Response of cyanobacteria and phytoplankton abundance to warming, extreme rainfall events and nutrient enrichment

Richardson, Jessica ORCID: https://orcid.org/0000-0002-3723-2361; Feuchtmayr, Heidrun ORCID: https://orcid.org/0000-0002-2028-4843; Miller, Claire; Hunter, Peter D.; Maberly, Stephen C. ORCID: https://orcid.org/0000-0003-3541-5903; Carvalho, Laurence. 2019 Response of cyanobacteria and phytoplankton abundance to warming, extreme rainfall events and nutrient enrichment. Global Change Biology, 25 (10). 3365-3380. 10.1111/gcb.14701

Before downloading, please read NORA policies.

Preview

Text
N524480JA.pdf - Published Version
Available under License Creative Commons Attribution 4.0.
Download (1MB) | Preview

Official URL: https://doi.org/10.1111/gcb.14701

Abstract/Summary

Cyanobacterial blooms are an increasing threat to water quality and global water security caused by the nutrient enrichment of freshwaters. There is also a broad consensus that blooms are increasing with global warming, but the impacts of other concomitant environmental changes, such as an increase in extreme rainfall events, may affect this response. One of the potential effects of high rainfall events on phytoplankton communities is greater loss of biomass through hydraulic flushing. Here we used a shallow lake mesocosm experiment to test the combined effects of: warming (ambient vs. +4°C increase), high rainfall (flushing) events (no events vs. seasonal events) and nutrient loading (eutrophic vs. hypertrophic) on total phytoplankton chlorophyll‐a and cyanobacterial abundance and composition. Our hypotheses were that: (a) total phytoplankton and cyanobacterial abundance would be higher in heated mesocosms; (b) the stimulatory effects of warming on cyanobacterial abundance would be enhanced in higher nutrient mesocosms, resulting in a synergistic interaction; (c) the recovery of biomass from flushing induced losses would be quicker in heated and nutrient‐enriched treatments, and during the growing season. The results supported the first and, in part, the third hypotheses: total phytoplankton and cyanobacterial abundance increased in heated mesocosms with an increase in common bloom‐forming taxa—Microcystis spp. and Dolichospermum spp. Recovery from flushing was slowest in the winter, but unaffected by warming or higher nutrient loading. Contrary to the second hypothesis, an antagonistic interaction between warming and nutrient enrichment was detected for both cyanobacteria and chlorophyll‐a demonstrating that ecological surprises can occur, dependent on the environmental context. While this study highlights the clear need to mitigate against global warming, oversimplification of global change effects on cyanobacteria should be avoided; stressor gradients and seasonal effects should be considered as important factors shaping the response.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	10.1111/gcb.14701
UKCEH and CEH Sections/Science Areas:	Water Resources (Science Area 2017-)
ISSN:	1354-1013
Additional Information. Not used in RCUK Gateway to Research.:	Open Access paper - full text available via Official URl link.
Additional Keywords:	climate change, experiment, harmful algal bloom, lake, mesocosm, Microcystis, multiple stressors, UK-SCAPE
NORA Subject Terms:	Ecology and Environment Biology and Microbiology
Date made live:	24 Jul 2019 16:20 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/524480

Item Type:

Publication - Article

Digital Object Identifier (DOI):

10.1111/gcb.14701

UKCEH and CEH Sections/Science Areas:

Water Resources (Science Area 2017-)

ISSN:

1354-1013

Additional Information. Not used in RCUK Gateway to Research.:

Open Access paper - full text available via Official URl link.

Additional Keywords:

climate change, experiment, harmful algal bloom, lake, mesocosm, Microcystis, multiple stressors, UK-SCAPE