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Soil phosphorus as a control of productivity and openness in temperate interglacial forest ecosystems

Identifieur interne : 000382 ( Main/Exploration ); précédent : 000381; suivant : 000383

Soil 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 :

RBID : ISTEX:623FE37FA60B7B527DDE83F3F0068C7DF961F185

English descriptors

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:


Links toward previous steps (curation, corpus...)


Le document en format XML

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