Raman analysis of octocoral carbonate ion structural disorder along a natural depth gradient, Kona coast, Hawai‘i
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Kyle Conner
Abstract
Both environmental and physiological factors cause carbonate ion structural disorder in biogenic Mg-calcites. A major component of this disorder is driven by the incorporation of Mg through environmental forcing and growth rate kinetics although non-Mg factors (e.g., other cation/anion impurities, organic molecules) also contribute. Understanding the drivers of Mg content in biogenic calcite and its effects on disorder has implications for octocoral Mg paleo-proxies and the stability and diagenetic alteration of their calcitic skeletons. However, prior studies of biogenic Mg-calcites have often been complicated by sampling inconsistencies over space and time and potential intra-sample Mg variability. This study aims to analyze the relative contributing factors of octocoral Mg-calcite structural disorder along gradients of both depth and growth rate. Calcitic octocorals (Coralliidae and Keratoisididae, N = 28) were collected from 221–823 m depths across a natural gradient in biogeochemical parameters (pH: 7.4–7.9, T: 5–16 °C) off the Kona coast of Hawai‘i Island and were analyzed using Raman spectroscopy. Samples were collected during the same month, controlling for potential seasonal variability. Raman spectral parameters from the ν1 peak quantified total carbonate ion structural disorder (full-width at half maximum height [FWHM] of ν1) and Mg content (ν1 position, Raman shift). The total structural disorder was then partitioned into Mg-driven and non-Mg driven components (residual ν1 FWHM). The total structural disorder and Mg content decreased significantly with increasing depth, correlating with temperature and carbonate system parameters. The Mg-temperature relationships from this study were also consistent with prior studies. Non-Mg structural disorder did not correlate to any environmental parameters. When measured across an intra-sample gradient of ontogenetic growth rate, total structural disorder, Mg content, and non-Mg structural disorder increased with growth rate for all but one taxon, demonstrating the kinetic effect of growth rate as well as potential taxon-specific physiological effects. These results provide insight into how environmental and growth rate kinetic effects independently afect different components of carbonate ion structural disorder (Mg content and non-Mg factors). These findings also suggest that Raman spectroscopy may be helpful in quantifying solubility within biogenic calcites.
Funding statement: Octocoral Raman analysis was supported by the Raman and Infrared Spectroscopy Laboratory at the Hawai‘i Institute for Geophysics and Planetary Sciences. Collection of octocoral samples and oceanographic data were made possible by the Hawai‘i Undersea Research Laboratory (HURL). Financial support for ship and submersible time were provided by the NOAA Deep Sea Coral and Sponge Research and Technology Program. We thank J. Sanchez and L. Dueñas at the Universidad de Los Andes in Colombia and B. Lendvay at the University of Zürich for morphological and genetic identification of the octocoral specimens. Sample M3 was provided by F. Parrish from the Pacific Islands Fisheries Science Center.
Acknowledgments
We thank J. Sanchez and L. Dueñas at the Universidad de Los Andes in Colombia and B. Lendvay at the University of Zürich for morphological and genetic identification of the octocoral specimens. Sample M3 was provided by F. Parrish from the Pacific Islands Fisheries Science Center. We specifically thank M. Egan for micro-Raman instrument training and troubleshooting.
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Artikel in diesem Heft
- Eu speciation in apatite at 1 bar: An experimental study of valence-state partitioning by XANES, lattice strain, and Eu/Eu* in basaltic systems
- The effect of composition on chlorine solubility and behavior in silicate melts
- High-temperature phase relations of hydrous aluminosilicates at 22 GPa in the AlOOH-AlSiO3OH system
- Crystallization of spinel from coexisting silicate and sulfide immiscible liquids: An equilibrium case with postcumulus reactions
- X-ray absorption spectroscopy study of Mn reference compounds for Mn speciation in terrestrial surface environments
- Heterogeneous and retarded phase transformation of ferrihydrite on montmorillonite surface: The important role of surface interactions
- Atomic-scale characterization of the oxidation state of Ti in meteoritic hibonite: Implications for early solar system thermodynamics
- Structural behavior of C2/m tremolite to 40 GPa: A high-pressure single-crystal X-ray diffraction study
- Optimizing Raman spectral collection for quartz and zircon crystals for elastic thermobarometry
- Measuring H2O concentrations in olivine by secondary ion mass spectrometry: Challenges and paths forward
- Arsenic clustering in arsenian pyrite: A combined photoemission and theoretical modeling study
- High-pressure electrical conductivity and elasticity of iron-bearing δ-AlOOH
- Nudged elastic band calculations of the (4H)XSi hydrogarnet type defect in Mg2SiO4 forsterite
- Mn substitution and distribution in goethite and influences on its photocatalytic properties: A combined study using first-principles calculations and photocatalytic experiments
- Incorporating previously neglected excess oxygen associated with ferric iron in matrix corrections of microprobe data from cubic and rhombohedral Fe-Ti oxides
- Recycled carbonates in the mantle sources of natural kamafugites: A zinc isotope perspective
- Raman analysis of octocoral carbonate ion structural disorder along a natural depth gradient, Kona coast, Hawai‘i
- Memorial of Charles Wilson Burnham, 1933–2021
- Erratum
Artikel in diesem Heft
- Eu speciation in apatite at 1 bar: An experimental study of valence-state partitioning by XANES, lattice strain, and Eu/Eu* in basaltic systems
- The effect of composition on chlorine solubility and behavior in silicate melts
- High-temperature phase relations of hydrous aluminosilicates at 22 GPa in the AlOOH-AlSiO3OH system
- Crystallization of spinel from coexisting silicate and sulfide immiscible liquids: An equilibrium case with postcumulus reactions
- X-ray absorption spectroscopy study of Mn reference compounds for Mn speciation in terrestrial surface environments
- Heterogeneous and retarded phase transformation of ferrihydrite on montmorillonite surface: The important role of surface interactions
- Atomic-scale characterization of the oxidation state of Ti in meteoritic hibonite: Implications for early solar system thermodynamics
- Structural behavior of C2/m tremolite to 40 GPa: A high-pressure single-crystal X-ray diffraction study
- Optimizing Raman spectral collection for quartz and zircon crystals for elastic thermobarometry
- Measuring H2O concentrations in olivine by secondary ion mass spectrometry: Challenges and paths forward
- Arsenic clustering in arsenian pyrite: A combined photoemission and theoretical modeling study
- High-pressure electrical conductivity and elasticity of iron-bearing δ-AlOOH
- Nudged elastic band calculations of the (4H)XSi hydrogarnet type defect in Mg2SiO4 forsterite
- Mn substitution and distribution in goethite and influences on its photocatalytic properties: A combined study using first-principles calculations and photocatalytic experiments
- Incorporating previously neglected excess oxygen associated with ferric iron in matrix corrections of microprobe data from cubic and rhombohedral Fe-Ti oxides
- Recycled carbonates in the mantle sources of natural kamafugites: A zinc isotope perspective
- Raman analysis of octocoral carbonate ion structural disorder along a natural depth gradient, Kona coast, Hawai‘i
- Memorial of Charles Wilson Burnham, 1933–2021
- Erratum