34 citations as recorded by crossref.

1. Elevated CO2 degassing rates prevented the return of Snowball Earth during the Phanerozoic B. Mills et al. 10.1038/s41467-017-01456-w
2. Reservoir heterogeneity of Ordovician sandstone reservoir (Bedinan Formation, SE Turkey): Diagenetic and sedimentological approachs G. Yıldız & İ. Yılmaz 10.1016/j.marpetgeo.2020.104444
3. Glacial onset predated Late Ordovician climate cooling A. Pohl et al. 10.1002/2016PA002928
4. Could land-based early photosynthesizing ecosystems have bioengineered the planet in mid-Palaeozoic times? D. Edwards et al. 10.1111/pala.12187
5. Comparative Lower-Middle Ordovician conodont oxygen isotope palaeothermometry of the Argentine Precordillera and Laurentian margins G. Albanesi et al. 10.1016/j.palaeo.2019.03.016
6. New conodont δ18O records of Silurian climate change: Implications for environmental and biological events J. Trotter et al. 10.1016/j.palaeo.2015.11.011
7. Hvordan vet vi det vi vet om globaloppvarming? K. Seip 10.18261/issn.1504-3118-2021-01-02
8. COPSE reloaded: An improved model of biogeochemical cycling over Phanerozoic time T. Lenton et al. 10.1016/j.earscirev.2017.12.004
9. Climate Sensitivity on Geological Timescales Controlled by Nonlinear Feedbacks and Ocean Circulation A. Farnsworth et al. 10.1029/2019GL083574
10. Co-existing climate attractors in a coupled aquaplanet M. Brunetti et al. 10.1007/s00382-019-04926-7
11. Aragonite depositional facies in a Late Ordovician calcite sea, Eastern Laurentia N. James et al. 10.1111/sed.12753
12. Testing the early Late Ordovician cool-water hypothesis with oxygen isotopes from conodont apatite P. QUINTON et al. 10.1017/S0016756817000589
13. Modelling the long-term carbon cycle, atmospheric CO2, and Earth surface temperature from late Neoproterozoic to present day B. Mills et al. 10.1016/j.gr.2018.12.001
14. Impacts of climate-ocean-tectonic changes on early Paleozoic conodont ecology and evolution evidenced by the Canadian part of Laurentia C. Barnes 10.1016/j.palaeo.2019.02.018
15. Early Palaeozoic diversifications and extinctions in the marine biosphere: a continuum of change D. Harper et al. 10.1017/S0016756819001298
16. New paleogeographic and degassing parameters for long-term carbon cycle models C. Marcilly et al. 10.1016/j.gr.2021.05.016
17. The climatic significance of Late Ordovician-early Silurian black shales A. Pohl et al. 10.1002/2016PA003064
18. IPSL-CM5A2 – an Earth system model designed for multi-millennial climate simulations P. Sepulchre et al. 10.5194/gmd-13-3011-2020
19. Impacts of Tibetan Plateau uplift on atmospheric dynamics and associated precipitation <i>δ</i><sup>18</sup>O S. Botsyun et al. 10.5194/cp-12-1401-2016
20. Oxygen isotope analysis of the eyes of pelagic trilobites: Testing the application of sea temperature proxies for the Ordovician C. Bennett et al. 10.1016/j.gr.2018.01.006
21. Truncated bimodal latitudinal diversity gradient in early Paleozoic phytoplankton A. Zacaï et al. 10.1126/sciadv.abd6709
22. Coordinated biotic and abiotic change during the Great Ordovician Biodiversification Event: Darriwilian assembly of early Paleozoic building blocks A. Stigall et al. 10.1016/j.palaeo.2019.05.034
23. Middle Ordovician acritarchs and problematic organic-walled microfossils from the Saq-Hanadir transitional beds in the QSIM-801 well, Saudi Arabia A. Le Hérissé et al. 10.1016/j.revmic.2017.08.001
24. An early Cambrian greenhouse climate T. Hearing et al. 10.1126/sciadv.aar5690
25. Improved efficiency of the biological pump as a trigger for the Late Ordovician glaciation J. Shen et al. 10.1038/s41561-018-0141-5
26. Earliest land plants created modern levels of atmospheric oxygen T. Lenton et al. 10.1073/pnas.1604787113
27. Baltoscandian conodont biofacies fluctuations and their link to Middle Ordovician (Darriwilian) global cooling J. Rasmussen et al. 10.1111/pala.12348
28. New age constraints on the duration and origin of the Late Ordovician Guttenberg δ13Ccarb excursion from high-precision U-Pb geochronology of K-bentonites J. Metzger et al. 10.1130/B35688.1
29. Possible patterns of marine primary productivity during the Great Ordovician Biodiversification Event A. Pohl et al. 10.1111/let.12247
30. High dependence of Ordovician ocean surface circulation on atmospheric CO2 levels A. Pohl et al. 10.1016/j.palaeo.2015.09.036
31. High potential for weathering and climate effects of non-vascular vegetation in the Late Ordovician P. Porada et al. 10.1038/ncomms12113
32. The onset of the ‘Ordovician Plankton Revolution’ in the late Cambrian T. Servais et al. 10.1016/j.palaeo.2015.11.003
33. Plate tectonic modelling: review and perspectives C. VÉRARD 10.1017/S0016756817001030
34. Persistent global marine euxinia in the early Silurian R. Stockey et al. 10.1038/s41467-020-15400-y