The DOI matches its Crossref record; 2 of the 2 references it cites were found in a registry or an index.
Effect of end-Triassic CO2 maximum on carbonate sedimentation and marine mass extinction
Overview
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Citations
Cites
Stanley, S. M., & Hardie, L. A. (1998) · Palaeogeography, Palaeoclimatology, Palaeoecology · doi:10.1016/s0031-0182(98)00109-6 · Cited by 830
An oscillating trend in Phanerozoic non-skeletal carbonate mineralogy
Sandberg, P. A. (1983) · Nature · doi:10.1038/305019a0 · Cited by 818 · cited 1×
“Replacement of shell aragonite by calcite at the T–J boundary was previously (Hautmann 2001a, 2001b) attributed to the shift from aragonite- to calcite-facilitating conditions in the oceans ( Sandberg 1983 ).”
Background
Cited by
Self, S., Widdowson, M., Thordarson, T., & Jay, A. E. (2006) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2006.05.041 · Cited by 287
On the potential for ocean acidification to be a general cause of ancient reef crises
KIESSLING, W., & SIMPSON, C. (2011) · Global Change Biology · doi:10.1111/j.1365-2486.2010.02204.x · Cited by 264
Life in Triassic Oceans: Links Between Planktonic and Benthic Recovery and Radiation
PAYNE, J. L., & VAN DE SCHOOTBRUGGE, B. (2007) · Evolution of Primary Producers in the Sea · doi:10.1016/b978-012370518-1/50010-2 · Cited by 35
Metadata
- Authors
- Hautmann, M.
- Venue
- Facies
- Published
- 2004-07-28
- Volume
- 50
- Issue
- 2
- ISSN
- 0172-9179 (ISSN-L)
- 1612-4820
- OpenAlex
- W2152700412
- Cited by
- 171
- References
- 2
- FWCI
- 6.78
- Type
- journal article
- Language
- en
- Open access
- closed
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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.
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How to cite
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- CoChat. (2026). Citation check: Effect of end-Triassic CO2 maximum on carbonate sedimentation and marine mass extinction. https://app.cochat.ai/papers/10.1007/s10347-004-0020-y
- The paper
- Hautmann, M. (2004). Effect of end-Triassic CO2 maximum on carbonate sedimentation and marine mass extinction. Facies. https://doi.org/10.1007/s10347-004-0020-y
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.