Correction To: Testing the Moss Layer Transfer Technique on Mineral Well Pads Constructed in Peatlands

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Correction To: Testing the Moss Layer Transfer Technique on Mineral Well Pads Constructed in Peatlands Wetlands Ecol Manage (2018) 26:489–490 https://doi.org/10.1007/s11273-018-9608-9 CORRECTION Correction to: Testing the moss layer transfer technique on mineral well pads constructed in peatlands Marie-Eve Gauthier . Line Rochefort . Leonie Nadeau . Sandrine Hugron . Bin Xu Published online: 28 May 2018 Ó Springer Science+Business Media B.V., part of Springer Nature 2018 Correction to: Wetlands Ecol Manage https://doi.org/10.1007/s11273-017-9532-4 In the original publication, the Table 1 was published incorrectly. The correct version of Table 1 is given in this correction. The original article has been corrected. The original article can be found online at https:// doi.org/10.1007/s11273-017-9532-4. M.-E. Gauthier Á L. Rochefort (&) Á S. Hugron Department of Plant Sciences and Centre for Northern Studies, Universite´ Laval, Que´bec, QC G1V 0A6, Canada e-mail: [email protected] L. Nadeau Á B. Xu NAIT Boreal Research Institute, Peace River, AB T8S 1R2, Canada 123 490 Wetlands Ecol Manage (2018) 26:489–490 Table 1 Description of fen plant communities used as source of propagules (donor sites) for the moss layer transfer experiment Treed Rich Fen Cover Shrubby Rich Fen Cover Plant composition Trees Picea mariana 10 – Shrubs Vaccinium vitis-idaea 12 Salix spp. 15 Larix laricina 9 Betula glandulosa 2 Chamaedaphne calyculata 8 Empetrum nigrum 4 Rhododendron groenlandicum 4 Salix spp. 4 Herbs Carex aquatilis 3 Carex aquatilis 7 Carex tenuiflora * Comarum palustre 2 Carex magellanica ssp. irrigua 1 Mosses Sphagum fuscum 55 Sphagnum angustifolium 30 Aulacomnium palustre 3 Tomentypnum nitens 15 Aulacomnium palustre 3 Water chem. pH 5.7 6.9 EC (lScm-1) 190 98 Ca (mg l-1)17 12 Water table (cm) - 22.0 ± 3.2 - 7.0 ± 3.0 Cover is in % and * = presence. Water table depth was measured five times (n = 5) during the summer, the data presented is the average ± SD 123.
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