48 citations as recorded by crossref.

1. 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
2. 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
3. The enigma of Oligocene climate and global surface temperature evolution C. O’Brien et al. 10.1073/pnas.2003914117
4. Patterns of variation in fleshy diaspore size and abundance from Late Triassic–Oligocene D. Naware & R. Benson 10.1111/brv.13029
5. Tectonics, climate and the diversification of the tropical African terrestrial flora and fauna T. Couvreur et al. 10.1111/brv.12644
6. 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
7. Sea surface temperature evolution of the North Atlantic Ocean across the Eocene–Oligocene transition K. Śliwińska et al. 10.5194/cp-19-123-2023
8. Toward a Cenozoic history of atmospheric CO 2 B. Hönisch et al. 10.1126/science.adi5177
9. 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
10. 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
11. 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
12. The Relationship Between Normal-range Ejection Fraction and Diastolic Function M. Yılmaz & M. Sonsöz 10.4274/jarem.galenos.2024.08870
13. 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
14. Near‐Future pCO2 During the Hot Miocene Climatic Optimum M. Steinthorsdottir et al. 10.1029/2020PA003900
15. 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
16. Cenozoic evolution of the steppe-desert biome in Central Asia N. Barbolini et al. 10.1126/sciadv.abb8227
17. Late Cenozoic sea-surface-temperature evolution of the South Atlantic Ocean F. Hoem et al. 10.5194/cp-19-1931-2023
18. 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
19. 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
20. 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
21. 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
22. 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
23. 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
24. 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
25. Evolutionary trade‐offs in stomatal spacing T. Lawson & J. McElwain 10.1111/nph.13972
26. 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
27. Heterogeneity in global vegetation and terrestrial climate change during the late Eocene to early Oligocene transition M. Pound & U. Salzmann 10.1038/srep43386
28. Middle Eocene CO2and climate reconstructed from the sediment fill of a subarctic kimberlite maar A. Wolfe et al. 10.1130/G39002.1
29. 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
30. Insect herbivory patterns in late Eocene coastal lowland riparian associations from central Germany C. Müller et al. 10.1016/j.palaeo.2017.12.006
31. A Resurrected Scenario: Single Gain and Massive Loss of Nitrogen-Fixing Nodulation R. van Velzen et al. 10.1016/j.tplants.2018.10.005
32. 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
33. 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
34. An energy balance model for paleoclimate transitions B. Dortmans et al. 10.5194/cp-15-493-2019
35. 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
36. Decline of soil respiration in northeastern Tibet through the transition into the Oligocene icehouse A. Licht et al. 10.1016/j.palaeo.2020.110016
37. An Antarctic stratigraphic record of stepwise ice growth through the Eocene-Oligocene transition S. Passchier et al. 10.1130/B31482.1
38. Topological Climate Change K. Kypke & W. Langford 10.1142/S0218127420300050
39. Moderate levels of Eocene pCO2 indicated by Southern Hemisphere fossil plant stomata M. Steinthorsdottir et al. 10.1130/G46274.1
40. Searching for Function: Reconstructing Adaptive Niche Changes Using Geochemical and Morphological Data in Planktonic Foraminifera L. Kearns et al. 10.3389/fevo.2021.679722
41. Impact of Eocene‐Oligocene Antarctic Glaciation on the Paleoceanography of the Weddell Sea V. Hojnacki et al. 10.1029/2022PA004440
42. 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
43. 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
44. Modelling evidence for late Eocene Antarctic glaciations J. Van Breedam et al. 10.1016/j.epsl.2022.117532
45. 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
46. 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
47. 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
48. Earth’s Climate History from 4.5 Billion Years to One Minute J. Lin & T. Qian 10.1080/07055900.2022.2082914