Shift from carbon flow through the microbial loop to the viral shunt in coastal Antarctic waters during austral summer

Evans, Claire ORCID: https://orcid.org/0000-0003-0569-7057; Brandsma, Joost; Meredith, Michael P. ORCID: https://orcid.org/0000-0002-7342-7756; Thomas, David N.; Venables, Hugh J. ORCID: https://orcid.org/0000-0002-6445-8462; Pond, David W.; Brussaard, Corina P.D.. 2021 Shift from carbon flow through the microbial loop to the viral shunt in coastal Antarctic waters during austral summer [in special issue: Polar Microbes] Microorganisms, 9 (2), 460. 13, pp. 10.3390/microorganisms9020460

Before downloading, please read NORA policies.

Preview

Text (Open Access) © 2021 by the authors. Licensee MDPI, Basel, Switzerland. microorganisms-09-00460-v2.pdf - Published Version Available under License Creative Commons Attribution 4.0. Download (1MB) | Preview

Abstract/Summary

The relative flow of carbon through the viral shunt and the microbial loop is a pivotal factor controlling the contribution of secondary production to the food web and to rates of nutrient remineralization and respiration. The current study examines the significance of these processes in the coastal waters of the Antarctic during the productive austral summer months. Throughout the study a general trend towards lower bacterioplankton and heterotrophic nanoflagellate (HNF) abundances was observed, whereas virioplankton concentration increased. A corresponding decline of HNF grazing rates and shift towards viral production, indicative of viral infection, was measured. Carbon flow mediated by HNF grazing decreased by more than half from 5.7 µg C L−1 day−1 on average in December and January to 2.4 µg C L−1 day−1 in February. Conversely, carbon flow through the viral shunt increased substantially over the study from on average 0.9 µg C L−1 day−1 in December to 7.6 µg C L−1 day−1 in February. This study shows that functioning of the coastal Antarctic microbial community varied considerably over the productive summer months. In early summer, the system favors transfer of matter and energy to higher trophic levels via the microbial loop, however towards the end of summer carbon flow is redirected towards the viral shunt, causing a switch towards more recycling and therefore increased respiration and regeneration.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	10.3390/microorganisms9020460
ISSN:	20762607
Additional Keywords:	prokaryotes; Antarctica; viruses; heterotrophic nanoflagellates; microbial loop; viral shunt; carbon; bacteriovory; viral lysis
Date made live:	28 Feb 2021 10:20 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/529763

Actions (login required)

View Item

Document Downloads

More statistics for this item...