Carbon and nutrient subsidies to a lowland river following floodplain inundation

D.L. Nielsen, R.A. Cook, N. Ning, B. Gawne, R. Petrie

    Research output: Contribution to journalArticle

    4 Citations (Scopus)

    Abstract

    Despite the perceived importance of floodplain inundation to the functioning of lowland rivers, there is limited understanding of the contribution that floodplains make to the main river channel during floods. In 2010, substantial
    flooding occurred throughout south-eastern Australia, which provided an opportunity to quantify the export of biological material and nutrients from a floodplain back in to the main river channel. We quantified the amounts of zooplankton, phytoplankton, dissolved organic carbon and nutrients within the main river channel of the River Murray immediately upstream of the Barmah–Millewa Forest, and at two sites immediately downstream of the forest during two flood events in July and October of 2010. Results demonstrated that although a smaller flood event in July did not contribute substantially to
    an increase in the measured parameters, a much larger flood in October contributed 0.4 tonnes (t) of phytoplankton; 7 t of zooplankton and 300 t of dissolved organic carbon. This suggests that small floods will provide minimal resource subsidies back into the main channel after the cessation of flooding. In comparison, larger floods that result in large volumes of floodplain water returning to the river will provide substantial subsidies of terrestrially derived resources.
    Original languageEnglish
    Pages (from-to)1302-1312
    Number of pages11
    JournalMarine and Freshwater Research
    Volume67
    Issue number9
    DOIs
    Publication statusPublished - 2016

    Fingerprint

    subsidies
    floodplains
    floodplain
    lowlands
    rivers
    carbon
    nutrient
    nutrients
    river channel
    river
    dissolved organic carbon
    zooplankton
    phytoplankton
    resource
    subsidy
    flooding
    water

    Cite this

    Nielsen, D.L. ; Cook, R.A. ; Ning, N. ; Gawne, B. ; Petrie, R. / Carbon and nutrient subsidies to a lowland river following floodplain inundation. In: Marine and Freshwater Research. 2016 ; Vol. 67, No. 9. pp. 1302-1312.
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    abstract = "Despite the perceived importance of floodplain inundation to the functioning of lowland rivers, there is limited understanding of the contribution that floodplains make to the main river channel during floods. In 2010, substantialflooding occurred throughout south-eastern Australia, which provided an opportunity to quantify the export of biological material and nutrients from a floodplain back in to the main river channel. We quantified the amounts of zooplankton, phytoplankton, dissolved organic carbon and nutrients within the main river channel of the River Murray immediately upstream of the Barmah–Millewa Forest, and at two sites immediately downstream of the forest during two flood events in July and October of 2010. Results demonstrated that although a smaller flood event in July did not contribute substantially toan increase in the measured parameters, a much larger flood in October contributed 0.4 tonnes (t) of phytoplankton; 7 t of zooplankton and 300 t of dissolved organic carbon. This suggests that small floods will provide minimal resource subsidies back into the main channel after the cessation of flooding. In comparison, larger floods that result in large volumes of floodplain water returning to the river will provide substantial subsidies of terrestrially derived resources.",
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    Nielsen, DL, Cook, RA, Ning, N, Gawne, B & Petrie, R 2016, 'Carbon and nutrient subsidies to a lowland river following floodplain inundation', Marine and Freshwater Research, vol. 67, no. 9, pp. 1302-1312. https://doi.org/10.1071/MF14390

    Carbon and nutrient subsidies to a lowland river following floodplain inundation. / Nielsen, D.L.; Cook, R.A.; Ning, N.; Gawne, B.; Petrie, R.

    In: Marine and Freshwater Research, Vol. 67, No. 9, 2016, p. 1302-1312.

    Research output: Contribution to journalArticle

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    T1 - Carbon and nutrient subsidies to a lowland river following floodplain inundation

    AU - Nielsen, D.L.

    AU - Cook, R.A.

    AU - Ning, N.

    AU - Gawne, B.

    AU - Petrie, R.

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    PY - 2016

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    N2 - Despite the perceived importance of floodplain inundation to the functioning of lowland rivers, there is limited understanding of the contribution that floodplains make to the main river channel during floods. In 2010, substantialflooding occurred throughout south-eastern Australia, which provided an opportunity to quantify the export of biological material and nutrients from a floodplain back in to the main river channel. We quantified the amounts of zooplankton, phytoplankton, dissolved organic carbon and nutrients within the main river channel of the River Murray immediately upstream of the Barmah–Millewa Forest, and at two sites immediately downstream of the forest during two flood events in July and October of 2010. Results demonstrated that although a smaller flood event in July did not contribute substantially toan increase in the measured parameters, a much larger flood in October contributed 0.4 tonnes (t) of phytoplankton; 7 t of zooplankton and 300 t of dissolved organic carbon. This suggests that small floods will provide minimal resource subsidies back into the main channel after the cessation of flooding. In comparison, larger floods that result in large volumes of floodplain water returning to the river will provide substantial subsidies of terrestrially derived resources.

    AB - Despite the perceived importance of floodplain inundation to the functioning of lowland rivers, there is limited understanding of the contribution that floodplains make to the main river channel during floods. In 2010, substantialflooding occurred throughout south-eastern Australia, which provided an opportunity to quantify the export of biological material and nutrients from a floodplain back in to the main river channel. We quantified the amounts of zooplankton, phytoplankton, dissolved organic carbon and nutrients within the main river channel of the River Murray immediately upstream of the Barmah–Millewa Forest, and at two sites immediately downstream of the forest during two flood events in July and October of 2010. Results demonstrated that although a smaller flood event in July did not contribute substantially toan increase in the measured parameters, a much larger flood in October contributed 0.4 tonnes (t) of phytoplankton; 7 t of zooplankton and 300 t of dissolved organic carbon. This suggests that small floods will provide minimal resource subsidies back into the main channel after the cessation of flooding. In comparison, larger floods that result in large volumes of floodplain water returning to the river will provide substantial subsidies of terrestrially derived resources.

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