94 citations as recorded by crossref.

1. Lithological and Geochemical Characteristics of the Paleocene/Eocene Sediments corresponding to the PETM Biospheric Event in the Eastern Crimea (Nasypnoe Section) Y. Gavrilov et al. 10.1134/S0024490218050048
2. PLANT COMMUNITY CHANGE ACROSS THE PALEOCENE–EOCENE BOUNDARY IN THE GULF COASTAL PLAIN, CENTRAL TEXAS J. WAGNER et al. 10.2110/palo.2022.008
3. Synchronous Marine and Terrestrial Carbon Cycle Perturbation in the High Arctic During the PETM Y. Cui et al. 10.1029/2020PA003942
4. Isotopic filtering reveals high sensitivity of planktic calcifiers to Paleocene–Eocene thermal maximum warming and acidification B. Hupp et al. 10.1073/pnas.2115561119
5. Carbon isotope chemostratigraphy, geochemistry, and biostratigraphy of the Paleocene–Eocene Thermal Maximum, deepwater Wilcox Group, Gulf of Mexico (USA) G. Sharman et al. 10.5194/cp-19-1743-2023
6. Authigenic Fe Mineralization in Shallow to Marginal Marine Environments: A Case Study from the Late Paleocene—Early Eocene Cambay Shale Formation T. Roy Choudhury et al. 10.3390/min13050646
7. Climate-driven hydrological change and carbonate platform demise induced by the Paleocene–Eocene Thermal Maximum (southern Pyrenees) J. Li et al. 10.1016/j.palaeo.2021.110250
8. Eutrophication and Deoxygenation Forcing of Marginal Marine Organic Carbon Burial During the PETM N. Papadomanolaki et al. 10.1029/2021PA004232
9. Coastal Response to Global Warming During the Paleocene-Eocene Thermal Maximum G. Sharman et al. 10.2139/ssrn.4200185
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11. Impact of Eocene‐Oligocene Antarctic Glaciation on the Paleoceanography of the Weddell Sea V. Hojnacki et al. 10.1029/2022PA004440
12. The importance of organic-rich shales to the geochemical cycles of rhenium and osmium A. Dubin & B. Peucker-Ehrenbrink 10.1016/j.chemgeo.2015.03.010
13. Widespread Warming Before and Elevated Barium Burial During the Paleocene‐Eocene Thermal Maximum: Evidence for Methane Hydrate Release? J. Frieling et al. 10.1029/2018PA003425
14. Hyperthermal events recorded in the Palaeogene carbonate sequence of southern Gulf of Mexico—Santa Elena borehole, Yucatan Peninsula E. García‐Garnica & L. Pérez‐Cruz 10.1002/gj.4285
15. Thermogenic methane release as a cause for the long duration of the PETM J. Frieling et al. 10.1073/pnas.1603348113
16. Global Changes in Terrestrial Vegetation and Continental Climate During the Paleocene‐Eocene Thermal Maximum V. Korasidis et al. 10.1029/2021PA004325
17. A new stratigraphic framework and constraints for the position of the Paleocene–Eocene boundary in the rapidly subsiding Hanna Basin, Wyoming M. Dechesne et al. 10.1130/GES02118.1
18. The DeepMIP contribution to PMIP4: methodologies for selection, compilation and analysis of latest Paleocene and early Eocene climate proxy data, incorporating version 0.1 of the DeepMIP database C. Hollis et al. 10.5194/gmd-12-3149-2019
19. Shallow Water Records of the PETM: Novel Insights From NE India (Eastern Tethys) S. Sarkar et al. 10.1029/2021PA004257
20. Eustatic change across the Paleocene-Eocene Thermal Maximum in the epicontinental Tarim seaway J. Jiang et al. 10.1016/j.gloplacha.2023.104241
21. Spatial and Temporal Patterns in Petrogenic Organic Carbon Mobilization During the Paleocene‐Eocene Thermal Maximum E. Hollingsworth et al. 10.1029/2023PA004773
22. Maastrichtian–Rupelian paleoclimates in the southwest Pacific – a critical re-evaluation of biomarker paleothermometry and dinoflagellate cyst paleoecology at Ocean Drilling Program Site 1172 P. Bijl et al. 10.5194/cp-17-2393-2021
23. Tropical ocean temperatures and changes in terrigenous flux during the Paleocene-Eocene Thermal Maximum in southern Tibet S. Jin et al. 10.1016/j.gloplacha.2023.104289
