Drivers of peatland water table dynamics in the central Andes, Bolivia and Peru

David J. Cooper, Jeremy Sueltenfuss, Eduardo Oyague, Karina Yager, Daniel Slayback, E. Marcelo Cabero Caballero, Jaime Argollo, Bryan G. Mark

Research output: Contribution to journalArticlepeer-review

14 Scopus citations

Abstract

Cushion plant dominated peatlands are key ecosystems in tropical alpine regions of the Andes in South America. The cushion plants have formed peat bodies over thousands of years that fill many valley bottoms, and the forage produced by the plants is critical for native and nonnative domesticated mammals. The sources and flow paths of water supporting these peatlands remain largely unknown. Some studies have suggested that glacier meltwater streams support some peatlands, and that the ongoing loss of glaciers and their meltwaters could lead to the loss or diminishment of peatlands. We analysed the hydrologic regime of 10 peatlands in four mountain regions of Bolivia and Peru using groundwater monitoring. Groundwater levels in peatlands were relatively stable and within 20 cm of the ground surface during the rainy season, and many sites had water tables 40–90 cm below the ground surface in the dry season. Topographic and groundwater elevations in the peatlands demonstrated that the water source of all 10 peatlands was hillslope groundwater flowing from lateral moraines, talus, colluvium, or bedrock aquifers into the peatlands. There was little to no input from streams, whether derived from glacier melt or other sources, and glacier melt could not have recharged the hillslope aquifers supporting peatlands. We measured the stable water isotopes in water samples taken during different seasons, distributed throughout the catchments, and the values are consistent with this interpretation. Our findings indicate that peatlands in the study region are recharged by hillslope groundwater discharge rather than stream water and may not be as vulnerable to glacial decline as other studies have indicated. However, both glaciers and peatlands are susceptible to changing thermal and precipitation regimes that could affect the persistence of peatlands.

Original languageEnglish
Pages (from-to)1913-1925
Number of pages13
JournalHydrological Processes
Volume33
Issue number13
DOIs
StatePublished - 30 Jun 2019

Bibliographical note

Funding Information:
Research in Bolivia was funded by a NASA LCLUC (Land‐Cover Land‐ Use Change) program grant (09‐LCLUC09‐2‐74). Research in Central Peru was partially funded by Nor Yauyos‐Cochas Landscape Reserve Patronage (Patronato de la Reserva Paisajística Nor Yauyos‐Cochas), and we thank Carmela Landeo and Niskar Peña for their help. Research in Southern Perú (Vilcanota Range) was funded by Amazon Conservation Association (ACA, FWS Bofedales Project), we thank Efraín Samochuallpa from ACA‐Cusco and Mariana Vedoveto from ACA‐Washington for their help.

Funding Information:
Research in Bolivia was funded by a NASA LCLUC (Land-Cover Land-Use Change) program grant (09-LCLUC09-2-74). Research in Central Peru was partially funded by Nor Yauyos-Cochas Landscape Reserve Patronage (Patronato de la Reserva Paisajística Nor Yauyos-Cochas), and we thank Carmela Landeo and Niskar Peña for their help. Research in Southern Perú (Vilcanota Range) was funded by Amazon Conservation Association (ACA, FWS Bofedales Project), we thank Efraín Samochuallpa from ACA-Cusco and Mariana Vedoveto from ACA-Washington for their help.

Publisher Copyright:
© 2019 John Wiley & Sons, Ltd.

Keywords

  • bofedale
  • fen
  • glaciers
  • groundwater
  • hydrology
  • mountain
  • peatland

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