Fossil leaves: Effective bioindicators of ancient CO2 levels?

Geochemistry, Geophysics, Geosystems

Volumn 4, Issue 7, 2003, Pages

  Rundgren, Mats ^a   Beerling, David ^b  

^a LUND UNIVERSITY   (Sweden)

^b UNIVERSITY OF SHEFFIELD   (United Kingdom)

Author keywords

Paleobotany; Quaternary; Stomata; Younger dryas

Indexed keywords

EID: 19944370768     PISSN: 15252027     EISSN: 15252027     Source Type: Journal    
DOI: 10.1029/2002GC000463     Document Type: Article

References (29)

1. Anderson, D. M., and D. A. Archer, Glacial-interglacial stability of ocean pH inferred from foraminifer dissolution rates, Nature, 416, 70-73, 2002.
2. Beerling, D. J., Stomatal density and index: Theory and application, in Fossil Plants and Spores. Modern Techniques, edited by T. P. Jones and N. P. Rowe, pp. 251-256, Geol. Soc. of London, London, 1999.
3. 2 signal from fossil stomata, New Phytol., 153, 387-398, 2002.
4. 2 changes reconstructed from the stomatal density record of fossil leaves, J. Quat. Sci., 10, 379-384, 1995.
5. 2 concentrations, Science, 286, 1815a-1815, 1999.
6. 2) of the paleoatmosphere, Global Biogeochem. Cycles, 6, 307-314, 1992.
7. 2 over the last 1000 years from air in Antarctic ice and firn, J. Geophys. Res., 101, 4115-4128, 1996.
8. 2 perception to stomatal development, Nature, 408, 713-716, 2000.
9. 2 trapped in ice at Taylor Dome, Antarctica, Nature, 398, 121-126, 1999.
10. 2 in the central equatorial Pacific during the last 255,000 years, Paleoceanography, 9, 781-798, 1994.
11. Johnsen, S. J., D. Dahl-Jensen, N. Gundestrup, J. P. Steffensen, H. B. Clausen, H. Miller, V. Masson-Delmotte, A. E. Sveinbjo ̈rnsdottir, and J. White, Oxygen isotope and palaeotemperature records from six Greenland ice-core stations: Camp Century, Dye-3, GRIP, GISP2, Renland and NorthGRIP, J. Quat. Sci., 16, 299-307, 2001.
12. McElwain, J. C., D. J. Beerling, and F. I. Woodward, Fossil plants and global warming at the Triassic-Jurassic boundary, Science, 285, 1386-1390, 1999.
13. 2 concentration during the Younger Dryas stadial: A comparison with Antarctic ice core records, J. Quat. Sci., 17, 21-29, 2002.
14. 2 concentrations over the last glacial termination, Science, 291, 112-114, 2001.
15. 2 content, temperature and global ice volume over the past 420 ka, Quat. Sci. Rev., 20, 583-589, 2001.
16. 2 proxy, Paleoceanography, 17(4), 1069, doi:10.1029/ 2002PA000756, 2002.
17. 2 in the Western equatorial Pacific Ocean, Science, 300, 480-482, 2003.
18. Petit, J. R., et al., Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica, Nature, 399, 429-436, 1999.
19. 2 concentration, Rev. Palaeobot. Palynol., 114, 1-28, 2001.
20. 2 change: Evaluating geochemical and paleobiological approaches, Earth Sci. Rev., 54, 349-392, 2001a.
21. 2 during part of the Tertiary, Science, 292, 2310-2313, 2001b.
22. 2 record from the stomatal index of subfossil Salix herbacea L. leaves from northern Sweden, The Holocene, 9, 509-513, 1999.
23. 2 during the last interglacial, Geology, 30, 187-189, 2002.
24. 2 concentration indicated by high-resolution stomatal index data, Earth Planet. Sci. Lett., in press, 2003.
25. Shackleton, N. J., The 100,000-year ice-age cycle identified and found to lag temperature, carbon dioxide, and orbital eccentricity, Science, 289, 1897-1902, 2000.
26. 2 concentration and millennial-scale climate change during the last glacial period, Nature, 392, 59-61, 1998.
27. Wagner, F., S. J. P. Bohncke, D. L. Dilcher, W. M. Kürschner, B. van Geel, and H. Visscher, Science, 284, 1971-1973, 1999.
28. 2 changes associated with the 8,200-years-B.P. cooling event, Proc. Natl. Acad. Sci. U.S.A., 99, 12,011-12,014, 2002.
29. 2 from pre-industrial levels, Nature, 327, 617-618, 1987.