Proxy records

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COnstructing Proxy Records from Age models (COPRA)

Reliable age models are fundamental for any palaeoclimate reconstruction. Available interpolation procedures between age control points are often inadequately reported, and very few translate age uncertainties to proxy uncertainties. Most available modeling algorithms do not allow incorporation of layer counted intervals to improve the confidence limits of the age model in question. We present ...

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Estimation of sedimentary proxy records together with associated uncertainty

Sedimentary proxy records constitute a significant portion of the recorded evidence that allows us to investigate paleoclimatic conditions and variability. However, uncertainties in the dating of proxy archives limit our ability to fix the timing of past events and interpret proxy record intercomparisons. While there are various age-modeling approaches to improve the estimation of the age–depth...

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Securing Healthcare Records Using Proxy Re-Encryption Scheme in Cloud

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Multi-proxy Records of Holocene Climate and Vegetation Change from Ethiopian Crater Lakes

The sediments of Ethiopian crater lakes have differentially sensitive palaeoclimate indicators that vary with time. Lake Tilo, in the south-central Rift Valley, shows a 10,000-year diatom and oxygen-isotope sequence that may be interpreted in terms of hydrochemical and hydrological responses to century-scale climate changes. The diatom record of lake salinity became sensitive to climate variabi...

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Natural waters universally show fractionation of uranium series (U-series) parent–daughter pairs, with the disequilibrium between U and U (U)/(U) commonly used as a tracer of groundwater flow. Because speleothems provide a temporal record of geochemical variations in groundwater precipitating calcite, (U)/(U) variations in speleothems provide a unique method of investigating water–rock interact...

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ژورنال

عنوان ژورنال: Nature

سال: 1984

ISSN: 0028-0836,1476-4687

DOI: 10.1038/308580c0