Phytoplankton and Bacterial Response to Desert Dust Deposition in the Coastal Waters of the Southeastern Mediterranean Sea: A Four-Year In Situ Survey

被引:18
|
作者
Rahav, Eyal [1 ]
Belkin, Natalia [1 ]
Paytan, Adina [2 ]
Herut, Barak [1 ]
机构
[1] Natl Inst Oceanog, Israel Oceanog & Limnol Res, IL-3108000 Haifa, Israel
[2] Univ Calif Santa Cruz, Inst Marine Sci, Santa Cruz, CA 95604 USA
来源
ATMOSPHERE | 2018年 / 9卷 / 08期
基金
美国国家科学基金会; 以色列科学基金会;
关键词
atmospheric deposition; chlorophyll a; primary production; bacterial production; N-2; fixation; desert dust; southeastern Mediterranean Sea; LEVANTINE BASIN; N-2; FIXATION; PRIMARY PRODUCTIVITY; CHLOROPHYLL-A; ATMOSPHERIC DEPOSITION; DINITROGEN FIXATION; NITROGEN-FIXATION; SURFACE-WATER; SAHARAN DUST; TRACE-METALS;
D O I
10.3390/atmos9080305
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Atmospheric dust/aerosol deposition is an important source of external nutrients for the surface of the ocean. This study shows high-resolution observational data gathered in situ over a period of four years on bacterial and phytoplankton abundance and activity during typical background atmospheric conditions and during intense dust storm events in the low-nutrient, low-chlorophyll (LNLC) coastal waters of the southeastern Mediterranean Sea (SEMS). Chlorophyll a (an estimate for phytoplankton biomass) and bacterial abundance show moderate changes in response to dust deposition/events (-10% and +20%, respectively), while primary production, bacterial production, and N-2 fixation rates were all significantly and positively affected by deposition (+25 to +40%; p < 0.05). The rapid changes in bacterial and/or phytoplankton rate parameters suggest that the released micro-/macronutrients from atmospheric deposition are tunneled directly in metabolic processes and, to a lesser extent, for biomass accumulation. The predicted expansion of LNLC areas in oceans in the future, and the projected increase in dust emission due to desertification, may affect the production of marine microbial communities in the surface of the ocean, yet only moderately affect their biomass or standing stock. Such alterations may impact carbon sequestration to the deep ocean.
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页数:14
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