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Ecosystem state shifts during long-term development of an Amazonian peatland

Research output: Contribution to journalArticle

  • Graeme T. Swindles
  • Paul J. Morris
  • Bronwen Whitney
  • Jennifer M. Galloway
  • Mariusz Gałka
  • Angela Gallego-Sala
  • Andrew L. Macumber
  • Donal Mullan
  • Mark W. Smith
  • Matthew J. Amesbury
  • Thomas P. Roland
  • Hamed Sanei
  • R. Timothy Patterson
  • Nicole Sanderson
  • Lauren Parry
  • Dan J. Charman
  • Omar Lopez
  • Elvis Valderamma
  • Elizabeth J. Watson
  • Ruza F. Ivanovic
  • Paul J. Valdeshttp://orcid.org/0000-0002-1902-3283
  • T. Edward Turner
  • Outi Lähteenoja
Original languageEnglish
Pages (from-to)738-757
Number of pages20
JournalGlobal Change Biology
Volume24
Issue number2
Early online date1 Dec 2017
DOIs
DateAccepted/In press - 8 Oct 2017
DateE-pub ahead of print - 1 Dec 2017
DatePublished (current) - 1 Feb 2018

Abstract

The most carbon (C)-dense ecosystems of Amazonia are areas characterized by the presence of peatlands. However, Amazonian peatland ecosystems are poorly understood and are threatened by human activities. Here, we present an investigation into long-term ecohydrological controls on C accumulation in an Amazonian peat dome. This site is the oldest peatland yet discovered in Amazonia (peat initiation ca. 8.9 ka BP), and developed in three stages: (i) peat initiated in an abandoned river channel with open water and aquatic plants; (ii) inundated forest swamp; and (iii) raised peat dome (since ca. 3.9 ka BP). Local burning occurred at least three times in the past 4,500 years. Two phases of particularly rapid C accumulation (ca. 6.6–6.1 and ca. 4.9–3.9 ka BP), potentially resulting from increased net primary productivity, were seemingly driven by drier conditions associated with widespread drought events. The association of drought phases with major ecosystem state shifts (open water wetland–forest swamp–peat dome) suggests a potential climatic control on the developmental trajectory of this tropical peatland. A third drought phase centred on ca. 1.8–1.1 ka BP led to markedly reduced C accumulation and potentially a hiatus during the peat dome stage. Our results suggest that future droughts may lead to phases of rapid C accumulation in some inundated tropical peat swamps, although this can lead ultimately to a shift to ombrotrophy and a subsequent return to slower C accumulation. Conversely, in ombrotrophic peat domes, droughts may lead to reduced C accumulation or even net loss of peat. Increased surface wetness at our site in recent decades may reflect a shift towards a wetter climate in western Amazonia. Amazonian peatlands represent important carbon stores and habitats, and are important archives of past climatic and ecological information. They should form key foci for conservation efforts.

    Research areas

  • Amazon rainforest, carbon accumulation, climate, Holocene, palaeoecology, peat, Peru, swamp, tropical peatland

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