Evaluating the use of testate amoebae for palaeohydrological reconstruction in permafrost peatlands

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Evaluating the use of testate amoebae for palaeohydrological reconstruction in permafrost peatlands. / Swindles, Graeme T.; Amesbury, Matthew J.; Turner, T. Edward; Carrivick, Jonathan L.; Woulds, Clare; Raby, Cassandra; Mullan, Donal; Roland, Thomas P.; Galloway, Jennifer M.; Parry, Lauren; Kokfelt, Ulla; Garneau, Michelle; Charman, Dan J.; Holden, Joseph.

I: Palaeogeography, Palaeoclimatology, Palaeoecology - An International Journal for the Geo-Sciences, Bind 424, 2015, s. 111-122.

Publikation: Bidrag til tidsskriftTidsskriftartikelForskningfagfællebedømt

Harvard

Swindles, GT, Amesbury, MJ, Turner, TE, Carrivick, JL, Woulds, C, Raby, C, Mullan, D, Roland, TP, Galloway, JM, Parry, L, Kokfelt, U, Garneau, M, Charman, DJ & Holden, J 2015, 'Evaluating the use of testate amoebae for palaeohydrological reconstruction in permafrost peatlands', Palaeogeography, Palaeoclimatology, Palaeoecology - An International Journal for the Geo-Sciences, bind 424, s. 111-122. https://doi.org/10.1016/j.palaeo.2015.02.004

APA

Swindles, G. T., Amesbury, M. J., Turner, T. E., Carrivick, J. L., Woulds, C., Raby, C., Mullan, D., Roland, T. P., Galloway, J. M., Parry, L., Kokfelt, U., Garneau, M., Charman, D. J., & Holden, J. (2015). Evaluating the use of testate amoebae for palaeohydrological reconstruction in permafrost peatlands. Palaeogeography, Palaeoclimatology, Palaeoecology - An International Journal for the Geo-Sciences, 424, 111-122. https://doi.org/10.1016/j.palaeo.2015.02.004

Vancouver

Swindles GT, Amesbury MJ, Turner TE, Carrivick JL, Woulds C, Raby C o.a. Evaluating the use of testate amoebae for palaeohydrological reconstruction in permafrost peatlands. Palaeogeography, Palaeoclimatology, Palaeoecology - An International Journal for the Geo-Sciences. 2015;424:111-122. https://doi.org/10.1016/j.palaeo.2015.02.004

Author

Swindles, Graeme T. ; Amesbury, Matthew J. ; Turner, T. Edward ; Carrivick, Jonathan L. ; Woulds, Clare ; Raby, Cassandra ; Mullan, Donal ; Roland, Thomas P. ; Galloway, Jennifer M. ; Parry, Lauren ; Kokfelt, Ulla ; Garneau, Michelle ; Charman, Dan J. ; Holden, Joseph. / Evaluating the use of testate amoebae for palaeohydrological reconstruction in permafrost peatlands. I: Palaeogeography, Palaeoclimatology, Palaeoecology - An International Journal for the Geo-Sciences. 2015 ; Bind 424. s. 111-122.

Bibtex

@article{79909c13e1dc45ce89aa699b12e40ab4,
title = "Evaluating the use of testate amoebae for palaeohydrological reconstruction in permafrost peatlands",
abstract = "The melting of high-latitude permafrost peatlands is a major concern due to a potential positive feedback on global climate change. We examine the ecology of testate amoebae in permafrost peatlands, based on sites in Sweden (similar to 200 km north of the Arctic Circle). Multivariate statistical analysis confirms that water-table depth and moisture content are the dominant controls on the distribution of testate amoebae, corroborating the results from studies in mid-latitude peatlands. We present a new testate amoeba-based water table transfer function and thoroughly test it for the effects of spatial autocorrelation, clustered sampling design and uneven sampling gradients. We find that the transfer function has good predictive power; the best-performing model is based on tolerance-downweighted weighted averaging with inverse deshrinking (performance statistics with leave-one-out cross validation: R-2 = 0.87, RMSEP = 5.25 cm). The new transfer function was applied to a short core from Stordalen mire, and reveals a major shift in peatland ecohydrology coincident with the onset of the Little Ice Age (c. AD 1400). We also applied the model to an independent contemporary dataset from Stordalen and find that it outperforms predictions based on other published transfer functions. The new transfer function will enable palaeohydrological reconstruction from permafrost peatlands in Northern Europe, thereby permitting greatly improved understanding of the long-term ecohydrological dynamics of these important carbon stores as well as their responses to recent climate change. (C) 2015 Elsevier B.V. All rights reserved.",
keywords = "Permafrost, Peatlands, Palaeohydrology, Testate amoebae, Transfer function, Arctic",
author = "Swindles, {Graeme T.} and Amesbury, {Matthew J.} and Turner, {T. Edward} and Carrivick, {Jonathan L.} and Clare Woulds and Cassandra Raby and Donal Mullan and Roland, {Thomas P.} and Galloway, {Jennifer M.} and Lauren Parry and Ulla Kokfelt and Michelle Garneau and Charman, {Dan J.} and Joseph Holden",
note = "CENPERM[2015]",
year = "2015",
doi = "10.1016/j.palaeo.2015.02.004",
language = "English",
volume = "424",
pages = "111--122",
journal = "Palaeogeography, Palaeoclimatology, Palaeoecology - An International Journal for the Geo-Sciences",
issn = "0031-0182",
publisher = "Elsevier",

