +/- 21% of total TEP, mean +/- SD) were in the smaller (GF/C-filtered) size fraction (0.4-1.2 mu m); however, after the crash of the diatom bloom, the majority of TEP were in the >1.2 mu m size fraction. In the GF/C-filtered fraction, BP averaged 59 +/- 12% and 93 +/- 5% of total BP in the upper water column and from 300 m, respectively. Significant correlations were observed between TEP and BP, suggesting that active heterotrophic bacteria may have been associated with these particles. During the 3 d of our study, PP and BP in the euphotic zone averaged 480 and 225 mg C m(-2) d(-1), respectively, suggesting that about half or more of the primary produced carbon was metabolized by heterotrophic bacteria in the upper water column. Coincident with strong mixing caused by the storm, TEP concentrations decreased in the surface water and increased at depth. We suggest that TEP acted to link carbon flux between the primary producers and heterotrophic bacteria, and that the downward movement of TEP from the upper water layers may be an important process in transferring organic carbon to deeper waters of the Gulf of Aquaba. Sinking TEP could provide not only organic carbon substrates for associated bacteria but also form 'hot spots' of elevated microbial metabolism and nutrient cycling throughout the water column.
引用
收藏
页码:217 / 225
页数:9
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