Long‐term insect herbivory slows soil development in an arid ecosystem

Although herbivores are well known to alter litter inputs and soil nutrient fluxes, their long‐term influences on soil development are largely unknown because of the difficulty of detecting and attributing changes in carbon and nutrient pools against large background levels. The early phase of prima...

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Main Authors: Aimee T. Classen, Samantha K. Chapman, Thomas G. Whitham, Stephen C. Hart, George W. Koch
Format: Article
Language:English
Published: Wiley 2013-05-01
Series:Ecosphere
Subjects:
Online Access:https://doi.org/10.1890/ES12-00411.1
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author Aimee T. Classen
Samantha K. Chapman
Thomas G. Whitham
Stephen C. Hart
George W. Koch
author_facet Aimee T. Classen
Samantha K. Chapman
Thomas G. Whitham
Stephen C. Hart
George W. Koch
author_sort Aimee T. Classen
collection DOAJ
description Although herbivores are well known to alter litter inputs and soil nutrient fluxes, their long‐term influences on soil development are largely unknown because of the difficulty of detecting and attributing changes in carbon and nutrient pools against large background levels. The early phase of primary succession reduces this signal‐to‐noise problem, particularly in arid systems where individual plants can form islands of fertility. We used natural variation in tree‐resistance to herbivory, and a 15 year herbivore‐removal experiment in an Arizona piñon‐juniper woodland that was established on cinder soils following a volcanic eruption, to quantify how herbivory shapes the development of soil carbon (C) and nitrogen (N) over 36–54 years (i.e., the ages of the trees used in our study). In this semi‐arid ecosystem, trees are widely spaced on the landscape, which allows direct examination of herbivore impacts on the nutrient‐poor cinder soils. Although chronic insect herbivory increased annual litterfall N per unit area by 50% in this woodland, it slowed annual tree‐level soil C and N accumulation by 111% and 96%, respectively. Despite the reduction in soil C accumulation, short‐term litterfall‐C inputs and soil C‐efflux rates per unit soil surface were not impacted by herbivory. Our results demonstrate that the effects of herbivores on soil C and N fluxes and soil C and N accumulation are not necessarily congruent: herbivores can increase N in litterfall, but over time their impact on plant growth and development can slow soil development. In sum, because herbivores slow tree growth, they slow soil development on the landscape.
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spelling doaj.art-b23a20f7cb20479e960474b9c84a595e2022-12-21T23:44:40ZengWileyEcosphere2150-89252013-05-014511410.1890/ES12-00411.1Long‐term insect herbivory slows soil development in an arid ecosystemAimee T. Classen0Samantha K. Chapman1Thomas G. Whitham2Stephen C. Hart3George W. Koch4Department of Ecology and Evolutionary Biology, University of Tennessee, Knoxville, Tennessee 37996 USADepartment of Biological Sciences, Villanova University, Villanova, Pennsylvania 19085 USADepartment of Biological Sciences and Merriam-Powell Center for Environmental Research, Northern Arizona University, Flagstaff, Arizona 86001 USASchool of Natural Sciences, University of California and Sierra Nevada Research Institute, Merced, California 95343 USADepartment of Biological Sciences and Merriam-Powell Center for Environmental Research, Northern Arizona University, Flagstaff, Arizona 86001 USAAlthough herbivores are well known to alter litter inputs and soil nutrient fluxes, their long‐term influences on soil development are largely unknown because of the difficulty of detecting and attributing changes in carbon and nutrient pools against large background levels. The early phase of primary succession reduces this signal‐to‐noise problem, particularly in arid systems where individual plants can form islands of fertility. We used natural variation in tree‐resistance to herbivory, and a 15 year herbivore‐removal experiment in an Arizona piñon‐juniper woodland that was established on cinder soils following a volcanic eruption, to quantify how herbivory shapes the development of soil carbon (C) and nitrogen (N) over 36–54 years (i.e., the ages of the trees used in our study). In this semi‐arid ecosystem, trees are widely spaced on the landscape, which allows direct examination of herbivore impacts on the nutrient‐poor cinder soils. Although chronic insect herbivory increased annual litterfall N per unit area by 50% in this woodland, it slowed annual tree‐level soil C and N accumulation by 111% and 96%, respectively. Despite the reduction in soil C accumulation, short‐term litterfall‐C inputs and soil C‐efflux rates per unit soil surface were not impacted by herbivory. Our results demonstrate that the effects of herbivores on soil C and N fluxes and soil C and N accumulation are not necessarily congruent: herbivores can increase N in litterfall, but over time their impact on plant growth and development can slow soil development. In sum, because herbivores slow tree growth, they slow soil development on the landscape.https://doi.org/10.1890/ES12-00411.1carbon cyclinginsect herbivorynitrogen cyclingpinepiñon-juniper woodlandprimary succession
spellingShingle Aimee T. Classen
Samantha K. Chapman
Thomas G. Whitham
Stephen C. Hart
George W. Koch
Long‐term insect herbivory slows soil development in an arid ecosystem
Ecosphere
carbon cycling
insect herbivory
nitrogen cycling
pine
piñon-juniper woodland
primary succession
title Long‐term insect herbivory slows soil development in an arid ecosystem
title_full Long‐term insect herbivory slows soil development in an arid ecosystem
title_fullStr Long‐term insect herbivory slows soil development in an arid ecosystem
title_full_unstemmed Long‐term insect herbivory slows soil development in an arid ecosystem
title_short Long‐term insect herbivory slows soil development in an arid ecosystem
title_sort long term insect herbivory slows soil development in an arid ecosystem
topic carbon cycling
insect herbivory
nitrogen cycling
pine
piñon-juniper woodland
primary succession
url https://doi.org/10.1890/ES12-00411.1
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