interdunal wetland
File:Interdunal wetland.jpg. ]]
An interdunal wetland, interdunal pond or dune slack is a water-filled depression between coastal sand dunes. It may be formed either by wind erosion or by dunal encroachment on an existing wetland.{{Cite web
|url=http://dnr.wi.gov/org/land/er/communities/index.asp?mode=detail&Code=CPHER068WI
|title=Interdunal Wetland
|work=Natural Communities of Wisconsin
|author=Wisconsin Department of Natural Resources
|access-date=2011-06-26
|date=2008-10-13
|archive-url=https://web.archive.org/web/20100604101934/http://dnr.wi.gov/org/land/er/communities/index.asp?mode=detail&Code=CPHER068WI
|archive-date=2010-06-04
|url-status=dead
}} The wind erosion process involves wind scooping out sufficient sand to reach the water table, and typically occurs behind the first line of foredunes.{{Cite web
|url=http://www1.dnr.wa.gov/nhp/refdesk/communities/pdf/eia/np_interdunal_wetland.pdf
|title=Ecological Integrity Assessment: North Pacific Coastal Interdunal Wetland
|author=Washington Department of Natural Resources
|access-date=2011-06-26
|archive-url=https://web.archive.org/web/20111003230547/http://www1.dnr.wa.gov/nhp/refdesk/communities/pdf/eia/np_interdunal_wetland.pdf
|archive-date=2011-10-03
|url-status=dead
}}
The Indiana Dunes contain interdunal wetlands.Smith, S. & Mark, S. (2009). The Historical Roots of the Nature Conservancy in the Northwest Indiana/Chicagoland Region: From Science to Preservation. The South Shore Journal, 3. {{cite web|url=http://www.southshorejournal.org/index.php/issues/volume-3-2009/83-journals/vol-3-2009/75-the-historical-roots-of-the-nature-conservancy-in-the-northwest-indianachicagoland-region-from-science-to-preservation |title=South Shore Journal - the Historical Roots of the Nature Conservancy in the Northwest Indiana/Chicagoland Region: From Science to Preservation |access-date=2015-11-22 |url-status=dead |archive-url=https://web.archive.org/web/20160101021140/http://www.southshorejournal.org/index.php/issues/volume-3-2009/83-journals/vol-3-2009/75-the-historical-roots-of-the-nature-conservancy-in-the-northwest-indianachicagoland-region-from-science-to-preservation |archive-date=2016-01-01 }} Many conservation efforts have been made to preserve parts of the Indiana Dunes.Smith, S. & Mark, S. (2006). Alice Gray, Dorothy Buell, and Naomi Svihla: Preservationists of Ogden Dunes. The South Shore Journal, {{cite web |url=1.http://www.southshorejournal.org/index.php/issues/volume-1-2006/78-journals/vol-1-2006/117-alice-gray-dorothy-buell-and-naomi-svihla-preservationists-of-ogden-dunes |title=South Shore Journal - Alice Gray, Dorothy Buell, and Naomi Svihla: Preservationists of Ogden Dunes |access-date=2012-06-13 |url-status=dead |archive-url=https://web.archive.org/web/20120913013557/http://www.southshorejournal.org/index.php/issues/volume-1-2006/78-journals/vol-1-2006/117-alice-gray-dorothy-buell-and-naomi-svihla-preservationists-of-ogden-dunes |archive-date=2012-09-13 }}Smith, S. & Mark, S. (2007). The cultural impact of a museum in a small community: The Hour Glass of Ogden Dunes. The South Shore Journal, 2. {{cite web|url=http://www.southshorejournal.org/index.php/issues/volume-2-2007/82-journals/vol-2-2007/104-the-cultural-impact-of-a-museum-in-a-small-community-the-hour-glass-in-ogden-dunes |title=South Shore Journal - the Cultural Impact of a Museum in a Small Community: The Hour Glass in Ogden Dunes |access-date=2012-06-11 |url-status=dead |archive-url=https://web.archive.org/web/20121130085605/http://www.southshorejournal.org/index.php/issues/volume-2-2007/82-journals/vol-2-2007/104-the-cultural-impact-of-a-museum-in-a-small-community-the-hour-glass-in-ogden-dunes |archive-date=2012-11-30 }}
Because they are typically very shallow, interdunal wetlands warm quickly, and provide an abundant source of invertebrates eaten by many species of shorebirds. Many interdunal wetlands are ephemeral, drying out during periods of low rain or low water.
In the Great Lakes region of North America, interdunal communities are typically mildly calcareous and dominated by rushes, sedges and shrubs.{{Cite web
|url=http://web4.msue.msu.edu/mnfi/communities/community.cfm?id=10668
|title=Interdunal Wetland
|first1=M.A.
|last1=Kost
|first2=D.A.
|last2=Albert
|first3=J.G.
|last3=Cohen
|first4=B.S.
|last4=Slaughter
|first5=R.K.
|last5=Schillo
|first6=C.R.
|last6=Weber
|first7=K.A.
|last7=Chapman
|year=2007
|work=Natural Communities of Michigan: Classification and Description
|access-date=2011-06-26
|archive-url=https://web.archive.org/web/20110816233757/http://web4.msue.msu.edu/mnfi/communities/community.cfm?id=10668
|archive-date=2011-08-16
|url-status=dead
}} They are tentatively classified as G2, or globally imperiled, under the NatureServe rankings.
A distinction is sometimes made between interdunal and intradunal wetlands such as pannes, which form within a single dune as part of a blowout.