Nitrogen and organic carbon isotope stratigraphy of the Yangtze Platform during the Ediacaran–Cambrian transition in South China
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Negative δ15N values are concentrated in black shale in interval 3 above the Ni-Mo sulfide layer.
“Further, negative δ15N values are concentrated in black shale in the interval 3 above the Ni-Mo sulfide layer20, 21.”
From Heterogenous oceanic redox conditions through the Ediacaran-Cambrian boundary limited the metazoan zonation (2017) · cites this paper as [20]
The existence of photic-zone anoxia is suggested by largely negative sedimentary N isotope values described from Ediacaran-Cambrian deposits of the Yangtze platform.
“yet the existence of photic-zone anoxia is suggested by largely negative sedimentary N isotope values described from Ediacaran-Cambrian deposits of the Yangtze platform20, 21.”
From Heterogenous oceanic redox conditions through the Ediacaran-Cambrian boundary limited the metazoan zonation (2017) · cites this paper as [20]
During this time, the water column of the shallow shelf remained oxygenated, accumulating widespread carbonate sediment.
“During this time, though, the water column of the shallow shelf remained oxygenated, accumulating widespread carbonate sediment as exemplified by the Xiaotan section in the eastern Yunnan province and studied sections in the Three Gorge Area (Fig. 1)20, 37.”
From Heterogenous oceanic redox conditions through the Ediacaran-Cambrian boundary limited the metazoan zonation (2017) · cites this paper as [20]
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The evolution of Earth's biogeochemical nitrogen cycle
Stüeken, E. E., Kipp, M. A., Koehler, M. C., & Buick, R. (2016) · Earth-Science Reviews · doi:10.1016/j.earscirev.2016.07.007 · Cited by 438 · see citing works
“A recent compilation of δ 15 N data through the Phanerozoic revealed a surprisingly dynamic picture with values near 0‰ and evidence of basinal stratification (Cremonese et al., 2014; Wang et al., 2013) in the early Paleozoic, a rise to values > +2‰ with a maximum of +8‰ from the early Carboniferous to the end of the…”
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MethodCoupling of ocean redox and animal evolution during the Ediacaran-Cambrian transition
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“The present study discusses published d15N profiles within this wider redox context (Cremonese et al., 2013, 2014).”
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“Moreover, the tendency toward low seawater oxygen concentrations subsequently appears to have increased during the Cambrian (Boyle et al., 2014; Cremonese et al., 2014), and persisted into the Ordovician (Railsback et al., 1990; Strauss, 2006; Kah and Bartley, 2011; Thompson and Kah, 2012; Wallace…”
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“From the late Neoproterozoic onwards, nitrate depletion is only reported during temporary anoxic events (e.g. Rau et al., 1987; Sephton et al., 2002; Ohkouchi et al., 2006; Junium and Arthur, 2007; LaPorte et al., 2009; Schoepfer et al., 2012; Wang et al., 2013; Cremonese et al., 2014); throughout most of the Phaneroz…”
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“…Lawrence Och, Dr. Ben Yang, Xi Chen for 2013), shallow platform 15Nbulk data are from Cremonese et al. (2013) and outer helf 15Nbulk data are from Cremonese et al. (2014) and Kikumoto et al. (2014). ndicate that the shallow waters of the basin were well connected ith the oxygenated open ocean…”
BackgroundMethodInfluentialSelf-citationControls on organic matter accumulation on the early-Cambrian western Yangtze Platform, South China
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“This section has 92 been well described in Wang et al. (2012a), Guo et al. (2013), Cremonese et al. (2014), 93 and Och et al. (2016).”
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“Organic-rich shale and mudstone deposition corresponding with low (< 1‰) δ15N values was widespread in South China during Cambrian Stages 1–4 (Cremonese et al., 2013, 2014; Kikumoto et al., 2014; Wang et al., 2015; Zhang et al., 2017), suggesting that these low nitrogen isotope values do not reflect an ecological resp…”
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Extensive primary production promoted the recovery of the Ediacaran Shuram excursion
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Marine C, S and N biogeochemical processes in the redox-stratified early Cambrian Yangtze ocean
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“2013), basal Niutitang Fm in Longbizui and between the Xiaoyanxi Fm and Liuchapo Fm in the Lijiatuo section (Cremonese et al. 2014).”
