Research article
22 Mar 2013
Research article
| 22 Mar 2013
Stable isotope and modelling evidence for CO2 as a driver of glacial–interglacial vegetation shifts in southern Africa
F. J. Bragg et al.
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Cited
23 citations as recorded by crossref.
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- Climate and CO 2 effects on the vegetation of southern tropical Africa over the last 37,000 years V. Khon et al. 10.1016/j.epsl.2014.06.043
- Bayesian Analysis of the Glacial‐Interglacial Methane Increase Constrained by Stable Isotopes and Earth System Modeling P. Hopcroft et al. 10.1002/2018GL077382
- Independent variations of CH4 emissions and isotopic composition over the past 160,000 years L. Möller et al. 10.1038/ngeo1922
- Climate versus carbon dioxide controls on biomass burning: a model analysis of the glacial–interglacial contrast M. Martin Calvo et al. 10.5194/bg-11-6017-2014
- Effects of fire and CO 2 on biogeography and primary production in glacial and modern climates M. Martin Calvo & I. Prentice 10.1111/nph.13485
- Data-based modelling and environmental sensitivity of vegetation in China H. Wang et al. 10.5194/bg-10-5817-2013
- Are Glacials Dry? Consequences for Paleoclimatology and for Greenhouse Warming J. Scheff et al. 10.1175/JCLI-D-16-0854.1
- The PMIP4 Last Glacial Maximum experiments: preliminary results and comparison with the PMIP3 simulations M. Kageyama et al. 10.5194/cp-17-1065-2021
- Past and future global transformation of terrestrial ecosystems under climate change C. Nolan et al. 10.1126/science.aan5360
- Changes in obliquity drive tree cover shifts in eastern tropical South America J. Ferreira et al. 10.1016/j.quascirev.2022.107402
- Reconstructing ice-age palaeoclimates: Quantifying low-CO2 effects on plants I. Prentice et al. 10.1016/j.gloplacha.2016.12.012
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- Contracting eastern African C4 grasslands during the extinction of Paranthropus boisei R. Quinn & C. Lepre 10.1038/s41598-021-86642-z
- Historical distribution of Sundaland’s Dipterocarp rainforests at Quaternary glacial maxima N. Raes et al. 10.1073/pnas.1403053111
- A new multivariable benchmark for Last Glacial Maximum climate simulations S. Cleator et al. 10.5194/cp-16-699-2020
- Broader niches revealed by fossil data do not reduce estimates of range loss and fragmentation of African montane trees S. Ivory et al. 10.1111/geb.12909
- CO2 and fire influence tropical ecosystem stability in response to climate change T. Shanahan et al. 10.1038/srep29587
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22 citations as recorded by crossref.
- Enhanced Australian carbon sink despite increased wildfire during the 21st century D. Kelley & S. Harrison 10.1088/1748-9326/9/10/104015
- The transition on North America from the warm humid Pliocene to the glaciated Quaternary traced by eolian dust deposition at a benchmark North Atlantic Ocean drill site D. Lang et al. 10.1016/j.quascirev.2014.04.005
- Effect of changing vegetation and precipitation on denudation – Part 1: Predicted vegetation composition and cover over the last 21 thousand years along the Coastal Cordillera of Chile C. Werner et al. 10.5194/esurf-6-829-2018
- Colonization of the Southern Hemisphere by Sagina and Colobanthus (Caryophyllaceae) D. Alban et al. 10.1007/s00606-021-01793-w
- Plant speciation in the Quaternary J. Kadereit & R. Abbott 10.1080/17550874.2021.2012849
- Climate and CO 2 effects on the vegetation of southern tropical Africa over the last 37,000 years V. Khon et al. 10.1016/j.epsl.2014.06.043
- Bayesian Analysis of the Glacial‐Interglacial Methane Increase Constrained by Stable Isotopes and Earth System Modeling P. Hopcroft et al. 10.1002/2018GL077382
- Independent variations of CH4 emissions and isotopic composition over the past 160,000 years L. Möller et al. 10.1038/ngeo1922
- Climate versus carbon dioxide controls on biomass burning: a model analysis of the glacial–interglacial contrast M. Martin Calvo et al. 10.5194/bg-11-6017-2014
- Effects of fire and CO 2 on biogeography and primary production in glacial and modern climates M. Martin Calvo & I. Prentice 10.1111/nph.13485
- Data-based modelling and environmental sensitivity of vegetation in China H. Wang et al. 10.5194/bg-10-5817-2013
- Are Glacials Dry? Consequences for Paleoclimatology and for Greenhouse Warming J. Scheff et al. 10.1175/JCLI-D-16-0854.1
- The PMIP4 Last Glacial Maximum experiments: preliminary results and comparison with the PMIP3 simulations M. Kageyama et al. 10.5194/cp-17-1065-2021
- Past and future global transformation of terrestrial ecosystems under climate change C. Nolan et al. 10.1126/science.aan5360
- Changes in obliquity drive tree cover shifts in eastern tropical South America J. Ferreira et al. 10.1016/j.quascirev.2022.107402
- Reconstructing ice-age palaeoclimates: Quantifying low-CO2 effects on plants I. Prentice et al. 10.1016/j.gloplacha.2016.12.012
- Spatiotemporal changes in C4 plant abundance in China since the Last Glacial Maximum and their driving factors W. Jiang et al. 10.1016/j.palaeo.2018.12.021
- Contracting eastern African C4 grasslands during the extinction of Paranthropus boisei R. Quinn & C. Lepre 10.1038/s41598-021-86642-z
- Historical distribution of Sundaland’s Dipterocarp rainforests at Quaternary glacial maxima N. Raes et al. 10.1073/pnas.1403053111
- A new multivariable benchmark for Last Glacial Maximum climate simulations S. Cleator et al. 10.5194/cp-16-699-2020
- Broader niches revealed by fossil data do not reduce estimates of range loss and fragmentation of African montane trees S. Ivory et al. 10.1111/geb.12909
- CO2 and fire influence tropical ecosystem stability in response to climate change T. Shanahan et al. 10.1038/srep29587
1 citations as recorded by crossref.
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