Articles | Volume 12, issue 2
https://doi.org/10.5194/cp-12-439-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue:
https://doi.org/10.5194/cp-12-439-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Fossil plant stomata indicate decreasing atmospheric CO2 prior to the Eocene–Oligocene boundary
Margret Steinthorsdottir
CORRESPONDING AUTHOR
Department of Geological Sciences and Bolin Centre for Climate Research, Stockholm University, 106 91 Stockholm, Sweden
Amanda S. Porter
School of Biology and Environmental Science, Earth Institute, University College Dublin, Dublin 4, Ireland
Aidan Holohan
School of Biology and Environmental Science, Earth Institute, University College Dublin, Dublin 4, Ireland
Lutz Kunzmann
Museum of Mineralogy and Geology, Senckenberg Natural History Collections Dresden, Dresden, Germany
Margaret Collinson
Department of Earth Sciences, Royal Holloway University of London, Egham, Surrey, UK
Jennifer C. McElwain
School of Biology and Environmental Science, Earth Institute, University College Dublin, Dublin 4, Ireland
Viewed
Total article views: 4,890 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 26 Oct 2015)
HTML | XML | Total | Supplement | BibTeX | EndNote | |
---|---|---|---|---|---|---|
2,655 | 2,021 | 214 | 4,890 | 420 | 156 | 181 |
- HTML: 2,655
- PDF: 2,021
- XML: 214
- Total: 4,890
- Supplement: 420
- BibTeX: 156
- EndNote: 181
Total article views: 4,065 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 25 Feb 2016)
HTML | XML | Total | Supplement | BibTeX | EndNote | |
---|---|---|---|---|---|---|
2,307 | 1,582 | 176 | 4,065 | 256 | 145 | 165 |
- HTML: 2,307
- PDF: 1,582
- XML: 176
- Total: 4,065
- Supplement: 256
- BibTeX: 145
- EndNote: 165
Total article views: 825 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 26 Oct 2015)
HTML | XML | Total | Supplement | BibTeX | EndNote | |
---|---|---|---|---|---|---|
348 | 439 | 38 | 825 | 164 | 11 | 16 |
- HTML: 348
- PDF: 439
- XML: 38
- Total: 825
- Supplement: 164
- BibTeX: 11
- EndNote: 16
Cited
49 citations as recorded by crossref.
- Contrasting responses of leaf stomatal characteristics to climate change: a considerable challenge to predict carbon and water cycles W. Yan et al. 10.1111/gcb.13654
- Searching for a nearest living equivalent for Bennettitales: a promising extinct plant group for stomatal proxy reconstructions of MesozoicpCO2 M. Steinthorsdottir et al. 10.1080/11035897.2021.1895304
- The enigma of Oligocene climate and global surface temperature evolution C. O’Brien et al. 10.1073/pnas.2003914117
- Patterns of variation in fleshy diaspore size and abundance from Late Triassic–Oligocene D. Naware & R. Benson 10.1111/brv.13029
- Tectonics, climate and the diversification of the tropical African terrestrial flora and fauna T. Couvreur et al. 10.1111/brv.12644
- Old origin for an European‐African amphitropical disjunction pattern: New insights from a case study on wingless darkling beetles M. Kamiński et al. 10.1111/jbi.14288
- Sea surface temperature evolution of the North Atlantic Ocean across the Eocene–Oligocene transition K. Śliwińska et al. 10.5194/cp-19-123-2023
- Toward a Cenozoic history of atmospheric CO 2 B. Hönisch et al. 10.1126/science.adi5177
