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Aquatic Sciences

, 80:38 | Cite as

Significance of metabolically active bacterioplankton in the frontal regions of the Northeastern Arabian Sea

  • Lidita Khandeparker
  • Ranjith Eswaran
  • Niyati Hede
  • A. C. Anil
Research Article

Abstract

The Northeastern Arabian Sea (NEAS) experiences convective mixing during winter monsoon, which facilitates nutrient enrichment in the surface layers. This region is also known to harbour several sea surface temperature (SST) fronts and filaments, hotspots of primary production and bacterioplankton activity, which play an important role in the microbial loop. Observations on bacterioplankton with an emphasis on their physiological state, i.e., metabolically active (HNA; high nucleic acid content) bacteria and metabolically inactive (LNA; low nucleic acid content) bacteria were carried out in the NEAS region during early and peak winter monsoon (EWM and PWM). HNA bacteria were dominant in frontal zones coupled with high bacterial production (BP) indicating their significant role, whereas, LNA bacteria were abundant in non-frontal regions irrespective of the seasons. The differentiation in bacterial metabolic types points out organic matter enrichment in the fronts. During PWM, the nutrient concentration increased resulting in a further increase in HNA bacteria and BP in frontal regions. The transparent exopolysaccharides (TEP) were also higher in frontal zones, and inversely related to total bacterial abundance indicating a fast turnover of the organic matter. The age of the front and background condition prior to the formation of the front influences the relative contribution by bacterioplankton food web dynamics and these attributes would probably also help predict bacterial activities.

Keywords

Bacteria Northeastern Arabian Sea (NEAS) Fronts Transparent exopolysaccharides (TEP) Protists Temperature 

Notes

Acknowledgements

The authors would like to thank The Director, NIO, for his support and the captain, officers and crew members of SSK # 041 and SSK # 060 cruise for helping us on-board. We are thankful to Dr. D Shankar and Dr. S.G. Aparna for the helpful discussion. We also thank other members of the cruise and Ocean Finder team mates. The present study was supported by the OCEAN FINDER programme PSC 0105 of CSIR-NIO. This is NIO contribution 6277.

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Copyright information

© Springer Nature Switzerland AG 2018

Authors and Affiliations

  • Lidita Khandeparker
    • 1
  • Ranjith Eswaran
    • 1
  • Niyati Hede
    • 1
  • A. C. Anil
    • 1
  1. 1.CSIR-National Institute of OceanographyDona PaulaIndia

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