Latitudinal and Vertical Variation of Synechococcus Assemblage Composition Along 170 degrees W Transect From the South Pacific to the Arctic Ocean

• Published in: Microbial Ecology
• Main Authors: Xia, Xiaomin, Cheung, Shunyuan, Endo, Hisashi, Suzuki, Koji, Liu, Hongbin
• Format: Report
• Language: English
• Published: SPRINGER 2019
• Subjects: Environmental Sciences & Ecology; Marine & Freshwater Biology; Microbiology; Horizontal and vertical variations; Synechococcus assemblage richness; CRD1; Clade I; Central Pacific Ocean; Ecology; MARINE CYANOBACTERIA PROCHLOROCOCCUS; PHYLOGENETIC DIVERSITY; EQUATORIAL PACIFIC; ECOTYPES; LINEAGES; RESOLUTION; PATTERNS; DISTINCT; SCALE; SEA; Arctic; Arctic Ocean; Pacific
• Online Access: http://ir.gig.ac.cn/handle/344008/52134; https://doi.org/10.1007/s00248-018-1308-8

Synechococcus is one of the most widely distributed and abundant picocyanobacteria in the global oceans. Although latitudinal variation of Synechococcus assemblage in marine surface waters has been observed, few studies compared Synechococcus assemblage composition in surface and subsurface waters at the basin scale. Here, we report marine Synechococcus diversity in the surface and deep chlorophyll maximum (DCM) layers along 170 degrees W from the South Pacific to the Arctic Ocean in summer. Along the transect, spatial niche partitioning of Synechococcus lineages in the surface waters was clearly observed. Species richness of surface Synechococcus assemblage was positively correlated with water temperature. Clade CRD1 was dominant in the areas (15 degrees S-10 degrees N and 35-40 degrees N) associated with upwelling, and there were 3 different subclades with distinct distribution. CRD1-A was restricted in the North Equatorial Current (5-10 degrees N), CRD1-B dominated in the equatorial upwelling region (15 degrees S-0.17 degrees N), and CRD1-C was only distributed in the North Pacific Current (35-40 degrees N). Similarities between the Synechococcus assemblages in the surface and DCM layers were high at the upwelling regions and areas where the mixed layer was deep, while low in the Subtropical Gyres with strong stratification. Clade I, CRD1-B, and CRD1-C were major Synechococcus lineages in the DCM layer. In particular, clade I, which is composed of 7 subclades with distinct thermal niches, was widely distributed in the DCM layer. Overall, our results provide new insights into not only the latitudinal distribution of Synechococcus assemblages, but also their vertical variation in the central Pacific.