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dc.contributor.advisorPotito, Aaron
dc.contributor.authorTaylor, Karen
dc.date.accessioned2018-03-08T14:50:26Z
dc.date.issued2017-12-20
dc.identifier.urihttp://hdl.handle.net/10379/7188
dc.description.abstractThis article-based PhD thesis explored the utility and performance of chironomid (Diptera: Chironomidae) autecology in the investigation of prehistoric farming impacts on freshwater lake systems. Chironomid subfossils, lake sediment geochemistry (δ13C, δ15N and C:N) and fossil pollen analyses were used in a comparative limnological assessment of three archaeologically rich study sites in County Sligo, Ireland. At all three study sites, pastoral farming and its associated nutrient inputs, as represented by non-arboreal pollen indicative of grassland/pasture (NAPp) and lake sediment geochemistry, were concomitant with increases in eutrophic chironomid taxa. Redundancy analysis (RDA) and partial RDAs established that δ15N and NAPp were controlling factors of chironomid community compositional change during the Neolithic (4000 - 2500 BC) and Bronze Age (2500 - 800/750 BC). Bronze Age farming had a considerably greater impact on the lake systems than Neolithic farming, as indicated by a higher proportion of eutrophic taxa and increases in δ15N, C:N and δ13C values, consistent with increased erosion and agricultural inputs. The timing and magnitude of change show that Neolithic and Bronze Age farming exhibited a strong control over chironomid communities at all three sites. Cultural eutrophication also led to the extirpation of several oligotrophic chironomid taxa present in the natural pre-impacted lake systems. In order to verify the importance of prehistoric agricultural influences on the human impacted lakes, an isolated high-elevation catchment was used as a control site to reconstruct chironomid and geochemical response to broad-scale environmental change, where the pollen record showed negligible human activity. Given the lack of prehistoric human influence on the control lake, the record was used to construct the first mid to late Holocene chironomid-inferred temperature (C-IT) record for Ireland, creating a climatic context for the development of Irish society during the Neolithic and Bronze Age. Findings from this PhD thesis provide valuable information about the timing, intensity and environmental impact of prehistoric farming in northwest Ireland.en_IE
dc.subjectChironomidsen_IE
dc.subjectPrehistoric farmingen_IE
dc.subjectNeolithicen_IE
dc.subjectBronze Ageen_IE
dc.subjectIrelanden_IE
dc.subjectStable isotopesen_IE
dc.subjectEutrophicationen_IE
dc.subjectChironomid-inferred temperature (C-IT)en_IE
dc.subjectMulti-proxyen_IE
dc.subjectGeographyen_IE
dc.titleChironomid response to prehistoric farming in northwest Irelanden_IE
dc.typeThesisen
dc.contributor.funderIRCSETen_IE
dc.contributor.funderHardiman Research Scholarship NUIGen_IE
dc.local.noteKaren’s research focuses on the ecological impact of prehistoric farming in Ireland, and specifically how prehistoric farming has impacted freshwater lake ecology. Recent projects also include the development of the first mid to late Holocene chironomid-inferred temperature record for Ireland, creating a valuable climatic context for the development of Irish society during the Neolithic and Bronze Age.en_IE
dc.description.embargo2019-03-06
dc.local.finalYesen_IE
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