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Holocene development and anthropogenic disturbance of a shallow lake system in Central Ireland recorded by diatoms

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Figure

Fig. 1 Location map of the Lough Kinale system, Central Ireland
Table 1 Characteristics of the three lacustrine cells in the Lough Kinale–Derragh Lough system (prior to hydrologicalengineering in the 1960s)
Fig. 2 The Holocene evolution of Lough Kinale: (a) early Holocene, (b) mid-late Holocene, and (c) late Holocene-present,(d) changing lough extent in the southern area and (e) simplified and generalised stratigraphic section of the lake system
Fig. 3 Summary diatom assemblage diagrams from Ballywillin Crannog core showing: trophic status, pH status andlife-form categories
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