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    <title>UTas ePrints - Vulnerability of mangroves and tidal wetlands of the Great Barrier Reef to climate change</title>
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    <meta content="Lovelock, C.E." name="eprints.creators_name" />
<meta content="Ellison, J.C." name="eprints.creators_name" />
<meta content="Johnson, J.E." name="eprints.editors_name" />
<meta content="Marshall, P.A." name="eprints.editors_name" />
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<meta content="2007-11-05 01:42:15" name="eprints.datestamp" />
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<meta content="Climate change will have an enormous influence on the intertidal wetlands of the Great Barrier Reef
(GBR). Increases in atmospheric carbon dioxide (CO2) concentrations and associated increases in air
and sea temperatures, rising sea level, changes in oceanic circulation, rainfall patterns and frequency
and intensity of storms are highly likely to affect the physiology, ecology and ultimately the stability
of wetland habitats (Table 9.1). The intertidal position of mangroves, salt marshes and salt flats makes
them particularly vulnerable to changes in sea level, although other climate change factors will also
exert a strong influence on wetland communities (Table 9.1). Past rises in sea level have led to increases
in the area of mangroves in northern Australia186. However, past climate change has occurred with
limited human modification of the coast compared to current levels of development. Human activities
have resulted in loss of wetlands, disruption to connectivity, enhanced availability of nutrients, changed
sediment dynamics and the creation of structures that will prevent landward migration of wetlands
with sea level rise (eg roads, berms, bunds and sea walls). Many of these human impacts will reduce
the resilience of intertidal wetlands to climate change. To conserve the intertidal wetlands of the GBR
and the ecosystem services they provide, we will need to manage the coastal zone in a way that
enhances the resilience of mangroves, salt marshes and salt flats during climate change." name="eprints.abstract" />
<meta content="2007" name="eprints.date" />
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<meta content="Climate change will have an enormous influence on the intertidal wetlands of the Great Barrier Reef
(GBR). Increases in atmospheric carbon dioxide (CO2) concentrations and associated increases in air
and sea temperatures, rising sea level, changes in oceanic circulation, rainfall patterns and frequency
and intensity of storms are highly likely to affect the physiology, ecology and ultimately the stability
of wetland habitats (Table 9.1). The intertidal position of mangroves, salt marshes and salt flats makes
them particularly vulnerable to changes in sea level, although other climate change factors will also
exert a strong influence on wetland communities (Table 9.1). Past rises in sea level have led to increases
in the area of mangroves in northern Australia186. However, past climate change has occurred with
limited human modification of the coast compared to current levels of development. Human activities
have resulted in loss of wetlands, disruption to connectivity, enhanced availability of nutrients, changed
sediment dynamics and the creation of structures that will prevent landward migration of wetlands
with sea level rise (eg roads, berms, bunds and sea walls). Many of these human impacts will reduce
the resilience of intertidal wetlands to climate change. To conserve the intertidal wetlands of the GBR
and the ecosystem services they provide, we will need to manage the coastal zone in a way that
enhances the resilience of mangroves, salt marshes and salt flats during climate change." name="DC.description" />
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    <h1 class="ep_tm_pagetitle">Vulnerability of mangroves and tidal wetlands of the Great Barrier Reef to climate change</h1>
