Seawater carbonate chemistry and elemental ratios in biogenic marine calcium carbonates
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| Natura: | Dataset Open Access |
| Lingua: | en |
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PANGAEA
2021
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| author | Ulrich, Robert N Guillermic, Maxence Campbell, Julia Hakim, Abbas Han, Rachel Singh, Shayleen Stewart, Justin D Román-Palacios, Cristian Carroll, Hannah M De Corte, Ilian Gilmore, Rosaleen E Doss, Whitney Tripati, Aradhna K Ries, Justin B Eagle, Robert A |
| author_facet | Ulrich, Robert N Guillermic, Maxence Campbell, Julia Hakim, Abbas Han, Rachel Singh, Shayleen Stewart, Justin D Román-Palacios, Cristian Carroll, Hannah M De Corte, Ilian Gilmore, Rosaleen E Doss, Whitney Tripati, Aradhna K Ries, Justin B Eagle, Robert A |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Elemental ratios in biogenic marine calcium carbonates are widely used in geobiology, environmental science, and paleoenvironmental reconstructions. It is generally accepted that the elemental abundance of biogenic marine carbonates reflects a combination of the abundance of that ion in seawater, the physical properties of seawater, the mineralogy of the biomineral, and the pathways and mechanisms of biomineralization. Here we report measurements of a suite of nine elemental ratios (Li/Ca, B/Ca, Na/Ca, Mg/Ca, Zn/Ca, Sr/Ca, Cd/Ca, Ba/Ca, and U/Ca) in 18 species of benthic marine invertebrates spanning a range of biogenic carbonate polymorph mineralogies (low-Mg calcite, high-Mg calcite, aragonite, mixed mineralogy) and of phyla (including Mollusca, Echinodermata, Arthropoda, Annelida, Cnidaria, Chlorophyta, and Rhodophyta) cultured at a single temperature (25°C) and a range of pCO2 treatments (ca. 409, 606, 903, and 2856 ppm). This dataset was used to explore various controls over elemental partitioning in biogenic marine carbonates, including species-level and biomineralization-pathway-level controls, the influence of internal pH regulation compared to external pH changes, and biocalcification responses to changes in seawater carbonate chemistry. The dataset also enables exploration of broad scale phylogenetic patterns of elemental partitioning across calcifying species, exhibiting high phylogenetic signals estimated from both uni- and multivariate analyses of the elemental ratio data (univariate: lambda = 0–0.889; multivariate: lambda = 0.895–0.99). Comparing partial R2 values returned from non-phylogenetic and phylogenetic regression analyses echo the importance of and show that phylogeny explains the elemental ratio data 1.4–59 times better than mineralogy in five out of nine of the elements analyzed. Therefore, the strong associations between biomineral elemental chemistry and species relatedness suggests mechanistic controls over element incorporation rooted in the evolution of biomineralization mechanisms. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_933051 |
| institution | PANGAEA |
| language | en |
| publishDate | 2021 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Seawater carbonate chemistry and elemental ratios in biogenic marine calcium carbonates Ulrich, Robert N Guillermic, Maxence Campbell, Julia Hakim, Abbas Han, Rachel Singh, Shayleen Stewart, Justin D Román-Palacios, Cristian Carroll, Hannah M De Corte, Ilian Gilmore, Rosaleen E Doss, Whitney Tripati, Aradhna K Ries, Justin B Eagle, Robert A Alkalinity, total; Alkalinity, total, standard deviation; Animalia; Annelida; Apparent partition coefficient, barium; Apparent partition coefficient, boron; Apparent partition coefficient, boron to aragonite incorporation x1000; Apparent partition coefficient, boron to calcite incorporation x1000; Apparent partition coefficient, cadmium; Apparent partition coefficient, lithium; Apparent partition coefficient, magnesium; Apparent partition coefficient, sodium; Apparent partition coefficient, strontium; Apparent partition coefficient, uranium; Apparent partition coefficient, zinc; Aragonite saturation state; Aragonite saturation state, standard deviation; Arbacia punctulata; Argopecten irradians; Arthropoda; Barium/Calcium ratio; Benthic animals; Benthos; Bicarbonate ion; Bicarbonate ion, standard deviation; Biomass/Abundance/Elemental composition; Boron/Calcium ratio; Cadmium/Calcium ratio; Calcite saturation state; Calculated using seacarb after Nisumaa et al. (2010); Callinectes sapidus; Carbon, inorganic, dissolved; Carbon, inorganic, dissolved, standard deviation; Carbonate ion; Carbonate ion, standard deviation; Carbonate system computation flag; Carbon dioxide; Carbon dioxide, partial pressure; Chlorophyta; Cnidaria; Coast and continental shelf; Containers and aquaria (20-1000 L or < 1 m**2); Crassostrea virginica; Crepidula fornicata; Echinodermata; Eucidaris tribuloides; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Halimeda incrassata; Homarus americanus; Hydroides crucigera; Identification; Instrument; Laboratory experiment; Lithium/Calcium ratio; Littorina littorea; Macroalgae; Magnesium/Calcium ratio; Material; Mercenaria mercenaria; Mollusca; Mya arenaria; Mytilus edulis; Neogoniolithon spectabile; North Atlantic; OA-ICC; Ocean acidification; Ocean