Cited by 277Paleontology and Stratigraphy of FossilsGeochemistry and Elemental AnalysisGeological and Geochemical Analysis

Suboxic deep seawater in the late Paleoproterozoic: evidence from hematitic chert and iron formation related to seafloor-hydrothermal sulfide deposits, central Arizona, USA

Slack, J.F., Grenne, T., Bekker, A., Rouxel, O.J., Lindberg, P.A.·2007·Earth and Planetary Science Letters

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Crossref · 10.1016/j.epsl.2006.12.018

Cites

72 of 72 references verified0 citation errors · 0 not checkable

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  • Redox heterogeneities in the oceans indicate that coeval regions of more and less oxygenated waters may have been a common feature during the boring billion.

    “Finally, the likelihood of redox heterogeneities in the oceans (Slack et al., 2007; Sperling et al., 2014; Reinhard et al., 2016) tells us that coeval regions of more and less oxygenated waters may also have been a common feature during the boring billion.”
  • Trace and rare-earth element systematics of similar volcanogenic massive sulfide deposits formed at approximately 1.8, 1.7, 1.4, and 1.2 Gya reflect weakly oxygenated (suboxic) conditions in the deep ocean for at least some periods of the mid-Proterozoic.

    “The trace and rare-earth element systematics of similar volcanogenic massive sulfide deposits formed at approximately 1.8 Gya, 1.7 Gya, 1.4 Gya, and 1.2 Gya have been interpreted to reflect weakly oxygenated (suboxic) conditions in the deep ocean for at least some periods of the mid-Proterozoic (Little et al. 2021;Slack et al. 2007Slack et al. , 2009)).”

    From The History of Ocean Oxygenation (2022) · cites this paper as Slack et al. 2007

  • The copper-rich composition of volcanogenic massive sulfide deposits requires hydrostatic pressure equivalent to a depth of at least ∼1 km to prevent loss of copper prior to mineralization at the seafloor.

    “Importantly, the copper-rich composition of these deposits requires hydrostatic pressure equivalent to a depth of at least ∼1 km to prevent loss of copper prior to mineralization at the seafloor (Slack et al. 2007(Slack et al. , 2009)).”

    From The History of Ocean Oxygenation (2022) · cites this paper as Slack et al. 2007

  • Volcanogenic massive sulfide deposits provide one of the few windows into true deep-ocean chemistry during mid-Proterozoic time.

    “Volcanogenic massive sulfide deposits, often containing iron-rich chemical sediments and associated sulfide ores rich in copper, provide one of the few windows into true deep-ocean chemistry during mid-Proterozoic time (Slack et al. 2007).”

    From The History of Ocean Oxygenation (2022) · cites this paper as Slack et al. 2007

  • A weakly oxygenated state is fully consistent with constraints based on stable uranium isotope systematics and the geochemistry of deep-sea volcanogenic massive sulfide deposits.

    “and is fully consistent with constraints based on stable uranium isotope systematics (Yang et al. 2017) and the geochemistry of deep-sea volcanogenic massive sulfide deposits (Slack et al. 2007(Slack et al. , 2009)).”

    From The History of Ocean Oxygenation (2022) · cites this paper as Slack et al. 2007

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Authors
Slack, J. F., Grenne, T., Bekker, A., Rouxel, O. J., & Lindberg, P. A.
Affiliations
  • United States Geological Survey (US)
  • Geological Survey of Norway (NO)
  • Carnegie Institution for Science (US)
  • Woods Hole Oceanographic Institution (US)
  • Laboratoire Interdisciplinaire des Énergies de Demain (FR)
Corresponding author
Slack, J.F.
Venue
Earth and Planetary Science Letters
Publisher
Elsevier BV
Published
2007-03
Volume
255
Issue
1-2
Pages
243-256
ISSN
0012-821X (ISSN-L)
OpenAlex
W2166950793
Cited by
277
References
75
Citations by year
2026: 9 · 2025: 13 · 2024: 20 · 2023: 20 · 2022: 17 · 2021: 14 · 2020: 19 · 2019: 7 · 2018: 24 · 2017: 8 · 2016: 21 · 2015: 18 · 2014: 13 · 2013: 18 · 2012: 13
FWCI
5.33
Type
journal article
Language
en
Open access
closed
Locations
Earth and Planetary Science Letters (publishedVersion)
Funders
  • Carnegie Institution of Washington
  • U.S. Geological Survey
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 › Geophysics › Geological and Geochemical Analysis
Keywords
Late Paleoproterozoic, banded iron formations, jasper, volcanogenic massive sulfide deposits, seafloor hydrothermal deposits, rare earth elements, cerium anomaly, central Arizona

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