2011
DOI: 10.1179/jwa.2011.11.1.63
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Early Mesolithic Activity in the Wetlands of the Lake Flixton Basin

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Cited by 15 publications
(23 citation statements)
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“…However this record does not continue later than ca 10,000 cal bp and only extends ca 10 m into the lake. A more spatially extensive record was established by the author at Flixton School House Farm (henceforth Flixton SHF), where plant macrofossil analysis was carried out on samples from two cores, one at the former lake edge and the other 50 m into the basin (Taylor 2011). Again, however, this provides no information on the timing and character of wetland succession in the deeper parts of the lake during the late Mesolithic.…”
Section: Electronic Supplementary Materialsmentioning
confidence: 99%
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“…However this record does not continue later than ca 10,000 cal bp and only extends ca 10 m into the lake. A more spatially extensive record was established by the author at Flixton School House Farm (henceforth Flixton SHF), where plant macrofossil analysis was carried out on samples from two cores, one at the former lake edge and the other 50 m into the basin (Taylor 2011). Again, however, this provides no information on the timing and character of wetland succession in the deeper parts of the lake during the late Mesolithic.…”
Section: Electronic Supplementary Materialsmentioning
confidence: 99%
“…The lake formed at the start of the Late-glacial interstadial (ca 14,600 ka cal bp) and gradually in-filled with calcareous and organic sediments that preserved a rich record of both the human and environmental history of the landscape (e.g. Clark 1954;Walker and Godwin 1954;Mellars and Dark 1998;Conneller and Schadla-Hall 2003;Taylor 2011;Milner et al 2018). The area is best known for the early Mesolithic site of Star Carr where a large assemblage of bone and antler artefacts, faunal remains and worked flint were recovered from sediments at the former lake edge (Clark 1954).…”
Section: Introductionmentioning
confidence: 99%
“…Within the woodland were small ponds, fringed with reeds and willow (Taylor 2012), and a shifting pattern of clearings created through ongoing processes such as windfall and animal action (Cummins 2003). At the lake shore, birch grew amongst aspen and willow, creating dense thickets in some places, whilst a suite of shrubs and fen plants thrived in areas with reduced tree cover (Taylor 2011(Taylor , 2012. Within the lake, extensive beds of swamp vegetation were growing in the areas of shallower water, filling many of the Fig.…”
Section: Aurochs Hunting Around the Palaeo-lake Flixtonmentioning
confidence: 99%
“…3 Aurochs remains from Flixton School House Farm, demonstrating the over-abundance of ribs, and the original location of the pelvis fragment. Note the morphological variation of the rib heads, indicating they originated from both the anterior and posterior portions of the rib cage (Conneller and Overton 2018) small embayments around the edges of the basin, whilst aquatic plants grew in the deeper water beyond (Taylor 2011(Taylor , 2012. A range of animal species also inhabited this landscape, including large mammals such as elk, red and roe deer, and wild boar; predators such as wolf and fox; and smaller mammals such as beaver, pine marten, and squirrel (Clark 1954).…”
Section: Aurochs Hunting Around the Palaeo-lake Flixtonmentioning
confidence: 99%
“…As such, the area would have been dry enough to allow in-situ activity during the summer months, when the site was inhabited, but would have been submerged during other times of the year (ibid). Alternatively, Taylor (2011) has argued that the assemblage actually spans a range of environments based on the results of environmental analysis at other parts of the basin (ibid: 80). By calculating minimum level for the lake, Taylor argued that deposition began in shallow standing water close to the lake shore, but continued into increasingly more terrestrialised environments as the wetlands developed (ibid:78-9).…”
Section: Changing Interpretation Of the Area Investigated By Clarkmentioning
confidence: 99%