Carbon balance of UK peatlands: current state of knowledge and future research challenges

被引:133
作者
Billett, M. F. [1 ]
Charman, D. J. [2 ]
Clark, J. M. [3 ]
Evans, C. D.
Evans, M. G. [4 ]
Ostle, N. J. [5 ]
Worrall, F. [6 ]
Burden, A.
Dinsmore, K. J. [1 ]
Jones, T.
McNamara, N. P. [5 ]
Parry, L. [2 ]
Rowson, J. G. [6 ]
Rose, R. [5 ]
机构
[1] Ctr Ecol & Hydrol, Penicuik EH26 0QB, Midlothian, Scotland
[2] Univ Exeter, Sch Geog, Exeter EX4 4QJ, Devon, England
[3] Bangor Univ, Sch Biol Sci, Wolfson Carbon Capture Lab, Bangor LL57 2UW, Gwynedd, Wales
[4] Univ Manchester, Sch Environm & Dev, Dept Geog, Manchester M13 9PL, Lancs, England
[5] Ctr Ecol & Hydrol, Lancaster LA1 4AP, England
[6] Univ Durham, Sci Labs, Dept Earth Sci, Durham DH1 3LE, England
基金
英国自然环境研究理事会;
关键词
Carbon; Peatland; Peat; DOC; Flux; Aquatic; DISSOLVED ORGANIC-CARBON; HOLOCENE LATERAL EXPANSION; WATER-TABLE; ATMOSPHERIC DEPOSITION; SOUTHERN PENNINES; PEAT CATCHMENTS; GULLY EROSION; BLANKET BOG; ACCUMULATION; DIOXIDE;
D O I
10.3354/cr00903
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The retention of peatland carbon (C) and the ability to continue to draw down and store C from the atmosphere is not only important for the UK terrestrial carbon inventory, but also for a range of ecosystem services, the landscape value and the ecology and hydrology of similar to 15% of the land area of the UK. Here we review the current state of knowledge on the C balance of UK peatlands using several studies which highlight not only the importance of making good flux measurements, but also the spatial and temporal variability of different flux terms that characterise a landscape affected by a range of natural and anthropogenic processes and threats. Our data emphasise the importance of measuring (or accurately estimating) all components of the peatland C budget. We highlight the role of the aquatic pathway and suggest that fluxes are higher than previously thought. We also compare the contemporary C balance of several UK peatlands with historical rates of C accumulation measured using peat cores, thus providing a long-term context for present-day measurements and their natural year-on-year variability. Contemporary measurements from 2 sites suggest that current accumulation rates (-56 to -72 g C m(-2) yr(-1)) are at the lower end of those seen over the last 150 yr in peat cores (-35 to -209 g C m(-2) yr(-1)). Finally, we highlight significant current gaps in knowledge and identify where levels of uncertainty are high, as well as emphasise the research challenges that need to be addressed if we are to improve the measurement and prediction of change in the peatland C balance over future decades.
引用
收藏
页码:13 / 29
页数:17
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