Chemical composition of phosphorites and host sediments
Paleotemperature curves were drawn from oxygen-isotope ratios in CaCO3 of planktonic foraminiferal tests and by the micropaleontological method using quantitative relationships of their species. Two series of curves yield similar results. These data confirm that isotope composition of oxygen reflect...
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Format: | Dataset |
Language: | English |
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PANGAEA
1974
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.753865 https://doi.org/10.1594/PANGAEA.753865 |