Soil phosphorus as a control of productivity and openness in temperate interglacial forest ecosystems
Identifieur interne : 000382 ( Main/Exploration ); précédent : 000381; suivant : 000383Soil phosphorus as a control of productivity and openness in temperate interglacial forest ecosystems
Auteurs : Petr Kuneš [Danemark, Niger] ; Bent Vad Odgaard [Danemark] ; Marie-José Gaillard [Suède]Source :
- Journal of Biogeography [ 0305-0270 ] ; 2011-11.
English descriptors
- KwdEn :
Abstract
Aim Observations of long chronosequences in forest ecosystems show that, after some millennia of build‐up, biomass declines in relation to the slow depletion of soil phosphorus. Plants that dominate during this period of soil impoverishment have specialized strategies for P acquisition, including ectomycorrhiza or root clusters. We use quantitative, pollen‐based reconstructions of regional vegetation in four Quaternary warm stages (Holocene, Eemian, Holsteinian, Harreskovian) to test whether inferred forest cover and productivity changes are consistent with long‐term modification of soil nutrient pools.
Url:
DOI: 10.1111/j.1365-2699.2011.02557.x
Affiliations:
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Le document en format XML
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<front><div type="abstract">Aim Observations of long chronosequences in forest ecosystems show that, after some millennia of build‐up, biomass declines in relation to the slow depletion of soil phosphorus. Plants that dominate during this period of soil impoverishment have specialized strategies for P acquisition, including ectomycorrhiza or root clusters. We use quantitative, pollen‐based reconstructions of regional vegetation in four Quaternary warm stages (Holocene, Eemian, Holsteinian, Harreskovian) to test whether inferred forest cover and productivity changes are consistent with long‐term modification of soil nutrient pools.</div>
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