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Late Pleistocene Paleoclimates and sea-level change in the Mediterranean as inferred from stable isotope and U-series studies of overgrowths on speleothems, Mallorca, Spain

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TLDR
In this article, a number of phreatic overgrowths on speleothems have been dated using the Th/U method in order to determine the position of the sea level during Late Quaternary.
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This article is published in Quaternary Science Reviews.The article was published on 2000-05-01. It has received 104 citations till now. The article focuses on the topics: Phreatic & Sea level.

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Uranium-series Chronology and Environmental Applications of Speleothems

TL;DR: Speleothems are bodies of mineral material formed in caves as the result of chemical precipitation from groundwater flowing or dripping in a cave as discussed by the authors, and they can be found in many locations of the globe, sampled at high-resolution and reliably dated using high-precision uranium series techniques.
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Patterns and processes in plant phylogeography in the Mediterranean Basin. A review

TL;DR: Future phylogeographic studies have a great potential to help explaining biodiversity patterns of plant groups and understanding why the Mediterranean Basin has come to be one of the biodiversity hotspots on earth.
References
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Journal ArticleDOI

On the Isotopic Chemistry of Carbonates and a Paleotemperature Scale

TL;DR: In this paper, the temperature variation of the fractionation of oxygen in exchange reactions between dissolved carbonate and water and between calcite and water was calculated on theoretical grounds, and checked experimentally.
Book

Principles of isotope geology

Gunter Faure
TL;DR: The roots of isotope geology can be found in this paper, where a geology of Neodymium and Strontium in meteorites and Igneous rocks is described.
Journal ArticleDOI

Age dating and the orbital theory of the ice ages: Development of a high-resolution 0 to 300,000-year chronostratigraphy

TL;DR: Using the concept of "orbital tuning", a continuous, high-resolution deep-sea chronostratigraphy has been developed spanning the last 300,000 yr as mentioned in this paper.
Journal ArticleDOI

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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