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dc.contributor.authorGladstone-Gallagher, Rebecca Vivianen_NZ
dc.contributor.authorSandwell, Dean R.en_NZ
dc.contributor.authorLohrer, Andrew M.en_NZ
dc.contributor.authorLundquist, Carolyn J.en_NZ
dc.contributor.authorPilditch, Conrad A.en_NZ
dc.date.accessioned2018-02-22T21:24:48Z
dc.date.available2017-01-01en_NZ
dc.date.available2018-02-22T21:24:48Z
dc.date.issued2017en_NZ
dc.identifier.citationGladstone-Gallagher, R. V., Sandwell, D. R., Lohrer, A. M., Lundquist, C. J., & Pilditch, C. A. (2017). Quantifying macrodetritus fluxes from a small temperate estuary. Marine and Freshwater Research, 68(12), 2289–2305. https://doi.org/10.1071/MF16408en
dc.identifier.issn1323-1650en_NZ
dc.identifier.urihttps://hdl.handle.net/10289/11675
dc.description.abstractEmpirical measurements of estuary-to-coast material fluxes usually exclude the fraction of primary production that is exported as macrodetritus (marine plant litter), potentially leaving a gap in our understanding of the role of estuaries as outwelling systems. To address this gap, we sampled water and suspended material seasonally from the mouth of Pepe Inlet, Tairua Estuary, New Zealand. From samples collected hourly over 24 h, we calculated the lateral tidal fluxes (import, export, net flux) of macrodetritus, particulate and dissolved forms of nitrogen (N) and phosphorus (P). Annually, the inlet was a net exporter of N and P (5145 and 362 kg respectively). However, macrodetritus accounted for <13 and <3% of seasonal N and P exports respectively. Macrodetritus is an obvious and visible source of estuary-to-coast subsidy, but our derived nutrient budgets suggest the dissolved and particulate forms dominate the net export of N and P (>87%). Nevertheless, seasonal pulses in the source and supply of macrodetritus may have consequences for the temporal scales over which this resource subsidy affects receiving ecosystems (e.g. intertidal sandflats). These mensurative investigations are useful to inform estuarine nutrient budgets that quantify the ecosystem services provided by temperate estuaries (e.g. contribution to fisheries food webs).
dc.format.mimetypeapplication/pdf
dc.language.isoenen_NZ
dc.publisherCSIRO Publishingen_NZ
dc.rightsThis is an author’s accepted version of an article published in the journal: Marine and Freshwater Research. © 2017 CSIRO Publishing.
dc.subjectScience & Technologyen_NZ
dc.subjectLife Sciences & Biomedicineen_NZ
dc.subjectPhysical Sciencesen_NZ
dc.subjectFisheriesen_NZ
dc.subjectLimnologyen_NZ
dc.subjectMarine & Freshwater Biologyen_NZ
dc.subjectOceanographyen_NZ
dc.subjectdetritusen_NZ
dc.subjectestuarine fluxen_NZ
dc.subjectmacrophyte detritusen_NZ
dc.subjectoutwelling hypothesisen_NZ
dc.subjectspatial subsidiesen_NZ
dc.subjectECOSYSTEM FUNCTIONen_NZ
dc.subjectMANGROVE FORESTSen_NZ
dc.subjectNORTH-INLETen_NZ
dc.subjectNEW-ZEALANDen_NZ
dc.subjectSALT-MARSHen_NZ
dc.subjectDETRITAL ENRICHMENTen_NZ
dc.subjectPARTICULATEen_NZ
dc.subjectASSEMBLAGESen_NZ
dc.subjectTRANSPORTen_NZ
dc.subjectDYNAMICSen_NZ
dc.titleQuantifying macrodetritus fluxes from a small temperate estuaryen_NZ
dc.typeJournal Article
dc.identifier.doi10.1071/MF16408en_NZ
dc.relation.isPartOfMarine and Freshwater Researchen_NZ
pubs.begin-page2289
pubs.elements-id214324
pubs.end-page2305
pubs.issue12en_NZ
pubs.publication-statusPublisheden_NZ
pubs.volume68en_NZ
dc.identifier.eissn1448-6059en_NZ


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