The DOI matches its Crossref record; 21 of the 21 references it cites were found in a registry or an index.
Sensitivity of biomarker properties to depositional environment and/or source input in the Lower Toarcian of SW-Germany
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Citations
Cites
Organic geochemical indicators of palaeoenvironmental conditions of sedimentation
Didyk, B. M., Simoneit, B. R. T., Brassell, S. C., & Eglinton, G. (1978) · Nature · doi:10.1038/272216a0 · Cited by 2,201
Advances in organic geochemistry 1981
Hedges, J. I. (1984) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(84)90367-3 · Cited by 1,932
Anoxic environments and oil source bed genesis
Demaison, G. J., & Moore, G. T. (1980) · Organic Geochemistry · doi:10.1016/0146-6380(80)90017-0 · Cited by 1,529
Relationship Between Petroleum Composition and Depositional Environment of Petroleum Source Rocks
J. Michael Moldowan (2), W. K. (1985) · AAPG Bulletin · doi:10.1306/ad462bc8-16f7-11d7-8645000102c1865d · Cited by 1,366
Seifert, W. K., & Michael Moldowan, J. (1978) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(78)90219-3 · Cited by 1,331
Advances in Organic Geochemistry
(1964) · Elsevier eBooks · doi:10.1016/c2013-0-01767-7 · Cited by 773
The effect of biodegradation on steranes and terpanes in crude oils
Seifert, W. K., & Michael Moldowan, J. (1979) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(79)90051-6 · Cited by 637
Factors controlling the proportionality of vanadium to nickel in crude oils
Lewan, M. D. (1984) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(84)90219-9 · Cited by 528
Paleoreconstruction by biological markers
Seifert, W. K., & Moldowan, J. M. (1981) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(81)90108-3 · Cited by 508
Self-citationRearranged sterenes in a shale: occurrence and simulated formation
Rubinstein, I., Sieskind, O., & Albrecht, P. (1975) · Journal of the Chemical Society, Perkin Transactions 1 · doi:10.1039/p19750001833 · Cited by 346
Cited by
Redox heterogeneity of subsurface waters in the Mesoproterozoic ocean
Sperling, E. A., Rooney, A. D., Hays, L., Sergeev, V. N., Vorob'eva, N. G., Sergeeva, N. D., Selby, D., Johnston, D. T., & Knoll, A. H. (2014) · Geobiology · doi:10.1111/gbi.12091 · Cited by 149
Fossil Lipids for Life-Detection: A Case Study from the Early Earth Record
Eigenbrode, J. L. (2008) · Space Science Reviews · doi:10.1007/s11214-007-9252-9 · Cited by 79
Metadata
- Authors
- Moldowan, J. M., Sundararaman, P., & Schoell, M.
- Venue
- Organic Geochemistry
- Publisher
- Elsevier BV
- Published
- 1986-01
- Volume
- 10
- Issue
- 4-6
- Pages
- 915-926
- ISSN
- 0146-6380 (ISSN-L)
- OpenAlex
- W2053113094
- Cited by
- 586
- References
- 21
- FWCI
- 10.53
- 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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- This page
- CoChat. (2026). Citation check: Sensitivity of biomarker properties to depositional environment and/or source input in the Lower Toarcian of SW-Germany. https://app.cochat.ai/papers/10.1016/s0146-6380(86)80029-8
- The paper
- Moldowan, J. M., Sundararaman, P., & Schoell, M. (1986). Sensitivity of biomarker properties to depositional environment and/or source input in the Lower Toarcian of SW-Germany. Organic Geochemistry. https://doi.org/10.1016/s0146-6380(86)80029-8
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.