Temperature control on the incorporation of magnesium, strontium, fluorine, and cadmium into benthic foraminiferal shells from Little Bahama Bank: Prospects for thermocline paleoceanography
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- Type
- article
- Published
- 1997-09-01
- Cited by
- 487
- References
- 55
- OpenAlex
- https://openalex.org/W2018065255
- Semantic Scholar
- https://api.semanticscholar.org/CorpusID:128824310
Keywords
Benthic zone, Foraminifera, Geology, Thermocline, Paleoceanography
References
- World Ocean Atlas 1994. Volume 4. Temperature
- Seasonal reconstructions of the earth's surface at the last glacial maximum
- δ18O values, 87Sr86Sr and Sr/Mg ratios of Late Devonian abiotic marine calcite: Implications for the composition of ancient seawater
- The modern and glacial thermoclines along the Bahama Banks
- Thermodynamic properties of minerals and related substances at 298.15 K and 1 bar (10[5] pascals) pressure and at higher temperatures
- The co-precipitation of cations with CaCO3-IV
- The influence of air and sea exchange on the carbon isotope distribution in the sea
- Sr/Mg ratios of modern marine calcite: Empirical indicators of ocean chemistry and precipitation rate
- Evidence of a dissolution effect on benthic foraminiferal shell chemistry: δ13C, Cd/Ca, Ba/Ca, and Sr/Ca results from the Ontong Java Plateau
- Sr, Cd, Mn and Co distribution coefficients in calcite as a function of calcite precipitation rate
- The applicability of trace elements in freshwater shells for paleogeochemical studies
- Partition coefficients in calcite: Examination of factors influencing the validity of experimental results and their application to natural systems
- An ion probe study of annual cycles of Sr/Ca and other trace elements in corals
- A biomineralization model for the incorporation of trace elements into foraminiferal calcium carbonate
- Planktonic Foraminifera: Selective solution and the lysocline
- Relationship of magnesium and other minor elements in tests of Cassidulina subglobosa and C. oriangulata to physical oceanic properties
- URANIUM IN FORAMINIFERAL CALCITE AS A RECORDER OF SEAWATER URANIUM CONCENTRATIONS
- Structure of the glacial thermocline at Little Bahama Bank
- The role of ocean-atmosphere reorganizations in glacial cycles
- Influence of temperature on the composition of magnesian calcite overgrowths precipitated from seawater
Cited by
- Complex exposure history of pre-LGM glacial drifts in Terra Nova Bay, Victoria Land, using a multiple cosmogenic nuclide approach
- Ocean-based heat transfer across the equator in the Arabian Sea over Glacial and Interglacial transitions
- Estimating Cenozoic ice volume from deep-sea records
- Response of the Elemental Chemistry of Carbonate Phases to Secular Change in Ocean Chemistry.
- Boron/Calcium in planktonic foraminifera: Proxy development and application to the Paleocene-Eocene boundary
- Li/Ca, B/Ca, and Mg/Ca Composition of Cultured Sea Urchin Spines and Paleo-Echinoderms Measured Using a Secondary Ion Mass Spectrometer
- A multi-proxy approach for reconstructing oceanographic dynamics during the HoloceneDevelopment and Application of benthic foraminifera as proxies in the Polar North Atlantic
- Nanoscale Effects of Strontium on Calcite Growth: A Baseline for Understanding Biomineralization in the Absence of Vital Effects
- Palaeomagnetism of Palaeogene strata from southern Zealandia: Implications for ice in the greenhouse
- Dynamics of tropical African climate and marine sedimentation during major climate transitions
- Sr/Ca- und U/Ca-Thermometrie an Korallen (Porites lutea) aus dem Indischen Ozean
- Climate transitions across the Cenozoic: Insight from elemental ratios in benthic foraminifera and marine gastropods
- Inorganic and stable isotope geochemistry of tropical Atlantic/Caribbean planktonic foraminifera : implications for the reconstruction of upper ocean temperatures and stratification
- Determination of multiple element/calcium ratios in foraminiferal calcite by quadrupole ICP‐MS
- Late Holocene climate variability from northern Gulf of Mexico sediments: Merging inorganic and molecular organic geochemical proxies
- Intracellular pH distribution in foraminifera determined by the fluorescent probe HPTS
- Impact of biomineralization processes on the Mg content of foraminiferal shells: A biological perspective
- Crystallography, stable isotope and trace element analysis of Mytilus edulis shells in the context of ontogeny
- The centennial and millennial variability of the IndoPacific warm pool and the Indonesian Throughflow
- Statolith extraction method improvements for use in microchemistry studies with laser ablation inductively coupled plasma mass spectrometry
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