2007
DOI: 10.1080/01433768.2007.10594588
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Reading the pastoral landscape: palynological and historical evidence for the impacts of long-term grazing on Wether Hill, Ingram, Northumberland

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Cited by 15 publications
(14 citation statements)
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“…These findings show that over the long run, human-induced biodiversity change was significant for these sites. While the analytical methods applied here are novel, the results support previous documentary and palaeoecological evidence for some deterioration in the quality or diversity of the UK uplands around 200-300 years ago, particularly post-1850 [17], [41], [42], [46]. That increases in grazing rates can lead to decreases in biodiversity in the uplands is well-recognised in contemporary ecological studies [28], [34], [44], [45].…”
Section: Discussionsupporting
confidence: 72%
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“…These findings show that over the long run, human-induced biodiversity change was significant for these sites. While the analytical methods applied here are novel, the results support previous documentary and palaeoecological evidence for some deterioration in the quality or diversity of the UK uplands around 200-300 years ago, particularly post-1850 [17], [41], [42], [46]. That increases in grazing rates can lead to decreases in biodiversity in the uplands is well-recognised in contemporary ecological studies [28], [34], [44], [45].…”
Section: Discussionsupporting
confidence: 72%
“…Paleoecological analysis has been combined with both archaeological techniques [17], [39] and historical sources [21], [46], [47] to understand the environmental impacts of human land use.…”
mentioning
confidence: 99%
“…In common with previous studies, changing grazing and burning regimes are likely to be the main mechanisms for heather and grass expansion in this study, possibly interacting with drainage and the deposition of atmospheric pollution (Chambers et al 2007a;Davies and Dixon 2007;Stevenson and Rhodes 2000;Yeloff et al 2006). However, interpretation of grazing proxies is by no means straightforward since pollen indicators (Behre 1981) and CFS values show similar trends at some sites and times, but contrasting relationships at others.…”
Section: Late Holocene Moorland Dynamicsmentioning
confidence: 52%
“…These features indicate an increase in the range of variability, extent and pace of turnover. The shifts occurred across a range of communities, from 'degraded' grassmoor on eroding and uneroded blanket peat (Bar Brook, Withens Moor; Chambers et al 1999Chambers et al , 2007aChambers et al , 2013Hicks 1971;Yeloff et al 2006), to fen peats (Cranberry Bed), drier moors (Davies and Dixon 2007;Tipping 2000), and 'high conservation value' heather moorland (Emlin Dike; Stevenson and Thompson 1993).…”
Section: Moorland Regime Shift and Conservation Implicationsmentioning
confidence: 99%
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