A palaeoecological and archaeological analysis of plant macrofossils from monolith 4A800B3-6 at L’Anse aux Meadows, Newfoundland
Peatlands are excellent foci of study due to their ability to act as archives of palaeoecological and archaeological proxy data, as the organic materials which constitute such data do not readily decompose within these waterlogged and acidic environments. Proxy data can be analyzed to discern how pe...
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Format: | Thesis |
Language: | English |
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Memorial University of Newfoundland
2022
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Online Access: | https://research.library.mun.ca/15833/ https://research.library.mun.ca/15833/3/converted.pdf |
Summary: | Peatlands are excellent foci of study due to their ability to act as archives of palaeoecological and archaeological proxy data, as the organic materials which constitute such data do not readily decompose within these waterlogged and acidic environments. Proxy data can be analyzed to discern how peatlands came to form through internal and external processes. Both natural and cultural (i.e., anthropogenic) forces are important external influences upon peatland formation. This study seeks to discern how a peat bog area at the archaeological site of L’Anse aux Meadows, Newfoundland formed as a result of natural successional processes and anthropogenic disturbance. This is accomplished through the use of a high temporal resolution (sub-centimetre) plant macrofossil analysis and radiocarbon age-depth modelling undertaken on a monolith (4A800B3-6) retrieved from a peat bog close to the main settlement terrace at the site. Through the application of this method, it is found that human-mediated disturbance (fire and trampling) and biophysical drivers (climate) each played a role in forming the peat sequence. Several different possibilities are offered for which particular cultural groups might be behind the disturbances in the peatland—which include the Norse but also Indigenous groups. |
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