<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>Gary P. Shaffer</dc:contributor>
  <dc:contributor>Denise J. Reed</dc:contributor>
  <dc:contributor>Donald R. Cahoon</dc:contributor>
  <dc:contributor>Louis D. Britsch</dc:contributor>
  <dc:contributor>Suzanne Hawes</dc:contributor>
  <dc:creator>John W. Day</dc:creator>
  <dc:date>2001</dc:date>
  <dc:description>&lt;p&gt;The coastal wetlands of Louisiana comprise a&amp;nbsp;vast expanse of marine to freshwater wetland plant&amp;nbsp;communities interspersed w-ith shallow bays and&amp;nbsp;bayous. These wetlands were built by processes associated with the present-day Mississippi and Atchatfalaya River deltas and older distributaries occupied by the river over the past 7,000 }rears. The&amp;nbsp;high rates of wetland loss identified in this system&amp;nbsp;during the 20th century have serious consequences for living resources (Boesch et al. 1994) and&amp;nbsp;coastal residents, and they affect our ability to&amp;nbsp;maintain navigation and flood control. The restoration and management response to this problem&amp;nbsp;must be grounded in a sound understanding of the&amp;nbsp;causative factors. The system has been highly altered by river levees, roads and railway embankments, impoundments, and canals of many dimensions dredged for a variety of purposes. These&amp;nbsp;changes have been imposed on a landscape that is&amp;nbsp;essentially the result of a delicate natural balance&amp;nbsp;between wetland building processes and compaction, subsidence, and sea-level rise. Many now recognize that coastal wetlands can cope with relatively high rates of subsidence and sea-level rise, as&amp;nbsp;long as the processes that ensure wetland sustainability through vertical accumulation of substrate&amp;nbsp;remain unimpaired (Boesch et al. 2000).&lt;br&gt;&lt;/p&gt;&lt;p&gt;The challenge facing both the scientific community and coastal resource managers in Louisiana&amp;nbsp;is to look to the future. We must use our understanding of the problem and how it evolved to develop a multi-use ecosystem management plan, and&amp;nbsp;some efforts have been made by state and federal&amp;nbsp;agencies towards this goal (LCWCRTF &amp;amp; WCRA&amp;nbsp;1998). The present discussions (Turner 1997,&amp;nbsp;2001; Day et al. 2000; Gosselink 2001) demonstrate&amp;nbsp;the complexity of the issues faced in Louisiana.&amp;nbsp;While such discourse is common in the scientific&amp;nbsp;community where varied approaches and interpretations are a sign of vitality, it is helpful to be clear&amp;nbsp;about the state of knowledge and what levels of&amp;nbsp;uncertainty exist. We seek to clarify some of the&amp;nbsp;issues that have been raised in the discussion, recognizing that our best-available science cannot yet&amp;nbsp;resolve many of them as completely as all would&amp;nbsp;like. &lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.2307/1353263</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Springer Link</dc:publisher>
  <dc:title>Patterns and processes of wetland loss in coastal Louisiana are complex: A reply to Turner 2001. Estimating the indirect effects of hydrologic change on wetland loss: If the Earth is curved, then how would we know it? </dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>