Paleo-marine environments of the Early Cambrian Yangtze Platform
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Benthic redox conditions likely fluctuated frequently in intra-shelf basin areas of the Yangtze Sea.
“Benthic redox conditions likely fluctuated frequently in intra-shelf basin areas of the Yangtze Sea as suggested by documented authigenic Mo-U co-variation18.”
From Heterogenous oceanic redox conditions through the Ediacaran-Cambrian boundary limited the metazoan zonation (2017) · cites this paper as [18]
Intra-shelf basins, including the depositional site of the Zhongnan section, became anoxic or even euxinic.
“Intra-shelf basins, including the depositional site of the Zhongnan section, became anoxic or even euxinic, as suggested by the present and previous investigations18, 35.”
From Heterogenous oceanic redox conditions through the Ediacaran-Cambrian boundary limited the metazoan zonation (2017) · cites this paper as [18]
Enrichment of trace metals accelerated across the basin at this time.
“Enrichment of trace metals appears to have accelerated across the basin at this time18, 34.”
From Heterogenous oceanic redox conditions through the Ediacaran-Cambrian boundary limited the metazoan zonation (2017) · cites this paper as [18]
Accelerated upwelling at this time enhanced surface water productivity, thereby increasing the flux of organic matter to the ocean floor, which further reduced bottom-water conditions.
“Accelerated upwelling at this time enhanced surface water productivity18 thereby increasing the flux of organic matter to the ocean floor, which further reduced bottom-water conditions.”
From Heterogenous oceanic redox conditions through the Ediacaran-Cambrian boundary limited the metazoan zonation (2017) · cites this paper as [18]
The intra-shelf basin within which deposits of the Zhongnan section accumulated was likely weakly restricted.
“According to this classification, the intra-shelf basin within which deposits of the Zhongnan section accumulated was likely weakly restricted18.”
From Heterogenous oceanic redox conditions through the Ediacaran-Cambrian boundary limited the metazoan zonation (2017) · cites this paper as [18]
Cites
Trace metals as paleoredox and paleoproductivity proxies: An update
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Self-citationEnvironmental analysis of paleoceanographic systems based on molybdenum–uranium covariation
Algeo, T. J., & Tribovillard, N. (2009) · Chemical Geology · doi:10.1016/j.chemgeo.2009.09.001 · Cited by 1,631 · see citing works
Self-citationAlgeo, T. J., & Lyons, T. W. (2006) · Paleoceanography · doi:10.1029/2004pa001112 · Cited by 1,194 · see citing works
Self-citationProterozoic Ocean Chemistry and Evolution: A Bioinorganic Bridge?
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Tracing the stepwise oxygenation of the Proterozoic ocean
Scott, C., Lyons, T. W., Bekker, A., Shen, Y., Poulton, S. W., Chu, X., & Anbar, A. D. (2008) · Nature · doi:10.1038/nature06811 · Cited by 1,098 · see citing works
Canfield, D. E., & Teske, A. (1996) · Nature · doi:10.1038/382127a0 · Cited by 869 · see citing works
Ferruginous Conditions Dominated Later Neoproterozoic Deep-Water Chemistry
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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 · see citing works
Self-citationCalibration of Sulfate Levels in the Archean Ocean
Habicht, K. S., Gade, M., Thamdrup, B., Berg, P., & Canfield, D. E. (2002) · Science · doi:10.1126/science.1078265 · Cited by 756 · see citing works
Paleoceanographic applications of trace-metal concentration data
Algeo, T. J., & Rowe, H. (2012) · Chemical Geology · doi:10.1016/j.chemgeo.2011.09.002 · Cited by 537 · see citing works
Self-citationSteiner, M., Li, G., Qian, Y., Zhu, M., & Erdtmann, B.-D. (2007) · Palaeogeography, Palaeoclimatology, Palaeoecology · doi:10.1016/j.palaeo.2007.03.046 · Cited by 479 · see citing works
Hydrogen sulphide release to surface waters at the Precambrian/Cambrian boundary
Wille, M., Nägler, T. F., Lehmann, B., Schröder, S., & Kramers, J. D. (2008) · Nature · doi:10.1038/nature07072 · Cited by 259 · see citing works
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Further SHRIMP geochronology on the early Cambrian of South China
Compston, W., Zhang, Z., Cooper, J. A., Ma, G., & Jenkins, R. J. F. (2008) · American Journal of Science · doi:10.2475/04.2008.01 · Cited by 159 · see citing works
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Zhang, J., Fan, T., Zhang, Y., Lash, G. G., Li, Y., & Wu, Y. (2017) · Scientific Reports · doi:10.1038/s41598-017-07904-3 · Cited by 39 · see citing works
Self-citationLi, W.-P., Zhao, Y.-Y., Zhao, M.-Y., Zha, X.-P., & Zheng, Y.-F. (2019) · Scientific Reports · doi:10.1038/s41598-019-47142-3 · Cited by 19 · see citing works
Fan, Q., Fan, T., Zhu, Z., & Li, Q. (2024) · Frontiers in Earth Science · doi:10.3389/feart.2024.1331413 · Cited by 1 · see citing works
Self-citation
- Authors
- Zhang, J., Fan, T., Algeo, T. J., Li, Y., & Zhang, J.
- Affiliations
- China University of Geosciences (CN)
- Corresponding author
- Zhang, Junpeng
- Venue
- Palaeogeography, Palaeoclimatology, Palaeoecology
- Publisher
- Elsevier BV
- Published
- 2016-02
- Volume
- 443
- Pages
- 66-79
- ISSN
- 0031-0182 (ISSN-L)
- OpenAlex
- W2185711520
- Cited by
- 72
- References
- 16
- Citations by year
- 2026: 4 · 2025: 9 · 2024: 6 · 2023: 4 · 2022: 7 · 2021: 6 · 2020: 10 · 2019: 7 · 2018: 9 · 2017: 7 · 2016: 3
- FWCI
- 4.80
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Palaeogeography Palaeoclimatology Palaeoecology (publishedVersion)
- Funders
- Ministry of Science and Technology of China (2009GYXQ15-04)
- U.S. National Science Foundation (EAR-0618003, EAR-0745574)
- NASA
- SKL-GPMR (GPMR201301)
- SKL-BGEG (BGL21407)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
- Keywords
- Lower Cambrian, Yangtze Platform, Niutitang Formation, redox-sensitive elements, deep-water oxygenation, trace metal enrichment, eustasy, Guizhou
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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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