Increased cyanophage infection at the bottom of the euphotic zone, especially in the fall

Abstract Picocyanobacteria contribute greatly to offshore primary production with cells extending through the deep euphotic zone. Literature indicates high viral infection of cyanobacteria in ocean transition zones. We postulate that the bottom of the euphotic zone is a transition zone, where commun...

Full description

Bibliographic Details
Published in:Environmental Microbiology
Main Authors: Fuchsman, Clara A., Hays, Matthew D.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Online Access:http://dx.doi.org/10.1111/1462-2920.16525
id crwiley:10.1111/1462-2920.16525
record_format openpolar
spelling crwiley:10.1111/1462-2920.16525 2024-06-02T08:11:14+00:00 Increased cyanophage infection at the bottom of the euphotic zone, especially in the fall Fuchsman, Clara A. Hays, Matthew D. 2023 http://dx.doi.org/10.1111/1462-2920.16525 en eng Wiley http://creativecommons.org/licenses/by-nc/4.0/ Environmental Microbiology volume 25, issue 12, page 3349-3363 ISSN 1462-2912 1462-2920 journal-article 2023 crwiley https://doi.org/10.1111/1462-2920.16525 2024-05-03T11:43:35Z Abstract Picocyanobacteria contribute greatly to offshore primary production with cells extending through the deep euphotic zone. Literature indicates high viral infection of cyanobacteria in ocean transition zones. We postulate that the bottom of the euphotic zone is a transition zone, where communities transition from phototrophic to aphotic processes. We use single‐copy core genes to examine cyanophage to cyanobacteria ratios in cellular metagenomes in the subtropical North Atlantic and Pacific. Cyanophage to cyanobacteria terL/rpoB ratios generally increase to >10 in the deep euphotic zone. As light levels decrease in the fall, Prochlorococcus in the deep euphotic zone experience reduced light levels. We find clear differences between spring (Geotraces GA02) and fall (GA03) in the North Atlantic, with terL/rpoB ratios increasing to >40 in the fall. When examining 23 months of the North Pacific Hawaii Ocean Timeseries, the depth of elevated cyanophage to cyanobacteria ratios in cellular metagenomes negatively correlated with surface photosynthetic radiation (PAR), particularly with the change in PAR, which reflected the season. In fall, all picocyanobacteria ecotypes were found at depths enriched with viruses, while in summer, only low light ecotypes were affected. Thus, we find high cyanophage infection both in the deep euphotic zone and during seasonal transitions. Article in Journal/Newspaper North Atlantic Wiley Online Library Pacific Environmental Microbiology
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract Picocyanobacteria contribute greatly to offshore primary production with cells extending through the deep euphotic zone. Literature indicates high viral infection of cyanobacteria in ocean transition zones. We postulate that the bottom of the euphotic zone is a transition zone, where communities transition from phototrophic to aphotic processes. We use single‐copy core genes to examine cyanophage to cyanobacteria ratios in cellular metagenomes in the subtropical North Atlantic and Pacific. Cyanophage to cyanobacteria terL/rpoB ratios generally increase to >10 in the deep euphotic zone. As light levels decrease in the fall, Prochlorococcus in the deep euphotic zone experience reduced light levels. We find clear differences between spring (Geotraces GA02) and fall (GA03) in the North Atlantic, with terL/rpoB ratios increasing to >40 in the fall. When examining 23 months of the North Pacific Hawaii Ocean Timeseries, the depth of elevated cyanophage to cyanobacteria ratios in cellular metagenomes negatively correlated with surface photosynthetic radiation (PAR), particularly with the change in PAR, which reflected the season. In fall, all picocyanobacteria ecotypes were found at depths enriched with viruses, while in summer, only low light ecotypes were affected. Thus, we find high cyanophage infection both in the deep euphotic zone and during seasonal transitions.
format Article in Journal/Newspaper
author Fuchsman, Clara A.
Hays, Matthew D.
spellingShingle Fuchsman, Clara A.
Hays, Matthew D.
Increased cyanophage infection at the bottom of the euphotic zone, especially in the fall
author_facet Fuchsman, Clara A.
Hays, Matthew D.
author_sort Fuchsman, Clara A.
title Increased cyanophage infection at the bottom of the euphotic zone, especially in the fall
title_short Increased cyanophage infection at the bottom of the euphotic zone, especially in the fall
title_full Increased cyanophage infection at the bottom of the euphotic zone, especially in the fall
title_fullStr Increased cyanophage infection at the bottom of the euphotic zone, especially in the fall
title_full_unstemmed Increased cyanophage infection at the bottom of the euphotic zone, especially in the fall
title_sort increased cyanophage infection at the bottom of the euphotic zone, especially in the fall
publisher Wiley
publishDate 2023
url http://dx.doi.org/10.1111/1462-2920.16525
geographic Pacific
geographic_facet Pacific
genre North Atlantic
genre_facet North Atlantic
op_source Environmental Microbiology
volume 25, issue 12, page 3349-3363
ISSN 1462-2912 1462-2920
op_rights http://creativecommons.org/licenses/by-nc/4.0/
op_doi https://doi.org/10.1111/1462-2920.16525
container_title Environmental Microbiology
_version_ 1800757303084843008