Stomatal index response of Quercus robur and Quercus petraea to the anthropogenic atmospheric CO2 increase

Plant Ecology

Volumn 183, Issue 2, 2006, Pages 237-243

  Van Hoof, Thomas B ^a   Kürschner, Wolfram M ^a   Wagner, Friederike ^a   Visscher, Henk ^a  

^a UTRECHT UNIVERSITY   (Netherlands)

Author keywords

Anthropogenic CO2; Quercus petraea; Quercus robur; Stomatal frequency analysis; Stomatal index

Indexed keywords

ANTHROPOGENIC EFFECT; ATMOSPHERIC CHEMISTRY; CARBON DIOXIDE; DECIDUOUS TREE; ENVIRONMENTAL CONDITIONS; HERBARIUM; LACUSTRINE DEPOSIT; STOMATAL CONDUCTANCE;

BENELUX; EURASIA; EUROPE; NETHERLANDS; WESTERN EUROPE;

QUERCUS PETRAEA; QUERCUS ROBUR;

EID: 33745027381     PISSN: 13850237     EISSN: None     Source Type: Journal    
DOI: 10.1007/s11258-005-9021-3     Document Type: Article

References (23)

1. 2 and temperature on stomatal density: observations from Quercus robur Lammas leaves. Ann. Bot. 71: 231-235.
2. Ellenberger H. 1979. Indicator values of vascular plants in Central Europe. Scripta Geobotanica 9, Göttingen, p. 122.
3. 2 concentrations, Mauna Loa observatory, Hawaii, 1958-2001. Website: http://cdiac.esd.ornl.gov/ndps/ndp001.html.
4. 2. Am. J. Bot. 90: 610-619.
5. 2 fluctuations during the past millennium reconstructed by stomatal frequency analysis of Tsuga heterophylla needles. Geology 33: 33-36.
6. 2 levels. Utrecht University, the Netherlands Ph.D thesis, LPP contribution series No. 5.
7. 2 concentrations. In: Poore R. and Sloane L.C. (eds), Pliocene climates. Mar. Micropaleontol. 27: 299-312.
8. 2 -enriched atmosphere: constraints from historical observations. Geol. Rundsch. 86: 512-517.
9. Levy G., Becker M. and Duhamel D. 1992. A comparison of the ecology of pendunculate and sessile oaks: radial growh in the Centre and Northwest of France. Forest Ecol. Manag. 55: 51-63.
10. 2 in the past two centuries. Nature 315: 45-47.
11. Poole I. and Kürschner W.M. 1999. Stomatal density and index: the practice. In: Jones T.P. and Rowe N.P. (eds.), Fossil Plants and Spores, modern techniques, The Geological Society, London, pp. 257-261.
12. 2 during part of the Tertiary. Science 292: 2310-2313.
13. 2 record from the stomatal index of subfossil Salix herbacea L. leaves from northern Sweden. Holocene 9: 509-513.
14. 2 concentration indicated by high-resolution stomatal index data. Earth Planet. Sci. Lett. 213: 191-204.
15. Salisbury E.J. 1927. On the causes and ecological significance of stomatal frequency, with special reference to the woodland flora. Philos. Trans. Roy. Soc. (London) B 216: 1-65.
16. Vander Burg J., Visscher H., Dilcher D.L. and Kürschner W.M. 1993. Paleoatmospherical signatures in Neogene fossil leaves. Science 260: 1788-1790.
17. 2 and temperature during the onset of the Little Ice Age. Ph.D thesis, LPP contributions series No. 18, Utrecht University, the Netherlands, http://igitur-archive.library.uu.nl/dissertations/2004-1214-121238/index.htm.
18. 2 increase. Proc. Nat. Acad. Sci. USA 93: 11705-11708.
19. 2 concentrations. Science 284: 1971-1973.
20. 2 increase. Am. J. Bot. 92(4): 162-168.
21. 2 records based on stomatal frequency. Quaternary Sci. Rev. 23: 1947-1954.
22. Wagner F., Neuvonen S., Kürschner W.M. and Visscher H. 2000. The influence of hybridization on epidermal properties of birch species and the consequences for palaeoclimatic interpretations. Plant Ecol. 148: 61-69.
23. 2 from pre-industrial levels. Nature 327: 617-618.