- East Asian hydroclimate responses to the Eocene-Oligocene transition in the Weihe Basin, central China Y. Wang et al. 10.1016/j.palaeo.2023.111436
- An inter-comparison study of three stomatal-proxy methods for CO2 reconstruction applied to early Jurassic Ginkgoales plants N. Zhou et al. 10.1016/j.palaeo.2019.109547
- Paleobotany and Global Change: Important Lessons for Species to Biomes from Vegetation Responses to Past Global Change J. McElwain 10.1146/annurev-arplant-042817-040405
- The Relationship Between Normal-range Ejection Fraction and Diastolic Function M. Yılmaz & M. Sonsöz 10.4274/jarem.galenos.2024.08870
- The evolution of hydroclimate in Asia over the Cenozoic: A stable-isotope perspective J. Caves Rugenstein & C. Chamberlain 10.1016/j.earscirev.2018.09.003
- Near‐Future pCO2 During the Hot Miocene Climatic Optimum M. Steinthorsdottir et al. 10.1029/2020PA003900
- First record of insects in lignite-bearing formations (upper Eocene) of the central German Leipzig Embayment L. Kunzmann et al. 10.1007/s12542-017-0367-3
- Cenozoic evolution of the steppe-desert biome in Central Asia N. Barbolini et al. 10.1126/sciadv.abb8227
- Late Cenozoic sea-surface-temperature evolution of the South Atlantic Ocean F. Hoem et al. 10.5194/cp-19-1931-2023
- The Eocene–Oligocene transition: a review of marine and terrestrial proxy data, models and model–data comparisons D. Hutchinson et al. 10.5194/cp-17-269-2021
- n-C27 Predominance and 13C enrichment by bicarbonate assimilation of race A of Botryococcus braunii in Chinese Maoming oilshales J. Liao et al. 10.1016/j.chemgeo.2022.120905
- Estimating palaeoatmospheric CO2 levels based on fossil Ginkgoites cuticles from the Middle Jurassic of Northeast Iran M. Badihagh et al. 10.1016/j.palwor.2023.01.011
- Testing the accuracy of new paleoatmospheric CO2 proxies based on plant stable carbon isotopic composition and stomatal traits in a range of simulated paleoatmospheric O2:CO2 ratios A. Porter et al. 10.1016/j.gca.2019.05.037
- Terrestrial cooling and changes in hydroclimate in the continental interior of the United States across the Eocene-Oligocene boundary M. Fan et al. 10.1130/B31732.1
- Eccentricity-paced monsoon variability on the northeastern Tibetan Plateau in the Late Oligocene high CO 2 world H. Ao et al. 10.1126/sciadv.abk2318
- Key traits of living fossil Ginkgo biloba are highly variable but not influenced by climate – Implications for palaeo-pCO2 reconstructions and climate sensitivity M. Steinthorsdottir et al. 10.1016/j.gloplacha.2022.103786
- Evolutionary trade‐offs in stomatal spacing T. Lawson & J. McElwain 10.1111/nph.13972
- Stomatal frequency of Quercus glauca from three material sources shows the same inverse response to atmospheric pCO2 J. Hu et al. 10.1093/aob/mcz020
- Heterogeneity in global vegetation and terrestrial climate change during the late Eocene to early Oligocene transition M. Pound & U. Salzmann 10.1038/srep43386
- Middle Eocene CO2and climate reconstructed from the sediment fill of a subarctic kimberlite maar A. Wolfe et al. 10.1130/G39002.1
- Fossil leaf traits as archives for the past — and lessons for the future? A. Roth-Nebelsick & W. Konrad 10.1016/j.flora.2018.08.006
