The DOI matches its Crossref record; 5 of the 5 references it cites were found in a registry or an index.
CO 2 -Forced Climate and Vegetation Instability During Late Paleozoic Deglaciation
Abstract
The late Paleozoic deglaciation is the vegetated Earth's only recorded icehouse-to-greenhouse transition, yet the climate dynamics remain enigmatic. By using the stable isotopic compositions of soil-formed minerals, fossil-plant matter, and shallow-water brachiopods, we estimated atmospheric partial pressure of carbon dioxide ( p CO 2 ) and tropical marine surface temperatures during this climate transition. Comparison to southern Gondwanan glacial records documents covariance between inferred shifts in p CO 2 , temperature, and ice volume consistent with greenhouse gas forcing of climate. Major restructuring of paleotropical flora in western Euramerica occurred in step with climate and p CO 2 shifts, illustrating the biotic impact associated with past CO 2 -forced turnover to a permanent ice-free world.
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Cites
87Sr/86Sr, δ13C and δ18O evolution of Phanerozoic seawater
Veizer, J., Ala, D., Azmy, K., Bruckschen, P., Buhl, D., Bruhn, F., Carden, G. A. F., Diener, A., Ebneth, S., Godderis, Y., et al. (1999) · Chemical Geology · doi:10.1016/s0009-2541(99)00081-9 · Cited by 2,694
Equilibrium and nonequilibrium oxygen isotope effects in synthetic carbonates
Kim, S.-T., & O'Neil, J. R. (1997) · Geochimica et Cosmochimica Acta · doi:10.1016/s0016-7037(97)00169-5 · Cited by 2,558
GEOCARB III: A revised model of atmospheric CO2 over Phanerozoic time
Berner, R. A. (2001) · American Journal of Science · doi:10.2475/ajs.301.2.182 · Cited by 1,323
Beck, W. C., Grossman, E. L., & Morse, J. W. (2005) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2005.02.003 · Cited by 240
Middle to Late Paleozoic Atmospheric CO 2 Levels from Soil Carbonate and Organic Matter
Mora, C. I., Driese, S. G., & Colarusso, L. A. (1996) · Science · doi:10.1126/science.271.5252.1105 · Cited by 239
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Environmental analysis of paleoceanographic systems based on molybdenum–uranium covariation
Algeo, T. J., & Tribovillard, N. (2009) · Chemical Geology · doi:10.1016/j.chemgeo.2009.09.001 · Cited by 1,631
Future climate forcing potentially without precedent in the last 420 million years
Foster, G. L., Royer, D. L., & Lunt, D. J. (2017) · Nature Communications · doi:10.1038/ncomms14845 · Cited by 774
A high resolution summary of Cambrian to early Triassic marine invertebrate biodiversity
Fan, J.-X., Shen, S.-Z., Erwin, D. H., Sadler, P. M., MacLeod, N., Cheng, Q.-M., Hou, X.-D., Yang, J., Wang, X.-D., Wang, Y., et al. (2020) · Science · doi:10.1126/science.aax4953 · Cited by 583
Breecker, D. O., Sharp, Z. D., & McFadden, L. D. (2009) · Geological Society of America Bulletin · doi:10.1130/b26413.1 · Cited by 429
Metadata
- Authors
- Montañez, I. P., Tabor, N. J., Niemeier, D., DiMichele, W. A., Frank, T. D., Fielding, C. R., Isbell, J. L., Birgenheier, L. P., & Rygel, M. C.
- Venue
- Science
- Published
- 2007-01-05
- Volume
- 315
- Issue
- 5808
- Pages
- 87-91
- ISSN
- 0036-8075 (ISSN-L)
- 1095-9203
- OpenAlex
- W2073986814
- Cited by
- 579
- References
- 5
- FWCI
- 21.12
- Type
- journal article
- Language
- en
- Open access
- closed
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