Topographical shifts in fine root lifespan in a mixed, mesic temperate forest.

Root lifespan, often is estimated in landscape- and ecosystem-level carbon models using linear approximations. In water manipulation experiments, fine root lifespan can vary with soil water content. Soil water content is generally structured by complex topography, which is largely unaccounted for in...

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Autores principales: Edward J Primka, Thomas S Adams, Alexandra Buck, David M Eissenstat
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Publicado: Public Library of Science (PLoS) 2021
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Acceso en línea:https://doaj.org/article/10dd1bbc6469480791557b9d632d19ec
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spelling oai:doaj.org-article:10dd1bbc6469480791557b9d632d19ec2021-12-02T20:07:00ZTopographical shifts in fine root lifespan in a mixed, mesic temperate forest.1932-620310.1371/journal.pone.0254672https://doaj.org/article/10dd1bbc6469480791557b9d632d19ec2021-01-01T00:00:00Zhttps://doi.org/10.1371/journal.pone.0254672https://doaj.org/toc/1932-6203Root lifespan, often is estimated in landscape- and ecosystem-level carbon models using linear approximations. In water manipulation experiments, fine root lifespan can vary with soil water content. Soil water content is generally structured by complex topography, which is largely unaccounted for in landscape- and ecosystem-scale carbon models. Topography governs the range of soil water content experienced by roots which may impact their lifespan. We hypothesized that root lifespan varied nonlinearly across a temperate, mesic, forested catchment due to differences in soil water content associated with topographic position. We expected regions of the landscape that were too wet or too dry would have soils that were not optimal for roots and thus result in shorter root lifespans. Specifically, we hypothesized that root lifespan would be longest in areas that consistently had soil water content in the middle of the soil water content spectrum, while in soils at either very low or very high soil water content, root lifespan would be relatively short. We tested this hypothesis by collecting and analyzing two years of minirhizotron and soil moisture data in plots widely distributed in the Shale Hills catchment of the Susquehanna-Shale Hills Critical Zone Observatory in Pennsylvania. We found that fine root lifespans were longer in traditionally wetter topographic regions, but detected no short term (biweekly) effect of soil moisture on root lifespan. Additionally, depth in soil, soil series, slope face orientation, and season of birth strongly affected root lifespans across the catchment. In contrast, lifespan was unaffected by root diameter or mycorrhizal association. Failure to account for these variables could result in erroneous estimates of fine root lifespan and, consequentially, carbon flux in temperate forested regions.Edward J PrimkaThomas S AdamsAlexandra BuckDavid M EissenstatPublic Library of Science (PLoS)articleMedicineRScienceQENPLoS ONE, Vol 16, Iss 7, p e0254672 (2021)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Edward J Primka
Thomas S Adams
Alexandra Buck
David M Eissenstat
Topographical shifts in fine root lifespan in a mixed, mesic temperate forest.
description Root lifespan, often is estimated in landscape- and ecosystem-level carbon models using linear approximations. In water manipulation experiments, fine root lifespan can vary with soil water content. Soil water content is generally structured by complex topography, which is largely unaccounted for in landscape- and ecosystem-scale carbon models. Topography governs the range of soil water content experienced by roots which may impact their lifespan. We hypothesized that root lifespan varied nonlinearly across a temperate, mesic, forested catchment due to differences in soil water content associated with topographic position. We expected regions of the landscape that were too wet or too dry would have soils that were not optimal for roots and thus result in shorter root lifespans. Specifically, we hypothesized that root lifespan would be longest in areas that consistently had soil water content in the middle of the soil water content spectrum, while in soils at either very low or very high soil water content, root lifespan would be relatively short. We tested this hypothesis by collecting and analyzing two years of minirhizotron and soil moisture data in plots widely distributed in the Shale Hills catchment of the Susquehanna-Shale Hills Critical Zone Observatory in Pennsylvania. We found that fine root lifespans were longer in traditionally wetter topographic regions, but detected no short term (biweekly) effect of soil moisture on root lifespan. Additionally, depth in soil, soil series, slope face orientation, and season of birth strongly affected root lifespans across the catchment. In contrast, lifespan was unaffected by root diameter or mycorrhizal association. Failure to account for these variables could result in erroneous estimates of fine root lifespan and, consequentially, carbon flux in temperate forested regions.
format article
author Edward J Primka
Thomas S Adams
Alexandra Buck
David M Eissenstat
author_facet Edward J Primka
Thomas S Adams
Alexandra Buck
David M Eissenstat
author_sort Edward J Primka
title Topographical shifts in fine root lifespan in a mixed, mesic temperate forest.
title_short Topographical shifts in fine root lifespan in a mixed, mesic temperate forest.
title_full Topographical shifts in fine root lifespan in a mixed, mesic temperate forest.
title_fullStr Topographical shifts in fine root lifespan in a mixed, mesic temperate forest.
title_full_unstemmed Topographical shifts in fine root lifespan in a mixed, mesic temperate forest.
title_sort topographical shifts in fine root lifespan in a mixed, mesic temperate forest.
publisher Public Library of Science (PLoS)
publishDate 2021
url https://doaj.org/article/10dd1bbc6469480791557b9d632d19ec
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