24 citations as recorded by crossref.

1. Coupled microbial bloom and oxygenation decline recorded by magnetofossils during the Palaeocene–Eocene Thermal Maximum L. Chang et al. 10.1038/s41467-018-06472-y
2. Increased export production during recovery from the Paleocene–Eocene thermal maximum constrained by sedimentary Ba isotopes L. Bridgestock et al. 10.1016/j.epsl.2018.12.036
3. Eustatic change across the Paleocene-Eocene Thermal Maximum in the epicontinental Tarim seaway J. Jiang et al. 10.1016/j.gloplacha.2023.104241
4. New geochemical constraints on the Paleocene–Eocene thermal maximum: Dababiya GSSP, Egypt H. Khozyem et al. 10.1016/j.palaeo.2015.04.003
5. Phylogenetic diversifications linked to the morphological traits and global phylogeographic pattern of closed pouch fishes in Syngnathidae Y. Zhang et al. 10.59717/j.xinn-geo.2025.100137
6. Carbon sequestration during the Palaeocene–Eocene Thermal Maximum by an efficient biological pump Z. Ma et al. 10.1038/ngeo2139
7. Paleoredox conditions and paleoproductivity of the early-Eocene sediments in the Gaga Section, Western Desert, Egypt A. Mahmoud et al. 10.1016/j.jafrearsci.2025.105640
8. Silicate weathering and North Atlantic silica burial during the Paleocene-Eocene Thermal Maximum D. Penman 10.1130/G37704.1
9. Maastrichtian to Eocene Subsurface Stratigraphy of the Cauvery Basin and Correlation with Madagascar G. Keller et al. 10.1007/s12594-016-0370-4
10. Complete mitochondrial genomes of eight seahorses and pipefishes (Syngnathiformes: Syngnathidae): insight into the adaptive radiation of syngnathid fishes X. Wang et al. 10.1186/s12862-019-1430-3
11. Water column barium sulfate dissolution and shielding by organic matter aggregates: Implications for the pelagic barite proxy T. Light et al. 10.1016/j.chemgeo.2023.121637
12. Productivity response of calcareous nannoplankton to Eocene Thermal Maximum 2 (ETM2) M. Dedert et al. 10.5194/cp-8-977-2012
13. Toward an Improved Understanding of the Marine Barium Cycle and the Application of Marine Barite as a Paleoproductivity Proxy S. Carter et al. 10.3390/min10050421
14. Rapid and sustained environmental responses to global warming: the Paleocene–Eocene Thermal Maximum in the eastern North Sea E. Stokke et al. 10.5194/cp-17-1989-2021
15. Black shale formation during the Latest Danian Event and the Paleocene–Eocene Thermal Maximum in central Egypt: Two of a kind? P. Schulte et al. 10.1016/j.palaeo.2012.11.027
16. Climatic and tectonic controls on shallow-marine and freshwater diatomite deposition throughout the Palaeogene C. Figus et al. 10.5194/cp-20-2629-2024
17. Global decline in ocean ventilation, oxygenation, and productivity during the Paleocene-Eocene Thermal Maximum: Implications for the benthic extinction A. Winguth et al. 10.1130/G32529.1
18. Controls on the barium isotope compositions of marine sediments L. Bridgestock et al. 10.1016/j.epsl.2017.10.019
19. Bentho‐Pelagic Decoupling: The Marine Biological Carbon Pump During Eocene Hyperthermals E. Griffith et al. 10.1029/2020PA004053
20. Eutrophication and Deoxygenation Forcing of Marginal Marine Organic Carbon Burial During the PETM N. Papadomanolaki et al. 10.1029/2021PA004232
21. Swift Weathering Response on Floodplains During the Paleocene‐Eocene Thermal Maximum E. Ramos et al. 10.1029/2021GL097436
22. INCORPORATING INFORMATION ON VARYING SEDIMENTATION RATES INTO PALEONTOLOGICAL ANALYSES N. HOHMANN 10.2110/palo.2020.038
23. Deep-sea redox across the Paleocene-Eocene thermal maximum C. Pälike et al. 10.1002/2013GC005074
24. The Paleocene-Eocene Thermal Maximum: A Perturbation of Carbon Cycle, Climate, and Biosphere with Implications for the Future F. McInerney & S. Wing 10.1146/annurev-earth-040610-133431