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Bottom‐up and top‐down effects of browning and warming on shallow lake food webs

Productivity and trophic structure of aquatic ecosystems result from a complex interplay of bottom‐up and top‐down forces that operate across benthic and pelagic food web compartments. Projected global changes urge the question how this interplay will be affected by browning (increasing input of ter...

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Published in:Global change biology 2019-02, Vol.25 (2), p.504-521
Main Authors: Vasconcelos, Francisco Rivera, Diehl, Sebastian, Rodríguez, Patricia, Hedström, Per, Karlsson, Jan, Byström, Pär
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description Productivity and trophic structure of aquatic ecosystems result from a complex interplay of bottom‐up and top‐down forces that operate across benthic and pelagic food web compartments. Projected global changes urge the question how this interplay will be affected by browning (increasing input of terrestrial dissolved organic matter), nutrient enrichment and warming. We explored this with a process‐based model of a shallow lake food web consisting of benthic and pelagic components (abiotic resources, primary producers, grazers, carnivores), and compared model expectations with the results of a browning and warming experiment in nutrient‐poor ponds harboring a boreal lake community. Under low nutrient conditions, the model makes three major predictions. (a) Browning reduces light and increases nutrient supply; this decreases benthic and increases pelagic production, gradually shifting productivity from the benthic to the pelagic habitat. (b) Because of active habitat choice, fish exert top‐down control on grazers and benefit primary producers primarily in the more productive of the two habitats. (c) Warming relaxes top‐down control of grazers by fish and decreases primary producer biomass, but effects of warming are generally small compared to effects of browning and nutrient supply. Experimental results were consistent with most model predictions for browning: light penetration, benthic algal production, and zoobenthos biomass decreased, and pelagic nutrients and pelagic algal production increased with browning. Also consistent with expectations, warming had negative effects on benthic and pelagic algal biomass and weak effects on algal production and zoobenthos and zooplankton biomass. Inconsistent with expectations, browning had no effect on zooplankton and warming effects on fish depended on browning. The model is applicable also to nutrient‐rich systems, and we propose that it is a useful tool for the exploration of the consequences of different climate change scenarios for productivity and food web dynamics in shallow lakes, the worldwide most common lake type. Productivity and trophic structure of aquatic ecosystems result from the interplay of bottom‐up and top‐down forces across benthic and pelagic food web compartments. Using a process‐based model, we investigated how shallow lake ecosystems respond to browning (terrestrial dissolved organic matter), nutrient enrichment and warming. The model predicts that browning and nutrient enrichment shift pro
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Projected global changes urge the question how this interplay will be affected by browning (increasing input of terrestrial dissolved organic matter), nutrient enrichment and warming. We explored this with a process‐based model of a shallow lake food web consisting of benthic and pelagic components (abiotic resources, primary producers, grazers, carnivores), and compared model expectations with the results of a browning and warming experiment in nutrient‐poor ponds harboring a boreal lake community. Under low nutrient conditions, the model makes three major predictions. (a) Browning reduces light and increases nutrient supply; this decreases benthic and increases pelagic production, gradually shifting productivity from the benthic to the pelagic habitat. (b) Because of active habitat choice, fish exert top‐down control on grazers and benefit primary producers primarily in the more productive of the two habitats. (c) Warming relaxes top‐down control of grazers by fish and decreases primary producer biomass, but effects of warming are generally small compared to effects of browning and nutrient supply. Experimental results were consistent with most model predictions for browning: light penetration, benthic algal production, and zoobenthos biomass decreased, and pelagic nutrients and pelagic algal production increased with browning. Also consistent with expectations, warming had negative effects on benthic and pelagic algal biomass and weak effects on algal production and zoobenthos and zooplankton biomass. Inconsistent with expectations, browning had no effect on zooplankton and warming effects on fish depended on browning. The model is applicable also to nutrient‐rich systems, and we propose that it is a useful tool for the exploration of the consequences of different climate change scenarios for productivity and food web dynamics in shallow lakes, the worldwide most common lake type. Productivity and trophic structure of aquatic ecosystems result from the interplay of bottom‐up and top‐down forces across benthic and pelagic food web compartments. Using a process‐based model, we investigated how shallow lake ecosystems respond to browning (terrestrial dissolved organic matter), nutrient enrichment and warming. The model predicts that browning and nutrient enrichment shift productivity from the benthic to the pelagic habitat, whereas warming relaxes control of grazers by fish, thus decreasing primary producer biomass. Predicted warming effects are, however, small compared to effects of browning and nutrient enrichment. 