- Insect herbivory patterns in late Eocene coastal lowland riparian associations from central Germany C. Müller et al. 10.1016/j.palaeo.2017.12.006
- A Resurrected Scenario: Single Gain and Massive Loss of Nitrogen-Fixing Nodulation R. van Velzen et al. 10.1016/j.tplants.2018.10.005
- New pollen genera and species from the Oligocene of northern Spain and a systematic, biostratigraphic and biogeographic re-evaluation of coeval taxa M. Casas-Gallego & E. Barrón 10.1080/14772019.2020.1863488
- The Paleoclimate Significance of the δ13C Composition of Individual Hydrocarbon Compounds in the Maoming Oil Shales, China X. Cao et al. 10.3389/feart.2021.648176
- An energy balance model for paleoclimate transitions B. Dortmans et al. 10.5194/cp-15-493-2019
- Late Eocene to early Oligocene productivity events in the proto-Southern Ocean and correlation to climate change G. Rodrigues de Faria et al. 10.5194/cp-20-1327-2024
- Decline of soil respiration in northeastern Tibet through the transition into the Oligocene icehouse A. Licht et al. 10.1016/j.palaeo.2020.110016
- An Antarctic stratigraphic record of stepwise ice growth through the Eocene-Oligocene transition S. Passchier et al. 10.1130/B31482.1
- Topological Climate Change K. Kypke & W. Langford 10.1142/S0218127420300050
- Moderate levels of Eocene pCO2 indicated by Southern Hemisphere fossil plant stomata M. Steinthorsdottir et al. 10.1130/G46274.1
- Heat stress reduces stomatal numbers in Ginkgo biloba: Implications for the stomatal method of palaeo-atmospheric [CO2] reconstruction during episodes of global warming A. Carli et al. 10.1016/j.scitotenv.2024.177962
- Searching for Function: Reconstructing Adaptive Niche Changes Using Geochemical and Morphological Data in Planktonic Foraminifera L. Kearns et al. 10.3389/fevo.2021.679722
- Impact of Eocene‐Oligocene Antarctic Glaciation on the Paleoceanography of the Weddell Sea V. Hojnacki et al. 10.1029/2022PA004440
- Global trends of pCO2 across the Cretaceous–Paleogene boundary supported by the first Southern Hemisphere stomatal proxy-based pCO2 reconstruction M. Steinthorsdottir et al. 10.1016/j.palaeo.2016.04.033
- Co-ordination in Morphological Leaf Traits of Early Diverging Angiosperms Is Maintained Following Exposure to Experimental Palaeo-atmospheric Conditions of Sub-ambient O2 and Elevated CO2 C. Evans-Fitz.Gerald et al. 10.3389/fpls.2016.01368
- Modelling evidence for late Eocene Antarctic glaciations J. Van Breedam et al. 10.1016/j.epsl.2022.117532
- Significant transient pCO2 perturbation at the New Zealand Oligocene-Miocene transition recorded by fossil plant stomata M. Steinthorsdottir et al. 10.1016/j.palaeo.2018.01.039
- A Paleogene leaf flora (Profen, Sachsen-Anhalt, Germany) and its potentials for palaeoecological and palaeoclimate reconstructions L. Kunzmann et al. 10.1016/j.flora.2018.11.005
- Cuticle surfaces of fossil plants as a potential proxy for volcanic SO2 emissions: observations from the Triassic–Jurassic transition of East Greenland M. Steinthorsdottir et al. 10.1007/s12549-017-0297-9
- Earth’s Climate History from 4.5 Billion Years to One Minute J. Lin & T. Qian 10.1080/07055900.2022.2082914
48 citations as recorded by crossref.