BackgroundSpatio-temporal evolution of ocean redox and nitrogen cycling in the early Cambrian Yangtze ocean
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Stepwise oxygenation of early Cambrian ocean controls early metazoan diversification
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“The Ediacaran–Cambrian transition interval exhibits decreasing d15N values (Ader et al. 2014), which are consistent with domination by nitrogen fixers and local nitrate starvation at eutrophic ocean margins during the Cambrian radiation (Cremonese et al. 2014).”
BackgroundShift in limiting nutrients in the late Ediacaran–early Cambrian marine systems of South China
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“…the widely distributed siliceous sedimentary rocks, including organic-rich black siliceous shales and cherts have been studied (Dong et al., 2015; Cremonese et al., 2014; Wang et al., 2014; Zhang et al., 2013; Zhou and Jiang, 2009), but more sustained efforts should be carried out to further…”
BackgroundMarine chemical structure during the Cambrian explosion
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“2708 approximately 2–3‰ (Carpenter et al., 1997; Cremonese et al., 2014; Fogel & Cifuentes, 1993; Struck, 2012; Struck et al., 2001, 2004).”
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Benthic redox conditions and nutrient dynamics in the ca. 2.1 Ga Franceville sub-basin
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“This has also been highlighted in the Ediacaran-Phanerozoic settings whereby enhanced denitrification/anammox and sometimes phosphate addition, together with eustatic fluctuations, would have allowed for the expression of N2 fixation in shallow depositional environments (Chang et al., 2019; Cremonese et al., 2014; Wan…”
BackgroundChemostratigraphy as a Formal Stratigraphic Method
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“These TOC/TN ratios, although higher than the Redfield ratio (∼6), are consistent with those reported for shales with similar depositional ages (e.g., Cremonese et al., 2014; Kikumoto et al., 2014).”
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“Paleoenvironmental implications agree favorably with a global anoxia model suggesting upwelling of anoxic water masses to have dramatically affected the biosphere during the Pc-C transition interval (Cremonese et al., 2014).”
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The Cambrian bioradiation event: A Chinese perspective Preface
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“The former process that fractionates nitrogen isotopes by up to −27‰ would have been favored when upwelling was strong, generating negative δ 15 N signatures (e.g., Higgins et al. 2012; Cremonese et al. 2014; Wang et al. 2015, 2018a; Chen et al. 2019).”
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- Authors
- Cremonese, L., Shields-Zhou, G. A., Struck, U., Ling, H.-F., & Och, L. M.
- Affiliations
- University College London (GB)
- Museum für Naturkunde (DE)
- Nanjing University (CN)
- Swiss Federal Institute of Aquatic Science and Technology (CH)
- Corresponding author
- Cremonese, Lorenzo
- Venue
- Palaeogeography, Palaeoclimatology, Palaeoecology
- Publisher
- Elsevier BV
- Published
- 2014-03
- Volume
- 398
- Pages
- 165-186
- ISSN
- 0031-0182 (ISSN-L)
- OpenAlex
- W2084897273
- Cited by
- 86
- References
- 0
- Citations by year
- 2026: 9 · 2025: 7 · 2024: 12 · 2023: 3 · 2022: 6 · 2021: 9 · 2020: 5 · 2019: 8 · 2018: 8 · 2017: 5 · 2016: 8 · 2015: 5 · 2014: 1
- FWCI
- 3.17
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Palaeogeography Palaeoclimatology Palaeoecology (publishedVersion)
- DORA Eawag (Swiss Federal Institute of Aquatic Science and Technology (Eawag)) (submittedVersion)
- 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
- nitrogen isotopes, organic carbon isotopes, Ediacaran-Cambrian transition, Yangtze Platform, biogeochemical cycles, nitrogen fixation, diazotrophic cyanobacteria, stratigraphic correlation, bioturbation, Lower Cambrian
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