Cape Cod National Sea Shore #provincetown #nationalseashore #artshack #capecod
Coastal dunes make up roughly one third of the Cape Cod National Seashore, covering approximately 8,500 acres from Chatham to Provincetown. Dunes predominate on barrier beach and spits, along the coastal margins of the Atlantic Ocean and Cape Cod Bay, and across the northern tip of the peninsula – an area known as the Province Lands. The Province Lands dunes began forming soon after glacial retreat (~18,000 y.b.p.) as eroded sediments from the outwash plain were transported north and deposited by longshore currents. Sand from the beaches of this elongating hook was then blown inland to form the dunes. Although mature forest eventually became established here, most of the vegetation was removed by Europeans settlers for use in building and to clear land for agriculture and livestock grazing. This resulted in a rapid destabilization of the ground surface and by the mid-1800s the area had been converted to a sparsely vegetated system of shifting dunes.
CACO dunes are variably covered with vegetation, some of which has established naturally and a small portion of which was planted at various times in an attempt to minimize dune migration. Successful dune species have adaptations to tolerate hot, dry, and sometimes salty conditions. Plants often have a thick, waxy cuticle to limit water loss. In the case of American beachgrass (Ammophila breviligulata), the leaves roll up during hot, dry weather, which reduces transpiration. Common plant species of the dunes include American beachgrass, seaside goldenrod (Solidago sempervirons), poison ivy (Toxicodendron radicans), wormwood (Artemesia campestris ssp. caudata), northern bayberry (Morella pensylvanica), and beach plum (Prunus maritima). In interdunal depressions that are low enough to intersect with the groundwater table for part of the growing season, seasonal wetlands form and support distinct plant communities.
A number of environmental factors have been shown to influence dune plant communities and their patterns of succession or regression. Wind c