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首页> 外文期刊>Journal of Coastal Research: An International Forum for the Littoral Sciences >Magnetic susceptibility and radioactivity changes of aegean and ionian sea sediments during last glacial/interglacial: Climatic and chronological markers
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Magnetic susceptibility and radioactivity changes of aegean and ionian sea sediments during last glacial/interglacial: Climatic and chronological markers

机译:最后一次冰川/间冰期期间爱琴海和爱奥尼亚海沉积物的磁化率和放射性变化:气候和年代学标记

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Five marine sediment boreholes from the Aegean and Ionian Sea have been measured here for their magnetic susceptibility and (in an earlier work) by alpha-and beta-particle radioactivity. The corresponding borehole cores cover the Holocene period and closely spaced data have been sampled from all cores. The obtained depth data series have been converted here to the time series by using appropriate conversions on the basis of sedimentation rates derived from dating of selected samples of each core. The spectral characteristics of the new statistical elaboration for the final time series exhibit a significant correlation of the magnetic susceptibility and radioactivity data. This correlation is prominent especially for intermediate periods (typically 110 ky) of the examined spectra and tends to disappear for higher frequency variations (<1 ky), suggesting that mainly long-period climatic and other changes are the ones that affect the examined quantities in a similar manner. This pattern is verified by the band-pass filtered time series for intermediate periods, which reveals well-correlated susceptibility and radioactivity changes. In addition, specific time markers are observed in the filtered time series, and comparison of their variation to certain climatic phases within the Holocene is recognized.
机译:在这里,已经测量了来自爱琴海和爱奥尼亚海的五个海洋沉积物钻孔的磁化率,并通过α-和β-粒子放射性对其进行了测量(在较早的工作中)。相应的钻孔岩心涵盖了全新世时期,并且已从所有岩心中采样到了近距离的数据。在此,根据从每个岩芯的选定样品测年得到的沉降速率,通过使用适当的转换,将获得的深度数据序列转换为时间序列。最终时间序列的新统计细节的光谱特征显示出磁化率和放射性数据之间的显着相关性。这种相关性尤其在被检查光谱的中间阶段(通常为110 ky)尤为突出,而对于更高的频率变化(<1 ky)则趋于消失,这表明主要是长期的气候变化和其他变化会影响所检查光谱的数量。类似的方式。通过中间阶段的带通滤波时间序列验证了此模式,该序列揭示了相关性良好的磁化率和放射性变化。此外,在过滤后的时间序列中观察到特定的时间标记,并且可以将它们的变化与全新世内某些气候相进行比较。

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