Relation between the relative abundance and collapse of Aphanizomenon flos-aquae and microbial antagonism in Upper Klamath Lake, Oregon

Author:

Underwood Jennifer C1ORCID,Hall Natalie C2,Mumford Adam C2ORCID,Harvey Ronald W1,Bliznik Paul A1,Jeanis Kaitlyn M1

Affiliation:

1. U.S. Geological Survey, Water Mission Area , 3215 Marine Street , Boulder, CO 80303, United States

2. U.S. Geological Survey, Maryland–Delaware–D.C. Water Science Center , 5522 Research Park Dr, Catonsville, MD 21228 , United States

Abstract

Abstract Aphanizomenon flos-aquae (AFA) is the dominant filamentous cyanobacterium that develops into blooms in Upper Klamath Lake, Oregon, each year. During AFA bloom and collapse, ecosystem conditions for endangered Lost River and shortnose suckers deteriorate, thus motivating the need to identify processes that limit AFA abundance and decline. Here, we investigate the relations between AFA and other members of the microbial community (photosynthetic and nonphotosynthetic bacteria and archaea), how those relations impact abundance and collapse of AFA, and the types of microbial conditions that suppress AFA. We found significant spatial variation in AFA relative abundance during the 2016 bloom period using 16S rRNA sequencing. The Pelican Marina site had the lowest AFA relative abundance, and this was coincident with increased relative abundance of Candidatus Sericytochromatia, Flavobacterium, and Rheinheimera, some of which are known AFA antagonists. The AFA collapse coincided with phosphorus limitation relative to nitrogen and the increased relative abundance of Cyanobium and Candidatus Sericytochromatia, which outcompete AFA when dissolved inorganic nitrogen is available. The data collected in this study indicate the importance of dissolved inorganic nitrogen combined with microbial community structure in suppressing AFA abundance.

Funder

USGS

Publisher

Oxford University Press (OUP)

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