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Proceedings of the Third International Conference on Invasive ...

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Chapter 3: Ecosystem Effects <str<strong>on</strong>g>of</str<strong>on</strong>g> <strong>Invasive</strong> Spartina<str<strong>on</strong>g>Proceedings</str<strong>on</strong>g> <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> <str<strong>on</strong>g>Third</str<strong>on</strong>g> <str<strong>on</strong>g>Internati<strong>on</strong>al</str<strong>on</strong>g> <str<strong>on</strong>g>C<strong>on</strong>ference</str<strong>on</strong>g> <strong>on</strong> <strong>Invasive</strong> SpartinaIMPACTS OF SPARTINA INVASIONThe introducti<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> S. anglica to <str<strong>on</strong>g>the</str<strong>on</strong>g> Tamar Estuary hasbrought about a dramatic and rapid change to <str<strong>on</strong>g>the</str<strong>on</strong>g> physiography<str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> intertidal z<strong>on</strong>e, illustrated well at a photo pointestablished in 1956 at Paper beach (Fig. 4a and b). The col<strong>on</strong>izati<strong>on</strong><str<strong>on</strong>g>of</str<strong>on</strong>g> what was essentially a vacant niche has transformed<str<strong>on</strong>g>the</str<strong>on</strong>g> gently grading sandy intertidal z<strong>on</strong>es, as shown in Fig. 5,and hard rock intertidal z<strong>on</strong>es (Fig. 6) into laterally extensivemuddy terraces (Figs. 7 and 8).The ecological impacts <str<strong>on</strong>g>of</str<strong>on</strong>g> Spartina invasi<strong>on</strong> in temperateestuaries <str<strong>on</strong>g>of</str<strong>on</strong>g> South Eastern Australia are poorly understood.Studies <str<strong>on</strong>g>of</str<strong>on</strong>g> benthic macro-invertebrate communities in <str<strong>on</strong>g>the</str<strong>on</strong>g>Little Swanport Estuary, Tasmania suggest that Spartinasignificantly increases macro-invertebrate species richnessand total species abundance when compared to previouslyn<strong>on</strong>-vegetated intertidal areas (Hedge 1997). Additi<strong>on</strong>ally,macro-invertebrate communities <str<strong>on</strong>g>of</str<strong>on</strong>g> Spartina marshesshowed remarkable similarity to those <str<strong>on</strong>g>of</str<strong>on</strong>g> native salt marshes(Hedge and Kriwoken 2000). It is suggested <str<strong>on</strong>g>the</str<strong>on</strong>g>refore thatSpartina invasi<strong>on</strong> has provided a niche <str<strong>on</strong>g>of</str<strong>on</strong>g> s<str<strong>on</strong>g>of</str<strong>on</strong>g>t substrate anddense protecti<strong>on</strong>, favoring macro-invertebrates and somebirds such as <str<strong>on</strong>g>the</str<strong>on</strong>g> purple swamphen (Porphyrio porphyrio).It is likely that this subsequently caused a displacement <str<strong>on</strong>g>of</str<strong>on</strong>g>species that formerly inhabited or utilized <str<strong>on</strong>g>the</str<strong>on</strong>g> intertidal z<strong>on</strong>e.Species assemblage and utilizati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> intertidal z<strong>on</strong>e priorto Spartina is not well documented, but likely was relativelyrich in fish and bird species.DISCUSSIONThis paper has provided background for <str<strong>on</strong>g>the</str<strong>on</strong>g> researchproject that assessed <str<strong>on</strong>g>the</str<strong>on</strong>g> alterati<strong>on</strong> to <str<strong>on</strong>g>the</str<strong>on</strong>g> intertidal z<strong>on</strong>e <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g>Tamar Estuary. Using transect based topographic surveys andcoring, <str<strong>on</strong>g>the</str<strong>on</strong>g> volume <str<strong>on</strong>g>of</str<strong>on</strong>g> material trapped under Spartina wascalculated to be 1,193,441 m 3 , comprised <str<strong>on</strong>g>of</str<strong>on</strong>g> approximately17% Spartina-derived organic matter and 83% silts andclays. Based <strong>on</strong> historical pr<str<strong>on</strong>g>of</str<strong>on</strong>g>iles, sedimentati<strong>on</strong> rates since<str<strong>on</strong>g>the</str<strong>on</strong>g> introducti<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> S. anglica have been estimated at between8.7 and 52.4 millimeters per year (mm yr-1).From <str<strong>on</strong>g>the</str<strong>on</strong>g> analysis <str<strong>on</strong>g>of</str<strong>on</strong>g> 80 cores from four sites, Spartinatrappedsediment was found to c<strong>on</strong>tain levels <str<strong>on</strong>g>of</str<strong>on</strong>g> cadmium,copper, lead and zinc elevated above background levels.However, <str<strong>on</strong>g>the</str<strong>on</strong>g>se generaly were below trigger values <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g>ANZECC/ARMCANZ (2000) interim sediment qualityguidelines. It is c<strong>on</strong>sidered unlikely that released sedimentswould impact <strong>on</strong> water quality or health <str<strong>on</strong>g>of</str<strong>on</strong>g> biota with respectto trace metals or organic c<strong>on</strong>taminati<strong>on</strong>.Behaviour <str<strong>on</strong>g>of</str<strong>on</strong>g> sediment with respect to erosi<strong>on</strong> rates,sediment redepositi<strong>on</strong> and causative hydrodynamics werealso m<strong>on</strong>itored within a test area from which Spartina coverwas removed. It has been dem<strong>on</strong>strated that <str<strong>on</strong>g>the</str<strong>on</strong>g> eradicati<strong>on</strong><str<strong>on</strong>g>of</str<strong>on</strong>g> S. anglica will result in elevati<strong>on</strong> loss from <str<strong>on</strong>g>the</str<strong>on</strong>g> Spartinamarsh surface at a rate six times greater than in vegetatedmarshes. The study assumed that this elevati<strong>on</strong> loss is causedby liberati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> sediments. The rate <str<strong>on</strong>g>of</str<strong>on</strong>g> elevati<strong>on</strong> loss orerosi<strong>on</strong> is likely to increase <strong>on</strong>ce <str<strong>on</strong>g>the</str<strong>on</strong>g> dead S. anglica root matdecomposes and <str<strong>on</strong>g>the</str<strong>on</strong>g> surface cohesi<strong>on</strong> and sediment-bindingcapacity is diminished. Elevati<strong>on</strong> loss increases by a factor <str<strong>on</strong>g>of</str<strong>on</strong>g>1.06 with every 10 m from <str<strong>on</strong>g>the</str<strong>on</strong>g> high water bank. Erosi<strong>on</strong> ratesin <str<strong>on</strong>g>the</str<strong>on</strong>g> outer 40 m <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> marsh were also significantly greaterthan <str<strong>on</strong>g>the</str<strong>on</strong>g> remainder <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> marsh at both sites, suggesting thata process o<str<strong>on</strong>g>the</str<strong>on</strong>g>r than S. anglica removal is c<strong>on</strong>tributing to thatretreat <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> lower marsh.Analysis <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g>se interdisciplinary lines <str<strong>on</strong>g>of</str<strong>on</strong>g> inquiryhave allowed for a greater understanding <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g>biogeomorphological resp<strong>on</strong>ses to restorati<strong>on</strong> attempts withinintertidal z<strong>on</strong>es and have provided a sound basis <strong>on</strong> which t<str<strong>on</strong>g>of</str<strong>on</strong>g>ormulate and implement future management <str<strong>on</strong>g>of</str<strong>on</strong>g> Spartina.Spartina eradicati<strong>on</strong> is recommended for <str<strong>on</strong>g>the</str<strong>on</strong>g> lower estuary(type 2 marshes) <strong>on</strong>ly, where trapped sediment volumesare