TY - JOUR
T1 - Widespread drying of European peatlands in recent centuries
AU - Swindles, Graeme T.
AU - Morris, Paul J.
AU - Mullan, Donal J.
AU - Payne, Richard J.
AU - Roland, Thomas P.
AU - Amesbury, Matthew J.
AU - Lamentowicz, Mariusz
AU - Turner, T. Edward
AU - Gallego-Sala, Angela
AU - Sim, Thomas
AU - Barr, Iestyn D.
AU - Blaauw, Maarten
AU - Blundell, Antony
AU - Chambers, Frank M.
AU - Charman, Dan J.
AU - Feurdean, Angelica
AU - Galloway, Jennifer M.
AU - Gałka, Mariusz
AU - Green, Sophie M.
AU - Kajukało, Katarzyna
AU - Karofeld, Edgar
AU - Korhola, Atte
AU - Lamentowicz, Łukasz
AU - Langdon, Peter
AU - Marcisz, Katarzyna
AU - Mauquoy, Dmitri
AU - Mazei, Yuri A.
AU - McKeown, Michelle M.
AU - Mitchell, Edward A.D.
AU - Novenko, Elena
AU - Plunkett, Gill
AU - Roe, Helen M.
AU - Schoning, Kristian
AU - Sillasoo, Ülle
AU - Tsyganov, Andrey N.
AU - van der Linden, Marjolein
AU - Väliranta, Minna
AU - Warner, Barry
N1 - © Crown 2019. This is an author-produced version of the published paper. Uploaded in accordance with the publisher’s self-archiving policy. Further copying may not be permitted; contact the publisher for details.
PY - 2019/10/21
Y1 - 2019/10/21
N2 - Climate warming and human impacts are thought to be causing peatlands to dry, potentially converting them from sinks to sources of carbon. However, it is unclear whether the hydrological status of peatlands has moved beyond their natural envelope. Here we show that European peatlands have undergone substantial, widespread drying during the last ~300 years. We analyse testate amoeba-derived hydrological reconstructions from 31 peatlands across Britain, Ireland, Scandinavia and Continental Europe to examine changes in peatland surface wetness during the last 2,000 years. We find that 60% of our study sites were drier during the period 1800–2000 ce than they have been for the last 600 years, 40% of sites were drier than they have been for 1,000 years and 24% of sites were drier than they have been for 2,000 years. This marked recent transition in the hydrology of European peatlands is concurrent with compound pressures including climatic drying, warming and direct human impacts on peatlands, although these factors vary among regions and individual sites. Our results suggest that the wetness of many European peatlands may now be moving away from natural baselines. Our findings highlight the need for effective management and restoration of European peatlands.
AB - Climate warming and human impacts are thought to be causing peatlands to dry, potentially converting them from sinks to sources of carbon. However, it is unclear whether the hydrological status of peatlands has moved beyond their natural envelope. Here we show that European peatlands have undergone substantial, widespread drying during the last ~300 years. We analyse testate amoeba-derived hydrological reconstructions from 31 peatlands across Britain, Ireland, Scandinavia and Continental Europe to examine changes in peatland surface wetness during the last 2,000 years. We find that 60% of our study sites were drier during the period 1800–2000 ce than they have been for the last 600 years, 40% of sites were drier than they have been for 1,000 years and 24% of sites were drier than they have been for 2,000 years. This marked recent transition in the hydrology of European peatlands is concurrent with compound pressures including climatic drying, warming and direct human impacts on peatlands, although these factors vary among regions and individual sites. Our results suggest that the wetness of many European peatlands may now be moving away from natural baselines. Our findings highlight the need for effective management and restoration of European peatlands.
UR - http://www.scopus.com/inward/record.url?scp=85074561623&partnerID=8YFLogxK
U2 - 10.1038/s41561-019-0462-z
DO - 10.1038/s41561-019-0462-z
M3 - Article
AN - SCOPUS:85074561623
SN - 1752-0894
VL - 12
SP - 922
EP - 928
JO - Nature Geoscience
JF - Nature Geoscience
ER -