Potentialities of the Oxygen Isotopic Method for Determination of the Subsurface Paleotemperatuares in Pre-Quaternary Oceans

S.D.Nikolaev

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Potentialities of the Oxygen Isotopic Method for Determination of the Subsurface Paleotemperatuares in Pre-Quaternary Oceans

机译：氧气同位素法测定第四纪前海表层古温度的潜力

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A model for the changes in the oxygen isotopic composition of the waters of the World Ocoean from the Eocene to the Pliocene is suggested. The previously elaborated techniques of the coupled use of the oxygen isotopic and foraminiferal techniques as applied to the pre-Quaternary time is refined and enhanced. The testing performed showed a fine reliability of the results obtained and the possibility of application of this method in paleoceanology. However, some discrepancies were observed probably caued both by the peculiar featuares of the distribution of the temperature field in the past and by certain technical reasons.

机译：提出了从始新世到上新世的世界海洋水域氧同位素组成变化的模型。改进并增强了先前阐述的将氧同位素和有孔虫技术联合应用的技术，该技术已应用到第四纪之前的时间。进行的测试表明所获得的结果具有良好的可靠性，并且该方法在古生物学中的应用可能性。但是，过去的温度场分布特征和某些技术原因可能会引起一些差异。

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《Oceanology》 |2001年第6期|共14页
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S.D.Nikolaev;
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中图分类海洋学;
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1. Potentialities of the Oxygen Isotopic Method for Determination of the Subsurface Paleotemperatuares in Pre-Quaternary Oceans [J] . S.D.Nikolaev Oceanology . 2001,第6期

机译：氧气同位素法测定第四纪前海表层古温度的潜力
2. Determination of carbon and oxygen isotopes of geological samples with a complicated matrix: comparison of different analytical methods [J] . Lin-Lin Cui, Xu Wang Analytical methods . 2014,第22期

机译：具有复杂基质的地质样品中碳氧同位素的测定：不同分析方法的比较
3. Comparison of the silver nitrate and bacterial denitrification methods for the determination of nitrogen and oxygen isotope ratios of nitrate in surface water [J] . Dongmei Xue, Bernard De Baets, Jorin Botte, Rapid Communications in Mass Spectrometry: RCM . 2010,第6期

机译：硝酸银和细菌反硝化方法测定地表水中硝酸盐氮，氧同位素比的比较
4. Determination of the oxygen diffusion characteristics in Li-Ti ferrite by isotopic method [C] . Lysenko, E.N., Gyngazov, . 2002

机译：同位素法测定锂钛铁氧体中氧的扩散特性
5. Geographic control of ocean circulation during the late Cretaceous: Comparison of results of an ocean general circulation model with oxygen isotope paleotemperatures. [D] . Yasuda, Memorie Kishiko. 1988

机译：白垩纪晚期海洋环流的地理控制：氧同位素古温度与海洋总环流模型结果的比较。
6. Uranium isotope evidence for two episodes of deoxygenation during Oceanic Anoxic Event 2 [O] . Matthew O. Clarkson, Claudine H. Stirling, Hugh C. Jenkyns, 2018

机译：铀同位素证据表明在海洋缺氧事件2中发生了两次脱氧
7. An oxygen isotope profile in a section of Cretaceous oceanic crust, Samail Ophiolite, Oman: Evidence for δ^(18)O buffering of the oceans by deep (>5 km) seawater-hydrothermal circulation at mid-ocean ridges [O] . Gregory Robert T., Taylor Hugh P. Jr. 1981

机译：阿曼Samail Ophiolite的白垩纪大洋地壳剖面中的氧同位素分布：海洋中脊深（> 5 km）海水-水热循环对δ^（18）O缓冲的证据
8. Determination of the Potentialities of the Mine Safety Appliance Self-Contained Swimming Outfit for Descents to 400 Feet Using Helium-Oxygen Breathing Mixtures [R] . Blockwick, T. N. 1950

机译：在梅思安自含游泳军团的再临，以400英尺的潜力的测定采用氦氧呼吸混合物

Potentialities of the Oxygen Isotopic Method for Determination of the Subsurface Paleotemperatuares in Pre-Quaternary Oceans

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