24. The PhanSST global database of Phanerozoic sea surface temperature proxy data E. Judd et al. 10.1038/s41597-022-01826-0
25. Assessing environmental change associated with early Eocene hyperthermals in the Atlantic Coastal Plain, USA W. Rush et al. 10.5194/cp-19-1677-2023
26. A heated mirror for future climate R. Alley 10.1126/science.aaf4837
27. Impact of organic carbon reworking upon GDGT temperature proxies during the Paleocene-Eocene Thermal Maximum G. Inglis et al. 10.1016/j.orggeochem.2023.104644
28. Enhanced phosphorus recycling during past oceanic anoxia amplified by low rates of apatite authigenesis N. Papadomanolaki et al. 10.1126/sciadv.abn2370
29. Iron fertilization–induced deoxygenation of eastern equatorial Pacific Ocean intermediate waters during the Paleocene–Eocene thermal maximum X. Jiang et al. 10.1130/G51770.1
30. Confounding effects of oxygen and temperature on the TEX 86 signature of marine Thaumarchaeota W. Qin et al. 10.1073/pnas.1501568112
31. Comparing Seawater Temperature Proxy Records for the Past 90 Myrs From the Shallow Shelf Record Bass River, New Jersey M. de Bar et al. 10.1029/2018PA003453
32. Coastal response to global warming during the Paleocene-Eocene Thermal Maximum G. Sharman et al. 10.1016/j.palaeo.2023.111664
33. Changes in the occurrence of extreme precipitation events at the Paleocene–Eocene thermal maximum M. Carmichael et al. 10.1016/j.epsl.2018.08.005
34. Changes in benthic ecosystems and ocean circulation in the Southeast Atlantic across Eocene Thermal Maximum 2 S. Jennions et al. 10.1002/2015PA002821
35. Life and death in the Chicxulub impact crater: a record of the Paleocene–Eocene Thermal Maximum V. Smith et al. 10.5194/cp-16-1889-2020
36. Southern Ocean carbonate dissolution paced by Antarctic Ice-Sheet expansion in the early Miocene G. Tagliaro et al. 10.1016/j.gloplacha.2021.103510
37. Palynology from ground zero of the Chicxulub impact, southern Gulf of Mexico V. Smith et al. 10.1080/01916122.2020.1813826
38. Glauconite authigenesis during the onset of the Paleocene-Eocene Thermal Maximum: A case study from the Khuiala Formation in Jaisalmer Basin, India T. Roy Choudhury et al. 10.1016/j.palaeo.2021.110388
39. Shallow marine ecosystem collapse and recovery during the Paleocene-Eocene Thermal Maximum S. Tian et al. 10.1016/j.gloplacha.2021.103649
40. Two types of hyperthermal events in the Mesozoic-Cenozoic: Environmental impacts, biotic effects, and driving mechanisms X. Hu et al. 10.1007/s11430-019-9604-4
41. 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
42. Spatial heterogeneity in carbonate-platform environments and carbon isotope values across the Paleocene–Eocene thermal maximum (Tethys Himalaya, South Tibet) J. Li et al. 10.1016/j.gloplacha.2022.103853
43. Extreme warmth and heat-stressed plankton in the tropics during the Paleocene-Eocene Thermal Maximum J. Frieling et al. 10.1126/sciadv.1600891
44. Glauconite authigenesis during the warm climatic events of Paleogene: Case studies from shallow marine sections of Western India T. Roy Choudhury et al. 10.1016/j.gloplacha.2022.103857
45. Gypsum in diatomaceous strata of the trans-urals region: Morphology, lithogeochemistry, and genetic link to global warming at the paleocene-eocene boundary P. Smirnov et al. 10.1016/j.sedgeo.2022.106295
46. Drivers and constraints on floral latitudinal diversification gradients P. Jardine et al. 10.1111/jbi.13216
47. Tracing North Atlantic volcanism and seaway connectivity across the Paleocene–Eocene Thermal Maximum (PETM) M. Jones et al. 10.5194/cp-19-1623-2023
48. Flood Basalts and Mass Extinctions M. Clapham & P. Renne 10.1146/annurev-earth-053018-060136
