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Global vegetation and terrestrial carbon cycle changes after the last ice age

Prentice, I. C., Harrison, S. P. and Bartlein, P. J. (2011) Global vegetation and terrestrial carbon cycle changes after the last ice age. New Phytologist, 189 (4). pp. 988-998. ISSN 1469-8137

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To link to this item DOI: 10.1111/j.1469-8137.2010.03620.x


•In current models, the ecophysiological effects of CO2 create both woody thickening and terrestrial carbon uptake, as observed now, and forest cover and terrestrial carbon storage increases that took place after the last glacial maximum (LGM). Here, we aimed to assess the realism of modelled vegetation and carbon storage changes between LGM and the pre-industrial Holocene (PIH). •We applied Land Processes and eXchanges (LPX), a dynamic global vegetation model (DGVM), with lowered CO2 and LGM climate anomalies from the Palaeoclimate Modelling Intercomparison Project (PMIP II), and compared the model results with palaeodata. •Modelled global gross primary production was reduced by 27–36% and carbon storage by 550–694 Pg C compared with PIH. Comparable reductions have been estimated from stable isotopes. The modelled areal reduction of forests is broadly consistent with pollen records. Despite reduced productivity and biomass, tropical forests accounted for a greater proportion of modelled land carbon storage at LGM (28–32%) than at PIH (25%). •The agreement between palaeodata and model results for LGM is consistent with the hypothesis that the ecophysiological effects of CO2 influence tree–grass competition and vegetation productivity, and suggests that these effects are also at work today.

Item Type:Article
Divisions:No Reading authors. Back catalogue items
Interdisciplinary Research Centres (IDRCs) > Walker Institute
Science > School of Archaeology, Geography and Environmental Science > Earth Systems Science
Science > School of Archaeology, Geography and Environmental Science > Department of Geography and Environmental Science
ID Code:33679
Uncontrolled Keywords:CO2; dynamic global vegetation model (DGVM); forest; last glacial maximum (LGM); productivity; sink; stable isotopes; woody thickening Summary

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