significantly smaller and tidal flushing is greatest. Thiswould enable significant areas <str<strong>on</strong>g>of</str<strong>on</strong>g> sand/gravel intertidal z<strong>on</strong>esto recover and reduce <str<strong>on</strong>g>the</str<strong>on</strong>g> likelihood <str<strong>on</strong>g>of</str<strong>on</strong>g> fur<str<strong>on</strong>g>the</str<strong>on</strong>g>r downstreamexpansi<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> Spartina swards. Retaining type 1 marshes in<str<strong>on</strong>g>the</str<strong>on</strong>g> upper estuary will prevent <str<strong>on</strong>g>the</str<strong>on</strong>g> remobilizati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> sedimentsthat c<strong>on</strong>tain <str<strong>on</strong>g>the</str<strong>on</strong>g> highest c<strong>on</strong>centrati<strong>on</strong>s <str<strong>on</strong>g>of</str<strong>on</strong>g> c<strong>on</strong>taminants, andwill retain <str<strong>on</strong>g>the</str<strong>on</strong>g> marshes for <str<strong>on</strong>g>the</str<strong>on</strong>g> ecological role <str<strong>on</strong>g>the</str<strong>on</strong>g>y currentlyperform.ACKNOWLEDGMENTSThis study was funded by <str<strong>on</strong>g>the</str<strong>on</strong>g> Australian ResearchCouncil Linkage Grant LP0214145, with support from <str<strong>on</strong>g>the</str<strong>on</strong>g>Department <str<strong>on</strong>g>of</str<strong>on</strong>g> Primary Industries and Water, Tasmania and<str<strong>on</strong>g>the</str<strong>on</strong>g> Rice Grass Advisory Group.REFERENCESANZECC/ARMCANZ, 2000. Australian and New Zealand guidelinesfor fresh and marine water quality. Australian and NewZealand Envir<strong>on</strong>ment and C<strong>on</strong>servati<strong>on</strong> Council/ Agricultureand Resource Management Council <str<strong>on</strong>g>of</str<strong>on</strong>g> Australia and NewZealand, Canberra, ACT.Brown, S. 1998. Sedimentati<strong>on</strong> <strong>on</strong> a Humber salt marsh. In: Cramp,A. ed., Sedimentary Processes in <str<strong>on</strong>g>the</str<strong>on</strong>g> Intertidal Z<strong>on</strong>e. GeologicalSociety, L<strong>on</strong>d<strong>on</strong>.Brown, S., E.A. Warman, S. McGrorty, M. Yates, R.J. Pakeman,L.A. Boorman, J.D. Goss-Custard and A.J. Gray. 1998. SedimentFluxes in Intertidal Biotopes: BIOTA II. Marine Polluti<strong>on</strong>Bulletin 37(3-7):173-181.Chapman, V.J., 1960. Salt marshes and salt deserts <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> world.Le<strong>on</strong>ard Hill, L<strong>on</strong>d<strong>on</strong> and New York.Chung, C., 1990. Twenty-five years <str<strong>on</strong>g>of</str<strong>on</strong>g> introduced Spartina anglicain China. In: Gray, A.J. and P.E.M. Benham, eds. Spartinaanglica: a research review, ITE research publicati<strong>on</strong>. NaturalEnvir<strong>on</strong>ment Research Council, Institute <str<strong>on</strong>g>of</str<strong>on</strong>g> Terrestrial Ecology,L<strong>on</strong>d<strong>on</strong>.Doody, J.P., 1990. Spartina – friend or foe? A c<strong>on</strong>servati<strong>on</strong> viewpoint. In: Gray, A.J. and P.E.M. Benham, eds. Spartina anglica: aresearch review, ITE research publicati<strong>on</strong>. Natural Envir<strong>on</strong>mentResearch Council, Institute <str<strong>on</strong>g>of</str<strong>on</strong>g> Terrestrial Ecology, L<strong>on</strong>d<strong>on</strong>.Foster, D.N., R. Nittim J. Walker. 1986. Tamar River siltati<strong>on</strong> study.Technical Report, No. 85/07, University <str<strong>on</strong>g>of</str<strong>on</strong>g> NSW Water ResearchLaboratory.Hatt<strong>on</strong>, R.S., R.D. Delaune and W.H. Patrick, Jr. 1983.Sedimentati<strong>on</strong>, accreti<strong>on</strong>, and subsidence in marshes <str<strong>on</strong>g>of</str<strong>on</strong>g> BaratariaBasin, Louisiana. Limnology and Oceanography 28: 494-502.- 132 -

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