Influence of ontogeny and atmospheric CO2 on stomata parameters of Osmunda regalis

CFS Courier Forschungsinstitut Senckenberg

Volumn , Issue 258, 2007, Pages 183-189

  Wagner, Friederike ^a   Visscher, Henk ^a   Kürschner, Wolfram M ^a   Dilcher, David L ^b  

^a UTRECHT UNIVERSITY   (Netherlands)

^b UNIVERSITY OF FLORIDA   (United States)

Author keywords

Atmospheric CO2; Leaf ontogeny; Osmunda ferns; Stomatal density; Stomatal index

Indexed keywords

CARBON DIOXIDE; FERN; MESOZOIC; ONTOGENY; PALEOBOTANY; PALEOZOIC; STOMATA;

FLORIDA [UNITED STATES]; NORTH AMERICA; UNITED STATES;

FILICOPHYTA; OSMUNDA; OSMUNDA REGALIS; OSMUNDACEAE;

EID: 37349117017     PISSN: 03414116     EISSN: None     Source Type: Book Series    
DOI: None     Document Type: Article

References (30)

1. 2 levels during the Permo-Carboniferous glaciation inferred from fossil lycopsids. - Proceedings of the National Academy of Sciences USA, 99: 12567-12571.
2. 2 reconstruction across the Cretaceous-Tertiary boundary from leaf megafossils. - Proceedings of the National Academy of Science USA, 99(12): 7836-7840.
3. 2 over Phanerozoic time. - American Journal of Science, 291: 339-375.
4. KEELING, C. D. & WHORF, T. P. (2000): http://cdiac. esd.ornl.gov/ndps/ndp001.html
5. KOUWENBERG, L. L. R., KÜRSCHNER, W. M. & VISSCHER, H. (2003): Changes in stomatal frequency and size during elongation of Tsuga heterophylla needles. - Annals of Botany, 94: 561-569.
6. 2 fluctuations during the last Millennium reconstructed by stomatal frequency analysis of Tsuga heterophylla needles. - Geology, 33(1): 33-36.
7. 2 concentrations. - Marine Micropaleontology, 27: 299-312.
8. 2-enriched atmosphere: constraints from historical observations. - Geologische Rundschau, 86: 512-517.
9. MCELWAIN, J. C. & CHALONER, W. G. (1995): Stomatal density and index of fossil plants track atmospheric carbon dioxide in the Paleozoic. - Annals of Botany, 76: 389-395.
10. 2 concentration during the Younger Dryas stadial: A comparison with Antarctic ice core records. - Journal of Quaternary Sciences, 17: 21-29.
11. MCELWAIN, J. C., WADE-MURPHY, J. & HESSELDO, S. P. (2005): Changes in carbon dioxide during an oceanic anoxic event linked to intrusion into Gondwana coals. - Nature, 435: 479-482.
12. 2 record from the Siple Station ice core. - In: Trends: A Compendium of Data on Global Change. - Carbon Dioxide Information Analysis Center, Oak Ridge National Laboratory, U.S. Department of Energy, Oak Ridge, Tenn., U.S.A.
13. PHIPPS, C. J., TAYLOR, T. N., TAYLOR, E. L., CÚNEO, R., BOUCHER, L. D. & YAO, X. (1998): Osmunda (Osmundaceae) from the Triassic of Antarctica: an example of evolutionary stasis. -American Journal of Botany, 85: 888-895.
14. PRYER, K. M., SCHUETTPELZ, E., WOLF, P. G., SCHNEIDER, H., SMITH, A. R. & CRANFILL, R. (2004): Phylogeny and evolution of ferns (monilophytes) with a focus on the early leptosporangiate divergences. - American Journal of Botany, 91: 1582-1598.
15. 2 from stomatal indices. - In: WING, S. L., GINGERICH, P. D., SCHMITZ, B. & THOMAS, E. (Eds.): Causes and Consequences of Globally Warm Climates in the Early Paleogene. - Geological Society of America Special Paper, 369: 79-93.
16. 2 during part of the Tertiary. - Science, 292: 2310-2313.
17. 2 record from the stomatal index of subfossil Salix herbacea L. leaves from northern Sweden. - The Holocene, 9: 509-513.
18. 2 concentration indicated by high-resolution stomatal index data. - Earth and Planetary Science Letters, 213: 191-204.
19. SALISBURY, E. J. (1927): On the causes and ecological significance of stomatal frequency, with special reference to the woodland flora. - Philosophical Transactions of the Royal Society of London, B (216): 1-65.
20. STEWART, W. N. & ROTHWELL, G. W. (Eds.) (1993): Paleobotany and the evolution of plants. - Second edition. - 1-521; Cambridge, (Cambridge University Press).
21. TICHÁ, I. (1982): Photosynthetic characteristics during ontogenesis of leaves: 7. Stomata density and sizes. - Photosynthetica, 16(2): 375-471.
22. VAN DER BURGH, J., VISSCHER, H., DILCHER, D. L. & KÜRSCHNER, W. M. (1993): Palaeoatmospheric signatures from in Neogene fossil leaves. - Science, 260: 1788-1790.
23. 12C ratios in Pinus flexilis during the last glacial-interglacial cycle. - Science, 264: 239-242.
24. 2 increase. - Plant Ecology, 183: 237-243.
25. 2 changes associated with the 8.200-years-B.P. cooling event. - Proceedings of the National Academy of Sciences USA, 99: 12011-12014.
26. 2 increase. - American Journal of Botany, 92(4): 690-695.
27. 2 records based on stomatal frequency. - Quaternary Science Reviews, 23: 1947-1954.
28. 2 Concentration. - Science, 284: 1971-1973.
29. 2 increase. - Proceedings of the National Academy of Science USA, 93: 11705-11708.
30. 2 concentration from pre-industrial levels. - Nature, 327: 617-618.