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D J Beerling

Showing results (1-10 of 22) with videos related to

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Tree Physiology|April 1, 1996
Ecophysiological responses of woody plants to past CO(2) concentrationsD J Beerling
Oecologia|March 18, 2017
<sup>13</sup>C discrimination by fossil leaves during the late-glacial climate oscillation 12-10 ka BP: measurements and physiological controlsD J Beerling
The New Phytologist|April 20, 2021
Predicting leaf gas exchange and δ<sup>13</sup> C responses to the past 30000 years of global environmental changeD J Beerling
Proceedings of the National Academy of Sciences of the United States of America|September 18, 2002
Low atmospheric CO(2) levels during the Permo- Carboniferous glaciation inferred from fossil lycopsidsD J Beerling
Trends in Ecology & Evolution|January 18, 2011
The future as the key to the past for palaeobotany?D J Beerling
Trends in Ecology & Evolution|January 18, 2011
Palaeo-ecophysiological perspectives on plant responses to global changeD J Beerling, F I Woodward
Proceedings 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 Berner
The New Phytologist|April 20, 2021
Ecophysiological responses of plants to global environmental change since the Last Glacial MaximumD J Beerling, F I Woodward
The New Phytologist|April 17, 2021
Reading a CO<sub>2</sub> signal from fossil stomataD J Beerling, D L Royer
Annals of Botany|July 5, 2002
Physiological ecology of Mesozoic polar forests in a high CO2 environmentD J Beerling, C P Osborne
Pageof 3

Showing results (1-10 of 22) with videos related to

Sort By:
Pageof 3
Tree Physiology|April 1, 1996
Ecophysiological responses of woody plants to past CO(2) concentrationsD J Beerling
Oecologia|March 18, 2017
<sup>13</sup>C discrimination by fossil leaves during the late-glacial climate oscillation 12-10 ka BP: measurements and physiological controlsD J Beerling
The New Phytologist|April 20, 2021
Predicting leaf gas exchange and δ<sup>13</sup> C responses to the past 30000 years of global environmental changeD J Beerling
Proceedings of the National Academy of Sciences of the United States of America|September 18, 2002
Low atmospheric CO(2) levels during the Permo- Carboniferous glaciation inferred from fossil lycopsidsD J Beerling
Trends in Ecology & Evolution|January 18, 2011
The future as the key to the past for palaeobotany?D J Beerling
Trends in Ecology & Evolution|January 18, 2011
Palaeo-ecophysiological perspectives on plant responses to global changeD J Beerling, F I Woodward
Proceedings 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 Berner
The New Phytologist|April 20, 2021
Ecophysiological responses of plants to global environmental change since the Last Glacial MaximumD J Beerling, F I Woodward
The New Phytologist|April 17, 2021
Reading a CO<sub>2</sub> signal from fossil stomataD J Beerling, D L Royer
Annals of Botany|July 5, 2002
Physiological ecology of Mesozoic polar forests in a high CO2 environmentD J Beerling, C P Osborne
Pageof 3