Distribution of the N2-fixing cyanobacterium Candidatus Atelocyanobacterium thalassa in the Mexican Pacific upwelling system under two contrasting El Niño Southern Oscillation conditions

被引:1
|
作者
Vieyra-Mexicano, Cinthya [1 ,2 ]
Souza, Valeria [3 ]
Pajares, Silvia [1 ]
机构
[1] Univ Nacl Autonoma Mexico, Inst Marine Sci & Limnol, Unidad Acad Ecol & Biodivers Acuat, Mexico City, Mexico
[2] Univ Nacl Autonoma Mexico, Posgrad Ciencias Mar & Limnol, Mexico City, Mexico
[3] Univ Nacl Autonoma Mexico, Inst Ecol, Dept Ecol Evolut, Mexico City, Mexico
来源
ENVIRONMENTAL MICROBIOLOGY REPORTS | 2024年 / 16卷 / 01期
关键词
NITROGEN-FIXATION; DINITROGEN FIXATION; TROPICAL PACIFIC; NORTH PACIFIC; N-2; FIXATION; NIFH GENES; UCYN-A; OXYGEN; DIAZOTROPHS; DIVERSITY;
D O I
10.1111/1758-2229.13237
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The unicellular cyanobacterium Candidatus Atelocyanobacterium thalassa (UCYN-A) is a key diazotroph in the global ocean owing to its high N-2 fixation rates and wide distribution in marine environments. Nevertheless, little is known about UCYN-A in oxygen-deficient zones (ODZs), which may be optimal environments for marine diazotrophy. Therefore, the distribution and diversity of UCYN-A were studied in two consecutive years under contrasting phases (La Ni & ntilde;a vs. El Ni & ntilde;o) of El Ni & ntilde;o Southern Oscillation (ENSO) along a transect in the ODZ of the Mexican Pacific upwelling system. Of the three UCYN-A sublineages found, UCYN-A1 and UCYN-A3 were barely detected, whereas UCYN-A2 was dominant in all the stations and showed a wide distribution in both ENSO phases. The presence of UCYN-A was associated with well-oxygenated waters, but it was also found for the first time under suboxic conditions (<20 mu M) at the bottom of a shallow coastal station, within the oxygen-poor and nutrient-rich Subsurface Subtropical water mass. This study contributes to the understanding of UCYN-A distribution under different oceanographic conditions associated with ENSO phases in upwelling systems, especially because of the current climate change and increasing deoxygenation in many areas of the world's oceans.
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页数:14
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