Acidification International Coordination Centre; Oculina arbuscula; Organisms; Partial pressure of carbon dioxide, standard deviation; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Penaeus plebejus; pH, NBS scale; pH, standard deviation; pH, total scale; Phylum; Plantae; Registration number of species; Rhodophyta; Salinity; Salinity, standard deviation; Single species; Sodium/Calcium ratio; Species; Strombus alatus; Strontium/Calcium ratio; Temperate; Temperature, water; Temperature, water, standard deviation; Type; Uniform resource locator/link to reference; Uranium/Calcium ratio; Urosalpinx cinerea; Zinc/Calcium ratio Elemental ratios in biogenic marine calcium carbonates are widely used in geobiology, environmental science, and paleoenvironmental reconstructions. It is generally accepted that the elemental abundance of biogenic marine carbonates reflects a combination of the abundance of that ion in seawater, the physical properties of seawater, the mineralogy of the biomineral, and the pathways and mechanisms of biomineralization. Here we report measurements of a suite of nine elemental ratios (Li/Ca, B/Ca, Na/Ca, Mg/Ca, Zn/Ca, Sr/Ca, Cd/Ca, Ba/Ca, and U/Ca) in 18 species of benthic marine invertebrates spanning a range of biogenic carbonate polymorph mineralogies (low-Mg calcite, high-Mg calcite, aragonite, mixed mineralogy) and of phyla (including Mollusca, Echinodermata, Arthropoda, Annelida, Cnidaria, Chlorophyta, and Rhodophyta) cultured at a single temperature (25°C) and a range of pCO2 treatments (ca. 409, 606, 903, and 2856 ppm). This dataset was used to explore various controls over elemental partitioning in biogenic marine carbonates, including species-level and biomineralization-pathway-level controls, the influence of internal pH regulation compared to external pH changes, and biocalcification responses to changes in seawater carbonate chemistry. The dataset also enables exploration of broad scale phylogenetic patterns of elemental partitioning across calcifying species, exhibiting high phylogenetic signals estimated from both uni- and multivariate analyses of the elemental ratio data (univariate: lambda = 0–0.889; multivariate: lambda = 0.895–0.99). Comparing partial R2 values returned from non-phylogenetic and phylogenetic regression analyses echo the importance of and show that phylogeny explains the elemental ratio data 1.4–59 times better than mineralogy in five out of nine of the elements analyzed. Therefore, the strong associations between biomineral elemental chemistry and species relatedness suggests mechanistic controls over element incorporation rooted in the evolution of biomineralization mechanisms. |
| title | Seawater carbonate chemistry and elemental ratios in biogenic marine calcium carbonates |
| topic | Alkalinity, total; Alkalinity, total, standard deviation; Animalia; Annelida; Apparent partition coefficient, barium; Apparent partition coefficient, boron; Apparent partition coefficient, boron to aragonite incorporation x1000; Apparent partition coefficient, boron to calcite incorporation x1000; Apparent partition coefficient, cadmium; Apparent partition coefficient, lithium; Apparent partition coefficient, magnesium; Apparent partition coefficient, sodium; Apparent partition coefficient, strontium; Apparent partition coefficient, uranium; Apparent partition coefficient, zinc; Aragonite saturation state; Aragonite saturation state, standard deviation; Arbacia punctulata; Argopecten irradians; Arthropoda; Barium/Calcium ratio; Benthic animals; Benthos; Bicarbonate ion; Bicarbonate ion, standard deviation; Biomass/Abundance/Elemental composition; Boron/Calcium ratio; Cadmium/Calcium ratio; Calcite saturation state; Calculated using seacarb after Nisumaa et al. (2010); Callinectes sapidus; Carbon, inorganic, dissolved; Carbon, inorganic, dissolved, standard deviation; Carbonate ion; Carbonate ion, standard deviation; Carbonate system computation flag; Carbon dioxide; Carbon dioxide, partial pressure; Chlorophyta; Cnidaria; Coast and continental shelf; Containers and aquaria (20-1000 L or < 1 m**2); Crassostrea virginica; Crepidula fornicata; Echinodermata; Eucidaris tribuloides; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Halimeda incrassata; Homarus americanus; Hydroides crucigera; Identification; Instrument; Laboratory experiment; Lithium/Calcium ratio; Littorina littorea; Macroalgae; Magnesium/Calcium ratio; Material; Mercenaria mercenaria; Mollusca; Mya arenaria; Mytilus edulis; Neogoniolithon spectabile; North Atlantic; OA-ICC; Ocean acidification; Ocean Acidification International Coordination Centre; Oculina arbuscula; Organisms; Partial pressure of carbon dioxide, standard deviation; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Penaeus plebejus; pH, NBS scale; pH, standard deviation; pH, total scale; Phylum; Plantae; Registration number of species; Rhodophyta; Salinity; Salinity, standard deviation; Single species; Sodium/Calcium ratio; Species; Strombus alatus; Strontium/Calcium ratio; Temperate; Temperature, water; Temperature, water, standard deviation; Type; Uniform resource locator/link to reference; Uranium/Calcium ratio; Urosalpinx cinerea; Zinc/Calcium ratio |
| url | https://doi.org/10.1594/PANGAEA.933051 |