ODP 846站点中上新世复合剖面的修正

T. Herbert, R. Caballero‐Gill, Joseph Novak
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引用次数: 0

摘要

摘要ODP 846站点的复合剖面提供了上新世稳定同位素和古气候时间序列的关键数据集。通过将高分辨率岩心测量与连续的井下电导率测井相结合,我们记录了上新世晚期包含M2冰期(约3.250-3.3 Ma)的稳定同位素和烯酮衍生的海表温度估算(SST)的原始数据集的错误。此外,我们还提供了新的稳定同位素和烯烃测量值,这些测量值与修改后的颜色反射率和伽马射线衰减孔隙度评估数据的拼接有很好的相关性。提出了一种新的复合剪接,并将复合同位素和烯烃时间序列整合到修正的上新世古气候叠加中。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A Revised Mid-Pliocene Composite Section for ODP Site 846
Abstract. The composite section from ODP Site 846 has provided key data sets for Pliocene stable isotope and paleoclimatic time series. We document here errors in primary data sets for stable isotopes and alkenone-derived sea surface temperature estimates (SST) in the late Pliocene interval containing the M2 glaciation (ca. 3.250–3.3 Ma) by tying high resolution core measurements to a continuous downhole conductivity log. In addition, we provide new stable isotopic and alkenone measurements that correlate well to the revised splices of color reflectance and gamma ray attenuation porosity evaluator data. A new composite splice is proposed, along with composite isotope and alkenone time series that should be integrated into revised Pliocene paleoclimatic stacks.
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