P.-T. Lee, S. L. Ho, J. Groeneveld, M. Mohtadi, C.-C. Shen, C.-C. Su
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引用次数: 0
Abstract
Single-specimen analysis of planktic foraminiferal geochemistry has gained increasing popularity for its potential in reconstructing climate variability. However, the comparability between single-specimen and conventional multi-specimen Mg/Ca data remains unclear, which has raised questions concerning the suitability of multi-specimen Mg/Ca-temperature calibrations for single-specimen data. This study developed and evaluated the effects of four single-specimen cleaning procedures on the Mg/Ca ratio of Trilobatus sacculifer. These procedures varied in their inclusion or exclusion of the reductive step and heating for chemical reactions. The most effective single-specimen cleaning procedure (procedure Dsingle) incorporated the oxidative step while excluding the reductive step and heating. This procedure was subsequently applied to five additional planktic foraminifera species. With procedure Dsingle, we obtained statistically indistinguishable mean Mg/Ca values for single-specimen and multi-specimen samples of T. sacculifer, Orbulina universa, and Pulleniatina obliquiloculata, regardless of the intensity of the multi-specimen cleaning procedures. For single-specimen samples of Globigerinoides ruber and Neogloboquadrina dutertrei, the mean Mg/Ca values only matched those of the multi-specimen samples when procedures excluded the reductive step and heating. In contrast, single-specimen mean Mg/Ca values of Globorotalia menardii were consistently higher than those obtained through multi-specimen cleaning. The mean Mg/Ca differences between single-specimen and multi-specimen cleaning procedures across species are likely attributable to differences in the microstructure of the calcite tests. In summary, when cleaning procedures involving identical steps and heating conditions were utilized, both single-specimen and multi-specimen analyses yielded comparable mean Mg/Ca values, suggesting that the multi-specimen Mg/Ca calibrations are applicable to single-specimen data.
期刊介绍:
Geochemistry, Geophysics, Geosystems (G3) publishes research papers on Earth and planetary processes with a focus on understanding the Earth as a system. Observational, experimental, and theoretical investigations of the solid Earth, hydrosphere, atmosphere, biosphere, and solar system at all spatial and temporal scales are welcome. Articles should be of broad interest, and interdisciplinary approaches are encouraged.
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The physics and chemistry of the Earth, including its structure, composition, physical properties, dynamics, and evolution
Principles and applications of geochemical proxies to studies of Earth history
The physical properties, composition, and temporal evolution of the Earth''s major reservoirs and the coupling between them
The dynamics of geochemical and biogeochemical cycles at all spatial and temporal scales
Physical and cosmochemical constraints on the composition, origin, and evolution of the Earth and other terrestrial planets
The chemistry and physics of solar system materials that are relevant to the formation, evolution, and current state of the Earth and the planets
Advances in modeling, observation, and experimentation that are of widespread interest in the geosciences.