49. Ecological Changes in the Nannoplankton Community Across A Shelf Transect During the Onset of the Paleocene‐Eocene Thermal Maximum I. León y León et al. 10.1029/2018PA003383
50. Resilience of marine invertebrate communities during the early Cenozoic hyperthermals W. Foster et al. 10.1038/s41598-020-58986-5
51. New fossils, systematics, and biogeography of the oldest known crown primate Teilhardina from the earliest Eocene of Asia, Europe, and North America P. Morse et al. 10.1016/j.jhevol.2018.08.005
52. End-Cretaceous to middle Eocene events from the Alpine Tethys: Multi-proxy data from a reference section at Kršteňany (Western Carpathians) J. Soták et al. 10.1016/j.palaeo.2021.110571
53. The Eurasian epicontinental sea was an important carbon sink during the Palaeocene-Eocene thermal maximum M. Kaya et al. 10.1038/s43247-022-00451-4
54. Geochemistry and depositional environments of Paleocene–Eocene phosphorites: Metlaoui Group, Tunisia H. Garnit et al. 10.1016/j.jafrearsci.2017.07.021
55. A study on benthic molluscs and stable isotopes from Kutch, western India reveals early Eocene hyperthermals and pronounced transgression during ETM2 and H2 events A. Mitra et al. 10.1186/s13358-022-00255-1
56. Estimating regional flood discharge during Palaeocene-Eocene global warming C. Chen et al. 10.1038/s41598-018-31076-3
57. Enhanced storm-induced turbiditic events during early Paleogene hyperthermals (Arabian continental margin, SW Iran) J. Jiang et al. 10.1016/j.gloplacha.2022.103832
58. Shallow-water hydrothermal venting linked to the Palaeocene–Eocene Thermal Maximum C. Berndt et al. 10.1038/s41561-023-01246-8
59. Warming and environmental changes in the eastern North Sea Basin during the Palaeocene–Eocene Thermal Maximum as revealed by biomarker lipids P. Schoon et al. 10.1016/j.orggeochem.2014.11.003
60. Paleoenvironmental Conditions during the Paleocene–Eocene Transition Imprinted within the Glauconitic Giral Member of the Barmer Basin, India T. Roy Choudhury et al. 10.3390/min12010056
61. The Oligo-Miocene siliciclastic foreland basin deposits of northern Tunisia:Stratigraphy, sedimentology and paleogeography K. Boukhalfa et al. 10.1016/j.jafrearsci.2020.103932
62. Did the PETM trigger the first important radiation of wetzelielloideans? Evidence from France and northern Kazakhstan A. Iakovleva 10.1080/01916122.2016.1173121
63. A mammal fauna from the Paleocene-Eocene Thermal Maximum of Croydon, London, UK J. Hooker 10.1016/j.pgeola.2018.01.001
64. Eocene paleoceanographic and paleoclimatic events recognized by assemblages of dinoflagellate cysts in the Southwest Atlantic Ocean E. Premaor et al. 10.1016/j.jsames.2023.104587
65. Cretaceous sea-surface temperature evolution: Constraints from TEX86 and planktonic foraminiferal oxygen isotopes C. O'Brien et al. 10.1016/j.earscirev.2017.07.012
66. Sulfur isotope composition of individual compounds in immature organic-rich rocks and possible geochemical implications L. Shawar et al. 10.1016/j.gca.2020.01.034
67. Carbon isotope and biostratigraphic evidence for an expanded Paleocene–Eocene Thermal Maximum sedimentary record in the deep Gulf of Mexico L. Vimpere et al. 10.1130/G50641.1
68. Towards quantitative environmental reconstructions from ancient non-analogue microfossil assemblages: Ecological preferences of Paleocene – Eocene dinoflagellates J. Frieling & A. Sluijs 10.1016/j.earscirev.2018.08.014
69. Perturbation to the nitrogen cycle during rapid Early Eocene global warming C. Junium et al. 10.1038/s41467-018-05486-w
70. A review on palaeogeographic implications and temporal variation in glaucony composition S. Banerjee et al. 10.1016/j.jop.2015.12.001
71. Simulation of Eocene extreme warmth and high climate sensitivity through cloud feedbacks J. Zhu et al. 10.1126/sciadv.aax1874
