The Palaeolimnology of Lough Murree, A Brackish Lake in the Burren, Ireland

Abstract

Lough Murree, a rock/karst barrier lagoon, is superficially isolated from the sea and seasonal variations in lake water level reflect precipitation and groundwater variation. Lake salinity is influenced by subsurface saline intrusions, occasional barrier overwash together with precipitation and groundwater inflow, leading to poikilohaline conditions. Palaeolimnological reconstructions in Murree support the supposition that the lagoon was once superficially connected to the sea around the mid-nineteenth century. Physical, chemical and biological proxies suggest an evolution to more freshwater conditions. Uncertainties about the timing of the transition persist because of an unresolved sediment chronology. The isolation of Murree from the Atlantic Ocean has promoted the formation of dense charophyte beds composed of lagoonal specialist species, which are able to tolerate large variations in salinity.

Mid- and late-Holocene environmental change in western Ireland: New evidence from coastal peats and fossil timbers with particular reference to relative sea-level change

“…On the other hand, palaeolimnological investigations of short cores from Lough Murree, a brackish shallow lake on the south shore of Galway Bay (Figure 1), indicate a shift towards freshwater conditions in the mid second millennium AD. This unexpected result is regarded as due to local factors rather than changes in RSL which is expected to be rising at this time (Cassina et al, 2013a).…”