232 related articles for article (PubMed ID: 27354522)
1. Temperature and atmospheric CO2 concentration estimates through the PETM using triple oxygen isotope analysis of mammalian bioapatite.
Gehler A; Gingerich PD; Pack A
Proc Natl Acad Sci U S A; 2016 Jul; 113(28):7739-44. PubMed ID: 27354522
[TBL] [Abstract][Full Text] [Related]
2. Continental warming preceding the Palaeocene-Eocene thermal maximum.
Secord R; Gingerich PD; Lohmann KC; Macleod KG
Nature; 2010 Oct; 467(7318):955-8. PubMed ID: 20962843
[TBL] [Abstract][Full Text] [Related]
3. Evolution of the earliest horses driven by climate change in the Paleocene-Eocene Thermal Maximum.
Secord R; Bloch JI; Chester SG; Boyer DM; Wood AR; Wing SL; Kraus MJ; McInerney FA; Krigbaum J
Science; 2012 Feb; 335(6071):959-62. PubMed ID: 22363006
[TBL] [Abstract][Full Text] [Related]
4. Transient floral change and rapid global warming at the Paleocene-Eocene boundary.
Wing SL; Harrington GJ; Smith FA; Bloch JI; Boyer DM; Freeman KH
Science; 2005 Nov; 310(5750):993-6. PubMed ID: 16284173
[TBL] [Abstract][Full Text] [Related]
5. Cenozoic mean greenhouse gases and temperature changes with reference to the Anthropocene.
Glikson A
Glob Chang Biol; 2016 Dec; 22(12):3843-3858. PubMed ID: 27151305
[TBL] [Abstract][Full Text] [Related]
6. The Palaeocene-Eocene carbon isotope excursion: constraints from individual shell planktonic foraminifer records.
Zachos JC; Bohaty SM; John CM; McCarren H; Kelly DC; Nielsen T
Philos Trans A Math Phys Eng Sci; 2007 Jul; 365(1856):1829-42. PubMed ID: 17513259
[TBL] [Abstract][Full Text] [Related]
7. A humid climate state during the Palaeocene/Eocene thermal maximum.
Bowen GJ; Beerling DJ; Koch PL; Zachos JC; Quattlebaum T
Nature; 2004 Nov; 432(7016):495-9. PubMed ID: 15565152
[TBL] [Abstract][Full Text] [Related]
8. Evidence for rapid climate change in the Mesozoic-Palaeogene greenhouse world.
Jenkyns HC
Philos Trans A Math Phys Eng Sci; 2003 Sep; 361(1810):1885-916; discussion 1916. PubMed ID: 14558900
[TBL] [Abstract][Full Text] [Related]
9. Plant response to a global greenhouse event 56 million years ago.
Wing SL; Currano ED
Am J Bot; 2013 Jul; 100(7):1234-54. PubMed ID: 23825133
[TBL] [Abstract][Full Text] [Related]
10. Thermogenic methane release as a cause for the long duration of the PETM.
Frieling J; Svensen HH; Planke S; Cramwinckel MJ; Selnes H; Sluijs A
Proc Natl Acad Sci U S A; 2016 Oct; 113(43):12059-12064. PubMed ID: 27790990
[TBL] [Abstract][Full Text] [Related]
11. The carbon isotope composition of ancient CO2 based on higher-plant organic matter.
Gröcke DR
Philos Trans A Math Phys Eng Sci; 2002 Apr; 360(1793):633-58. PubMed ID: 12804297
[TBL] [Abstract][Full Text] [Related]
12. Constraints on the onset duration of the Paleocene-Eocene Thermal Maximum.
Turner SK
Philos Trans A Math Phys Eng Sci; 2018 Oct; 376(2130):. PubMed ID: 30177565
[TBL] [Abstract][Full Text] [Related]
13. A Palaeogene perspective on climate sensitivity and methane hydrate instability.
Dunkley Jones T; Ridgwell A; Lunt DJ; Maslin MA; Schmidt DN; Valdes PJ
Philos Trans A Math Phys Eng Sci; 2010 May; 368(1919):2395-415. PubMed ID: 20403834
[TBL] [Abstract][Full Text] [Related]
14. Widespread Warming Before and Elevated Barium Burial During the Paleocene-Eocene Thermal Maximum: Evidence for Methane Hydrate Release?
Frieling J; Peterse F; Lunt DJ; Bohaty SM; Sinninghe Damsté JS; Reichart GJ; Sluijs A
Paleoceanogr Paleoclimatol; 2019 Apr; 34(4):546-566. PubMed ID: 31245790
[TBL] [Abstract][Full Text] [Related]
15. Spatial patterns of climate change across the Paleocene-Eocene Thermal Maximum.
Tierney JE; Zhu J; Li M; Ridgwell A; Hakim GJ; Poulsen CJ; Whiteford RDM; Rae JWB; Kump LR
Proc Natl Acad Sci U S A; 2022 Oct; 119(42):e2205326119. PubMed ID: 36215472
[TBL] [Abstract][Full Text] [Related]
16. Environment and evolution through the Paleocene-Eocene thermal maximum.
Gingerich PD
Trends Ecol Evol; 2006 May; 21(5):246-53. PubMed ID: 16697910
[TBL] [Abstract][Full Text] [Related]
17. Phosphate oxygen isotope analysis on microsamples of bioapatite: removal of organic contamination and minimization of sample size.
Wiedemann-Bidlack FB; Colman AS; Fogel ML
Rapid Commun Mass Spectrom; 2008 Jun; 22(12):1807-16. PubMed ID: 18470876
[TBL] [Abstract][Full Text] [Related]
18. Changes in carbon dioxide during an oceanic anoxic event linked to intrusion into Gondwana coals.
McElwain JC; Wade-Murphy J; Hesselbo SP
Nature; 2005 May; 435(7041):479-82. PubMed ID: 15917805
[TBL] [Abstract][Full Text] [Related]
19. Changing atmospheric CO2 concentration was the primary driver of early Cenozoic climate.
Anagnostou E; John EH; Edgar KM; Foster GL; Ridgwell A; Inglis GN; Pancost RD; Lunt DJ; Pearson PN
Nature; 2016 May; 533(7603):380-4. PubMed ID: 27111509
[TBL] [Abstract][Full Text] [Related]
20. Evidence for a rapid release of carbon at the Paleocene-Eocene thermal maximum.
Wright JD; Schaller MF
Proc Natl Acad Sci U S A; 2013 Oct; 110(40):15908-13. PubMed ID: 24043840
[TBL] [Abstract][Full Text] [Related]
[Next] [New Search]