72. Control of climate and Tethyan legacy on distribution of Paleocene–Eocene gastropods and establishment of the Northern Tropical Realm S. Das & K. Halder 10.1007/s12040-018-0959-7
73. The large decline in carbonate δ238U from a PETM section at Tingri (South Tibet) was driven by local sea-level changes, not global oceanic anoxia Q. Zhang et al. 10.1016/j.epsl.2023.118164
74. Stratigraphic and sedimentological aspects of the worldwide distribution ofApectodiniumin Paleocene/Eocene Thermal Maximum deposits C. Denison 10.1144/SP511-2020-46
75. Dynamics of sediment flux to a bathyal continental margin section through the Paleocene–Eocene Thermal Maximum T. Dunkley Jones et al. 10.5194/cp-14-1035-2018
76. Paleoclimate determines diversification patterns in the fossorial snake family Uropeltidae Cuvier, 1829 V. Cyriac & U. Kodandaramaiah 10.1016/j.ympev.2017.08.017
77. Shelf hypoxia in response to global warming after the Cretaceous-Paleogene boundary impact J. Vellekoop et al. 10.1130/G45000.1
78. Productivity and organic carbon trends through the Wilcox Group in the deep Gulf of Mexico: Evidence for ventilation during the Paleocene-Eocene Thermal Maximum R. Cunningham et al. 10.1016/j.marpetgeo.2022.105634
79. Terrestrial environmental change across the onset of the PETM and the associated impact on biomarker proxies: A cautionary tale G. Inglis et al. 10.1016/j.gloplacha.2019.102991
80. The formation of authigenic deposits during Paleogene warm climatic intervals: a review S. Banerjee et al. 10.1186/s42501-020-00076-8
81. Plate tectonics controls ocean oxygen levels K. Meissner & A. Oschlies 10.1038/d41586-022-02187-9
82. New specimens of the mesonychid Dissacus praenuntius from the early Eocene of Wyoming and evaluation of body size through the PETM in North America F. Solé et al. 10.1016/j.geobios.2021.02.005
83. Changes in sulfur cycling in a large lake during the Paleocene-Eocene Thermal Maximum and implications for lake deoxygenation X. Wang et al. 10.1016/j.gloplacha.2021.103716
84. Tropical Atlantic climate and ecosystem regime shifts during the Paleocene–Eocene Thermal Maximum J. Frieling et al. 10.5194/cp-14-39-2018
85. Little lasting impact of the Paleocene-Eocene Thermal Maximum on shallow marine molluscan faunas L. Ivany et al. 10.1126/sciadv.aat5528
86. Hydrological and associated biogeochemical consequences of rapid global warming during the Paleocene-Eocene Thermal Maximum M. Carmichael et al. 10.1016/j.gloplacha.2017.07.014
87. Manifestation, Drivers, and Emergence of Open Ocean Deoxygenation L. Levin 10.1146/annurev-marine-121916-063359
88. Eocene sediments and a fresh to brackish water biota from the early rifting stage of the Upper Rhine Graben (west of oil field Landau, southwest Germany): implications for biostratigraphy, palaeoecology and source rock potential C. Hartkopf-Fröder et al. 10.1007/s12549-023-00577-z
89. Biostratigraphically significant palynofloras from the Paleocene–Eocene boundary of the USA V. Korasidis et al. 10.1080/01916122.2022.2115159
90. Redox-controlled carbon and phosphorus burial: A mechanism for enhanced organic carbon sequestration during the PETM N. Komar & R. Zeebe 10.1016/j.epsl.2017.09.011
91. Descent toward the Icehouse: Eocene sea surface cooling inferred from GDGT distributions G. Inglis et al. 10.1002/2014PA002723
92. The spread of marine anoxia on the northern Tethys margin during the Paleocene-Eocene Thermal Maximum A. Dickson et al. 10.1002/2014PA002629
93. Carbon Isotope Record of Trace n‐alkanes in a Continental PETM Section Recovered by the Bighorn Basin Coring Project (BBCP) A. Baczynski et al. 10.1029/2019PA003579
94. Upper limits on the extent of seafloor anoxia during the PETM from uranium isotopes M. Clarkson et al. 10.1038/s41467-020-20486-5