Psammosere, dune succession in Umbra Nature Reserve Flashcards
Dunes are formed by
deposition of sand on the landward side of wide beaches
Waves and onshore winds carry material above the tide line…
…where it may be trapped behind small obstacles forming small embryo dunes
these small embryo dunes, often less than a metre in height…
…can provide a home for a group of specialist pioneer plants, including sand couch grass. These species can tolerate the low nutrient saline and windswept conditions
Root systems of pioneer plants can help stabilize dunes…
…trapping more sand and the dunes grow. Marram grass is the most important plant species here; it thrives on burial by sand, forming a complex rhizome root network which binds the dune in place
Over time a series of ridges can be created parallel to the shoreline…
…nearest the sea are embryo dunes, then foredunes, then yellow and grey dunes. Between these ridges lie low sheltered areas termed dune slacks.
In dune slacks the conditions may be wet or dry but are always more sheltered…
…and provide a habitat for plants, insects and animals less suited to the dune ridges.
A walk inland from a beach through dunes is essentially a walk through time…
…starting with the initial colonization of the embryo dunes to the final stage in the sere - the climax vegetation community
Expected changes in characteristics moving inland:
Proportion of bare sand decreases as more species invade and conditions improve.
Proportion of soil that is organic in origin from plants and animals increases.
pH decreases from salty alkaline environment of shore as decomposing dead plant material adds organic material.
Expected changes in characteristics moving inland:
Ability of soil to retain water improves as organic material is added.
Range of plant, insect and animal species increases, although pioneer species are replaced.
The height and stability of both the dunes and vegetation increases.
Magilligan, 32km squared of land is Ireland’s largest area of coastal deposition… the psammosere studied is:
Umbra Nature Reserve Dunes
Umbra: youngest embryo dunes - hostile environment for plant life…
…very dry, salty and lacks humus; alkaline pH of 8-9 partly due to shell fragments. Pioneer plant - sand couch grass - stores water in succulent leaves. Helps slow and collect sand blown from beach. Vegetation cover sparse; 80% of dune is exposed sand.
Umbra: Foredunes - first seral stage of pioneer community..;.
…older slightly higher foredunes - sometimes referred to as yellow dunes because of high proportion (over 20%) of visible sand. Mobile dunes, collecting sand and growing in height. Marram grass dominates. well adapted to dry conditions(rolled leaves, waxy surface). Long rhizomes which grow laterally and vertically. Long tap roots reach groundwater deep below the surface and help stabilize the dunes, allowing other plant species to colonise.
Umbra: Dune slacks - between dune ridges. Often near or below water table. More sheltered environments, plant range:
wild strawberries, buttercups, violets
Umbra: Grey dunes - older, fixed dunes at later seral stage of succession…
…gradually conditions for plant growth improves with distance from beach. pH of grey or mature dunes is reduced (6.5-7.5 - slightly acidic or alkaline). More shelter, less salt. Better conditions - number and diversity of plant species increases, covering the sand surface. Less than 10% of dunes now visible sand. Plants die and decay - thin layer of humus develops, hence name grey dunes. Moisture and nutrients present in humus help colonization of this part of the dune system.
Umbra: grey dunes - plants grow in rosettes, helping to maintain moisture:
dandelions, plantains, ragwort.
Plants with leafy stems - bird’s foot trefoil, clover.
Fescue and meadow grass replace marram.
Further inland, burnet rose and sea buckthorn