首页> 外文学位 >Laurentide ice sheet meltwater influences and millennial-scale climate oscillations on the northwestern slope of the Gulf of Mexico during Marine Isotope Stage 6 and Termination II.
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Laurentide ice sheet meltwater influences and millennial-scale climate oscillations on the northwestern slope of the Gulf of Mexico during Marine Isotope Stage 6 and Termination II.

机译:在海洋同位素第6阶段和第II阶段终止期间,Laurentide冰盖融水对墨西哥湾西北坡的影响和千年尺度的气候振荡。

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摘要

Sub-Milankovitch climate oscillations are well documented phenomena in the Gulf of Mexico during Marine Isotope Stage (MIS) 3 and Termination I, however very little is known about equivalent events during older time intervals. Basin 4 is located on the northwest slope of the Gulf of Mexico and has provided a detailed record of late MIS 6 and Termination II. The results of this study show that the delta18O record of planktonic foraminifer G. ruber contains millennial-scale climate oscillations during MIS 6, a series of meltwater spikes, and a climate reversal during Termination II. Paired delta18O -- Mg/Ca data across these events reveal that the unusually large amplitudes in the delta 18O record cannot be explained by sea surface temperature (SST) or ice volume, but rather are a response to isotopically light glacial meltwater from the paleo-Mississippi river. This conclusion supports the studies of similar oscillations during Termination I and MIS 3.
机译:在海洋湾同位素阶段(MIS)3和I终端期间,Milankovitch次气候振荡是墨西哥湾地区的有据可查的现象,但是,对于较旧的时间间隔内的等效事件知之甚少。盆地4位于墨西哥湾的西北坡上,并提供了详细的MIS 6和II终结的详细记录。这项研究的结果表明,浮游有孔虫G. ruber的delta18O记录包含MIS 6期间千年尺度的气候振荡,一系列融化水的尖峰和Terminal II期间的气候逆转。这些事件中成对的delta18O-Mg / Ca数据显示,delta 18O记录中异常大的振幅不能用海表温度(SST)或冰量来解释,而是对来自古太平洋的同位素轻质冰川融水的响应密西西比河。该结论支持对终端I和MIS 3期间类似振荡的研究。

著录项

  • 作者

    O'Hayer, Walter Werley.;

  • 作者单位

    Rice University.;

  • 授予单位 Rice University.;
  • 学科 Geochemistry.
  • 学位 M.S.
  • 年度 2009
  • 页码 60 p.
  • 总页数 60
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地质学;
  • 关键词

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