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dc.contributor.authorSwindles, GT
dc.contributor.authorReczuga, M
dc.contributor.authorLamentowicz, M
dc.contributor.authorRaby, CL
dc.contributor.authorTurner, TE
dc.contributor.authorCharman, Dan J.
dc.contributor.authorGallego-Sala, Angela V.
dc.contributor.authorValderrama, E
dc.contributor.authorWilliams, C
dc.contributor.authorDraper, F
dc.contributor.authorHonorio Coronado, EN
dc.contributor.authorRoucoux, KH
dc.contributor.authorBaker, Tim
dc.contributor.authorMullan, DJ
dc.date.accessioned2015-04-16T11:40:01Z
dc.date.issued2014-04-02
dc.description.abstractTropical peatlands represent globally important carbon sinks with a unique biodiversity and are currently threatened by climate change and human activities. It is now imperative that proxy methods are developed to understand the ecohydrological dynamics of these systems and for testing peatland development models. Testate amoebae have been used as environmental indicators in ecological and palaeoecological studies of peatlands, primarily in ombrotrophic Sphagnum-dominated peatlands in the mid- and high-latitudes. We present the first ecological analysis of testate amoebae in a tropical peatland, a nutrient-poor domed bog in western (Peruvian) Amazonia. Litter samples were collected from different hydrological microforms (hummock to pool) along a transect from the edge to the interior of the peatland. We recorded 47 taxa from 21 genera. The most common taxa are Cryptodifflugia oviformis, Euglypha rotunda type, Phryganella acropodia, Pseudodifflugia fulva type and Trinema lineare. One species found only in the southern hemisphere, Argynnia spicata, is present. Arcella spp., Centropyxis aculeata and Lesqueresia spiralis are indicators of pools containing standing water. Canonical correspondence analysis and non-metric multidimensional scaling illustrate that water table depth is a significant control on the distribution of testate amoebae, similar to the results from mid- and high-latitude peatlands. A transfer function model for water table based on weighted averaging partial least-squares (WAPLS) regression is presented and performs well under cross-validation (rapparent = 0.76, RMSE = 4.29; r2jack = 0.68, RMSEP = 5.18). The transfer function was applied to a 1-m peat core, and sample-specific reconstruction errors were generated using bootstrapping. The reconstruction generally suggests near-surface water tables over the last 3,000 years, with a shift to drier conditions at c. cal. 1218-1273 AD. © 2014 Springer Science+Business Media New York.en_GB
dc.description.sponsorshipRoyal Societyen_GB
dc.identifier.citationVol. 68, Iss. 2 pp. 284 - 298en_GB
dc.identifier.doi10.1007/s00248-014-0378-5
dc.identifier.grantnumber481831en_GB
dc.identifier.urihttp://hdl.handle.net/10871/16840
dc.language.isoenen_GB
dc.publisherSpringer New York LLCen_GB
dc.relation.urlhttp://link.springer.com/article/10.1007%2Fs00248-014-0378-5en_GB
dc.titleEcology of Testate Amoebae in an Amazonian Peatland and Development of a Transfer Function for Palaeohydrological Reconstructionen_GB
dc.typeArticleen_GB
dc.date.available2015-04-16T11:40:01Z
dc.identifier.issn0095-3628
dc.descriptionJournal Articleen_GB
dc.descriptionCopyright © 2014 Springer International Publishing AGen_GB
dc.descriptionAuthor’s accepted version. The final publication is available at Springer via http://dx.doi.org/ 10.1007/s00248-014-0378-5en_GB
dc.identifier.journalMicrobial Ecologyen_GB


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