- Contrasting responses of leaf stomatal characteristics to climate change: a considerable challenge to predict carbon and water cycles W. Yan et al. 10.1111/gcb.13654
- Searching for a nearest living equivalent for Bennettitales: a promising extinct plant group for stomatal proxy reconstructions of MesozoicpCO2 M. Steinthorsdottir et al. 10.1080/11035897.2021.1895304
- The enigma of Oligocene climate and global surface temperature evolution C. O’Brien et al. 10.1073/pnas.2003914117
- Patterns of variation in fleshy diaspore size and abundance from Late Triassic–Oligocene D. Naware & R. Benson 10.1111/brv.13029
- Tectonics, climate and the diversification of the tropical African terrestrial flora and fauna T. Couvreur et al. 10.1111/brv.12644
- Old origin for an European‐African amphitropical disjunction pattern: New insights from a case study on wingless darkling beetles M. Kamiński et al. 10.1111/jbi.14288
- Sea surface temperature evolution of the North Atlantic Ocean across the Eocene–Oligocene transition K. Śliwińska et al. 10.5194/cp-19-123-2023
- Toward a Cenozoic history of atmospheric CO 2 B. Hönisch et al. 10.1126/science.adi5177
- East Asian hydroclimate responses to the Eocene-Oligocene transition in the Weihe Basin, central China Y. Wang et al. 10.1016/j.palaeo.2023.111436
- An inter-comparison study of three stomatal-proxy methods for CO2 reconstruction applied to early Jurassic Ginkgoales plants N. Zhou et al. 10.1016/j.palaeo.2019.109547
- Paleobotany and Global Change: Important Lessons for Species to Biomes from Vegetation Responses to Past Global Change J. McElwain 10.1146/annurev-arplant-042817-040405
- The Relationship Between Normal-range Ejection Fraction and Diastolic Function M. Yılmaz & M. Sonsöz 10.4274/jarem.galenos.2024.08870
- The evolution of hydroclimate in Asia over the Cenozoic: A stable-isotope perspective J. Caves Rugenstein & C. Chamberlain 10.1016/j.earscirev.2018.09.003
- Near‐Future pCO2 During the Hot Miocene Climatic Optimum M. Steinthorsdottir et al. 10.1029/2020PA003900
- First record of insects in lignite-bearing formations (upper Eocene) of the central German Leipzig Embayment L. Kunzmann et al. 10.1007/s12542-017-0367-3
- Cenozoic evolution of the steppe-desert biome in Central Asia N. Barbolini et al. 10.1126/sciadv.abb8227
- Late Cenozoic sea-surface-temperature evolution of the South Atlantic Ocean F. Hoem et al. 10.5194/cp-19-1931-2023
- The Eocene–Oligocene transition: a review of marine and terrestrial proxy data, models and model–data comparisons D. Hutchinson et al. 10.5194/cp-17-269-2021
- n-C27 Predominance and 13C enrichment by bicarbonate assimilation of race A of Botryococcus braunii in Chinese Maoming oilshales J. Liao et al. 10.1016/j.chemgeo.2022.120905
- Estimating palaeoatmospheric CO2 levels based on fossil Ginkgoites cuticles from the Middle Jurassic of Northeast Iran M. Badihagh et al. 10.1016/j.palwor.2023.01.011
- Testing the accuracy of new paleoatmospheric CO2 proxies based on plant stable carbon isotopic composition and stomatal traits in a range of simulated paleoatmospheric O2:CO2 ratios A. Porter et al. 10.1016/j.gca.2019.05.037
- Terrestrial cooling and changes in hydroclimate in the continental interior of the United States across the Eocene-Oligocene boundary M. Fan et al. 10.1130/B31732.1
- Eccentricity-paced monsoon variability on the northeastern Tibetan Plateau in the Late Oligocene high CO 2 world H. Ao et al. 10.1126/sciadv.abk2318
- Key traits of living fossil Ginkgo biloba are highly variable but not influenced by climate – Implications for palaeo-pCO2 reconstructions and climate sensitivity M. Steinthorsdottir et al. 10.1016/j.gloplacha.2022.103786
- Evolutionary trade‐offs in stomatal spacing T. Lawson & J. McElwain 10.1111/nph.13972
- Stomatal frequency of Quercus glauca from three material sources shows the same inverse response to atmospheric pCO2 J. Hu et al. 10.1093/aob/mcz020
- Heterogeneity in global vegetation and terrestrial climate change during the late Eocene to early Oligocene transition M. Pound & U. Salzmann 10.1038/srep43386
