Articles | Volume 11, issue 9
Biogeosciences, 11, 2531–2542, 2014

Special issue: The impact of anthropogenic perturbations on open ocean carbon...

Biogeosciences, 11, 2531–2542, 2014

Research article 13 May 2014

Research article | 13 May 2014

Lytic viral infection of bacterioplankton in deep waters of the western Pacific Ocean

Y. Li1,2,*, T. Luo1,2,*, J. Sun1,2, L. Cai1,2, Y. Liang1,2, N. Jiao1,2, and R. Zhang1,2 Y. Li et al.
  • 1State Key Laboratory of Marine Environmental Science, Xiamen University, Xiamen 361005, China
  • 2Institute of Marine Microbes and Ecospheres, Xiamen University, Xiamen, 361005, China
  • *These authors contributed equally to this work.

Abstract. As the most abundant biological entities in the ocean, viruses influence host mortality and nutrient recycling mainly through lytic infection. Yet, the ecological characteristics of virioplankton and viral impacts on host mortality and biogeochemical cycling in the deep sea are largely unknown. In the present study, viral abundance and lytic infection were investigated throughout the water column in the western Pacific Ocean. Both the prokaryotic and viral abundance and production showed a significantly decreasing trend from epipelagic to meso- and bathypelagic waters. Viral abundance decreased from 0.36–1.05 × 1010 particles L−1 to 0.43–0.80 × 109 particles L−1, while the virus : prokaryote ratio varied from 7.21 to 16.23 to 2.45–23.40, at the surface and 2000 m, respectively. Lytic viral production rates in surface and 2000 m waters were, on average, 1.03 × 1010 L−1 day−1 and 5.74 × 108 L−1 day−1. Relatively high percentages of prokaryotic cells lysed by viruses at 1000 and 2000 m were observed, suggesting a significant contribution of viruses to prokaryotic mortality in the deep ocean. The carbon released by viral lysis in deep western Pacific Ocean waters was from 0.03 to 2.32 μg C L−1 day−1. Our findings demonstrated a highly dynamic and active viral population in these deep waters and suggested that virioplankton play an important role in the microbial loop and subsequently biogeochemical cycling in deep oceans.

Final-revised paper