997 resultados para 160-963


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In a deep-sea sediment core recovered from a site lying well above the local lysocline, several organic geochemical proxies, and two different calcite dissolution indicators, are compared in order to evaluate the relationship between calcite dissolution and paleoproductivity over the past three glacial-interglacial cycles. The degree of foraminiferal break-up, and the CaCO3 particle size distribution, both point to significant periods of dissolution every 22 kyr during glacial stages and substages. These dissolution events are concomitant with periods of enhanced primary productivity, as indicated by the abundance of several biomarkers (alkenones, cholesterol, brassicasterol, keto-ol), used here to indicate changes in paleoproductivity. Dissolution fluctuations are highly coherent and in phase with the estimated paleoproductivity variations providing strong evidence that the observed dissolution is due to organic matter remineralization within the sediments rather, than to changes in CO32? concentration in the overlying water column.

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On double leaves, oriental style, in 3 cases.

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Caption title: nos. 1-4, Atlantic journal, and firend of knowledge; a cyclopedic journal and review of universal science and knowledge: historical, natural, and medical arts and sciences. -- nos. 5-8, Atlantic journal and friend of knowledge; a quarterly journal of historical and natural sciences, useful knowledge, &c.

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On double leaves, oriental style, in cases.

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Vol. [2] has imprint: Washington, D.C., Press of Judd & Detweiler, inc., 1926.