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A 600&thinsp;kyr reconstruction of deep Arctic seawater <i>δ</i><sup>18</sup>O from benthic foraminiferal <i>δ</i><sup>18</sup>O and ostracode Mg&thinsp;∕&thinsp;Ca paleothermometry

<p>The oxygen isotopic composition of benthic foraminiferal tests (<span class="inline-formula"><i>δ</i><sup>18</sup>O</span><span class="inline-formula"><sub>b</sub></span>) is one of the pre-eminent tools for correlating marine sediments and interpreting past terrestrial ice volume and deep-ocean...

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Xehetasun bibliografikoak
Egile Nagusiak: J. R. Farmer, K. J. Keller, R. K. Poirier, G. S. Dwyer, M. F. Schaller, H. K. Coxall, M. O'Regan, T. M. Cronin
Formatua: Artigo
Hizkuntza:Inglês
Argitaratua: Copernicus Publications 2023-03-01
Saila:Climate of the Past
Sarrera elektronikoa:https://cp.copernicus.org/articles/19/555/2023/cp-19-555-2023.pdf
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