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Projected global changes urge the question how this interplay will be affected by browning (increasing input of terrestrial dissolved organic matter), nutrient enrichment and warming. We explored this with a process‐based model of a shallow lake food web consisting of benthic and pelagic components (abiotic resources, primary producers, grazers, carnivores), and compared model expectations with the results of a browning and warming experiment in nutrient‐poor ponds harboring a boreal lake community. Under low nutrient conditions, the model makes three major predictions. (a) Browning reduces light and increases nutrient supply; this decreases benthic and increases pelagic production, gradually shifting productivity from the benthic to the pelagic habitat. (b) Because of active habitat choice, fish exert top‐down control on grazers and benefit primary producers primarily in the more productive of the two habitats. (c) Warming relaxes top‐down control of grazers by fish and decreases primary producer biomass, but effects of warming are generally small compared to effects of browning and nutrient supply. Experimental results were consistent with most model predictions for browning: light penetration, benthic algal production, and zoobenthos biomass decreased, and pelagic nutrients and pelagic algal production increased with browning. Also consistent with expectations, warming had negative effects on benthic and pelagic algal biomass and weak effects on algal production and zoobenthos and zooplankton biomass. Inconsistent with expectations, browning had no effect on zooplankton and warming effects on fish depended on browning. The model is applicable also to nutrient‐rich systems, and we propose that it is a useful tool for the exploration of the consequences of different climate change scenarios for productivity and food web dynamics in shallow lakes, the worldwide most common lake type. Productivity and trophic structure of aquatic ecosystems result from the interplay of bottom‐up and top‐down forces across benthic and pelagic food web compartments. Using a process‐based model, we investigated how shallow lake ecosystems respond to browning (terrestrial dissolved organic matter), nutrient enrichment and warming. The model predicts that browning and nutrient enrichment shift productivity from the benthic to the pelagic habitat, whereas warming relaxes control of grazers by fish, thus decreasing primary producer biomass. Predicted warming effects are, however, small compared to effects of browning and nutrient enrichment. 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Fisheries Abstracts (ASFA) 3: Aquatic Pollution &amp; Environmental Quality</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>MEDLINE - Academic</collection><collection>SwePub</collection><collection>SwePub Articles</collection><collection>SWEPUB Umeå universitet</collection><jtitle>Global change biology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Vasconcelos, Francisco Rivera</au><au>Diehl, Sebastian</au><au>Rodríguez, Patricia</au><au>Hedström, Per</au><au>Karlsson, Jan</au><au>Byström, Pär</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Bottom‐up and top‐down effects of browning and warming on shallow lake food webs</atitle><jtitle>Global change biology</jtitle><addtitle>Glob Chang Biol</addtitle><date>2019-02</date><risdate>2019</risdate><volume>25</volume><issue>2</issue><spage>504</spage><epage>521</epage><pages>504-521</pages><issn>1354-1013</issn><issn>1365-2486</issn><eissn>1365-2486</eissn><abstract>Productivity and trophic structure of aquatic ecosystems result from a complex interplay of bottom‐up and top‐down forces that operate across benthic and pelagic food web compartments. Projected global changes urge the question how this interplay will be affected by browning (increasing input of terrestrial dissolved organic matter), nutrient enrichment and warming. We explored this with a process‐based model of a shallow lake food web consisting of benthic and pelagic components (abiotic resources, primary producers, grazers, carnivores), and compared model expectations with the results of a browning and warming experiment in nutrient‐poor ponds harboring a boreal lake community. Under low nutrient conditions, the model makes three major predictions. (a) Browning reduces light and increases nutrient supply; this decreases benthic and increases pelagic production, gradually shifting productivity from the benthic to the pelagic habitat. (b) Because of active habitat choice, fish exert top‐down control on grazers and benefit primary producers primarily in the more productive of the two habitats. (c) Warming relaxes top‐down control of grazers by fish and decreases primary producer biomass, but effects of warming are generally small compared to effects of browning and nutrient supply. Experimental results were consistent with most model predictions for browning: light penetration, benthic algal production, and zoobenthos biomass decreased, and pelagic nutrients and pelagic algal production increased with browning. Also consistent with expectations, warming had negative effects on benthic and pelagic algal biomass and weak effects on algal production and zoobenthos and zooplankton biomass. Inconsistent with expectations, browning had no effect on zooplankton and warming effects on fish depended on browning. The model is applicable also to nutrient‐rich systems, and we propose that it is a useful tool for the exploration of the consequences of different climate change scenarios for productivity and food web dynamics in shallow lakes, the worldwide most common lake type. Productivity and trophic structure of aquatic ecosystems result from the interplay of bottom‐up and top‐down forces across benthic and pelagic food web compartments. Using a process‐based model, we investigated how shallow lake ecosystems respond to browning (terrestrial dissolved organic matter), nutrient enrichment and warming. The model predicts that browning and nutrient enrichment shift productivity from the benthic to the pelagic habitat, whereas warming relaxes control of grazers by fish, thus decreasing primary producer biomass. Predicted warming effects are, however, small compared to effects of browning and nutrient enrichment. A pond‐scale manipulation of browning and warming corroborated many of these expectations.</abstract><cop>England</cop><pub>Blackwell Publishing Ltd</pub><pmid>30430702</pmid><doi>10.1111/gcb.14521</doi><tpages>18</tpages><orcidid>https://orcid.org/0000-0002-3860-5051</orcidid><orcidid>https://orcid.org/0000-0002-2327-9716</orcidid><oa>free_for_read</oa></addata></record>
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ispartof Global change biology, 2019-02, Vol.25 (2), p.504-521
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subjects Algae
Aquatic ecosystems
benthic and pelagic habitats
Benthos
Biomass
bottom-up and top-down control
Browning
Carnivores
Carnivorous animals
Climate change
Dissolved organic matter
Dynamics
Ecosystems
Environmental changes
Exploration
Fish
Food chains
Food production
Food webs
Habitats
Lakes
light and nutrients
Light penetration
Mathematical models
Mineral nutrients
Nutrient cycles
Nutrient enrichment
Nutrients
Organic matter
Plankton
Productivity
shallow lake
Terrestrial environments
top predator
Trophic structure
warming
Zoobenthos
Zooplankton
title Bottom‐up and top‐down effects of browning and warming on shallow lake food webs
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