The DOI matches its Crossref record; 72 of the 72 references it cites were found in a registry or an index.
The origin of decoupled carbonate and organic carbon isotope signatures in the early Cambrian (ca. 542–520 Ma) Yangtze platform
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Citations
Cites
Isotopic evidence for source of diagenetic carbonates formed during burial of organic-rich sediments
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“, 2010) to the latest Ediacaran Period (b560 Ma; Fike et al., 2006; McFadden et al., 2008; Rothman et al., 2003).”
BackgroundInfluentialHayes, J. M., Strauss, H., & Kaufman, A. J. (1999) · Chemical Geology · doi:10.1016/s0009-2541(99)00083-2 · Cited by 843 · cited 3×
“Statistic review of paired carbonate and organic carbon isotopes from the geological record suggests that organic matter with Δδ13C values ≥32‰ must have involved chemoautotrophic biomass contribution (Hayes et al., 1999).”
BackgroundFerruginous Conditions Dominated Later Neoproterozoic Deep-Water Chemistry
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Cited by
Marine productivity changes during the end-Permian crisis and Early Triassic recovery
Shen, J., Schoepfer, S. D., Feng, Q., Zhou, L., Yu, J., Song, H., Wei, H., & Algeo, T. J. (2015) · Earth-Science Reviews · doi:10.1016/j.earscirev.2014.11.002 · Cited by 329
Feng, L., Li, C., Huang, J., Chang, H., & Chu, X. (2014) · Precambrian Research · doi:10.1016/j.precamres.2014.03.002 · Cited by 193
Extensive marine anoxia during the terminal Ediacaran Period
Zhang, F., Xiao, S., Kendall, B., Romaniello, S. J., Cui, H., Meyer, M., Gilleaudeau, G. J., Kaufman, A. J., & Anbar, A. D. (2018) · Science Advances · doi:10.1126/sciadv.aan8983 · Cited by 180
Self-citationNew Ediacara fossils preserved in marine limestone and their ecological implications
Chen, Z., Zhou, C., Xiao, S., Wang, W., Guan, C., Hua, H., & Yuan, X. (2014) · Scientific Reports · doi:10.1038/srep04180 · Cited by 167
Self-citationTrace fossil evidence for Ediacaran bilaterian animals with complex behaviors
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Metadata
- Authors
- Jiang, G., Wang, X., Shi, X., Xiao, S., Zhang, S., & Dong, J.
- Venue
- Earth and Planetary Science Letters
- Publisher
- Elsevier BV
- Published
- 2012-02
- Volume
- 317-318
- Pages
- 96-110
- ISSN
- 0012-821X (ISSN-L)
- OpenAlex
- W1989230282
- Cited by
- 276
- References
- 72
- FWCI
- 6.03
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- www.elsevier.com/tdm/userlicense/1.0/ (tdm)
- www.elsevier.com/legal/tdmrep-license (tdm)
- doi.org/10.15223/policy-017 (stm-asf)
- doi.org/10.15223/policy-037 (stm-asf)
- doi.org/10.15223/policy-012 (stm-asf)
- doi.org/10.15223/policy-029 (stm-asf)
- doi.org/10.15223/policy-004 (stm-asf)
- Funders
- National Science Foundation (EAR-0745825, EAR-0745827)
- National Natural Science Foundation of China (40621002)
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- CoChat. (2026). Citation check: The origin of decoupled carbonate and organic carbon isotope signatures in the early Cambrian (ca. 542–520 Ma) Yangtze platform. https://app.cochat.ai/papers/10.1016/j.epsl.2011.11.018
- The paper
- Jiang, G., Wang, X., Shi, X., Xiao, S., Zhang, S., & Dong, J. (2012). The origin of decoupled carbonate and organic carbon isotope signatures in the early Cambrian (ca. 542–520 Ma) Yangtze platform. Earth and Planetary Science Letters. https://doi.org/10.1016/j.epsl.2011.11.018
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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.