- Middle Eocene CO2and climate reconstructed from the sediment fill of a subarctic kimberlite maar A. Wolfe et al. 10.1130/G39002.1
- Fossil leaf traits as archives for the past — and lessons for the future? A. Roth-Nebelsick & W. Konrad 10.1016/j.flora.2018.08.006
- Insect herbivory patterns in late Eocene coastal lowland riparian associations from central Germany C. Müller et al. 10.1016/j.palaeo.2017.12.006
- A Resurrected Scenario: Single Gain and Massive Loss of Nitrogen-Fixing Nodulation R. van Velzen et al. 10.1016/j.tplants.2018.10.005
- New pollen genera and species from the Oligocene of northern Spain and a systematic, biostratigraphic and biogeographic re-evaluation of coeval taxa M. Casas-Gallego & E. Barrón 10.1080/14772019.2020.1863488
- The Paleoclimate Significance of the δ13C Composition of Individual Hydrocarbon Compounds in the Maoming Oil Shales, China X. Cao et al. 10.3389/feart.2021.648176
- An energy balance model for paleoclimate transitions B. Dortmans et al. 10.5194/cp-15-493-2019
- Late Eocene to early Oligocene productivity events in the proto-Southern Ocean and correlation to climate change G. Rodrigues de Faria et al. 10.5194/cp-20-1327-2024
- Decline of soil respiration in northeastern Tibet through the transition into the Oligocene icehouse A. Licht et al. 10.1016/j.palaeo.2020.110016
- An Antarctic stratigraphic record of stepwise ice growth through the Eocene-Oligocene transition S. Passchier et al. 10.1130/B31482.1
- Topological Climate Change K. Kypke & W. Langford 10.1142/S0218127420300050
- Moderate levels of Eocene pCO2 indicated by Southern Hemisphere fossil plant stomata M. Steinthorsdottir et al. 10.1130/G46274.1
- Heat stress reduces stomatal numbers in Ginkgo biloba: Implications for the stomatal method of palaeo-atmospheric [CO2] reconstruction during episodes of global warming A. Carli et al. 10.1016/j.scitotenv.2024.177962
- Searching for Function: Reconstructing Adaptive Niche Changes Using Geochemical and Morphological Data in Planktonic Foraminifera L. Kearns et al. 10.3389/fevo.2021.679722
- Impact of Eocene‐Oligocene Antarctic Glaciation on the Paleoceanography of the Weddell Sea V. Hojnacki et al. 10.1029/2022PA004440
- Global trends of pCO2 across the Cretaceous–Paleogene boundary supported by the first Southern Hemisphere stomatal proxy-based pCO2 reconstruction M. Steinthorsdottir et al. 10.1016/j.palaeo.2016.04.033
- Co-ordination in Morphological Leaf Traits of Early Diverging Angiosperms Is Maintained Following Exposure to Experimental Palaeo-atmospheric Conditions of Sub-ambient O2 and Elevated CO2 C. Evans-Fitz.Gerald et al. 10.3389/fpls.2016.01368
- Modelling evidence for late Eocene Antarctic glaciations J. Van Breedam et al. 10.1016/j.epsl.2022.117532
- Significant transient pCO2 perturbation at the New Zealand Oligocene-Miocene transition recorded by fossil plant stomata M. Steinthorsdottir et al. 10.1016/j.palaeo.2018.01.039
- A Paleogene leaf flora (Profen, Sachsen-Anhalt, Germany) and its potentials for palaeoecological and palaeoclimate reconstructions L. Kunzmann et al. 10.1016/j.flora.2018.11.005
- Cuticle surfaces of fossil plants as a potential proxy for volcanic SO2 emissions: observations from the Triassic–Jurassic transition of East Greenland M. Steinthorsdottir et al. 10.1007/s12549-017-0297-9
1 citations as recorded by crossref.
Saved (preprint)
Discussed (final revised paper)
Latest update: 26 Dec 2024
Short summary
Our manuscript "Fossil plant stomata indicate decreasing atmospheric CO2 prior to the Eocene–Oligocene boundary" reports that ~ 40 % decrease in pCO2 preceded the large shift in marine oxygen isotope records that characterizes the Eocene–Oliogocene climate transition. The results endorse the theory that pCO2 drawdown was the main forcer of the Eocene–Oligocene climate change, and a "tipping point" was reached in the latest Eocene, triggering the plunge of the Earth System into icehouse conditions.
Our manuscript "Fossil plant stomata indicate decreasing atmospheric CO2 prior to the...
Special issue