Journal Article10.1016/0277-3791(87)90003-5
Oxygen isotopes, ice volume and sea level
TL;DR: In this paper, a comparison is made between the most detailed records of sea level over the last glacial cycle, and two high-quality oxygen isotope records, and a combined record is generated which may be a better approximation to ice volume than was previously available.
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About: This article is published in Quaternary Science Reviews. The article was published on 01 Jan 1987. The article focuses on the topics: Interglacial & Deglaciation.
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References
Oxygen isotope and palaeomagnetic stratigraphy of Equatorial Pacific core V28-238: Oxygen isotope temperatures and ice volumes on a 105 year and 106 year scale☆
TL;DR: The core Vema 28-238 as discussed by the authors preserves an excellent oxygen isotope and magnetic stratigraphy and is shown to contain undisturbed sediments deposited continuously through the past 870,000 yr.
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Oxygen isotopes and sea level
TL;DR: In this article, the authors re-examine the data and conclude that the temperature of the abyssal ocean has been an actively varying component of the climate system, and that there has been a discrepancy between the ice volume record that these records imply and that derived from the altitude of dated coral terraces around the world.
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Global synchroneity of late Quaternary coccolith datum levels Validation by oxygen isotopes
TL;DR: The first appearance of E. huxleyi has an age of 268,000 B.P, occurring consistently in the middle of oxygen isotope stage 12, whereas the first appearance E. lacunosa has been shown to have occurred in the early stages of the second stage as mentioned in this paper.
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The Astronomical Theory of Climatic Change: Barbados Data
TL;DR: In this article, Radiometric dating of successive reef terraces suggests periods of high sea level and associated individual reef tract developments about 82,000, 105,000 and 125,000 years ago.
442
Atmospheric Carbon Dioxide, Orbital Forcing, and Climate
Nicholas J Shackleton,Nicklas G Pisias +1 more
- 18 Mar 2013
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