}

RIS

TY - JOUR

T1 - Evaluating the use of testate amoebae for palaeohydrological reconstruction in permafrost peatlands

AU - Swindles, Graeme T.

AU - Amesbury, Matthew J.

AU - Turner, T. Edward

AU - Carrivick, Jonathan L.

AU - Woulds, Clare

AU - Raby, Cassandra

AU - Mullan, Donal

AU - Roland, Thomas P.

AU - Galloway, Jennifer M.

AU - Parry, Lauren

AU - Kokfelt, Ulla

AU - Garneau, Michelle

AU - Charman, Dan J.

AU - Holden, Joseph

N1 - CENPERM[2015]

PY - 2015

Y1 - 2015

N2 - The melting of high-latitude permafrost peatlands is a major concern due to a potential positive feedback on global climate change. We examine the ecology of testate amoebae in permafrost peatlands, based on sites in Sweden (similar to 200 km north of the Arctic Circle). Multivariate statistical analysis confirms that water-table depth and moisture content are the dominant controls on the distribution of testate amoebae, corroborating the results from studies in mid-latitude peatlands. We present a new testate amoeba-based water table transfer function and thoroughly test it for the effects of spatial autocorrelation, clustered sampling design and uneven sampling gradients. We find that the transfer function has good predictive power; the best-performing model is based on tolerance-downweighted weighted averaging with inverse deshrinking (performance statistics with leave-one-out cross validation: R-2 = 0.87, RMSEP = 5.25 cm). The new transfer function was applied to a short core from Stordalen mire, and reveals a major shift in peatland ecohydrology coincident with the onset of the Little Ice Age (c. AD 1400). We also applied the model to an independent contemporary dataset from Stordalen and find that it outperforms predictions based on other published transfer functions. The new transfer function will enable palaeohydrological reconstruction from permafrost peatlands in Northern Europe, thereby permitting greatly improved understanding of the long-term ecohydrological dynamics of these important carbon stores as well as their responses to recent climate change. (C) 2015 Elsevier B.V. All rights reserved.

AB - The melting of high-latitude permafrost peatlands is a major concern due to a potential positive feedback on global climate change. We examine the ecology of testate amoebae in permafrost peatlands, based on sites in Sweden (similar to 200 km north of the Arctic Circle). Multivariate statistical analysis confirms that water-table depth and moisture content are the dominant controls on the distribution of testate amoebae, corroborating the results from studies in mid-latitude peatlands. We present a new testate amoeba-based water table transfer function and thoroughly test it for the effects of spatial autocorrelation, clustered sampling design and uneven sampling gradients. We find that the transfer function has good predictive power; the best-performing model is based on tolerance-downweighted weighted averaging with inverse deshrinking (performance statistics with leave-one-out cross validation: R-2 = 0.87, RMSEP = 5.25 cm). The new transfer function was applied to a short core from Stordalen mire, and reveals a major shift in peatland ecohydrology coincident with the onset of the Little Ice Age (c. AD 1400). We also applied the model to an independent contemporary dataset from Stordalen and find that it outperforms predictions based on other published transfer functions. The new transfer function will enable palaeohydrological reconstruction from permafrost peatlands in Northern Europe, thereby permitting greatly improved understanding of the long-term ecohydrological dynamics of these important carbon stores as well as their responses to recent climate change. (C) 2015 Elsevier B.V. All rights reserved.

KW - Permafrost

KW - Peatlands

KW - Palaeohydrology

KW - Testate amoebae

KW - Transfer function

KW - Arctic

U2 - 10.1016/j.palaeo.2015.02.004

DO - 10.1016/j.palaeo.2015.02.004

M3 - Journal article

VL - 424

SP - 111

EP - 122

JO - Palaeogeography, Palaeoclimatology, Palaeoecology - An International Journal for the Geo-Sciences

JF - Palaeogeography, Palaeoclimatology, Palaeoecology - An International Journal for the Geo-Sciences

SN - 0031-0182

ER -

ID: 140717690