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C-Isotope stratigraphy, a monitor of paleoenvironmental change: A case study from the early cretaceous
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Apatite-glauconite associations off Peru and Chile: palaeo-oceanographic implications
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The High-Latitude Ocean as a Control of Atmospheric CO2
Wenk, T., & Siegenthaler, U. (2011) · Geophysical monograph · doi:10.1029/gm032p0185 · Cited by 64
Predicted shift in the 13C/12C ratio of atmospheric carbon dioxide
Keeling, C. D., Bacastow, R. B., & Tans, P. P. (1980) · Geophysical Research Letters · doi:10.1029/gl007i007p00505 · Cited by 64
Southam, J. R., Peterson, W. H., & Brass, G. W. (1982) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/0031-0182(82)90089-x · Cited by 59
The acceleration of the hydrogeochemical cycling of phosphorus
Stumm, W. (1973) · Water Research · doi:10.1016/0043-1354(73)90158-9 · Cited by 54
Stable isotopes in recent larger foraminifera
Wefer, G., Killingley, J. S., & Lutze, G. F. (1981) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/0031-0182(81)90042-0 · Cited by 53
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Palaeo-upwelling and the distribution of organic-rich rocks
Parrish, J. T. (1987) · Geological Society London Special Publications · doi:10.1144/gsl.sp.1987.026.01.12 · Cited by 43
Continental drift and the global pattern of sedimentation
Hay, W. W., Barron, E. J., Sloan, J. L., & Southam, J. R. (1981) · Geologische Rundschau · doi:10.1007/bf01764330 · Cited by 43
The Climate-Chemistry Connection
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A model of organic sedimentation on present-day continental margins
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Is there a tie between atmosphere CO2 content and ocean circulation
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High frequency sea-level fluctuations in Cretaceous time: An emerging geophysical problem
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Stable Isotopes in Foraminifera
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Changes in the organic carbon burial during the Early Cretaceous
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Turbidites, the principal mechanism yielding black shales in the early deep Atlantic Ocean
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THE ACCELERATION OF THE HYDROGEOCHEMICAL CYCLING OF PHOSPHORUS
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Cited by
Jenkyns, H. C., Gale, A. S., & Corfield, R. M. (1994) · Geological Magazine · doi:10.1017/s0016756800010451 · Cited by 666
Weissert, H., Lini, A., Föllmi, K. B., & Kuhn, O. (1998) · Palaeogeography, Palaeoclimatology, Palaeoecology · doi:10.1016/s0031-0182(97)00109-0 · Cited by 561
Self-citationJones, C. E. (2001) · American Journal of Science · doi:10.2475/ajs.301.2.112 · Cited by 537
High‐resolution δ13C stratigraphy through the Early Aptian “Livello selli” of the Alpine tethys
Menegatti, A. P., Weissert, H., Brown, R. S., Tyson, R. V., Farrimond, P., Strasser, A., & Caron, M. (1998) · Paleoceanography · doi:10.1029/98pa01793 · Cited by 521
Self-citationHerrle, J. O., Pross, J., Friedrich, O., Kößler, P., & Hemleben, C. (2003) · Palaeogeography, Palaeoclimatology, Palaeoecology · doi:10.1016/s0031-0182(02)00616-8 · Cited by 260
Metadata
- Authors
- Weissert, H.
- Venue
- Surveys in Geophysics
- Published
- 1989-02
- Volume
- 10
- Issue
- 1
- Pages
- 1-61
- ISSN
- 0046-5763 (ISSN-L)
- 0169-3298
- 1573-0956
- OpenAlex
- W2008060356
- Cited by
- 270
- References
- 151
- FWCI
- 3.26
- Type
- journal article
- Language
- en
- Open access
- closed
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.
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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.