The DOI matches its Crossref record; 8 of the 8 references it cites were found in a registry or an index.
Atmospheric oxygen over Phanerozoic time
Open accessAbstract
It is quite possible that the level of atmospheric oxygen has varied (roughly between 15 and 30% O 2 ) over the past 550 million years. This variation is suggested by modeling of the carbon and sulfur cycles, by the excessive sediment burial of organic matter that accompanied the advent of large vascular land plants, and by recent physiological studies that relate to biological evolution.
Overview
The claims and statistics of this paper haven’t been checked yet.
Run the check — free, no account needed. It reads the open-access text and checks the sources it cites.
Integrity signals
Registry
Cites
Statistics
Verification
Claims the paper makes
The claims and statistics of this paper haven’t been checked yet.
Run the check — free, no account needed. It reads the open-access text and checks the sources it cites.
Self-check
Percentages, sums and reported differences re-computed from the paper’s own numbers.
The self-check needs the paper’s full text.
Citations
Cites
The Chemical Evolution of the Atmosphere and Oceans
Holland, H. D. (1984) · doi:10.1515/9780691220239 · Cited by 1,836
Canfield, D. E., & Teske, A. (1996) · Nature · doi:10.1038/382127a0 · Cited by 869
The Rise of Plants and Their Effect on Weathering and Atmospheric CO 2
Berner, R. A. (1997) · Science · doi:10.1126/science.276.5312.544 · Cited by 546
Self-citationRedox Stabilization of the Atmosphere and Oceans by Phosphorus-Limited Marine Productivity
Van Cappellen, P., & Ingall, E. D. (1996) · Science · doi:10.1126/science.271.5248.493 · Cited by 412
Beginnings of biospheric evolution and their biogeochemical consequences
Cloud, P. (1976) · Paleobiology · doi:10.1017/s009483730000498x · Cited by 333
Coupling of the sedimentary sulfur and carbon cycles; an improved model
Garrels, R. M., & Lerman, A. (1984) · American Journal of Science · doi:10.2475/ajs.284.9.989 · Cited by 228
Modeling atmospheric O 2 in the global sedimentary redox cycle
Kump, L. R., & Garrels, R. M. (1986) · American Journal of Science · doi:10.2475/ajs.286.5.337 · Cited by 191
Terrestrial feedback in atmospheric oxygen regulation by fire and phosphorus
Kump, L. R. (1988) · Nature · doi:10.1038/335152a0 · Cited by 115
Cited by
Bowman, D. M. J. S., Balch, J. K., Artaxo, P., Bond, W. J., Carlson, J. M., Cochrane, M. A., D’Antonio, C. M., DeFries, R. S., Doyle, J. C., Harrison, S. P., et al. (2009) · Science · doi:10.1126/science.1163886 · Cited by 3,351
Burdige, D. J. (2007) · Chemical Reviews · doi:10.1021/cr050347q · Cited by 1,310
Sedimentary Corg:P ratios, paleocean ventilation, and Phanerozoic atmospheric pO2
Algeo, T. J., & Ingall, E. (2007) · Palaeogeography, Palaeoclimatology, Palaeoecology · doi:10.1016/j.palaeo.2007.02.029 · Cited by 769
Hohmann-Marriott, M. F., & Blankenship, R. E. (2011) · Annual Review of Plant Biology · doi:10.1146/annurev-arplant-042110-103811 · Cited by 744
Hypoxia Tolerance in Reptiles, Amphibians, and Fishes: Life with Variable Oxygen Availability
Bickler, P. E., & Buck, L. T. (2007) · Annual Review of Physiology · doi:10.1146/annurev.physiol.69.031905.162529 · Cited by 687
The diversification of Paleozoic fire systems and fluctuations in atmospheric oxygen concentration
Scott, A. C., & Glasspool, I. J. (2006) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.0604090103 · Cited by 437
Ordovician and Silurian sea–water chemistry, sea level, and climate: A synopsis
Munnecke, A., Calner, M., Harper, D. A. T., & Servais, T. (2010) · Palaeogeography, Palaeoclimatology, Palaeoecology · doi:10.1016/j.palaeo.2010.08.001 · Cited by 375
Taylor, C. T., & McElwain, J. C. (2010) · Physiology · doi:10.1152/physiol.00029.2010 · Cited by 135
The importance of ocean temperature to global biogeochemistry
Archer, D., Martin, P., Buffett, B., Brovkin, V., Rahmstorf, S., & Ganopolski, A. (2004) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2004.03.011 · Cited by 98
Wheat, C. W., & Wahlberg, N. (2013) · Systematic Biology · doi:10.1093/sysbio/sys074 · Cited by 80
Low oxygen and argon in the Neoproterozoic atmosphere at 815 Ma
Yeung, L. Y. (2017) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2017.09.044 · Cited by 25
Hovering Performance of Hummingbirds in Hyperoxic Gas Mixtures
Altshuler, D. L., Chai, P., & Chen, J. S. P. (2001) · Journal of Experimental Biology · doi:10.1242/jeb.204.11.2021 · Cited by 7
Metadata
- Authors
- Berner, R. A.
- Venue
- Proceedings of the National Academy of Sciences
- Published
- 1999-09-28
- Volume
- 96
- Issue
- 20
- Pages
- 10955-10957
- ISSN
- 0027-8424 (ISSN-L)
- 1091-6490
- OpenAlex
- W2131731927
- Cited by
- 280
- References
- 8
- FWCI
- 5.81
- Type
- journal article
- Language
- en
- Open access
- green
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
Are you an author, or do you see a problem with this page? Request a review
Data sources
Bibliographic data: Semantic Scholar, OpenAlex, Crossref.
Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.
