Tectonic-driven climate change and the diversification of angiosperms

Proceedings of the National Academy of Sciences of the United States of America

Volumn 111, Issue 39, 2014, Pages 14066-14070

  Chaboureau, Anne Claire ^a   Sepulchre, Pierre ^a   Donnadieu, Yannick ^a   Franc, Alain ^b  

^a LABORATOIRE DES SCIENCES DU CLIMAT ET DE L ENVIRONNEMENT   (France)

^b CEMAGREF   (France)

Author keywords

Climate modeling; Paleogeography

Indexed keywords

ANGIOSPERM; BIOLOGICAL MODEL; CLASSIFICATION; CLIMATE CHANGE; ECOSYSTEM; EVOLUTION; FOSSIL; GENETIC VARIABILITY; GENETICS; HISTORY; PALEONTOLOGY; SPECIES DIFFERENTIATION;

ANGIOSPERMS; BIOLOGICAL EVOLUTION; CLIMATE CHANGE; ECOSYSTEM; FOSSILS; GENETIC SPECIATION; GENETIC VARIATION; HISTORY, ANCIENT; MODELS, BIOLOGICAL; PALEONTOLOGY;

EID: 84907588598     PISSN: 00278424     EISSN: 10916490     Source Type: Journal    
DOI: 10.1073/pnas.1324002111     Document Type: Review

References (43)

