<?xml version="1.0" encoding="UTF-8"?>
<rdf:RDF xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#"
         xmlns:dc="http://purl.org/dc/terms/"
         xmlns:foaf="http://xmlns.com/foaf/0.1/"
         xmlns:bibo="http://purl.org/ontology/bibo/"
         xmlns:fabio="http://purl.org/spar/fabio/"
         xmlns:owl="http://www.w3.org/2002/07/owl#"
         xmlns:event="http://purl.org/NET/c4dm/event.owl#"
         xmlns:ore="http://www.openarchives.org/ore/terms/">

    <rdf:Description rdf:about="https://www.th-owl.de/elsa/record/12237">
        <ore:isDescribedBy rdf:resource="https://www.th-owl.de/elsa/record/12237"/>
        <dc:title>Decreased nitrogen loading controls summer cyanobacterial blooms without promoting nitrogen‐fixing taxa: Long‐term response of a shallow lake</dc:title>
        <bibo:authorList rdf:parseType="Collection">
            <foaf:Person>
                <foaf:name></foaf:name>
                <foaf:surname></foaf:surname>
                <foaf:givenname></foaf:givenname>
            </foaf:Person>
            <foaf:Person>
                <foaf:name></foaf:name>
                <foaf:surname></foaf:surname>
                <foaf:givenname></foaf:givenname>
            </foaf:Person>
        </bibo:authorList>
        <bibo:abstract>The effectiveness of controlling nitrogen (N) to manage lake eutrophication is debated. Long-term, whole-lake case studies are required to determine whether diazotrophic cyanobacteria can fix sufficient N to offset a reduction of N-inputs. We document the recovery of shallow, productive Lake Müggelsee (Germany) over 37 yr (sampling interval 1–2 weeks) during a decrease of N and phosphorus (P) loading of 79% and 69%, respectively. Nitrogen concentrations in the lake responded immediately to loading reduction whereas P concentrations remained elevated for about 20 yr. Total nitrogen (TN) in the lake was always lower than TN in the inflow. Accordingly, estimated denitrification and N-burial rates substantially exceeded N2 fixation rates in the long term. Phosphorus was growth limiting in spring whereas N was clearly limiting in summer due to high sediment P-release. TN : TP ratios, normalized to phytoplankton biovolume by regression, were 25.5 (weight) in spring and 3.3 in summer. During the study period, dissolved inorganic N (DIN) concentrations in summer decreased and the duration of low DIN concentrations increased by ca. 100 d. The biovolume of cyanobacteria and total phytoplankton decreased by 89% and 76%, respectively. The proportion of N2-fixing cyanobacteria during summer decreased from 36% to 14% of the total phytoplankton biovolume. The total concentration of heterocysts and estimated total N2 fixation did not change over time. In the long term, decreasing N-inputs effectively controlled summer cyanobacteria including N2-fixing taxa, which did not compensate for the N-deficit. A P-only control strategy would not have been as successful.</bibo:abstract>
        <bibo:volume>64</bibo:volume>
        <bibo:issue>S1</bibo:issue>
        <dc:publisher>Wiley</dc:publisher>
        <bibo:doi rdf:resource="10.1002/lno.11002" />
        <ore:similarTo rdf:resource="info:doi/10.1002/lno.11002"/>
    </rdf:Description>
</rdf:RDF>
