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Science (New York, N.Y.)|March 4, 2000
Isotope fractionation and atmospheric oxygen: implications for phanerozoic O(2) evolutionBerner, Petsch, Lake, et al.Functional Plant Biology : FPB|July 22, 2020
13C discrimination patterns in oceanic phytoplankton: likely influence of CO2 concentrating mechanisms, and implications for palaeoreconstructionsEdward A Laws, Brian N Popp, Nicolas Cassar, et al.Science (New York, N.Y.)|August 28, 1999
Fossil Plants and Global Warming at the Triassic-Jurassic BoundaryMcElwain, Beerling, WoodwardThe New Phytologist|April 17, 2021
Stomatal development and CO<sub>2</sub> : ecological consequencesF I Woodward, J A Lake, W P QuickJournal of Experimental Botany|January 25, 2002
Long-distance CO(2) signalling in plantsJanice A Lake, F Ian Woodward, W Paul QuickProceedings of the National Academy of Sciences of the United States of America|October 26, 2000
Impact of a Permo-Carboniferous high O2 event on the terrestrial carbon cycleD J Beerling, R A BernerProceedings of the National Academy of Sciences of the United States of America|January 26, 2005
Feedbacks and the coevolution of plants and atmospheric CO2David J Beerling, Robert A BernerTrends in Ecology & Evolution|January 18, 2011
Palaeo-ecophysiological perspectives on plant responses to global changeD J Beerling, F I WoodwardThe New Phytologist|April 20, 2021
Ecophysiological responses of plants to global environmental change since the Last Glacial MaximumD J Beerling, F I WoodwardPlant Physiology|September 12, 2000
Long-term growth of Ginkgo with CO(2) enrichment increases leaf ice nucleation temperatures and limits recovery of the photosynthetic system from freezingA C Terry, W P Quick, D J BeerlingPageof 5,021