Abstract

Large areas of upland mire and moorland in Northwest Europe are regarded as degraded, not actively peat-forming, and releasing carbon. Conservation agencies have short-term targets to restore such areas, but often have no clear knowledge of the timing and nature of degradation. It has been suggested that palaeoecology can be used to inform conservation management about past vegetation states, so as to help identify feasible restoration targets. Our research study in northern England, commissioned by the national statutory conservation agency, applied multiple palaeoecological techniques to establish the vegetation history of several mire and moorland sites, specifically to ascertain the nature and timing of degradation. Techniques applied included pollen analysis, plant macrofossil and charcoal analyses, determination of peat humification and mineral magnetic susceptibility, with ages ascertained using spheroidal carbonaceous particle analysis, 210Pb and 14C dating. Data are presented from case-study sites in the North York Moors, North- and South Pennines to illustrate how palaeoecology can extend long-term monitoring and guide conservation management. Palaeoecological data from a site within a National Nature Reserve, subject to exceptionally long-term (half-centennial) ecological monitoring, showed that this period does not include its pre-degradation state and that its current valued vegetation is novel and may have established after major fire. Overall, the studies suggest that the principal vegetation change at the sites took place after the start of the Industrial Revolution, and that the current landscape appearance not only has no long history, but that valued aspects, such as extensive heather moorland, feature only recently in the cultural landscape. These findings pose challenging questions for conservation management. We offer a non-specialist guide to the palaeoecological techniques that considers level of skill, cost, and comparability with ecological aspects of conservation and monitoring interest. We suggest palaeoecological data can provide valuable information and insights to aid practical conservation. While mires are particularly suitable, palaeoecological techniques could be applied in many other degraded landscapes internationally.

Highlights

  • Restoration of degraded ecosystems varies from re-vegetating areas void of vegetation as a result of strip mining, to encouraging selected species in tracts whose vegetation is depleted as a result of one or a range of causative factors

  • The studies suggest that the principal vegetation change at the sites took place after the start of the Industrial Revolution, and that the current landscape appearance has no long history, but that valued aspects, such as extensive heather moorland, feature only recently in the cultural landscape

  • The two from the North York Moors were from May Moss, adjacent to the Early Warning Station at RAF Fylingdales, from a relatively intact area of peatland; that from Egglestone Common was from an extensive area of relatively depauperate moorland; the relatively deep peat profile from Valley Bog, Moor House National Nature Reserve (NNR) was in extensive heather moorland; that from Blackstone Edge Moor was from an intact, relatively dry-surfaced upstanding hagg of peat in partly eroded peatland

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Summary

Introduction

Restoration of degraded ecosystems varies from re-vegetating areas void of vegetation as a result of strip mining, to encouraging selected species in tracts whose vegetation is depleted as a result of one or a range of causative factors. Both initial states are possible for degraded peatlands. Continued cultural effects over centuries, and/or sudden, major changes to cultural practice may result in these mires being in at least a partly degraded state This degradation is often, but not always, more pronounced in areas close to major human habitation or industry

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