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Research Article

Fish as major carbonate mud producers and missing components of the tropical carbonate factory

Chris T. Perry, Michael A. Salter, Alastair R. Harborne, Stephen F. Crowley, Howard L. Jelks, and Rod W. Wilson
PNAS March 8, 2011 108 (10) 3865-3869; https://doi.org/10.1073/pnas.1015895108
Chris T. Perry
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  • For correspondence: c.t.perry@mmu.ac.uk r.w.wilson@ex.ac.uk
Michael A. Salter
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Alastair R. Harborne
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Stephen F. Crowley
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Howard L. Jelks
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Rod W. Wilson
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  • For correspondence: c.t.perry@mmu.ac.uk r.w.wilson@ex.ac.uk
  1. Edited* by George N. Somero, Stanford University, Pacific Grove, CA, and approved January 6, 2011 (received for review November 2, 2010)

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    Fig. 1.

    Fish carbonate production and precipitation products. Schematic diagram illustrating the processes associated with carbonate precipitation within the intestines of fish and the dominant crystallite morphologies identified in this study to be produced by tropical fish species.

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    Fig. 2.

    Common morphologies of tropical fish-produced carbonate precipitates. (A) Type 1—Ellipsoidal crystallites (size range: < 0.25 to 3 μm long); (B) Type 2—Straw-bundle crystallites (size range: 1–3 μm long); (C) Type 3—Polycrystalline dumbbell-shaped aggregates (size range: typically 1–3 μm long, but large examples to ∼10–15 μm also occur); (D) Type 4—Polycrystalline spheroidal aggregates (size range: < 10 to 30 μm diameter). Occur both as discrete spheres and as multilobate aggregations of spheres; (E) Large polycrystalline aggregates with a semisphere morphology (size range: ∼5 to ∼30 μm diameter); (F) Elongate rod-like crystallites which often occur as intergrown bundles of crystallites (size range: 2–3 μm long); (G) Splayed ellipsoidal crystallites (size range ∼2 μm long and narrow towards their terminal points).

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    Fig. 3.

    Comparison of mole% MgCO3 of fish-derived carbonates and skeletal Mg-calcite producing benthic organisms. Latitudinal data for skeletal benthic organisms (white circles) from Chave (25). Fish-derived data from Eleuthera at 25° N plotted as average MgCO3 contents (+/-1 s.d.) (black circles) based on EDX analysis (n = 50 analyses per fish) of dominant crystallite morphologies observed in each species. Samples are grouped based on the dominant crystal morphology associated with each fish species.

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    Fig. 4.

    Estimates of fish carbonate production across the Bahamian archipelago. Summary diagram showing estimated volumes of carbonate (millions kg CaCO3/yr) produced in different habitats across the Bahamas. Production volume estimates are based on measured fish body mass and carbonate excretion data, combined with known habitat-specific fish biomass data for the region (see SI Appendix: Methods).

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    Fig. 5.

    Crystallites in the fine-sediment fractions from a range of modern environments across the Eleuthera Bank, Bahamas. (A) Discrete dumbbell morphology crystallites from reefal environments (15 m water depth); (B) Splayed ellipsoidal morphology crystallites from reefal environments (15 m water depth); (C) Cluster of ellipsoidal morphology crystallites from shallow mangrove-fringed coastal inlet site

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Fish as major carbonate mud producers and missing components of the tropical carbonate factory
Chris T. Perry, Michael A. Salter, Alastair R. Harborne, Stephen F. Crowley, Howard L. Jelks, Rod W. Wilson
Proceedings of the National Academy of Sciences Mar 2011, 108 (10) 3865-3869; DOI: 10.1073/pnas.1015895108

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Fish as major carbonate mud producers and missing components of the tropical carbonate factory
Chris T. Perry, Michael A. Salter, Alastair R. Harborne, Stephen F. Crowley, Howard L. Jelks, Rod W. Wilson
Proceedings of the National Academy of Sciences Mar 2011, 108 (10) 3865-3869; DOI: 10.1073/pnas.1015895108
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