    <p style="margin-bottom: 1em" class="not_ep_block"><span class="person_name">Lovelock, C.E.</span> and <span class="person_name">Ellison, J.C.</span> (2007) <xhtml:em>Vulnerability of mangroves and tidal wetlands of the Great Barrier Reef to climate change.</xhtml:em> In: Climate Change and the Great Barrier Reef: A Vulnerability Assessment. . Great Barrier Reef Marine Park Authority and Australian Greenhouse Office, Australia, pp. 237-269.</p><p style="margin-bottom: 1em" class="not_ep_block"></p><table style="margin-bottom: 1em" class="not_ep_block"><tr><td valign="top" style="text-align:center"><a onmouseover="EPJS_ShowPreview( event, 'doc_preview_2766' );" href="http://eprints.utas.edu.au/2218/1/LovelockEllison2007.pdf" onmouseout="EPJS_HidePreview( event, 'doc_preview_2766' );"><img alt="[img]" src="http://eprints.utas.edu.au/style/images/fileicons/application_pdf.png" class="ep_doc_icon" border="0" /></a><div class="ep_preview" id="doc_preview_2766"><table><tr><td><img alt="" src="http://eprints.utas.edu.au/2218/thumbnails/1/preview.png" class="ep_preview_image" border="0" /><div class="ep_preview_title">Preview</div></td></tr></table></div></td><td valign="top"><a href="http://eprints.utas.edu.au/2218/1/LovelockEllison2007.pdf"><span class="ep_document_citation">PDF</span></a> - Requires a PDF viewer<br />961Kb</td></tr></table><div class="not_ep_block"><h2>Abstract</h2><p style="padding-bottom: 16px; text-align: left; margin: 1em auto 0em auto">Climate change will have an enormous influence on the intertidal wetlands of the Great Barrier Reef&#13;
(GBR). Increases in atmospheric carbon dioxide (CO2) concentrations and associated increases in air&#13;
and sea temperatures, rising sea level, changes in oceanic circulation, rainfall patterns and frequency&#13;
and intensity of storms are highly likely to affect the physiology, ecology and ultimately the stability&#13;
of wetland habitats (Table 9.1). The intertidal position of mangroves, salt marshes and salt flats makes&#13;
them particularly vulnerable to changes in sea level, although other climate change factors will also&#13;
exert a strong influence on wetland communities (Table 9.1). Past rises in sea level have led to increases&#13;
in the area of mangroves in northern Australia186. However, past climate change has occurred with&#13;
limited human modification of the coast compared to current levels of development. Human activities&#13;
have resulted in loss of wetlands, disruption to connectivity, enhanced availability of nutrients, changed&#13;
sediment dynamics and the creation of structures that will prevent landward migration of wetlands&#13;
with sea level rise (eg roads, berms, bunds and sea walls). Many of these human impacts will reduce&#13;
the resilience of intertidal wetlands to climate change. To conserve the intertidal wetlands of the GBR&#13;
and the ecosystem services they provide, we will need to manage the coastal zone in a way that&#13;
enhances the resilience of mangroves, salt marshes and salt flats during climate change.</p></div><table style="margin-bottom: 1em" cellpadding="3" class="not_ep_block" border="0"><tr><th valign="top" class="ep_row">Item Type:</th><td valign="top" class="ep_row">Book Chapter</td></tr><tr><th valign="top" class="ep_row">Subjects:</th><td valign="top" class="ep_row"><a href="http://eprints.utas.edu.au/view/subjects/300801.html">300000 Agricultural, Veterinary and Environmental Sciences &gt; 300800 Environmental Sciences &gt; 300801 Environmental Management and Rehabilitation</a></td></tr><tr><th valign="top" class="ep_row">ID Code:</th><td valign="top" class="ep_row">2218</td></tr><tr><th valign="top" class="ep_row">Deposited By:</th><td valign="top" class="ep_row"><span class="ep_name_citation"><span class="person_name">Dr Joanna Ellison</span></span></td></tr><tr><th valign="top" class="ep_row">Deposited On:</th><td valign="top" class="ep_row">05 Nov 2007 12:42</td></tr><tr><th valign="top" class="ep_row">Last Modified:</th><td valign="top" class="ep_row">09 Jan 2008 02:30</td></tr><tr><th valign="top" class="ep_row">ePrint Statistics:</th><td valign="top" class="ep_row"><a target="ePrintStats" href="/es/index.php?action=show_detail_eprint;id=2218;">View statistics for this ePrint</a></td></tr></table><p align="right">Repository Staff Only: <a href="http://eprints.utas.edu.au/cgi/users/home?screen=EPrint::View&amp;eprintid=2218">item control page</a></p>
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