Bioavailability of zinc in marine systems through time
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The Cu concentration record for IFs and shales is relatively constant in abundance, reminiscent of the Zn record, raising the possibility of stabilisation of these trace metals by organic ligand complexation.
“Although the Cu concentration record presented by Chi Fru et al. (2016) for IFs and shales is relatively constant in terms of abundance reminiscent of the Zn record raising the possibility of stabilisation of these trace metals by organic ligand complexation (see Robbins et al., 2013; Scott et al., 2013) - there is a clear trend in the stable isotopes values of Cu.”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Scott et al., 2013
An alternative model holds that organismal elemental requirements are driven almost entirely by cellular function, with biological requirements decoupled from environmental abundances.
“The leading alternative to this model is that organismal elemental requirements are driven almost entirely by utility, i.e., cellular function, with shifts in biological requirements decoupled from corresponding environmental abundances (Scott et al., 2013;Robbins et al., 2013;Stüeken et al., 2015a).”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Scott et al., 2013
A direct relationship between concentrations in organic-rich sediments and dissolved concentrations in overlying anoxic and sulfidic bottom waters has been demonstrated for some trace elements such as Mo and Zn.
“(4) a direct relationship between concentrations in organic-rich sediments and dissolved concentrations in overlying anoxic and sulfidic bottom waters has been demonstrated for some trace elements (e.g., Mo, Zn; Algeo and Lyons, 2006;Scott et al., 2013).”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Scott et al., 2013
In the case of Zn, enrichments in black shales and IFs suggest the oceanic Zn reservoir has been relatively constant since the Archean.
“In the case of Zn, the records of enrichments in both black shales and IFs suggest that the size of the oceanic Zn reservoir has been relatively constant since the Archean (Scott et al., 2013;Robbins et al., 2013).”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Scott et al., 2013
For elements like Zn, black shales yield independent data on seawater trace element reservoir evolution that supplements the iron formation record.
“For some trace elements, the black shale record provides valuable independent information about the evolution of seawater trace element reservoirs, such as Zn, complementing the IF record (c.f.Scott et al., 2013 andRobbins et al., 2013).”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Scott et al., 2013
The paleomarine Zn reservoir was on the order of 10 nM, several orders of magnitude above the biolimiting concentration of about 10^-13 M and in excellent agreement with the black shale record.
“Zn reservoir on the order of 10 nM.This value is several orders of magnitude above the ~10 -13 M concentration considered as biolimiting (Brand et al., 1983) and in excellent agreement with the black shale record”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Scott et al., 2013
Seawater Zn levels remained broadly uniform through time at near modern levels and several orders of magnitude above biolimiting concentrations.
“Accordingly, they suggested that seawater Zn levels remained broadly uniform throughout time at near modern levels and several orders of magnitude above concentrations that would be biolimiting.”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Scott et al. (2013)
Scott et al. found no evidence in the Precambrian black shale record for a depleted paleomarine Zn reservoir because average Zn concentrations in Precambrian and Phanerozoic euxinic shales are not significantly different.
“Scott et al. (2013) found there was no evidence in the Precambrian black shale record to infer a depleted paleomarine Zn reservoir-because the average Zn concentration in Precambrian and Phanerozoic euxinic shales are not significantly different.”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Scott et al. (2013)
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- Authors
- Scott, C., Planavsky, N. J., Dupont, C. L., Kendall, B., Gill, B. C., Robbins, L. J., Husband, K. F., Arnold, G. L., Wing, B. A., Poulton, S. W., Bekker, A., Anbar, A. D., Konhauser, K. O., & Lyons, T. W.
- Affiliations
- University of California, Riverside (US)
- University of Waterloo (CA)
- Virginia Tech (US)
- University of Alberta (CA)
- University of Leeds (GB)
- Max Planck Institute for Marine Microbiology (DE)
- McGill University (CA)
- University of Manitoba (CA)
- Arizona State University (US)
- Corresponding author
- Scott, Clint
- ORCID
- Venue
- Nature Geoscience
- Published
- 2012-12-23
- Volume
- 6
- Issue
- 2
- Pages
- 125-128
- ISSN
- 1752-0894 (ISSN-L)
- 1752-0908
- OpenAlex
- W2169895881
- Cited by
- 120
- References
- 33
- Citations by year
- 2026: 7 · 2025: 13 · 2024: 10 · 2023: 10 · 2022: 11 · 2021: 6 · 2020: 7 · 2019: 10 · 2018: 11 · 2017: 13 · 2016: 4 · 2015: 7 · 2014: 7 · 2013: 3 · 2012: 1
- FWCI
- 4.28
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- www.springer.com/tdm (tdm)
- Locations
- Nature Geoscience (publishedVersion)
- Max Planck Digital Library (submittedVersion)
- MPG.PuRe (Max Planck Society) (submittedVersion)
- Funders
- Natural Environment Research Council (NE/I005862/2)
- 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 › Oceanography › Marine and coastal ecosystems
- Keywords
- zinc bioavailability, euxinia, black shales, Precambrian, eukaryotic diversification, hydrothermal flux, ocean redox state, zinc-binding proteins
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