240 related articles for article (PubMed ID: 21071667)
1. Effects of rapid global warming at the Paleocene-Eocene boundary on neotropical vegetation.
Jaramillo C; Ochoa D; Contreras L; Pagani M; Carvajal-Ortiz H; Pratt LM; Krishnan S; Cardona A; Romero M; Quiroz L; Rodriguez G; Rueda MJ; de la Parra F; Morón S; Green W; Bayona G; Montes C; Quintero O; Ramirez R; Mora G; Schouten S; Bermudez H; Navarrete R; Parra F; Alvarán M; Osorno J; Crowley JL; Valencia V; Vervoort J
Science; 2010 Nov; 330(6006):957-61. PubMed ID: 21071667
[TBL] [Abstract][Full Text] [Related]
2. Cenozoic plant diversity in the neotropics.
Jaramillo C; Rueda MJ; Mora G
Science; 2006 Mar; 311(5769):1893-6. PubMed ID: 16574860
[TBL] [Abstract][Full Text] [Related]
3. Nannoplankton extinction and origination across the Paleocene-Eocene Thermal Maximum.
Gibbs SJ; Bown PR; Sessa JA; Bralower TJ; Wilson PA
Science; 2006 Dec; 314(5806):1770-3. PubMed ID: 17170303
[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. A transient rise in tropical sea surface temperature during the Paleocene-Eocene thermal maximum.
Zachos JC; Wara MW; Bohaty S; Delaney ML; Petrizzo MR; Brill A; Bralower TJ; Premoli-Silva I
Science; 2003 Nov; 302(5650):1551-4. PubMed ID: 14576441
[TBL] [Abstract][Full Text] [Related]
6. 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]
7. 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]
8. Tropical forest carbon balance in a warmer world: a critical review spanning microbial- to ecosystem-scale processes.
Wood TE; Cavaleri MA; Reed SC
Biol Rev Camb Philos Soc; 2012 Nov; 87(4):912-27. PubMed ID: 22607308
[TBL] [Abstract][Full Text] [Related]
9. 48,000 years of climate and forest change in a biodiversity hot spot.
Bush MB; Silman MR; Urrego DH
Science; 2004 Feb; 303(5659):827-9. PubMed ID: 14764876
[TBL] [Abstract][Full Text] [Related]
10. Termination of global warmth at the Palaeocene/Eocene boundary through productivity feedback.
Bains S; Norris RD; Corfield RM; Faul KL
Nature; 2000 Sep; 407(6801):171-4. PubMed ID: 11001051
[TBL] [Abstract][Full Text] [Related]
11. Diversity in neotropical wet forests during the Cenozoic is linked more to atmospheric CO2 than temperature.
Royer DL; Chernoff B
Proc Biol Sci; 2013 Aug; 280(1764):20131024. PubMed ID: 23760866
[TBL] [Abstract][Full Text] [Related]
12. Decoupled plant and insect diversity after the end-Cretaceous extinction.
Wilf P; Labandeira CC; Johnson KR; Ellis B
Science; 2006 Aug; 313(5790):1112-5. PubMed ID: 16931760
[TBL] [Abstract][Full Text] [Related]
13. 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]
14. Impact ejecta at the Paleocene-Eocene boundary.
Schaller MF; Fung MK; Wright JD; Katz ME; Kent DV
Science; 2016 Oct; 354(6309):225-229. PubMed ID: 27738171
[TBL] [Abstract][Full Text] [Related]
15. Net carbon dioxide losses of northern ecosystems in response to autumn warming.
Piao S; Ciais P; Friedlingstein P; Peylin P; Reichstein M; Luyssaert S; Margolis H; Fang J; Barr A; Chen A; Grelle A; Hollinger DY; Laurila T; Lindroth A; Richardson AD; Vesala T
Nature; 2008 Jan; 451(7174):49-52. PubMed ID: 18172494
[TBL] [Abstract][Full Text] [Related]
16. A tropical rainforest in Colorado 1.4 million years after the Cretaceous-Tertiary boundary.
Johnson KR; Ellis B
Science; 2002 Jun; 296(5577):2379-83. PubMed ID: 12089439
[TBL] [Abstract][Full Text] [Related]
17. Deep-sea temperature and circulation changes at the Paleocene-Eocene Thermal Maximum.
Tripati A; Elderfield H
Science; 2005 Jun; 308(5730):1894-8. PubMed ID: 15976299
[TBL] [Abstract][Full Text] [Related]
18. Late Paleocene fossils from the Cerrejon Formation, Colombia, are the earliest record of Neotropical rainforest.
Wing SL; Herrera F; Jaramillo CA; Gómez-Navarro C; Wilf P; Labandeira CC
Proc Natl Acad Sci U S A; 2009 Nov; 106(44):18627-32. PubMed ID: 19833876
[TBL] [Abstract][Full Text] [Related]
19. 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]
20. Long series relationships between global interannual CO2 increment and climate: evidence for stability and change in role of the tropical and boreal-temperate zones.
Adams JM; Piovesan G
Chemosphere; 2005 Jun; 59(11):1595-612. PubMed ID: 15878607
[TBL] [Abstract][Full Text] [Related]
[Next] [New Search]