1. Friis EM, Crane PR, Pedersen KR (2011) Early Flowers and Angiosperm Evolution (Cambridge Univ Press, Cambridge, UK).
2. Magallón S, Castillo A (2009) Angiosperm diversification through time. Am J Bot 96(1):349-365.
3. Darwin F, Seward AC (1903) More Letters of Charles Darwin. A Record of His Work in a Series of Hitherto Unpublished Letters (John Murray, London), Vols 1 and 2.
4. Lupia R, Crane PR, Lidgard S (2000) Biotic Response to Global Change: The Last 145 Million Years, eds Culver SJ, Rawson PF (Cambridge Univ Press, Cambridge, UK), pp 223-243.
5. Crepet WL, Niklas KJ (2009) Darwin's second 'abominable mystery': Why are there so many angiosperm species? Am J Bot 96(1):366-381.
6. Grimaldi D (1999) The co-radiations of pollinating insects and angiosperms in the Cretaceous. Ann Mo Bot Gard 86(2):373-406.
7. Farrell BD (1998) "Inordinate fondness" explained: Why are there so many beetles? Science 281(5376):555-559.
8. Busch A, Zachgo S (2009) Flower symmetry evolution: Towards understanding the abominable mystery of angiosperm radiation. BioEssays 31(11):1181-1190.
9. Boyce CK, Lee JE (2010) An exceptional role for flowering plant physiology in the expansion of tropical rainforests and biodiversity. Proc Biol Sci 277(1699):3437-3443.
10. de Boer HJ, Eppinga MB, Wassen MJ, Dekker SC (2012) A critical transition in leaf evolution facilitated the Cretaceous angiosperm revolution. Nat Commun 3(1221): 1221.
11. Feild TS, et al. (2011) Fossil evidence for Cretaceous escalation in angiosperm leaf vein evolution. Proc Natl Acad Sci USA 108(20):8363-8366.
12. Davies TJ, et al. (2004) Darwin's abominable mystery: Insights from a supertree of the angiosperms. Proc Natl Acad Sci USA 101(7):1904-1909.
13. McElwain JC, Willis K, Lupia R (2005) A History of Atmospheric CO2 and Its Effects on Plants, Animals, and Ecosystems, eds Baldwin IT, et al. (Springer, New York), pp 133-165.
14. Coiffard C, Gómez B (2012) Influence of latitude and climate on spread, radiation and rise to dominance of early angiosperms during the Cretaceous in the Northern Hemisphere. Geol Acta 10(2):181-188.
15. Coiffard C, Gomez B, Daviero-Gomez V, Dilcher DL (2012) Rise to dominance of angiosperm pioneers in European Cretaceous environments. Proc Natl Acad Sci USA 109(51):20955-20959.
16. Pucéat E, Lécuyer C, Sheppard SMF, Dromart G, Reboulet S, Grandjean P (2003) Thermal evolution of Cretaceous Tethyan marine waters inferred from oxygen isotope composition of fish tooth enamels. Paleoceanography 18(2):7-1-7-12.
17. Price GD, Passey BH (2013) Dynamic polar climates in a greenhouse world: Evidence from clumped isotope thermometry of early Cretaceous belemnites. Geology 41(8): 923-926.
18. Littler K, Robinson SA, Bown PR, Nederbragt AJ, Pancost RD (2011) High sea-surface temperatures during the Early Cretaceous Epoch. Nat Geosci 4(3):169-172.
19. Sinninghe Damsté JS, van Bentum ZC, Reichart G-J, Pross J, Schouten S (2010) A CO2 decrease-driven cooling and increased latitudinal temperature gradient during the mid-Cretaceous Oceanic Anoxic Event 2. Earth Planet Sci Lett 248(1-2):426-437.
20. Mutterlose J, Malkoc M, Schouten S, Sinninghe Damsté JS, Forste A (2010) TEX86 and stable 18O paleothermometry of early Cretaceous sediments: Implications for belemnite ecology and paleotemperature proxy application. Earth Planet Sci Lett 298(3-4):286-298.
21. Pucéat E, et al. (2010) Revised phosphate-water fractionation equation reassessing paleotemperatures derived from biogenic apatite. Earth Planet Sci Lett 298(1-2): 135-142.
22. Pucéat E, et al. (2007) Fish tooth 18 O revising Late Cretaceous meridional upper ocean water temperature gradients. Geology 35(2):107-110.
23. Steuber T, Rauch M, Masse J-P, Graaf J, Malkoc M (2005) Low-latitude seasonality of Cretaceous temperatures in warm and cold episodes. Nature 437(7063):1341-1344.
24. Bice KL, Norris RD (2002) Possible atmospheric CO2 extremes of the Middle Cretaceous (late Albian-Turonian). Paleoceanography 17(4):22-1-22-17.
25. Pearson PN, et al. (2001) Warm tropical sea surface temperatures in the Late Cretaceous and Eocene epochs. Nature 413(6855):481-487.
26. Donnadieu Y, Goddéris Y, Pierrehumbert R, Fluteau F, Dromart G (2006) Modelling the primary control of paleogeography on Cretaceous climate. Geochem Geophys Geosyst 7(11):Q11019.
27. Lidgard S, Crane PR (1990) Angiosperm diversification and Cretaceous floristic trends: a comparison of palynofloras and leaf macrofloras. Paleobiology 16(1):77-93.
28. Spicer RA, et al. (2008) The Late Cretaceous continental interior of Siberia: A challenge for climate models. Earth Planet Sci Lett 267(1-2):228-235.
29. Kump LR, Pollard D (2008) Amplification of Cretaceous warmth by biological cloud feedbacks. Science 320(5873):195.
30. Beerling DJ, Fox A, Stevenson DS, Valdes PJ (2011) Enhanced chemistry-climate feedbacks in past greenhouse worlds. Proc Natl Acad Sci USA 108(24):9770-9775.
31. Wikström N, Savolainen V, Chase MW (2001) Evolution of the angiosperms: calibrating the family tree. Proc Biol Sci 268(1482):2211-2220.
32. Zhou Z, Barrett PM, Hilton J (2003) An exceptionally preserved Lower Cretaceous ecosystem. Nature 421(6925):807-814.
33. Wang H, et al. (2009) Rosid radiation and the rapid rise of angiosperm-dominated forests. Proc Natl Acad Sci USA 106(10):3853-3858.
34. Miller KG, Mountain GS, Wright JD, Browning JVA (2011) 180-million-year record of sea level and ice volume variations from continental margin and deep-sea isotopic records. Oceanography 24(2):40-53.
35. Boyce CK, Brodribb TJ, Feild TS, Zwieniecki MA (2009) Angiosperm leaf vein evolution was physiologically and environmentally transformative. Proc Biol Sci 276(1663): 1771-1776.
36. Jacob RL (1997) Low frequency variability in a simulated atmosphere ocean system. Thesis (Univ of Wisconsin, Madison).
37. Poulsen CJ, Pierrehumbert RT, Jacob RL (2001) Impact of ocean dynamics on the simulation of the Neoproterozoic "snowball Earth". Geophys Res Lett 28(8): 1575-1578.
38. Poulsen CJ, Jacob RL, Pierrehumbert RT, Huynh TT (2002) Testing paleogeographic controls on a Neoproterozoic snowball Earth. Geophys Res Lett 29(11):10-1-10-4.
39. Poulsen CJ (2003) Absence of a runaway ice-albedo feedback in the Neoproterozoic. Geology 31(6):473-476.
40. Sitch S, et al. (2003) Evaluation of ecosystem dynamics, plant geography and terrestrial carbon cycling in the LPJ dynamic global vegetation model. Global Change Biol 9(2):161-185.
41. Donnadieu Y, Goddéris Y, Bouttes N (2009) Exploring the climatic impact of the continental vegetation on the Mezosoic atmospheric CO2 and climate history. Clim Past 5(1):85-96.
42. Sewall JO, Wal RSW, van de Zwan CJ, van der Oosterhout C, Dijkstra HA, Scotese CR (2007) Climate model boundary conditions for four Cretaceous time slices. Clim Past 3(4):647-657.
43. Dera G, Donnadieu Y (2012) Modeling evidences for global warming, Arctic seawater freshening, and sluggish oceanic circulation during the Early Toarcian anoxic event. Paleoceanography 27(2):PA2211.