Cited by 234Paleontology and Stratigraphy of FossilsGeology and Paleoclimatology ResearchGeological formations and processes

Global synchronous changes in the carbon isotopic composition of carbonate sediments unrelated to changes in the global carbon cycle

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Swart, Peter K.·2008·Proceedings of the National Academy of Sciences

Abstract

The carbon isotopic (delta(13)C) composition of bulk carbonate sediments deposited off the margins of four carbonate platforms/ramp systems (Bahamas, Maldives, Queensland Plateau, and Great Australian Bight) show synchronous changes over the past 0 to 10 million years. However, these variations are different from the established global pattern in the delta(13)C measured in the open oceans over the same time period. For example, from 10 Ma to the present, the delta(13)C of open oceanic carbonate has decreased, whereas platform margin sediments analyzed here show an increase. It is suggested that the delta(13)C patterns in the marginal platform deposits are produced through admixing of aragonite-rich sediments, which have relatively positive delta(13)C values, with pelagic materials, which have lower delta(13)C values. As the more isotopically positive shallow-water carbonate sediments are only produced when the platforms are flooded, there is a connection between changes in global sea level and the delta(13)C of sediments in marginal settings. These data indicate that globally synchronous changes in delta(13)C can take place that are completely unrelated to variations in the global carbon cycle. Fluctuations in the delta(13)C of carbonate sediments measured during previous geological periods may also be subject to similar processes, and global synchroniety of delta(13)C can no longer necessarily be considered an indicator that such changes are related to, or caused by, variati…

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Crossref · 10.1073/pnas.0802841105

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  • Modern Bahama Bank water masses and related carbonate sediments are up to 5% enriched in 13C compared to the adjacent open ocean.

    “For example, the water masses, and related carbonate sediments, on modern Bahama Bank are up to 5% enriched in 13C compared to the adjacent open ocean (Swaart, 2008).”

    From Evolution of Sedimentary Rocks (2014) · cites this paper as Swaart, 2008

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Authors
Swart, P. K.
Affiliations
University of Miami (US)
Corresponding author
Swart, Peter K.
Venue
Proceedings of the National Academy of Sciences
Published
2008-09-16
Volume
105
Issue
37
Pages
13741-13745
ISSN
  • 0027-8424 (ISSN-L)
  • 1091-6490
OpenAlex
W2065756726
Cited by
234
References
5
Citations by year
2026: 15 · 2025: 16 · 2024: 15 · 2023: 13 · 2022: 12 · 2021: 18 · 2020: 24 · 2019: 19 · 2018: 12 · 2017: 16 · 2016: 8 · 2015: 15 · 2014: 7 · 2013: 12 · 2012: 13
FWCI
4.29
Type
journal article
Language
en
Open access
Locations
  • Proceedings of the National Academy of Sciences (publishedVersion)
  • PubMed Central (publishedVersion)
  • PubMed (publishedVersion)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
  • Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
  • Physical Sciences › Earth and Planetary Sciences › Earth-Surface Processes › Geological formations and processes
Keywords
carbon isotopes, carbonate sediments, carbonate platform, carbonate ramp, aragonite, pelagic carbonates, sediment mixing, global sea level change, organic carbon burial, carbon cycle, Bahamas, Maldives, Queensland Plateau, Great Australian Bight, Miocene-Pliocene
MeSH terms
Calcium Carbonate, Carbon, Carbon Isotopes, Carbonates, X-Ray Diffraction, Ecosystem, Geologic Sediments

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